PHOTOCHEMICAL REACTIVITY WORKSHOP

             U.S. Environmental Protection Agency

                      May 12-14,1998
                PROCEEDINGS
                    Regal University Hotel
                  2800 Campus Walk Avenue
                 Durham, North Carolina 27705

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                                                          950R98003
                              TABLE OF CONTENTS
PRESENTATIONS

SESSION I
Introductions 	1-1
       Moderators:   Jake Hales, NARSTO International. ENVAIR
                    Howard Feldman, American Petroleum Institute
Welcoming Remarks	1-3
       Gary Foley, National Exposure Research Laboratory, EPA
       Sally Shaver, Air Quality Strategies and Standards Division, EPA
The Public-Private Partnership Process	1-4
       Ron Patterson, NARSTO International. National Exposure Research Laboratory, EPA
Current EPA Regulatory Viewpoint on Reactivity	1-7
       Bill Johnson, Ozone Policy and  Strategies Group, EPA
Current EPA Research Viewpoint on Reactivity	1-12
       Basil Dimitriades, National Exposure Research Laboratory, EPA
California's Hydrocarbon Reactivity Program	1-17
       Randy Pasek, California Air Resources Board
The NAS/NRC Project on Reactivity	(no materials available)
       William Chameides, Georgia Institute of Technology
VOC Reactivity - Beyond Ozone 	1-29
       Alan Hansen, EPRI

SESSION II
Current Status of VOC Reactivity Research  	2-1
       William Carter, University of California at Riverside
VOC Reactivity Quantification: Approaches, Uncertainties, and Variabilities  	2-13
       Ted Russell, Georgia Institute of Technology
Quantification of Uncertainties in Reactivity Estimates for Volatile Organic Compounds .  . 2-27
       Jana Milford, University of Colorado at Boulder
Comparison ofPOCP and MIR Scales  	2-28
       Richard Derwent, Meteorological Office, United Kingdom
EPA's MODELS3 Framework and the Community Multi-Scale Air Quality Model	2-42
       Robin Dennis, National Exposure Research Laboratory, EPA
Establishing a Community Modeling Capability	2-63
       Kenneth Galluppi, University of North Carolina at Chapel Hill
Emissions Modeling Issues for Reactivity Calculations: State and Status of the Sparse Matrix
Operator Kernel Emissions (SMOKE) Modeling System  	2-74
       Neil Wheeler, Microelectronics  Center of North Carolina-NC Supercomputing
Desirable Scientific and Operational Criteria for Use ofEulerian Model to Compute VOC
Reactivity	2-85
       Harvey Jeffries, University of North Carolina at Chapel Hill

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SESSION III
Dunn-Edwards Proposed NARSTO Research on Ozone Formation Potential ofVOC Emissions
from Architectural Coatings 	->~
       Edward Edwards, Dunn-Edwards Corporation
                                                                                  •JO
CMA Research Initiatives  	-3"0
       Jonathan Kurland, Union Carbide Corporation
CSMA Position on the Importance of Relative Reactivity	3-17
       Doug Fratz, Chemical Specialties Manufacturers Association
Reactivity Concerns	3-31
       Phil Ostrowski, Occidental Chemical Corporation
Categorization of Low Reactivity Compounds 	3-41
       John Owens, 3M Company
Impact of a Molar Ethane Standard on the Number and Type ofVOC-Exemptible Compounds:
Practical and Environmental Implications 	3-45
       Daniel Pourreau, ARCO Chemical Company
General Industry Concerns with the Process 	3-54
       Donna Carvalho, Pennzoil Company/Magie Brothers Company

SESSION IV
A Global 3-D Radiative-Dynamical-Chemical Model for Determining Large-Scale Impacts of
Atmospheric Ozone Precursors	4-1
       Eduardo Olaguer, Dow Chemical Company
Reactivity Calculations with the Regional Atmospheric Chemistry Mechanism	4-2
       William Stockwell, Fraunhofer Institute
Hydrocarbon Reactivity and Ozone Production in Urban Pollution According to the Stockwell
el. al. (1990) Reaction Mechanism 	4-15
       Chris Walcek, State University of NY at Albany
Multi-day Impacts from Low Reactivity Compounds	4-24
       Gary Whitten, Systems Application International, Inc.
Computing Volatile Organic Compound Reactivities with a 3-DAQM	4-29
       Zion Wang, University of North Carolina at Chapel Hill
The Use of NAPS Data to Generate Sensitivities of Ozone Production Towards Changes in NOx
and VOCs	4_30
       Paul Makar, Atmospheric Environment Service
Temperature Dependence of Ozone Chemiluminescent Reactions with Organics: Potential
Screening Method for VOC Reactivities  	4.42
       Jeffrey Gaffney, Argonne National Laboratory
VOC Receptor Modeling as an Aid to Evaluating the Effect of Reactivity Changes on Ozone
Formation 	4.44
       Donna Kenski, US Environmental Protection Agency
The Impact ofBiogenic VOC Emission Modeling on the Simulation of a Long-term Ozone Time
Series  	4_59
       John Sherwell, Maryland Department of Natural Resources
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TV A's Research Efforts in Tropospheric Ozone Formation and the Contribution of Natural
Hydrocarbons to the Reactivity of Summertime VOCs in the Rural Southeastern US	4-69
      Roger Tanner, Tennessee Valley Authority
Computational Studies ofOxidant Reactions of Volatile Organic Compounds Relevant to the
Formation of Tropospheric Ozone	4-70
      David Dixon, Pacific NW National Laboratory

SESSION V
Atmospheric Chemistry of Organic Compounds	5-1
      Roger Atkinson, University of California at Riverside
Atmospheric Chemistry of Oxygenated Organic Compounds	5-14
      Ray Wells, US Air Force
Multicomponent Aerosol Generation System (MAGS) for the Study of Fine Particulates on
Photochemical Reactivity ofOrganics	5-28
      Shri Kulkarni, Kultech Incorporated, M. B. Ranade, Particle Technology, Inc.
Numerical Study of the Development of Ozone Episodes in  Germany; Relation of Anthropogenic
and Biogenic Hydrocarbons 	5-29
      Franz Fiedler, University of Kalsruhe, Germany
European Studies on the Photooxidation Mechanisms of Aromatic Hydrocarbons and
Oxygenates: Reactivity Implications	5-34
      Ian Barnes, Bergische University at Wuppertal, Germany
QUESTION/DISCUSSION SUMMARIES

PRESENTATION SUMMARIES	6-1
FREE FORUM SUMMARY	6-9
POLICY AND SCIENCE QUESTIONS SUMMARY	6-15
PUBLIC/PRIVATE PARTNERSHIP SUMMARY	6-19
AD-HOC OPERATOR TASK FORCE SUMMARY	6-20
APPENDICES

Appendix A - Attendees List	  A-l
Appendix B - Ad-Hoc Task Force - Minutes of Initial Meeting	B-l
                                        in

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PRESENTATIONS

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            Reactivity Workshop
                Meeting  Objectives
        1.  Obtain participant input on important reactivity-related issues.
           ( Incorporate finalized list in Proceedings Report)

        2.  Obtain participant input on reactivity-related research needs.
           (Incorporate finalized list in Proceedings Report)

        3.  Establish a volunteer Reactivity Research Planning Group to
           develop  a responsive research program plan.

        4.  Identify follow-up action items and an associated time table.

        5.  Determine type of partnership forum to be used in planning
           and implementing the reactivity research program
  J M Hales. May
          Some Design  Features
                  of this Meeting	
   Focus on scientific aspocts of reactivity concepts"Policy-relevant,
   but not policy-driven science;" (the NARSTO paradigm).

•  Structured around "science questions" and related "policy
   questions." (Initial sets to be modified by group process).

•  Define science issues associated with policy issues; don't
   attempt to resolve policy issues.

•  No pre-conceptions; no loaded agendas; a level playing field.
   This is an information-gathering and distillation process.

•  "Everybody wins" environment. (Including the citizen and
   the taxpayer).           .'
   J M Hales. M.iy I I'l'f

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           Having Said This  .  .  .
     . . There are some "complicating realities:"

     The term "reactivity" is used, but not defined explicitly in the 1990 CAAA.

     Any attempt to define this term explicitly, including adoption of any
     particular reactivity scale, has immediate policy implications.

     Associated legal action is contemplated and/or in progress.
   J M Hales. May
                 Therefore  .  .  .
  ...  If s critically important that we maintain an
  objective and scientifically oriented atmosphere
  at this workshop.
      Howard
        &
       Jake ^,-V
Science
   J M Hales MJV J'.
                          Policy
Legal
                         1-2

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                                 Welcoming Remarks
                                 Dr. Gary Foley, Director
                          National Exposure Research Laboratory
                           US Environmental Protection Agency
                           Office of Research and Development
Welcoming remarks were offered on behalf of EPA by Dr. Gary Foley, Director, National Exposure
Research Laboratory, EPA Office of Research and Development, and Ms. Sally Shaver, Director,
Air Quality Strategies and Standards Division, EPA Office of Air Quality Planning and Standards.
Dr. Foley welcomed the idea of incorporating reactivity research into the North America Research
Strategy for Tropospheric Ozone (NARSTO) program.  He stressed that the NARSTO partnership
between  government and the  private sector  has been  very  effective  in investigating the
photochemical ozone problem and that he is confident that the reactivity research effort will be
equally successful.
                                  Sally ShaVer, Director
                       Air Quality Strategies and Standards Division
                       Office of Air Quality Planning and Standards
                           US Environmental Protection Agency
Sally Shaver made welcoming remarks on behalf of EPA's Office of Air Quality Planning and
Standards.  She stated that it is important that EPA's policies reflect the best science, and she said
EPA looked forward to hearing the information which participants would provide.
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                                  A Public-Private Partnership
                                              for
                               Photochemical Reactivity Research
                                      Ronald K. Patterson
                               Associate Management Coordinator
                                     NARSTO International

                              U.S. Environmental Protection Agency
                               Office of Research and Development
                             National Exposure Research Laboratory

                                         ABSTRACT

The decision of the U.S. Environmental Protection Agency to re-evaluate its policy on photochemical
reactivity in an open forum, where regulated industries, the science community, and other stakeholders
can participate, sets the stage for forming a public-private partnership to resolve the science and policy
issues identified by the process.  The partnership approach to complex environmental issues normally
provides an opportunity for joint research planning, and a platform that the stakeholder community can
use to coordinate research activities, limit research gaps and duplication, leverage resources, and share
results.

NARSTO is a model for this type of partnership. NARSTO was established, under a non-binding
Charter in 1995, as a science-driven, tri-national, public-private partnership. To date, membership
consists of science agencies, regulatory agencies, regulated industries, academic institutions and public
interest groups in Canada, Mexico, and the United States. NARSTO facilitates, plans, and coordinates
policy-relevant research on atmospheric processes in the troposphere over North America. Ozone and
particulate matter are the current focus of the NARSTO program.  However, the research emphasis is
placed on atmospheric chemistry, modeling, emissions, monitoring, meteorology, methods development,
and integrated analysis and assessment. NARSTO provides quality assurance, data management, data
archival, and data accessibility guidelines and services to its members. Peer review of major NARSTO
outputs is provided by the National Research Council.

Photochemical reactivity is an integral part of the NARSTO research agenda, and this area of research
could be expanded under the NARSTO Modeling and Chemistry Team. If this workshop selects the
NARSTO partnership as its forum for conducting future reactivity research, then a NARSTO
subcommittee could be formed from volunteers identified in this audience. The subcommittee would
develop a strategic research plan for implementation  by the member organizations.  Each member
organization would accomplish its portion of the work using their individual institutional planning and
funding mechanisms. Under the NARSTO scenario,  each organization involved must sign the NARSTO
Charter as a sponsoring or participating partner.  Participating partners are usually academic and
contractor institutions. Many of the organizations attending this workshop are already NARSTO
partners.

This workshop will be declared a success, if those in  attendance can (1) identify the major policy and
science issues, (2) agree upon & partnership arrangement for planning and implementing future reactivity
research, (3) commit to participation in the planning  process, and  (4) commit to funding the research
agenda.
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                A PUBLIC-PRIVATE PARTNERSHIP
                            FOR
             PHOTOCHEMICAL REACTIVITY RESEARCH
                       Ronald K. Patterson
                  Associate Management Coordinator
                      NARSTO International
   Purpose of this Reactivity Workshop


 i Examine the policy issues

 i Evaluate the state-of-the-science

 i Commit to forming a partnership to resolve the
  science and policy issues

 i Commit to funding research under the
  partnership
           Public-Private Partnership



         • Involves all stakeholders

         • Provides a forum for joint research planning

         • Leverages resources         v

         • Coordinates research agenda

         • Limits research gaps and duplication

         • Shares data and information
          The NARSTO  Forum
• Science driven, tri-national, public-private partnership

• Established by a non-binding Charter in 1995

• Facilitates, plans, and coordinates policy relevant research
 on atmospheric processes in the troposphere over North
 America

• Provides quality assurance, data management, data
 archival, and data accessibility guidelines and services

• Provides NRC peer review of major products
           The  NARSTO Organization
             i Members
              • Science Agencies
              • Regulatory Agencies
              • Regulated Industries
              • Academic Institutions
              • United States, Canada, Mexico, (Europe)
            • Membership Types
              • Sponsoring Partners  (54)
              • Participating Partners (20)
              • Arfllliated Partners    (2)
                •EUROTRAC
                • IGAC

            (See Poster: 'A New Approach to Complex Environmental
            Problems in the  Continental Troposphere')
Reactivity - 05/07/98
                                                           1-5
         The NARSTO Program
    • Programmatic focus on Ozone and PM

    • Research emphasis on:
      • atmospheric chemistry
      • modeling
      • emissions
      • monitoring
      • meteorology
      • methods development
      • Integrated analysis and assessment

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                    The NARSTO Process
             (if selected as your partnership forum)
  Success for this Workshop
       • Organized as a Subcommittee under the Modeling and
        Chemistry Science Team

       • Planned and Coordinated by the Subcommittee

       • Implemented through the normal planning and funding
        mechanisms of the sponsoring Institutions

       • Quality assured, peer reviewed, archived, and assimilated
        using existing NARSTO systems
• Identify the major Policy and Science Issues

• Agree Upon a Research Partnership Arrangement

• Commit to Participation in the Strategic Planning
  Process

• Commit to Funding the Research Plan
            COMMITMENT QUESTIONNAIRE
            ii in lavor of a public
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          EPA Current
    Regulatory Viewpoint
           on Reactivity

             Bill Johnson
 Photochemical Reactivity Workshop
           May 12-14,1998
What is the History of...
        EPA's VOC Reactivity Policy?
EPA announced its reactivity policy on July 8,1977.
This policy classified VOC's into categories ...
    * Reactive
    • Negligibly Reactive

Four compounds were originally classified Negligibly
Reactive...
    * Methane
    • Ethane
    • Methyl chloroform
    « Freon 113

Today EPA still uses this 1977 Reactivity Policy.
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What VOC's have been ...
     Classified as Negligibly Reactive ?
  Early additions to the Negligibly Reactive list tended
  to be chlorofluorocarbons which possessed Sow
  reactivity and which could serve as replacements for
  stratospheric ozone depleters.

  Later Ethane was used as the standard cut-off
  comparing the reactivity of compounds. Those
  compounds with reactivities below ethane might be
  considered for Exemption

  Since 1977 more than 42 additional compounds or
  classes of compounds have been classified
  Negligibly Reactive and added to the Exempt list.
  How is the Reactivity of...
            a Compound Determined?
Most Exemptions were determined using the kOH value
(the reaction rate constant for the reaction of a
compound with the OH hydroxyl radical), expressed in
units of cm3/moiecule-sec, and compared to the kOH
value of Ethane.

In 1993, EPA began receiving VOC Exemption Petitions
based on the Maximum incremental Reactivity (MIR)
scale developed by Dr. William Carter at the University
of California at Riverside.  MIR values are expressed in
units of grams ozone produced per gram of compound
reacted.

Acetone was the first compound evaluated for
Exemption using MIR values.  This evaluation was made
on a per gram basis as stated in the Federal Register.
                     1-8

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  Questions Raised in using ...
            Values to Compare Reactivity
 The MIR values raised a number of questions.

   > Are MIR values better to use than kOH values for
     comparing reactivity?

   > Should a per gram or per mole be used for
     comparing compounds to ethane?

   > Could the ranking of compounds in order of
     reactivity by MIR value be used in some kind of
     substitution scheme of control?  How would such a
     scheme work?

 A review of the original 1977 experimental work used to
 select ethane as the Exempt cut-off showed that the
 experiments were done on a  mole basis.  Comparisons
 to ethane on a per gram basis may not be valid.
  Qu£sti|>ns Retitjpns Raised ab^ut;.,
      Consideration of Collateral Effects
Recent Petitions have raised questions about considering
collateral effects in granting exemptions to compounds.

  >• Should special consideration be given to exempting a
    compound slightly more reactive than ethane, but may
    displace more reactive and/or toxic compounds such
    as xylene? Would this be a positive environmental
    move, even if unlimited amounts of the exempt
    compound could then be used?

  > Should very toxic compounds or stratospheric ozone
    depleters be exempted if they are of low reactivity?

The 1977 policy indicates;EPA should consider such
environmental impacts in making exemption decisions (e.g.
we have never exempted benzene even though of low
reactivity.)
                       1-9

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     What is the Current Status of ...
                              Submitted to EPA?
       EPA has received 14 petitions on which action is
       pending. Most of these compounds are:
            > Not less reactive than ethane on a per
              mole basis or
            *- Hazardous air pollutants (under section
              112) or are stratospheric ozone depleters.
         Text for vapor pressure figure
EPA's definition of VOC does not include a vapor pressure cut off. At one time in
the late 1970's, EPA recommended a 0.1 mm Hg vapor pressure cut off.  In 1987,
EPA asked States to remove this from the VOC definition in their regulations.
The reason for removing the 0.1 mm Hg cut off can be seen from Figure 1.

The 0.1 mm Hg at 20 °C cutoff would only control compounds with carbon
number lower than about C12. The older Los Angles Rule 66 cut point (0.5 mm
Hg at 104°C) was actually more strict and would control compounds up to about
C18.

Studies have shown that compounds 
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                      FIGURE
  Vapor Pressure and Temperature in Relation to

                  VOC Definition
Vapor  pressure (mm Hg)
   1,000 F	
     100
      10
     0. 1
    0 0 i
                 Rule 66 cutoff - 0.5 mm Hg at 104 degrees C.
                  0. 1 mm Hg ot 20 degrees C.
            0        100       200       300

              Temperature (degrees C)
                         1-11

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               CURRENT EPA RESEARCH VIEWPOINT ON REACTIVITY
                                           by
                                    Basil Dimitriades
                             EPA/ORD/NERI7HEASD/ACPB
                                        RTP,NC

       EPA's main reason for wanting to update its reactivity policy, is the simple fact that the
"now science", that is, the scientific understanding we now have about the reactivity property of
organic compounds, is considerably different than the "then science", that is the scientific
understanding we had some two and a half decades ago, during the early 1970s, when the current
policy was conceived and formulated. Therefore, it would be useful to include in this workshop
this and other presentations that would help convey to this audience some understanding of the
changes in reactivity science that took place during the past two and a half decades.

       In this presentation, I will give you some historical information on the development of the
current policy, and after that, I will describe the scientific bases of the policy and point out
whatever weaknesses were revealed by the recent scientific evidence. This presentation and the
presentations later by the active researchers in this area, should make it possible to judge the
significance of the reactivity science changes that occurred during the last two and a half decades.
I should mention that nearly all of the material I will be discussing today is in a report I submitted
for publication in the Journal of the Air and Waste Management Association, some 3 months
ago.

       The initial version of the reactivity policy now in effect was developed in 1971, as part of
EPA's guidance to the States for preparation of State Implementation Plans for ozone attainment.
(Appendix B in EPA's  1971 Guidance...). In that version, EPA emphasized reduction of total
mass of organic emissions , but it also did take into account reactivity.  Specifically, it allowed
for substitution of a less reactive for a more reactive organic emission, if it could be shown that
such substitution would result in a reduction of the total reactivity of the emissions mixture. This
latter concession encouraged States to develop organic emission substitution regulations, such as
LA's Rule 66, which allowed a large number of organic emission species and emission mixtures
to be exempted from the ozone control regulations on grounds that they had if not negligible, at
least tolerably high reactivities.

       A few years after that, the researchers came out with the finding that pollutant transport
conditions in the atmosphere enhance ozone formation so as to make many of those organics that
were previously thought to be unreactive, to act as significant ozone producers.  This led EPA to
rethink its reactivity policy, and in 1977 it issued its next policy, under the title "Recommended
Policy on Control of Volatile Organic Compounds", which is the policy version now in effect,
and which policy, in contrast to the preceding one, it went from an extremely tolerant policy to an
extremely conservative one.  Specifically, by the 1977 policy only four organics were accepted as
negligibly reactive: methane, ethane, 1,1,1-trichloroethane (methyl chloroform), and
Trichlorotrifluoroethane (Freon 113). All other organic were assumed to be reactive, and, of
course, subject to the ozone regulations.  The policy, however, was flexible in that it allowed for
reactive organics to  be re-classified as negligibly reactive if and when new scientific evidence is

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produced and shown to support the reclassification. It should be noted at this point that at that
time EPA had not had standard test methods issued for determining whether an organic
compound is negligibly reactive or not — the burden for making this determination rested outside
the Agency. The Agency did support, however, development of such methods, and eventually
accepted them and offered them, unofficially at least, for public use. These methods, known as
the kOH and MIR methods, have been used routinely in the recent years to produce reactivity
evidence for many previously unstudied organics, and, as a result, several tens of organic
compounds have been re-classified and placed in the list of negligibly reactive or exempt
organics.

       Lastly, in 1992, EPA restated its reactivity policy, except that this time it used the term
"VOC" to denote organic compounds with significant potential for producing ozone, and
declared all organic emission species to be VOCs except those that were determined by EPA to
be non-VOCs.

       So much about the history of the EPA reactivity policy development. Next, I will talk
about the scientific basis of the existing policy and its weaknesses as?we see them now.

       There are five key components or elements that constitute the existing reactivity policy.
Subjects of these components are:

       (1)    Exemption of Organic Emissions on Reactivity Bases.

       (2)    Use of the, ethane reactivity as the "bright line" separating VOCs from non-VOCs.

       (3)    Reactivity Classification Guideline Methods.

       (4)    Assumed universal validity of reactivity scales

       (5)    Consideration of Emission Volatility.

(1)    "Exemption policy".  This policy element mandates that non-VOCs must be exempted
from the ozone-related control and inventory requirements. The bases for exempting the non-
VOCs are two judgments made by EPA at that time:

       - While all organic compounds are capable of producing more or less ozone in the
       atmosphere, not exempting those that produce only negligible amounts of ozone would be
       impractical.

       - The other judgment was based on the perception at the time that there is a significant
       number of organic compounds that have negligible reactivity ~ so, it would be worth the
       effort to classify organics into VOCs and non-VOCs.

       And so, in 1975 EPA decided to develop for official use a two-class reactivity
classification scale. To develop the requisite scale, EPA conducted a smog chamber study in


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which several organic compounds were irradiated under a standard set of extremely favorable
conditions, and resultant ozone yields were compared with the ozone air quality standard which
at the time was 0.08 ppm O3. The conditions used were 4ppm in moles of organic reactant -- a
concentration representative of the most polluted urban atmospheres at the time in the US --
0.2ppm in moles of NOX (giving a VOC-to-NOx ratio of 20:1, extremely favorable for ozone
formation), radiation comparable to that of natural sunlight in Los Angeles during summer, and
the test mixture was irradiated until the ozone concentration peaked out.  Results showed that
only four organics produced less than 0.08 ppm ozone: methane, ethane, trichloroethane, and the
trichlorotrifluoroethane, and these were, therefore, the only entries in the table of negligibly
reactive organics included in the 1977 policy.

       Obviously, that reasoning behind the  1977 reactivity classification was judged by EPA to
be consistent with the scientific evidence available and the best that could be thought of at the
time. Today, however, we have several reasons for questioning the validity of that evidence and
thinking.  One specific and strong objection we now have is to exempting the non-VOCs from
the emission inventory requirement.  Non-VOCs exempted from control will accumulate in the
atmosphere due to growth, and their ambient concentration will eventually reach the point at
which they will contribute to ambient ozone significantly. At that point, of course, they should
be taken into account in calculating control requirements. This would be impossible, however,
because the models used to compute control requirements require emission inventory data. Thus,
this "Non-VOC exemption" part of the EPA policy, clearly, must be re-considered.

(2)    Ethane reactivity bright line.  According to this policy element, organic emissions with
reactivity at or below the, ethane reactivity bright line  shall be exempted from the ozone
regulations as being non-VOCs. This policy  element was never issued by EPA officially. It
acquired the policy status when EPA began to use the comparison with ethane as the basis for
judging whether an organic is a non-VOC, and the rationale of this basis was, of course, the fact
that ethane is the most reactive species of those identified by EPA in 1977 as being negligibly
reactive. Regarding the validity of this policy element, there are several questions at issue. I will
discuss the most important ones, namely:

       (a) Is the choice of ethane as the boundary reactivity species an appropriate one?

       (b) To determine VOC or non-VOC nature of an organic, should the comparison of the
       organic with ethane be made on a per-unit-weight or on a per-mole basis?

       (c) Is the distinction between VOCs and non-VOCs really necessary?

       To answer the first question, of whether the ethane reactivity is the appropriate boundary
separating VOCs from non-VOCs, we need to go back to the reasoning EPA used in 1977 to
classify organics into VOCs and non-VOCs.   In that study there were some 20 low reactivity
organic compounds tested, and of those, four were found to produce ozone less than 0.08 ppm.
Of those four, ethane was the most reactive one and on those bases, ethane was taken,
unofficially, to be the "boundary" reactivity species. Are these bases valid?  Today we don't
think so, for several reasons. First, we believe today that ethane, if allowed to accumulate in the

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atmosphere at higher than 4 ppm levels, will produce more ozone than 0.08 ppm.  Second, we
also know today that testing organics using modern smog chamber methodology gives much
higher ozone concentration results, the main reason being that nowadays the test organic is not
irradiated in the smog chamber alone, as was done then; instead, it is irradiated in the presence of
other organics, and this, of course, is much more realistic and it results in much more ozone.

       The second question, whether organics should be compared with ethane on a per-unit-
weight basis or a per-mole basis, is raised because it makes a difference  whether we use the  one
or the other basis. Relative to the per-mole basis, comparison with ethane on a per-unit-weight
basis tends to cause reactive, high molecular weight organics to have artificially reduced
reactivity values and be classified as negligibly reactive, in conflict with the per-mole
comparison. Which is correct?  To answer this question, once again we need to go back to the
EPA smog chamber study of the mid-1970s, that led to the selection of ethane as the boundary
species.  If you recall, the comparison of the organics in that smog chamber study was done  for
equimolar concentrations. Based on that, and for consistency shake, the comparison with ethane
must be made on a per-mole basis. Needless to say, we could have compared the test organics in
the EPA study for equal weight, rather than mole concentrations, but then the boundary
reactivity species would have been not ethane but some other species. Comparing organics with
that species on a per-unit-weight basis would alleviate but not eliminate the problem. In fact, our
conclusion is that regardless of how we compare the reactivities of organics to the boundary
level, it is not possible to avoid this problem completely, and this constitutes a conceptual
weakness of this policy element that calls for classifying organics into VOCs and non-VOCs
based on comparison with a given organic compound's reactivity.
                      V
       The final question, whether the VOC-vs-nonVOC distinction is necessary is to some
extent of policy nature. The need for making such a distinction depends on whether the Agency
wants to stay with the existing policy of exempting only those organics which are shown to be
negligibly reactive, or decides to adopt, another policy instead, for example,  a policy of
exempting organics that have non-negligible reactivity but are to be used as substitutes for other
much more reactive organics.

       3. Reactivity Classification Guideline Methods Existing EPA guidelines for such
methods are unofficial. The kOH and MIR methods acquired the status  of guideline methods
because data obtained with such methods have been accepted by EPA in processing petitions for
exempting organic emissions from ozone regulations. What do we think today about these
methods?

       We now believe that the kOH method has very limited utility because it represents how
fast the organic reacts with the OH radical ~ the first reaction step in the ozone forming process
 but it tells us very little about the follow-up chemistry that results in formation of ozone. The
MIR method has greater validity in that it does provide a direct measure of ozone production,  but
it is based on use of the EKMA model, a model now thought to be outdated. We still consider
the MIR method very useful, but we believe  that current science allows  for development of other
modeling methods which, while much more  complex, can provide more accurate reactivity
estimates. [More about these methods in subsequent presentations]

                                     1-15

-------
       4. Universal validity of reactivity scales. The existing policy is based on the assumption
that the current classification of organics into VOCs and non-VOCs is universally valid,
independent of ambient conditions. We now know, however, that the ozone formation chemistry
is such that reactivity varies with conditions such as organic-to-NOx ratio, ambient organic
composition, sun light intensity, and pollutant transport conditions. This, obviously, raises
questions about the practicality of a reactivity scale that is not universally valid. We need to
think about this and find some way of using the reactivity concept in a way that the effect of this
problem is minimized.  For example, consideration should be given to the fact that the
uncertainty introduced by this ambient condition variability factor is much smaller for relative
reactivities than for absolute reactivities. This means, of course, that  policies that place the
emphasis on relative reactivity data, e.g., emission substitution, may be more reliable in so far as
this problem is concerned than policies that place the emphasis on absolute reactivity data, as the
existing policy is.

       5. Emission Volatility.  The existing EPA policy distinguishes between VOCs and non-
VOCs and cites reactivity as the basis for the distinction but says nothing about volatility. There
are guideline methods for determining whether an organic is negligibly reactive or not, but there
are no such methods for determining  whether an organic is negligibly volatile or not.  Thus, the
reactivity and volatility properties of  organic emissions have been receiving different regulatory
treatments, apparently without scientific justification, and this inconsistency should perhaps be
rethought.


            CONCLUSIONS

In contrast to the mid-1970s thinking, our current thinking suggests that

       1. exemption of non-VOCs from the inventory requirement is  unjustifiable;

       2. use of the ethane reactivity  as the boundary level separating VOCs from non-VOCs has
       both validity and operational problems (basis of comparison);

       3. current science allows for development of more reliable guideline methods for
       classifying organics into "reactive" and negligibly reactive.

       4. policies that place the emphasis on relative reactivities are probably-subject to less
       uncertainty relative to those that rely on use of absolute reactivity data; and

       5. it is unjustifiable for the current policy to treat the reactivity and volatility properties of
       organic emissions differently with respect to the photochemical ozone pollution problem.
                                           1-16

-------
     California's
    Hydrocarbon
Reactivity Program
           By
     Randy Pasek Ph.D.
 California Air Resources Board
            at
    U.S. EPA Reactivity
        Workshop
      May 12-14, 1998
 California's Reactivity
       Beginnings

+ In 1987 ARE formed advisory
  board on fuels.

+ Needed way to compare
  alternatively fueled vehicle's
  emissions.

+ Use of reactivity of vehicle
  exhaust for comparisons.

+ Adopted LEV/CF regulations
  in late 1990 (RAF).

+ VOC exemptions

-------
oo
     Other Possible
    Reactivity Based
         Programs

+ Future Possibilities
  - Aerosol Coatings
  - Consumer Products
  - Emissions Trading
  - Aerosol Forming Reactivity
  - Motor Vehicles
       Challenges
      Encountered

+ Reactivity Scale
  - MIR
     • Dual control program in CA
     • MIR scale complements NOx
      controls
+ Uncertainty
  - Alternative fuels program
    (LEV/CF)
     • MIRs -30 - 70%
     • RAFs ~5 - 15%
  - Consumer Products
     • Most-used compounds well
      characterized

-------
        Challenges
          (continued)
+ Speciation Profiles
  - Uncertainty
  - Inventory and modeling
+ Unstudied Compounds
  - Alternative fuels program
    (LEV/CF)
     • Most compounds — some data
  - Consumer Products
     • Some compounds ~ no data
     • Upper limit MIR Estimation
        Challenges
          (continued)

+ Regulation Development
  - Good science
  - Flexibility
  - Simple
  - Equivalent ozone benefits
  - Enforceable
  - Cost effectiveness

-------
to
o
       Challenges              California's Reactivity


         (continued)                        Program


+ How to incorporate exemptions

  into reactivity regulations.             ^
                                   + Research
  - VOC exemptions

     • CA has own review                 + Reactivity Team

     • Methane or ethane

  - Other policy exemptions              + External Assistance

-------
         Research
+ Uncertainty

   - Chamber parameters' effect on
    MIR values

+ Reactivity Value Estimates
   - Consumer product compounds
   - Auto exhaust
   - Other important mixtures

+ Improvement of Reactivity
  Value Estimates
   - Lower cost
   - Lower uncertainty
          Research
          (continued)

+ Atmospheric Chemistry
   - C10 alkanes

+ Speciation
   - Architectural & Aerosol coatings
   - "Complete picture profiles"
   - Surveys to obtain formulation
    data

+ Model Improvement
  - Chemical mechanisms
  - Regional Scale
  - Aerosols
  - Photolysis

-------
Feature*
Chemistry
Physics
Emissions
Melric
MIR (Carter)
- SAPRC-90
- SAPRC-97 (ongoing)
- Simple box model
- Represents urban airshed
- No transport
- Simple "meteorology"
- EKMA type
- Represents 39 cities
- Maximum change in O,
concentration
Previous Grid-Based Simulations
(McNairtt al., and Bergin el al.)
- Lurman, Coyner and Carter (LCC)
• Complex 3-D grid-based domain
- Represents urban airshed
- No long-range NO, transport
- Diagnostic meteorology
- Carnegie/California Inslitulte of
Technology (CIT) with Diagnostic
Wind Model
- Detailed grid-based urban and rural
emissions from most source
categories
• August 30 -September 1 , 1 982 (SC)
- August 27-29. I987(SC)
- Maximum change in peak O,
concentration(l-hr)
- Exposure above National and State
AAQS
ARB'i Grid-Based Simulations
- SAPRC-97
- possible aqueous-phase
chemistry in the near future
- Complex 3-D grid-based domain
- Represents regional airshed
- Long-range NO, transport
- Prognostic meteorology
- SAQM with MM5
- Detailed grid-based urban and
rural emissions from most
source categories
• Maximum change in peak O,
concentration (1-hr, 8-hr)
- Exposure above National and
State AAQS
-Others?
     Reactivity Team
+ Airshed Modeling

+ Uncertainty Analysis

   - Perform overall analysis for
    stationary sources
      • Includes uncertainties in speciation
       and reactivity estimates

+ Exploring Aerosol forming
  potential

   - Determine implications for
    different control strategies
               1-22

-------
K)
UJ
     External Assistance
+ Reactivity Research Advisory
  Committee
+ Reactivity Scientific Advisory
  Committee
  Reactivity Research
  Advisory Committee

+ Over 20 representatives from
  industry.

+ Provide technical assistance on
  reactivity related issues —
  consumer products and
  coatings.

+ Forum to coordinate research
  activities between industry and
  government.

-------
to
 Reactivity Scientific

Advisory Committee

Six independent, respected
scientists
 - Professors John Seinfeld,
  Roger Atkinson, Jack Calvert,
  Harvey Jeffries, Jana Milford, and
  Armistead Russell
Offer recommendations on
reactivity related scientific
issues
   Development of a
Reactivity Program  for
Consumer Products in
       California

-------
   Current Qzone Control Strategy for
   Consumer Products (Mass Based)
Antiperspirant
& Deodorant
Phases I, II, III
  Aerosol
  Coatings
                 80
Categories
Regulated
                                VOC Limits
                Innovative Product
                   Provision
                (product-lo-product comparison)
                   Alternative
                  Control Plan
                   (emissions averaging)
       Using Photochemical
  Reactivity as a VOC Control
               Strategy

 + Formed Workgroup with Industry
  July 1995
 + Draw on Experience from LEV Program
 + MIR Scale Developed by Dr. Carter
 + Voluntary Alternative
 + Ensure Equivalent Ozone Reductions
                 1-25

-------
        Main Goal:  Flexibility While Reducing
     Ozone Formation Potential More Efficiently
Existing Program: Decreased VOC, Decreased O3
                                       Reformulation Costs
                                       Water-Based System
                                       Apparent Change
                                       Lower Performance?
    Non-Complying             Complying
Reactivity Program: Decreased O3, Little/No Change in VOC
                                       Reformulation Costs
                                       Solvent-Based System
                                       Transparent Switch
                                       Higher Performance?
Non-Complying
                         Complying
         Proposed Draft Voluntary
     Regulation for Aerosol Coatings

 + Law Requires 60% Reduction in VOC
   Emissions (by end of 1999)
 + Goal to Establish Equivalent Reactivity
   Limits to Existing Mass-based Limits
 + Speciated Data are Necessary to Establish
   Limits
                      1-26

-------
     Hypothetical Paint Formula and
     Calculation of Weighted Reactivity
            Weight     MIR   Weighted
    Contents  Percent  (Relative) Reactivity
acetone
toluene
propane
xylene
butane
solids
30%
20%
20%
10%
10%
10%
0
1.26
0.14
2.09
0.29
0
0.00
0.25
0.03
0.21
0.03
0.00
    Total    100%               0.52
    Product MIRabs = 0.52 x 4.06 = 2.11 g O3/g product
            Aerosol Coatings
                  Schedule
Workshop, 5/19/98 | Draft Reactivity Reg. for
                             •-<.
                        Aerosol Coatings
Workshop, 7/98
Workshop, Late
Summer 1998
November 1998
Draft reactivity-based
  VOC limits for Aerosol
  Coatings
Revised draft reactivity
  reg. (if necessary)
Board Hearing
                  1-27

-------
              O3 Equivalence to Percent
                        Reduction

          Steps                    Example
(1) Determine % reduction of the—*• Reduce emissions by 50%
   VOC limit
(2) Calculate abs. SWA-MIR for-*. MIRcat = 2.0 (g O3/ g VOC)
   Aerosol Paint Category
(3) Apply % reduction to MIR of-*- Reduce MIR by 50%
   category                  = 0.5 x 2.0 = 1.0 (g O3/ g VOC)
(4) Result = abs. wtd-MIR of   -*- Wtd-MIR Limit
   category equal in percent      = 1.0 ( g O / g VOC)
   ozone reduction from VOC             3
   limit
                  Summary


        + ARB has successfully used
          reactivity in regulations since
          1990
        + ARB has an integrated program
          to address challenges associated
          with using reactivity in
          regulations
           - Research
           - Internal Expertise
           - External expertise
                        1-28

-------
VOC Reactivity  -  Beyond Ozone
            D. Alan Hansen
                 EPRI
      Photochemical Reactivity Workshop
               Durham, NC
              12-14 May 1998
                   1-29

-------
                          VOC Reactivity - Beyond Ozone

Outline

1. Purpose of talk: In keeping with the principle of integrating assessments of emissions
   management across air quality issues as promoted by the FACA subcommittee on
   ozone, PM and regional haze, I want to emphasize the point that considerations of VOC
   reactivity in managing tropospherk ozone should also take fine particles into account.
   Fine particles, of course, are largely responsible for the optical effects associated with
   regional haze.
2. I will briefly summarize the interplay between VOCs and NOx in the photochemical
   production of ozone and fine particles.
3. I wfll then show some modeling results that demonstrate, assuming that the models
   capture the essence of the precursor chemical interactions among themselves and with
   meteorology, the complexity of the responses of ozone and selected fine particle
   constituents to reductions in precursor emissions.
4. I wfll finish with some issues related to VOC reactivity that should be resolved if we are
   to manage tropospheric ozone and fine particles (and, by extension, regional haze)
   effectively.

Chemistry

Referring to the chemical mechanism schematic (taken from the as yet unpublished
NARSTO Critical Review paper, "Oxidant  Production and Fine Particles: Issues and
Needs" by Hidy, Hales, Roth and Scheffc):

1. Note precursors :JVOx, VOCs, SOj.
2. Note route to ozone: Daytime, O3->O1 D->OH->RO2->NO2->O3;
3. Note routes to fine PM:
   Daytime: OH+VOC-> PM ; O3+VOC-> PM ;  OH+SO2 (NH3)->PM ; OH+NO2
   (NH3)->PM
   Nightime: O3+olefins->OH etc.; NO3+VOO PM; N2O5 (H2O, NH3)->PM
4. Note VOCs and NOx play prominent roles in both ozone and PM formation chemistry

So what happens if we change the concentrations of VOC and NOx through emissions
changes? The picture is sufficiently complex that answering this question can rely on
environmental chamber experiments. However, these cannot account for meteorological
effects and usually cannot be conducted at precursor concentrations as low as those
prevailing in real urban and  regional atmospheres. To explore how VOC reactivity
influences ozone and PM behavior under realistic conditions, we must rely on modeling.

Model Results

The modeling results shown in the four tables are taken from runs made with UAM-AERO
simulating SCAQS episodes in June and December 1987. The may not be representative of
results obtained with other models or from other geographical locations or episodes.  They
                                    1-30

-------
have been selected only to demonstrate the complex interplay between changes in
precursor NOx and VOC emissions and changes in ozone and various components of PM
2.5. In the tables PM2.5 OM denotes the "organic material" component of fine particles.
The values shown for PM2.5 and it components are averaged over the two days of each
episode. The discussion below focuses on the Percentage Change tables:

Points to note for the June 1987 episode:

1. With 50% NOx reduction:
   •  O3 can increase substantially (>20%) or decrease (<15%)
   •  PM2.5 NO3 decreases substantially (20-46%)
   •  PM2.5 OM increases slightly (3-6%)
   •  PM2.5 SO4 is relatively unaffected (±2%)
   •  PM2.5 Mass decreases slightly (6-12%)
   •  Question: What if the material of interest from a health effects perspective was in
      the OM component, which did not decrease with a 50% NOx reduction?
2. With a 50% VOC reduction:
   •  O3 decreases substantially (20-42%)
   •  PM2.5 NO3 decreases slightly (6-13%
   •  PM2.5 OM decreases slightly (8-10%)
   •  PM2.5 SO4 is relatively unaffected (+2%)
   •  PM2.5 Mass decreases slightly (4-9%)
3. With 50% NOx and VOC reduction:
   •  O3 increases less than with NOx reduction only and decreases less than with VOC
      reduction only.
   •  PM2.5 NO3 decreases about the same as with NOx reduction only.
   •  PM2.5 OM decreases less than with VOC reduction only and with no increases.
   •  PM2.5 Mass decreases the same or slightly more than with either NOx or VOC
      reduction alone.

Bottom line:

4. With 50% NOx reduction:
   •  O3 can go up or down
   •  PM2.5 NO3 and Mass go down
   •  PM2.5 OM goes up
   •  PM2.5 SO4 is relatively unaffected.
5. With 50% VOC reduction:
   •  Everything goes down.
However, PM2.5 OM is relatively insensitive to both NOx and VOC reductions.

Points to note for the December 1987 episode:

1. With 50% NOx reduction:
   •  O3 increases 60-138% (even the highest value, 122 ppb, more than doubles)
                                       1-31

-------
   •  PM2.5 NO3 increases (counterintuitively) 10-42%
   •  PM2.5 OM increases 4-9%
   •  PM2.5 SO4 is relatively unaffected, increasing up to 3%.
   •  PM2.5 Mass increases 4-17%.
2.  With 50% VOC reduction:
   •  O3 decreases 0-37% (again a counterintuitive lack of response in some parts of the
      domain)
   •  PM2.5 NO3 decreases 27-42% (about the same as in summer)
   •  PM2.5 OM decreases 5-9% (about the same as in summer)
   •  PM2.5 SO4 is relatively unaffected, decreasing 2-5%, but with no small increases as
      in summer.
   •  PM2.5 Mass decreases 8-13%, slightly more than in summer.
3.  With 50% NOx and VOC reduction:
   •  O3 generally increases, but less than with NOx reduction alone.
   •  PM2.5 NO3 decreases about the same as with VOC reduction alone, except the
      domain max, which decreases half as much as with VOC reduction alone.
   •  PM2.5 OM decreases slightly (3-5%).
   •  PM2.5 SO4 is essentially unchanged.

Bottom line:
      •  NOx reduction increases everything.
      •  VOC reduction decreases everything.
      •  NOx and VOC reduction decreases PM 2.5, but not O3.
                  V
Outstanding Questions
•  If higher reactivity VOCs prompt ozone formation and lower reactivity VOCs delay
   ozone formation, how does the relative amount of ozone formed per carbon atom
   compare?

•  Is there a relationship between VOC reactivity and amount of PM formed?

•  Does the chemical mechanism accurately reflect the SVOC produced from oxidation of
   HC*s? From unsaturated oxygenates?

«  Do current lumping schemes hi chemical mechanisms accurately reflect the nuances of
   reactivity with respect to ozone aerosol production as well as the role of reactive
   intermediates in the process?

•  How will the composition and rate of production of SVOC respond to changes in VOC
   reactivity?
                                      1-32

-------
•  How will rate of production and yield of nitrate and sulfate respond to changes in VOC
   reactivity?

•  How will deposition of N and S respond to changes in VOC reactivity?
                                         1-33

-------
                                                               NighlthitNSOS
                                                               Chemtrtry
                       Radical Pool
                       HO2-; RO2-
                                                   SOx

                                                Clouds/Aqueous
Figure 9. Process diagram illustrating tropospheric chemistry pathways linking oxidant and secondary
PMi.s formation. The gas phase reactions leading to atmospheric oxidant formation, including O3, are
generally to the left and the top right of the diagram. The aerosol particle formation processes are linked
with the oxidant forming cycle, and are indicated in the middle and lower right of diagram.
                           f
                                                1-34

-------
                        ABSOLUTE CHANGE
  Jun-87
        Baseline
50% Red. NOx
50% Red. VOC
50% Red. NOX&VOC
          DOMAIN MAX
DAY 175 DAY 176       Day 175 or 176          PM
  O3     O3  PM2.5NO3 PM2.5OM PM2.5SO4 2.5 Mass
404.8
451.2
272.0
337.8
353.5
300.5
230.1
261.2
48.1
33.5
42.0
33.7
19.1
19.6
17.4
17.8
32.7
32.2
32.4
32.2
100.8
93.8
91.7
91.7
                         HIGHEST STATION
                 DAY 175 DAY 176       Day 175 or 176          PM
                    O3     O3  PM2.5NO3 PM2.5OM PM2.5SO4 2.5 Mass
        Baseline
50% Red. NOx
50% Red. VOC
50% Red. NOX&VOC
152.2
183.1
88.9
146.6
199.1
185.0
118.2
164.1
26.8
14.4
25.1
15.9
8.7
9.2
7.8
8.1
7.4
7.4
7.4
7.4
68.0
60.0
63.9
58.8
                       AVERAGE OF STATIONS
                 Day 175  Day 176        Day 175 or 176          PM
                    03      O3  PM2.5NO3 PM2.5OM PM2.5SO4 2.5 Mass
        Baseline
50% Red. NOx
50% Red. VOC
50% Red. NOX&VOC
90.6
103.7
72.2
89.4
85.5
103.8
66.3
86.3
16.8
13.4
15.5
13.0
6.4
6.7
5.9
6.1
8.1
8.2
8.0
8.1
53.1
50.1
50.8
48.7
                        ABSOLUTE CHANGE
    Dec-87
         Baseline
 50% Red. NOx
 50% Red. VOC
 50% Red. NOX&VOC
           DOMAIN MAX
                  Day 344 Day 345
                    O3
                     Day 344 or 345
PM
          O3   PM2.5NO3 PM2.5OM PM2.5SO4 2.5 Mass
90.0
185.0
90.0
104.0
122.0
280.0
80.0
108.0
61.4
87.0
35.6
49.0
37.5
40.7
34.3
35.6
26.0
26.0
25.4
25.6
190.0
223.0
166.0
167.0
                         HIGHEST STATION
                  Day 344 Day 345
         Baseline
 50% Red. NOx
 50% Red. VOC
 50% Red. NOX&VOC
                    O3
                     Day 344 or 345
PM
          O3  PM2.5NO3 PM2.5OM PM2.5SO4 2.5 Mass
40.8
73.0
33.0
51.5
39.7
62.8
34.1
49.8
20.3
24.5
14.7
14.5
23.7
24.8
22.6
22.9
3.9
3.9
3.7
3.8
116.0
123.0
107.0
107.0
                       AVERAGE OF STATIONS
                  Day 344 Day 345
                     Day 344 or 345
PM
         Baseline
 50% Red. NOx
 50% Red. VOC
 50% Red. NOX&VOC
                    03
          O3  PM2.5NO3 PM2.5OM PM2.5SO4 2.5 Mass
34.7
75.8
21.9
45.3
30.4
< 72.1
19.2
42.5
18.7
20.5
13.6
13.3
18.0
18.8
17.1
17.4
2.9
3.0
2.8
2.9
86.0
89.0
79.0
79.0
                            1-35

-------
                          PERCENT CHANGE
  Jun-87
Baseline, ppb or ug/m3
50% Red. NOx
50% Red. VOC
50% Red. NOX&VOC
           DOMAIN MAX
DAY 175 DAY 176        Day 175 or 176
                                                               PM
                    O3     Q3   PM2.5NO3 PM2.5OM PM2.5SO4 2.5 Mass
    11.5
   -32.8
   -16.6
-15.0
-34.9
-26.1
"-30.4
 -12.7
 -29.9
 2.6
-8.9
-6.8
         -1.5
         -0.9
         -1.5
                            -6.9
                            -9.0
                            -9.0
                           HIGHEST STATION
                  DAY 175 DAY 176        Day 175 or 176
                                             PM
                     O3     O3  PM2.5NO3 PM2.5OM PM2.5SO4 2.5 Mass
Baseline, ppb or ug/m3
50% Red. NOx
50% Red. VOC
50% Red. NOX&VOC
20.3
-41.6
-3.7
••^^••^•^••w™™™
-7.1
-40.6
-17.6
-46.3
-6.3
-40.7
5.7
-10.3
-6.9
0.0
0.0
0.0
-11.8
-6.0
-13.5
                         AVERAGE OF STATIONS
                  Day 175 Day 176         Day 175 or 176
                                             PM
                                  PM2.5NO3 PM2.5OM PM2.5SO4 2.5 Mass
Baseline, ppb or ug/m3
50% Red. NOx
50% Red. VOC
50% Red. NOX&VOC
                          PERCENT CHANGE
     Dec-87
  Baseline, ppb or ug/m3
  50% Red. NOx
  50% Red. VOC
  50% Red. NOX&VOC
            DOMAIN MAX
                   Day 344 Day 345
                       Day 344 or 345
                                  PM
   O3      O3   PM2.5NO3 PM2.5OM PM2.5SO4  2.5 Mass
   nrifflMBrifflffl^^                          '111 ~
   105.6   129.5      41.7      8.5       0.0      17.4
     0.0   -34.4     -42.0      -8.5      -2.3     -12.6
    15.6   -11.5     -20.2      -5.1      -1.5     -12.1
                           HIGHEST STATION
                   Day 344 Day 345        Day 344 or 345
                                             PM
  Baseline, ppb or ug/m3
  50% Red. NOx
  50% Red. VOC
  50% Red. NOX&VOC
   O3
    m
    78.9
    -19.1
    26.2
                             O3   PM2.5NO3 PM2.5OM PM2.5SO4 2.5 Mass
 58.2
-14.1
 25.4
 20.7
-27.6
-28.6
 4.6
-4.6
-3.4
         0.0
         -5.1
         -2.6
                             6.0
                            -7.8
                            -7.8
  Baseline, ppb or ug/m3
  50% Red. NOx
  50% Red. VOC
  50% Red. NOX&VOC
       AVERAGE OF STATIONS
 Day 344 Day 345        Day 344 or 345           PM
   O3     O3   PM2.5NO3 PM2.5OM PM2.5SO4 2.5 Mass
 ||jB|y2||jjUH^JiJR[fdH^H|^^^^^^^^^^^^^^^^IIj5g~0
 •^^^^^•^^^^^^^^^^^•^^^^^•^•••••^•^^•••••••^^^^••••^••••••••WKli^'MtfV
   118.4   137.2       9.6      4.4      3.4      3.5
    -36.9   -36.8     -27.3      -5.0      -3.4     -8.1
    30.5    39.8     -28.9      -3.3      0.0     -8.1
                                 1-36

-------
Current Status of VOC
  Reactivity Research
          William Carter
      University of California
            at Riverside
            Presented at:
   Photochemical Reactivity Workshop
        Durham, North Carolina
           May 12-14, 1998
  CURRENT STATUS OF REACTIVITY RESEARCH


BACKGROUND

  •  DEFINITION OF REACTIVITY

  •  FACTORS AFFECTING REACTIVITY

  •  MEASUREMENT OR CALCULATION OF REACTIVITY

RESEARCH AREAS AND UNCERTAINTIES

  •  CHEMICAL MECHANISM

     • STATUS OF MECHANISM DEVELOPMENT

     • DATA NEEDS FOR MECHANISM AND REACTIVITY
       EVALUATION

     • UNCERTAINTY ANALYSIS

  •  AIRSHED MODEL UNCERTAINTY

  •  DEPENDENCE OF REACTIVITY ON  ENVIRONMENTAL
    CONDITIONS AND OZONE QUANTIFICAITON METHOD

-------
                     INCREMENTAL REACTIVITY
                                                                  FACTORS AFFECTING INCREMENTAL REACTIVITY
to
NJ




Lim
OZONE
FORMED
WHEN VOC
ADDED TO
EPISODE


-


OZONE '.
FORMED
IN
EPISODE

[VOC]-» 0
[VOC ADDED]
           INCREMENTAL
           REACTIVITY
           OF  A VOC IN
           AN  EPISODE
NOT AN INTRINSIC PROPERTY OF THE MOLECULE.
DEPENDS ON THE EPISODE AS WELL AS THE VOC.

THIS IS THE MOST DIRECTLY RELEVANT REACTIVITY
MEASURE FOR APPLICATION TO CONTROL STRATEGIES:

CAN BE MEASURED EXPERIMENTALLY IN SMOG CHAMBERS
OR CALCULATED FOR POLLUTION EPISODES USING
AIRSHED MODELS.

NOT SAME AS OZONE PRODUCTIVITY, THE AMOUNT OF O3
ATTRIBUTABLE TO NO TO N02 CONVERSIONS CAUSED BY
PEROXY RADICALS FORMED FROM THE VOC.
                                                            INCREMENTAL
                                                             REACTIVITY

                                                            MECHANISTIC
                                                             REACTIVITY
                     KINETIC   y
                    REACTIVITY

                     DIRECT
                   MECHANISTIC +
                    REACTIVITY
MECHANISTIC
 REACTIVITY

  INDIRECT
MECHANISTIC
 REACTIVITY
KINETIC REACTIVITY:  FRACTION OF EMITTED MOLECULE
WHICH REACTS.
  • PROPORTIONAL TO REACTION RATE FOR SLOWLY
    REACTING COMPOUNDS
  • INDEPENDENT OF REACTION RATE (APPROACHES 1.0)
    FOR RAPIDLY REACTING COMPOUNDS

MECHANISTIC REACTIVITY:  AMOUNT OF OZONE FORMED
PER MOLECULE REACTING

    DIRECT REACTIVITY ("PRODUCTIVITY"):  03 FORMED
    FROM THE PEROXY RADICALS FROM THE VOC.

    INDIRECT REACTIVITY:  CHANGE IN O3 FORMED FROM
    PEROXY RADICALS FROM THE OTHER VOCs PRESENT.

      • EFFECTS ON RADICAL LEVELS AFFECTS HOW
        MUCH THE OTHER VOCs REACT.

      • EFFECTS ON NO, CONSUMPTION AFFECTS HOW
        MUCH 03 IS FORMED FROM A PEROXY RADICAL.

-------
             ENVIRONMENTAL FACTORS WHICH
             AFFECT INCREMENTAL REACTIVITY
                                                                 MEASUREMENT OR CALCULATION
                                                            OF ATMOSPHERIC INCREMENTAL REACTIVITY
K)
UJ
NO, AVAILABILITY IS MOST IMPORTANT SINGLE FACTOR
AFFECTING MECHANISTIC REACTIVITIES.

  • 03 MOST SENSITIVE TO VOCs WHEN NO, IS HIGH, NOT
    SENSITIVITY TO VOCs WHEN NO. LOW.

  • REACTIVITIES AT HIGH NO, ARE SENSITIVE TO
    MECHANISTIC FACTORS WHICH AFFECT RATES OF O3
    FORMATION (E.G. RADICAL INITIATION/TERMINATION).

  • REACTIVITIES AT LOW NO, ARE SENSITIVE TO
    FACTORS WHICH AFFECT RATES OF NO, REMOVAL.

DURATION OF SCENARIO AND RADICAL LEVELS AFFECTS
REACTIVITIES OF SLOWLY REACTING COMPOUNDS.

SENSITIVITY TO RADICAL INITIATION/TERMINATION IS
AFFECTED BY LEVELS OF OTHER RADICAL INITIATORS.

OTHER FACTORS (E.G., SUNLIGHT AND TEMPERATURE)
AFFECT DEPENDENCE OF REACTIVITY ON NO,
REACTIVITY CAN BE MEASURED IN ENVIRONMENTAL
CHAMBER EXPERIMENTS. BUT THE RESULTS ARE NOT THE
SAME AS REACTIVITY IN THE ATMOSPHERE.

   • NOT PRACTICAL TO EXPERIMENTALLY DUPLICATE ALL
    ATMOSPHERIC CONDITIONS AFFECTING REACTIVITY

   • CHAMBER EXPERIMENTS HAVE WALL EFFECTS,
    USUALLY HIGHER LEVELS OF NO, AND ADDED TEST
    VOC, STATIC CONDITIONS, ETC.

ATMOSPHERIC REACTIVITY MUST BE CALCULATED USING
COMPUTER AIRSHED MODELS, GIVEN:

   • MODELS FOR AIRSHED CONDITIONS

   • CHEMICAL MECHANISMS FOR THE VOC's
    ATMOSPHERIC REACTIONS

CALCULATIONS OF ATMOSPHERIC REACTIVITY CAN BE NO
MORE RELIABLE THAN THE CHEMICAL MECHANISM USED.

ENVIRONMENTAL CHAMBER EXPERIMENTS ARE
NECESSARY TO TEST THE RELIABILITY OF A MECHANISM
TO PREDICT ATMOSPHERIC REACTIVITY.

-------
to
   MECHANISMS FOR REACTIVITY ASSESSMENT

               SAPRC-90 MECHANISM

 REFLECTS KNOWLEDGE AS OF 1989.

 03 PREDICTION EVALUATED AGAINST CHAMBER DATA FOR
 REPRESENTATIVES OF MAJOR VOC CLASSES

 HIGHLY SIMPLIFIED REPRESENTATION OF LOW-NO,
 CHEMISTRY.

 HIGHLY SIMPLIFIED REPRESENTATION OF HIGHER
 OXYGENATED PRODUCTS.

 OVER > 100 TYPES OF VOCs REPRESENTED

  • A FEW SIMPLE COMPOUNDS (FORMALDEHYDE,
    ACETALDEHYDE, ETC.) REPRESENTED EXPLICITLY.

  • AROMATICS REACTIONS BASED ON PARAMETERIZED
    MECHANISMS ADJUSTED TO FIT CHAMBER DATA.

  • ALKANE MECHANISMS GENERATED BY A COMPUTER
    PROGRAM USING PUBLISHED ESTIMATION  METHODS

  • MECHANISMS FOR MANY TYPES OF COMPOUNDS
    HIGHLY APPROXIMATE AND UNTESTED.

USED TO DERIVE VARIOUS REACTIVITY SCALES FOR > 100
VOCs, INCLUDING THE WIDELY-USED MIR SCALE.
         SAPRC MECHANISM UPDATES

              SAPRC-93 MECHANISM

CHANGES TO PAN KINETICS CAUSED HIGHER ABSOLUTE
REACTIVITIES FOR ALMOST ALL VOCs.

ALKENE MECHANISMS CHANGED TO REFLECT NEW DATA
ON O3 + ALKENE REACTIONS

MECHANISMS FOR MTBE AND A FEW OTHER VOCs
MODIFIED BASED ON AVAILABLE DATA.

UPDATED ISOPRENE CHEMISTRY ADDED

NOW BEING USED IN SEVERAL RESEARCH-GRADE AIRSHED
MODELS


              SAPRC-97 MECHANISM

AROMATICS MECHANISMS MODIFIED TO FIT NEW
CHAMBER DATA AND TO ACCOUNT FOR ISOMERIC
DIFFERENCES.  MOST MORE REACTIVE.

MECHANISMS FOR A NUMBER OF VOCs UPDATED BASED
ON ONGOING REACTIVITY STUDIES

USED TO DERIVE REACTIVITY DATA AND UNCERTAINTY
SUMMARY RECENTLY PREPARED FOR THE CARB.

CURRENT WORKING MECHANISM AVAILABLE ON THE
INTERNET.

-------
                SAPRC MECHANISM UPDATES

           SAPRC-98 MECHANISM (UNDER DEVELOPMENT)

       BASE MECHANISM HAS BEEN COMPLETELY UPDATED.
       MANY SMALL CHANGES.

       THE IMPORTANT OH + N02 RATE CONSTANT FOUND TO
       BE HIGHLY UNCERTAIN BUT WAS NOT CHANGED.

       MORE DETAILED REPRESENTATION OF LOW NOX ORGANIC
       REACTIONS.  CHANGES IN PRODUCT DISTRIBUTION AT
       LOW NO. CAN NOW BE PREDICTED.

       ESTIMATED MECHANISMS FOR ALKANES, ALKENES, AND
to      MANY OXYGENATES ARE GENERATED AS FOLLOWS:
I
           COMPUTERIZED ESTIMATION PROCEDURE GENERATES
           EXPLICIT MECHANISMS WHICH ARE USED TO DERIVE
           PRODUCT YIELD PARAMETERS FOR THE MODEL.

           PROCEDURE USES ESTIMATED OR ASSIGNED RATE
           CONSTANTS FOR THE COMPETING REACTIONS.

       REPRESENTATION OF ORGANIC PRODUCTS BEING
       UPDATED USING PREDICTED PRODUCT DISTRIBUTIONS.

       STILL NECESSARY TO USE PARAMETERIZED MECHANISMS
       FOR AROMATICS ADJUSTED TO FIT CHAMBER DATA.

       MECHANISM  IS INCORPORATING  RESULTS OF RECENT
       STUDIES OF CONSUMER PRODUCT AND OTHER VOCs.
     STATUS OF MECHANISM DEVELOPMENT
       AND UNCERTAINTIES BY VOC CLASS

                    ALKANES

MECHANISMS FOR LOWER ALKANES WELL ESTABLISHED,
ESTIMATION METHODS USED FOR HIGHER ALKANES.

THE CB+ N-ALKANE MECHANISMS WHICH FIT CHAMBER
DATA HAVE UNREASONABLE ASSUMPTIONS.

MINERAL SPIRITS DATA SUGGEST REACTIVITIES FOR C10,
BRANCHED AND CYCLIC ALKANES ARE OVERESTIMATED.

                    ALKENES

SAPRC-98 EVALUATION SHOW MORE PROBLEMS WITH
ALKENE MECHANISMS THAN PREVIOUS SUSPECTED.

MODELS USING ACCEPTED OH YIELDS FOR O3 REACTIONS
GREATLY OVERPREDICT REACTIVITIES OF C4< 1-ALKENES.

UNCERTAIN 0(3P) REACTIONS AFFECT MECHANISM
ADJUSTMENTS FOR PROPENE, BUTENES, AND ISOPRENE.

EXTENT TO WHICH MECHANISMS MODIFICATIONS WILL
AFFECT ALKENE REACTIVITY IS UNCERTAIN.

-------
     STATUS OF MECHANISM DEVELOPMENT
       AND UNCERTAINTIES BY VOC CLASS

            AROMATICS HYDROCARBONS

 STILL NECESSARY TO USE PARAMETERIZED MECHANISMS.

 YIELDS AND PHOTOLYSIS RATES OF UNCHARACTERIZED
 PRODUCTS CANNOT BE UNAMBIGUOUSLY DETERMINED.

 NO MECHANISM CAN SATISFACTORILY FIT ALL CHAMBER
 DATA FOR BENZENE.

 NO OBVIOUS EXPLANATION FOR LOWER MECHANISTIC
 REACTIVITY FOR ETHYLBENZENE COMPARED TO TOLUENE.

 CURRENT MECHANISMS PROBABLY ARE INCONSISTENT
 WITH PRODUCT DATA FOR REACTIONS OF PHENOLS

 UNCERTAIN WHETHER PARAMETERIZED MECHANISMS
 EXTRAPOLATE CORRECTLY TO LOW NO, CONDITIONS.

        HIGHER OXYGENATES (HIGHER KETONES.
           ETHERS, ESTERS. GLYCOLS, ETC.)

EXPERIMENTAL REACTIVITY DATA ARE BECOMING
AVAILABLE, SIGNIFICANTLY REDUCING UNCERTAINTIES.

CURRENT ESTIMATION METHODS OFTEN PERFORM POORLY
IN SIMULATING CHAMBER DATA PRIOR TO ADJUSTMENTS.

ATTEMPTS TO IMPROVE PERFORMANCE OF ESTIMATION
METHODS ARE UNDERWAY.
     STATUS OF MECHANISM DEVELOPMENT
      AND UNCERTAINTIES BY VOC CLASS

            HALOGENATED COMPOUNDS

REACTIVITY DATA ONLY AVAILABLE FOR CHLOROPICRIN
(CCI3NO2), TRICHLOROETHYLENE, AND ALKYL BROMIDES.

NO REASONABLE MECHANISM SATISFACTORILY FITS ALL
CHAMBER DATA FOR TCE AND ALKYL BROMIDES.

STUDIES ARE NEEDED ON SIMPLER SYSTEMS.

         NITROGEN-CONTAINING COMPOUNDS

REACTIVITY DATA LIMITED TO N-METHYL PYRROLIDINONE
(NMP) AND SEVERAL AROMATIC ISOCYANATES.

NMP  IS UNUSUAL IN THAT NO3 REACTIONS CONTRIBUTE
TO ITS REACTIVITY.

THE AROMATIC ISOCYANATES STUDIED DO NOT PROMOTE
OZONE FORMATION. MECHANISM UNKNOWN.

                   SILOXANES

CHAMBER DATA SHOW THAT THESE ARE O3 INHIBITORS,
BUT MECHANISMS WHICH FIT CHAMBER  DATA ARE NOT
CONSISTENT WITH RESULTS OF  PRODUCT STUDIES.

-------
to
           MECHANISM UNCERTAINTY ANALYSIS
REACTIVITY-BASED CONTROL STRATEGIES WILL PROBABLY
NEED TO TAKE INTO ACCOUNT VARYING LEVELS OF
UNCERTAINTIES FOR DIFFERENT VOCs.

PROPOSALS TO USE ADJUSTMENT FACTORS OR UPPER
LIMITS FOR UNCERTAIN VOCs IN REACTIVITY-BASED VOC
CONTENT REGULATIONS.

        UNCERTAINTY ANALYSIS APPROACHES

FORMAL UNCERTAINTY ANALYSIS

  • ULTIMATELY THE BEST APPROACH, BUT HAS ITS OWN
    UNCERTAINTIES.

  • RELIES ON SUBJECTIVE UNCERTAINTIES FOR INPUT
    DATA. INCONSISTENCES AMONG  EVALUATORS.

  • DIFFICULT TO TREAT POSSIBILITIES OF  FOR "MISSING-
    REACTIONS OR INCORRECT PARAMETERIZATIONS.

  • NOT PRACTICAL TO DO FOR ALL TYPES OF VOCs IN
    USEFUL TIME FRAME.

  • NEAR-TERM UTILITY IS TO AID EVALUATION OF
    SUBJECTIVE OR CATEGORIZATION APPROACHES.

  • PROJECT UNDERWAY TO ANALYZE UNCERTAINTIES IN
    MECHANISMS ADJUSTED TO FIT CHAMBER DATA.
     UNCERTAINTY ANALYSIS APPROACHES
                  (CONTINUED)

CATEGORIZATION BASED ON EXPERT ASSESSMENT OF
QUALITY OF MECHANISM AND EXTENT TO WHICH
MECHANISM EVALUATED.

  • PRELIMINARY CATEGORIZATION HAS BEEN DONE FOR
    ALL VOCs IN THE SAPRC-97 MECHANISM.

  • NEED TO  BE UPDATED AND PEER-REVIEWED BEFORE
    INCORPORATED IN ANY REGULATIONS.

  • DOES NOT GIVE NUMERICAL UNCERTAINTIES.

UPPER AND LOWER LIMIT REACTIVITY ANALYSIS

  • CAN BE USED FOR QUANTIFYING UNCERTAINTIES FOR
    ALL VOCs.

  • RELATIVELY STRAIGHTFORWARD TO ESTIMATE UPPER
    LIMIT REACTIVITIES FOR A GIVEN SCALE.  PROPOSED
    APPROACH HAS BEEN DEVELOPED.

  • LOWER LIMIT REACTIVITIES FOR VOCs OF UNKNOWN
    MECHANISM IS ZERO, SINCE THEY MAY INHIBIT 03.

  • THIS METHOD GIVES HIGH UNCERTAINTY RANGES.
    MAY NOT BE ACCEPTABLE FOR REGULATORY USE.

  • UNCERTAINTY RANGES FOR SOME VOC CLASSES CAN
    BE NARROWED BY MECHANISTIC CONSIDERATIONS.

-------
to
oo
            CHEMICAL MECHANISM UNCERTAINTIES
 BASE MECHANISM (INORGANIC, COMMON PRODUCT
 REACTIONS) HAS NON-NEGLIGIBLE UNCERTAINTIES.  '

   •  REACTIVITIES VOCs WITH LARGE INDIRECT
     REACTIVITIES (E.G., INITIATORS/INHIBITORS)
     SENSITIVE TO BASE MECHANISM CHANGES.

   •  REACTIVITY UNCERTAINTIES FOR WELL-STUDIED
     VOCs ESTIMATED TO BE -30%

 UNCERTAINTIES IN MECHANISMS FOR INDIVIDUAL VOCs
 CAN  BE MUCH GREATER IF VOC INADEQUATELY STUDIED.

   •  ONGOING RESEARCH IS REDUCING NUMBER OF VOC
     CLASSES WITH INADEQUATE DATA.

   •  UNSTUDIED VOCs MORE OF A CONCERN FOR
     STATIONARY SOURCES THAN MOBILE SOURCES.

REACTIVITY CHANGES DUE TO UPDATING MECHANISM
GIVE  AN INDICATION OF UNCERTAINTIES

  • REFLECTS RESULTS OF ONGOING RESEARCH.

  • CHANGES FOR WELL-STUDIED CONSISTENT WITH
    -30% MINIMUM UNCERTAINTY ESTIMATE.
     TYPES OF ENVIRONMENTAL CHAMBER
        EXPERIMENTS CURRENTLY USED
       TO TEST CHEMICAL MECHANISMS

SINGLE VOC-NO.-AIR RUNS:

  • MOST STRAIGHTFORWARD TEST OF A VOC's
    MECHANISM, THOUGH ONLY USEFUL FOR VOCs WITH
    RADICAL SOURCES.

  • NOT A "REALISTIC" ENVIRONMENT. CORRELATES
    POORLY WITH REACTIVITY.

COMPLEX MIXTURE-NO.-AIR RUNS:

  • TESTS MECHANISMS' ABILITY TO SIMULATE O3
    FORMATION UNDER REALISTIC CONDITIONS

  • NOT USEFUL FOR MECHANISM DEVELOPMENT

REACTIVITY EXPERIMENTS (MIXTURE-NO.-AIR COMBINED
WITH MIXTURE-NOX-AIR RUNS WITH TEST VOC ADDED):

  • CAN TEST MECHANISMS OF SINGLE VOCs UNDER
    REALISTIC CONDITIONS

  • BEST TEST OF MECHANISM'S ABILITY TO PREDICT
    INCREMENTAL REACTIVITY

  • NOT SAME AS ATMOSPHERIC REACTIVITY.

-------
MS
  DATA NEEDS FOR MECHANISM EVALUATION
                  (NEAR TERM)

MECHANISM EVALUATION DATA NEEDED FOR CLASSES OF
COMPOUNDS NOT PREVIOUSLY STUDIED.

  • GOOD PROGRESS BEING MADE FOR SOLVENT SPECIES
    SUCH AS ESTERS, GLYCOLS, ETC.

  • BUT EPA EXEMPTION POLICY HAS CAUSED FOCUS OF
    RESEARCH TO BE ON LOW-REACTIVITY COMPOUNDS.

  • REACTIVITY-BASED CONTROLS WILL ENCOURAGE
    RESEARCH ON COMPOUNDS OF ALL REACTIVITIES.

BETTER METHODS NEEDED TO EVALUATE REACTIVITY

  • HIGH COST OF OBTAINING REACTIVITY DATA LIMITS
    ACCEPTABILITY OF REACTIVITY-BASED CONTROLS.

  • CURRENTLY NO WAY TO ASSESS REACTIVITIES OF
    VERY LOW VOLATILITY COMPOUNDS.

  • ONLY A FEW LABORATORIES ARE PRESENTLY
    CAPABLE OF GENERATING REACTIVITY DATA.
                                                                     DEVELOPMENT OF NEW REACTIVITY
                                                                          MEASUREMENT METHODS
PROJECT UNDERWAY TO DEVELOP NEW REACTIVITY
MEASUREMENT METHODS.

INITIAL FOCUS IS ON USE OF HONO/VOC STIRRED FLOW
SYSTEM. CALCULATIONS INDICATE THIS CAN GIVE
USEFUL DATA ON FACTORS AFFECTING REACTIVITY.

  • LOW TO MODERATE VOC TO HONO RATIOS: DATA
    SENSITIVE TO kOH AND NO TO NO2 CONVERSIONS.

  • HIGH VOC TO HONO: ALSO SENSITIVE TO RADICAL
    TERMINATION EFFECTS.

POTENTIALLY LOWER COST WAY TO OBTAIN DATA FOR
MECHANISM EVALUATION, REACTIVITY SCREENING,
DERIVING EMPIRICAL REACTIVITY-RELATED PARAMETERS.

FLOW SYSTEM POTENTIALLY ADAPTABLE TO VERY LOW
VOLATILITY COMPOUNDS

CLEAN HONO GENERATION SYSTEM HAS BEEN
CONSTRUCTED. FLOW SYSTEM BEING  CONSTRUCTED FOR
INITIAL TESTING WITH PROPANE.

-------
N)

O
   DATA NEEDS FOR MECHANISM EVALUATION
                  (LONGER TERM)

 MAJOR INVESTMENT IN CHAMBER FACILITIES NEEDED TCI
 IMPROVE EVALUATION OF EXISTING MECHANISMS

   • MECHANISMS INADEQUATELY EVALUATED FOR LOW
    NO, (REGIONAL OR NEAR-ATTAINMENT) CONDITIONS.

   • CHAMBERS CURRENTLY USED FOR MECHANISM
    EVALUATION UNSUITABLE FOR LOW NO. STUDIES.

   • ANALYTICAL CAPABILITIES AT OPERATING CHAMBER
    FACILITIES NOT ADEQUATE FOR FULL MECHANISM
    EVALUATION OR DETERMINING ALL VOC IMPACTS.

   • TEMPERATURE EFFECTS UNCERTAIN. CURRENT
    CHAMBERS INADEQUATE TO STUDY THIS.

   • LARGE TEMPERATURE-CONTROLLED INDOOR
    CHAMBER NEEDED TO STUDY PARTICULATE
    FORMATION UNDER CONTROLLED CONDITIONS.

STUDIES FOCUSED ON SPECIFIC COMPOUNDS CANNOT BE
USED TO FUND THE NEEDED FACILITY IMPROVEMENTS.
        AIRSHED MODEL UNCERTAINTIES

UNCERTAINTIES IN REPRESENTATION OF A GIVEN
SCENARIO. (EMISSION UNCERTAINTIES, ETC.)

  • LESS OF A PROBLEM FOR GENERAL SCALES
    REPRESENTING A RANGE OF CONDITIONS

USE OF SIMPLIFIED PHYSICAL SCENARIOS (EKMA MODELS)
FOR COMPUTATIONAL TRACTABILITY

  • LESS OF A PROBLEM FOR GENERAL SCALES
    REPRESENTING A RANGE OF CONDITIONS

  • STUDIES SUGGEST NOT A MAJOR PROBLEM WHEN
    PREDICTING REACTIVITIES RELATIVE TO O3 EXPOSURE

UNCERTAINTIES IN DISTRIBUTION OF CONDITIONS
RELEVANT TO ASSESSING OZONE CONTROL

  • NOT ADEQUATELY STUDIED. EPA SCENARIOS USED
    BY CARTER (1994) WERE NOT DEVELOPED FOR
    REACTIVITY ASSESSMENT.

  • MAJOR PROBLEM FOR DEVELOPING GENERAL SCALES
    REPRESENTING A RANGE OF CONDITIONS.

LACK OF ADEQUATE STUDIES OF INCREMENTAL
REACTIVITIES IN REGIONAL SCALE MODELS

  • IMPORTANT WHEN ASSESSING WHAT IS "NEGLIGIBLE-
    REACTIVITY.

-------
 APPROACHES FOR DEALING WITH DEPENDENCE
    OF REACTIVITY ON AIRSHED CONDITIONS
     AND OZONE QUANTIFICATION METHOD
USE A "REPRESENTATIVE" OR "WORST CASE" EPISODE.

  • MAY NOT BE OPTIMUM FOR ALL CONDITIONS.

BASE THE SCALE ON CONDITIONS WHERE VOCs HAVE
MAXIMUM INCREMENTAL REACTIVITIES (MIR SCALE).

  • REFLECTS CONDITIONS MOST SENSITIVE TO VOCs
    AND CORRELATES WITH EFFECTS ON 03 EXPOSURE.

  • BUT DOES NOT REPRESENT CONDITIONS WHERE
    HIGHEST OZONE CONCENTRATIONS ARE FORMED.

USE MULTIPLE SCALES REPRESENTING THE RANGE OF
APPLICABLE CONDITIONS.

  • ALLOWS ASSESSMENT OF EFFECTS OF VARIABILITY
    BUT NOT USEFUL WHEN SINGLE SCALE REQUIRED.

USE A SCALE OPTIMIZED FOR A RANGE OF CONDITIONS.

  • REQUIRES IMPROVED ASSESSMENT OF RANGE OF
    CONDITIONS RELEVANT TO OZONE FORMATION

  • REQUIRES AN OBJECTIVE DEFINITION OF "OPTIMUM"

  • HAS NOT RECEIVED ADEQUATE ATTENTION TO DATE.
 APPROACHES FOR DEALING WITH DEPENDENCE
         OF REACTIVITY ON CONDITIONS
                  (CONTINUED)

CARB VEHICLE REGULATIONS USE THE MIR SCALE, BASED
ON PEAK 03 IN EKMA SCENARIOS WITH NO, ADJUSTED TO
GIVE MAXIMUM SENSITIVITY OF 03 TO VOCs.

VOC EXEMPTION PROPOSALS HAVE USED DISTRIBUTIONS
OF INTEGRATED AND PEAK 03 REACTIVITIES  IN THE 1-DAY
EKMA SCENARIOS, AND OTHER CONSIDERATIONS.

IF THESE METHODS CHANGE, IT MAY CHANGE REACTIVITY
SCALES MORE THAN UPDATES IN MECHANISM OR MODELS

POLICY ISSUES

  • HOW SHOULD OZONE IMPACTS BE QUANTIFIED?

  • WHAT CRITERIA SHOULD BE USED TO DETERMINE
    WHAT IS AN OPTIMUM  REACTIVITY SCALE?

  • WHAT ARE THE MOST APPROPRIATE ENVIRONMENTAL
    CONDITIONS TO USE WHEN ASSESSING  REACTIVITY?

SCIENTIFIC CHALLENGE IS TO DERIVE SCENARIOS, MODELS
AND PROTOCOLS BEST ADDRESSING POLICY  PRIORITIES.

THE MIR SCALE HAS BECOME THE DEFAULT.  IF NOTHING
IS DONE, IT WILL CONTINUE  TO BE USED.

-------
                                  INFORMATION AVAILABLE ON THE INTERNET
                                REACTIVITY TABULATIONS AND UNCERTAINTY
                                CLASSIFICATIONS:

                                    http://cert.ucr.edu/ ~ carter/rcttab.htm

                                REPORTS ON RECENT REACTIVITY AND CHAMBER STUDIES
                                AND SAPRC-97 MECHANISM DEVELOPMENT:

                                    http://cert.ucr.edu/ ~ carter/bycarter.htm
K>                              SAPRC-97 MECHANISM:
t—»
to
                                    http://cert.ucr.edu/~carter/saprc97.htm

                               CHAMBER DATA BASE FOR MECHANISM EVALUATION
                               (THROUGH 1995):

                                    ftp://cert.ucr.edu/pub/carter/chdata/

                               SOFTWARE FOR REACTIVITY CALCULATION AND
                               MECHANISM EVALUATION

                                    ftp://cert.ucr.edu/pub/carter/model/

-------
      VOC Reactivity Quantification
       Methods, Uncertainties and
                 Variabilities
       Jim Wilkinson, YJ Yang, M. Kahn, Lewis Qi, Ted
                    Russell and others
         School of Civil and Environmental Engineering
              Georgia Institute of Technology
                trussell@pollution.ce.gatech.edu
Georgia Institute of Technology
     Issues/Outline

     * What are we trying to do and why?
     * What have we done
     * Available/future methods
     * Uncertainties
     * Variabilities
Georgia Institute of Technology
                      2-13

-------
     What we are trying to do

     * Quantify reactivity of VOCs
     * Understand and quantify uncertainties
     * Understand variabilities
     * Address related issues
Georgia Institute of Technology
    V
    * Save money
      - Provide incentives to save even more
    * Protect human health
      - Relevant reactivity measures
Georgia Institute of Technology
                       2-14

-------
      Approach(es)
        Air quality modeling
        -  Box modeling
        -  Three-dimensional
        Reactivity quantification
        -  Brute force
        -  Direct sensitivity analysis
            * DDM-3D
        Uncertainty assessment
        -  Monte Carlo and other
        Variability analysis
        -  Multiple domains
        -  Multiple periods
        -  Multiple endpoints
              50-200
      Air Quality
        Model
Atmospheric Diffusion Equation

             Discretize

       ~^ + L(x,Oc-f(x.t)
            I
            ^ Operator splitting
c(t-v2Al) -L,;At)L.. (At! Ls/;2.A'-i I.yi All Lt(Ai
Georgia fnsttiute of Technology
      AQM Reactivity  Quantification
      Methods
       * Brute force
          - Run base case
          - Perturb inventory
              » Add dE, of species in emissions
              * Find d[O3]
              * Reactivity: 1^ = d[03]/dEj
              » Problems
                 - Tedious
                 - Numerical errors
       * Direct sensitivity analysis
          - Find d[O3]/dEi directly using DDM
          - Multiple reactivities simultaneously
          - Not as prone to numerical errors
Georgia InsiUule of Technology
                                2-15

-------
      Brjrte Force
                                    O^t.x.y.z)
                                    NO(t,x,y,z)
                                    VOCjt,x,y,z)
                                    Oj(t,x.y.z)
                                    NO'(t,x,y,z)
                                    N02(l,x,y,z)
Georgia Institute of Technology
                 Sensitivity (DDM-3D)
                                               03(t,x,y,z)
                                               N0(t,x,y,z)
                                            |f N02(t,x,y,z)
                                            -'
Georgia Institute of Technology
                              2-16

-------
      Sadies
	1
   * California LEV/Clean Fuels Assessment
      - Assess MIR reactivity weighting of exhaust emissions
   * Auto/Oil & NREL reactivity quantification and uncertainty
     assessment
      - Compare box and airshed model reactivities
      - 3-D modeling of reactivity and 1&3 D modeling of uncertainties
   * National Aerosol Association relative reactivity study
      - Economic assessment of using reactivity in control strategies
   * National Science Foundation
      - Developed and applied DDM-3D, multi-domain analyses-
      - 3D Monte Carlo reactivity uncertainty assessment
   <• Others
      - Solvent studies, variability analyses, regional domains
Georgia Institute of Technology
      Arjshed Vs. Box Model Reactivities
     ^p|s$$:"'
     * Compared alternative fuel MIRs, box
        model and L.A.-based airshed modeling

Results usually
similar, but aromatics,
in particular, can differ.

- , • . wn .
1


^^ ..^
J
m i


QL A. Peak
• Box

8 t 8 § I .8
5 ° £ a 3
1 ! ! s
Compound
Georgia Institute of Technology ^~
                               2-17

-------
    Mjj&ric Differences
     * Compared peak ozone reactivity Vs.

       exposure-based reactivities
                       Compound
Georgia Institute of Technology
                                           * Slightly negative
     Dijnain Differences



     * Compared Peak 1-hr reactivities calculated

       for L.A., Swiss Plateau, Mexico City
            0.01
Georgia InsliluU of Technology
                     1   I   1   I   I   I
                     PS   S?   £   >-   f,
I  a  s
•8  o-  <
                         Compounds
                                           *Slightly negative
                         2-18

-------
               lities : Box Model Analysis
     * Compared net reactivity with relative exhaust
       reactivity (RAF, in each domain)
        - Little variability in RAF, lots in net reactivity
             Absolute Reactivity
Relative Reactivity
       f § "
       o E J-°
       03 01 X
       IE
Gtorgia Institute of Technology
              MS5   LPG  Phiist 2
                CNO  E85  RPA
              1.0


              LL
              CC
                                MS5 CNG LPC E85 Pluist :
                           Fl'EL
     Uncertainties
       ;;"
     •:» Conducted uncertainty analysis using 3-D
       airshed (L.A. case)
     * Perturbed rate constants and product splits
     * Re-normalized reactivities
     * Found about a 15-30% uncertainty
        - Species dependent
Georgia Institute of Technology
                         2-19

-------
•a
o
u
OS
35-

 3-

as--

 2

1.5 ••
              Figure 2c. Btect of 2o Rate Constant Pwtuibatlont on Normalized
              Reactivities Bawd on Peak Ozone          	
o  NO2»OH
x  N02 Pholdyiit
A  Aldehyde Photdysls
x  Peroxyacylt + NO
x  PeroxyacyU * NO2
»  O3» NO
-  PAN, PPN Decanpoilllvi
      3D Monte Carlo Reactivity
     ^Uncertainty Assessment

      * 3D Monte Carlo assessment of
        uncertainties
         - Los Angeles basin
         - Chemical mechanism and emissions
           uncertainties
         - Direct sensitivity
         - Found reactivity uncertainties
            * Species and metric dependent
            * Spatial variations in reactivities and uncertainties
 Georgia Institute of Technology
                           2-20

-------
  \  Methods
     \
     * Urban/Regional air quality models
       - Advanced chemistry (SAPRC97+)
     * Direct sensitivity analysis
       - Faster, more accurate
     * Uncertainty analysis approaches
       - Guided Monte Carlo and others
Georgia Institute of Technology
     Direct Sensitivity  Vs. Brute
     Force

     * Direct sensitivity provides a more rapid,
       accurate approach
             DDM Reactivities Vs. Brute Force
Georgia Institute of Technology
                   Fuel .-Species
                        2-21

-------
    Economic Assessment (Back to  Why)
   ^

  * Compared costs of reactivity and mass-based
    control strategies
    - Mixed integer, non-linear programming of control
      cost effectiveness in Los Angeles
    - Understates potential savings (reformulations)
            I.i
            o
            O
                                Reactivity-based
ings
Georgia Institute of Technology     % flf "
                            02006
  ;  Midway Summary: Use of Reactivity
     ~--<

     * Scientifically compelling
        - Significant differences in ozone impacts
        - Still some issues to resolve
     * Economically compelling
        - Significant economic benefits
        - More to be found if incentives are provided
Georgia Institute of Technology
                        2-22

-------
     Gaps  in our understanding

    * Regional reactivity assessments
       - Little work on eastern U.S., Texas, etc.
       - Assess variabilities
    * Episodic reactivity Vs. longer term impact
    * More comprehensive uncertainty analysis
Georgia Institute of Technology
     Looming Issues

    * Metric(s) of importance
      - Peak 8-hr: Standard
      - Human exposure: Health
      - Regional exposure: welfare
         * Most likely of less relevance
            - NOx limitations
Georgia Institute of Technology
                         2-23

-------
     Regional Reactivity Assessment
         Texas-Mexico Border
       Sensitivity of ozone to butane
         (preliminary study underway)
Eastern U.S.
(To be done)
Georgia Institute of Technology
     Related Issues
     * Secondary PM formation
        - Can we develop a PM-formation potential
          scale
        - Will it be similar to ozone formation potential
          (reactivity) scale(s)
           * No
Georgia Institute of Technology
                        2-24

-------
  ^  Exemptions
   \
                                           Bad       Good
  *  Mistakes have been made
  *  Traffic can go both ways
     -  Highly reactive ==> less reactive exempt          Reactivity
     -  Less reactive => marginally reactive exempt
  •:•  Does not account for change in mass emissions
     -  Solvent/propellant changes can impact mass emissions
        •» Twice as much of something half as reactive is not a good
         deal
  *  Reactivity scale scientifically more sound
  •*  Less policy inertia
     -  Do not have to "unexempt" a compound
        * Regulatory uncertainty can be expensive


Georgia Institute of Technology
      Research Needs
     ff
      * Regional reactivity assessments
      * Further sensitivity/uncertainty analysis
         - Regional scale
         - Updated chemistry (e.g., SAPRC98?)
            * Further species mechanism development
      * Assess dependence on metric
         - Peak Vs. exposure
         - Episodic Vs. long term
      * PM impact scale
Georgia Institute of Technology
                           2-25

-------
 \  Summary
     V.
* Investigated reactivity quantification issues:
   - Fuels, Solvents, Propellants
   - Methods
      * Air quality models and direct sensitivity analysis
   - Uncertainties
   - Variabilities
* Uncertainties reasonably small
   	30% by species (depending on metric), less by source
* Variabilities decrease using relative reactivities
* Scientifically and economically compelling
* Brightline approach is flawed
Georgia Institute of Technology
     Acknowledgements
    \
    * Jana Milford, Michelle Bergin, Bart Croes,
      Bill Carter, Basil Dimitriades and Lauri
      McNair
    * California Air Resources Board, National
      Science Foundation, National Aerosol
      Association, Occidental Chemical
      Company, Coordinating Research Council,
      Georgia Power, CONACyT, NREL
Georgia Institute of Technology
                       2-26

-------
               Quantification of Uncertainties in Reactivity Estimates
                          for Volatile Organic Compounds

                                     Presented by
                                    Jana B.Milford

                                      Co-authors
                            Michelle Bergin and Lihua Wang
                          Department of Mechanical Engineering
                          University of Colorado, Boulder 80309
Abstract
The research to be presented quantifies uncertainties in air quality model-based estimates of
absolute and relative  reactivities  for  volatile organic compounds  (VOCs).   Monte Carlo
techniques have been used to propagate estimates of uncertainty in model inputs and parameters
                   V
to generate confidence intervals for estimates of VOC reactivity.  In this presentation, previously
published  estimates of reactivity uncertainties due  to chemical parameters alone (Yang et al.3
1995; 1996a;b; Bergin ct al., 1998) will be compared to new estimates that also account for
uncertainties in emissions and meteorological conditions for a specific time and location, namely
August 27-28, 1987, in California's South Coast Air Basin.  For selected aromatic compounds,
new estimates of uncertainties attributable to smog chamber-derived reaction parameters will
also be presented. The results suggest priorities  for future  research  to  reduce  modeling
uncertainties, but also indicate that the effect of existing uncertainties can  be minimized by
formulating reactivity policies in terms of relative reactivity estimates, as opposed to absolute
reactivities. Implications of modeling uncertainties for a prospective photochemical reactivity
policy, and recommendations for additional research, will be discussed.
                                      2-27

-------
    COMPARISON  OF  PHOTOCHEMICAL  OZONE  CREATION POTENTIALS
   CALCULATED USING A MASTER CHEMICAL MECHANISM WITH THE MIR
      REACTIVITY VALUES  FOR UP TO  120  ORGANIC COMPOUNDS


                         Dick Derwent
                Atmospheric Processes Research
                     Meteorological Office
                           Bracknell
                           Berkshire
                        United Kingdom

                           ABSTRACT


Photochemical  ozone  creation  potentials  POCPs for  120  organic
compounds have been  calculated with a  photochemical trajectory
model for  realistic European conditions.  The model employs  a
Master Chemcial Mechanism  (Jenkin  et al.  1997)  containing 2410
chemical-species and over 7100 chemical reactions.  POCPs provide
an estimate of the likely contribution to European regional scale
ozone formation over a five day timescale from unit mass emission
of each organic  compound  relative to ethylene.  Photochemical PAN
creation potentials  have also been estimated. The  POCP values
have  been  carefully  compared  with  the corresponding  MIR
incremental reactivities of Carter  et  al.  (1995),  developed for
the single  photochemical day situation appropriate  to  the Los
Angeles  airshed.  For the  vast majority  of organic compounds,
there is a  clbse  functional relationship between POCP  and MIR
values. Some differences  are apparent between the single day and
multi-day indices  and they provide important  insights  into the
quantification of  reactivity. Organic  compounds which generate
specific highly unreactive  organic compounds in their degradation
schemes  tend to show lower POCPs relative to  their  MIR values.
Such unreactive compounds  include:  acetone, alkyl nitrates and
formate  esters.  Furthermore,  aldehydes,  and  in   particular
formaldehyde,  show lower POCPs in multi-day situations where OH-
degradation predominates  over photolysis compared with single day
or  smog chamber situations.  Work  is   in  hand with  the Master
Chemical  Mechanism  to   improve   the  representation  of  the
degradation schemes for aromatic hydrocarbons and incorporate the
recent mechanistic work by Jeffries et  al.  (1997) to improve the
reliability of  the POCP  estimates  for this important  group of
organic  compounds.
                             2-28

-------
to
tb
                  MODELLING OZONE FORMATION
                    FOR POLICY FORMULATION
Models are required to

* quantify transbbundary transport

* define what is needed to meet environmental criteria

* define the balance between emission controls in the UK
and beyond

* assess the rotes of VOC and NOx controls

* examine the different VOCs and VOC emitting sectors
                                                                                   MO PHOTOCHEMICAL TRAJKTORY MODEL

-------
                                                            EMEP
                                                            1991
                                                          UKNAEI
                                                           1W1
                                                      10km x10km
FIGURE 2. A diacruamibc representation of the nesting between the emissions
Ifnds employed in the photochemical trajectory model
      ORGANIC COMPOUNDS DEGRADED
         MASTER CHEMICAL MECHANISM
ALKANES
ALKENES
DIALKENES
ALKYNES
AROMATICS
ALDEHYDES
KETONES
ALCOHOLS
ETHERS
ESTERS
ORGANIC ACIDS
CHLOROCARBONS

total
22
15
 2
 1
18
 6
10
17
10
 8
 3
 8
C1-C12
C2-C6
C4-C5
C2
C6-C11
C1-C5
C3-C6
C1-C6
C2-C7
C2-C6
C1-C3
C1-C2
120  organic compourKJs
                     2-30

-------
               DEVELOPMENT OF MASTER CHEMICAL
                           MECHANISM
to
              7000 chemical reactions
              2500 chemical species
            120 emitted organic species

Master Chemical Mechanism development uses:

* ACCORD for EXCEL as a chemical spreadsheet
* FACSIMILE as a variable order Gear's method

For example, the butane scheme contains 510 chemical
reactions and 186 chemical species (of which 20 are
primary emitted species)

Following processes initiate ozone production from the
organic compounds:

• OH radical attack
* ozone reactions
• N03 radical attack
* photolysis
* Q atom attack

Available on WWW web page:





TION


* 1
PHOTOLYSIS
Gtrtonyli
ROOM RC(O)OOH
•ndRONO!



OH rtaclion
MVOCm)
oiyg«nil*0 produdi

+
•«,«•.
r^,rr,
1

OXY(BO)
rSr
L



X


PEROXY (ROi)
nu wjj r«jj
HC>2 Rt),


i


DO r»»ct*on
pnxJoct*


EicMOCRlEGEE
(RRtX)0*)
\ SUMlUIIW
KwxxiipoMie



C*itnny«
RC(O)OOH R
m



PANl.
XDH ROH
C(O)OH CO


'


(RR-COO)
SOj NO NOj


CO,

                                                                     FIGURE 1. Summary of chemistry of organic species considered in the
                                                                     mechanism construction protocol (JenMn et al., 1997).
         WWWhttp://chem.leeds.ac.uk:80/Atmospheric/MCM

-------
              DESCRIPTION OF CHAMBER-INDEPENDENT
           ATMOSPHERIC CHEMISTRY MECHANISMS FROM
                      SMOG CHAMBER DATA
U)
 SMOG CHAMBER DATABASES

 1.  Dual outdoor smog chamber data (University of North
 Carolina)

 2. Indoor teflon chamber (SAPRC)

 3. Indoor evacuable chamber (SAPRC)

 4. Dual outdoor chamber (CSIRO)


 INPUT DATA REQUIRED

a. concentration measurements

b. chamber-dependent photolysis rates

c. smog chamber auxiliary mechanism

d. evaluated mechanistic data
OUPTUT ATMOSPHERIC CHEMISTRY MECHANISMS

i  Carbon Bond Mechanisms  (CBM-IV)

ii. CAL, SAPRC-90

iii. Generic Reaction Set

-------
140-1
120-
100-
                   COMPARISON OF THE MCM WITH CBM-IV
                                 MECHANISM
              It is concluded that the differences between CBM-IV and
              the MCM for the estimation of daytime photochemical
              ozone production are small, within +-6 ppb in about 100
              ppb.
              There is a significant difference in the treatment of tow-
              NOx nighttime chemistry wtthin the MCM.
              This dose correspondence may not follow for all the
              secondary products and free radicate. However, this is
              the reason why the MCM has been developed.
                   Comparison between the MCM and the smog chamber database
                                  Travel time, hours
             FIGURE 2. Comparison between the explicit chemkal mechanisms: MCM and
             DJ&S and the smog chamber mechanisms: CBM-IV and CAL, and the ozone
             concentrations produced along the five day trajectory.
                                        2-33

-------
      Rtductlort In Oiont for 35% reductloi In NO« and HC •millions plotted coalnit OVNOx
                 Hydrocarbons »nd Irantporl of ozone and PAN
                                                                                        1669
Fig. 2(b). The itme development of ozone in the F.R.G.-Rcpublic of Ireland trajectory case.
                                       2-34

-------
1 AHU. 1 Itx:)1 and I'PCI' value* for I20 orpiimc orxniKuniV Uolcrmini-U wiih ihr MCM nnd tho UK Photochemical Trnj<«clory Mixlol

Organic compound

AlxanM

methane
ethane
propane
n-buLane
i-bulane
n-pentane
i-penlane
neopenlane
n-hexane
2-melhylpenlane
3-methylpentane
2 2-djmethylbutane
2,3-djmethylbuume
n-heptane
2-methylhexane
3-methylhexane
n-octane
n-nonane
n-decane
n-undecane
n-dodecane







TOC I1


06
123
176
352
307
395
405
17.3
482
•120
479
24 1
54 1
494
41 1
36.4
463
41 4
384
38.4
367







PPCF


09
173
137
31 4
117
297
427
67
448
294
666
163
634
61.9
31.9
40.1
42.9
349
2S.S
29 1
372






Organic compound

DiaLXonw

1.3-buladiene
isoprene

Alkvnes

acetylene

Aromalica

benrene
toluene
oxylene
m-xylene
p-xylene
ethyloenzene
propylbenrene
i-propylbenzene
1,2,3-lrimethyIbeniene
1.2,4-tnmethylbeniene
1.3,6-lnmethylb«niene
o-ethyltoluene
m-ethyltoluene
p-ethyltoluene
3, 6-dun ethy lethy Iben Mne
3,6-dielhylloKiene



POCP


8!> 1
1002



86



21.8
63.7
106.3
110.8
101 0
73.0
63.6
50.0
126.7
127.8
138 1
898
101.9
90.6
132.0
129.5



PPCP


20 H
774



22



4.5
478
960
946
922
44.9
34.8
162
119.1
1185
122.4
71.8
80.8
73.2
108.9
99.8


Organic compound

Ketonai

acetone
methylethylketone
methyl-i-butylketone
methylprop;lk«ton«
dielhyUt«ton«
mslhyl-i-propylketone
h«xan-2
-------
     IDENTIFICATION OF THE IMPORTANT PARAMETERS
      WHICH DETERMINE OZONE FORMING POTENTIAL
to
U)
ov
            THESE FOUR FACTORS ARE:


                  MASS EMISSION RATE

                  MOLECULAR WEIGHT

                  OH RATE COEFFICIENT

                  CHEMICAL STRUCTURE
   HOW DOES CHEMICAL STRUCTURE
INFLUENCE REACTIVITY VALUES SUCH AS
               POCPs
                                                        Mainly through the formation of intermediate
                                                        compounds which degrade much more slovdy
                                                        than the parent compounds.
Examples of unreactive intermediates include


* carbon monoxide

* alkyl nitrates

* acetone

* formate esters

-------
       FIGURE 4. The POCPa for alkanes, alkenes and aromatic compounds with NOx

       emissions halved, standard and doubled.
NJ
      ii
      d>
      C
      CL
      O
      O
      0_
           180-1
           160-
           140-
           120-
100-
 80-
            60-
            40-
            20-

                                                        LOW REACTIVITY ORGANIC COMPOUNDS
                                                                   ON A BY MASS BASIS
2-methylbutan-2-ol      14.2
styrene               14.2
i-propanol             14.0
methanol             13.1
ethane                12.3
t-butanol              12.3
acetic acid             9.7
acetone                9.4
acetylene              8.5
methylene dichloride    6.8
t-butyl acetate          6.5
methyl acetate         4.6
methyl formate         3.3
formic acid             3.2
tetrachloroethylene     2.9
chloroform             2.3
methylchloroform        0.9
methane               0.6
methyl chloride         0.5
benzaldehyde          -9.2
                       	1	1	1	1	1	T
                        Halved       Standard      Doubled
                         NOx        NOx         NOX

-------
  "T
                 COMPARISON OF POCP AND MIR
                       REACTIVITY VALUES
            POCPs address regional scale ozone
            formation over the 1-5 day timescale
            appropriate to Europe.

            MIR values address urban scale ozone
            formation.

            For the majority of organic compounds the
            scales are  in excellent agreement.
            There are some differences:

            * role of formaldehyde

            * 1,3-butadiene

            * butylene

            * ethyl t-butyl ether

           FIGURED. Comparison between the MIR and POCP reactivity scales for up to 70
           organic compounds.
                          X fomultfehyd*
I *
                                               O   A
                                                                    Xolluft
                ••
                                 2-38

-------
              WHAT NEXT WITH POCPs
     Expansion of Master Chemical Mechanism to
     include latest aromatic compound degradation
     pathway studies of Jeffries and co-workers and
     Barnes and co-workers.

     Include an additional 20 organic compounds
     mainly CIQ aromatic compounds making 140
     in all.

     Expanding the range of oxygenated organic
     compounds.

     Deriving estimation procedures for POCPs.

     Derive equivalent of POCPs for large industrial
     emission sources of organic compounds for
     controlling downwind ozone formation.
         FIGURE 5. Comparison of ozone-formation indices for the reactive alknnes,
           \
         alkenes and dienes.
300
  •°  .2 *
  t  5
  ID

  T!>
  to
  CJ
JT
>.

«


oi
$jS£SIS3lS||3SI1lfII
"11 ^-^i^-I^S^^l^.-
                                  >.
                   >,
                   .c
                   Q)
CM
c £" c
I I  £
                                           
                                           c
                                           0)
                                           c
                                           0)
                                           a.
                                                       a> CD
                                                       c c
                                                       a> 
                 c
                 0)
                 Q.
                 O
PJ
VI
C
                           Organic compound
                               2-39

-------
      UTILITY OF REACTIVITY VALUES
            INCLUDING POCPs
 In the exact limit, no two ozone footprints from
 different organic compounds can be
 superimposed.

 Single number reactivity values must involve
 some form of approximation and assumption.

 A reactivity value is not a geophysical quantity
 such as a rate coefficient though it may
 depend  on one or many.

 Reactivity values are user-oriented constructs
 whose calculation depend on understanding of
 a few environmental processes but also on
 some policy-oriented choices, such as the
 spatial scale of interest.

 Reactivity values are not subject to observation
and testing but are best judged by the insights
they give into the role of each organic
compound in forming ozone in real situations
and their usefulness to policy-makers.
  TOP TEN HYDROCARBONS ACCORDING
      TO INVENTORIES AND POCPs
1
2
3
4
5
6
7
8
9
10
       toluene
       n-butane
       ethyiene
       m-xylene
       p-xylene
       o-xylene
       i-pentane
       ethyl alcohol
       propyteoe
Together these account for 49% of the ozone
forming potential of UK emissions

-------
                                   Ozone reduction In ppb p«r thousand tonn«s p«r year abated
010
                                                                                                 t
                                                     VCX: emitting sector

-------
                                         Reactivity: 05/12/98
       EPA's Models-3 Framework and the
Community Multi-scale Air Quality Model (CMAQ)
                  Robin L. Dennis

           Atmospheric Modeling Division
        National Exposure Research Laboratory
        U.S. Environmental Protection Agency
             Research Triangle Park, NC
         Photochemical Reactivity Workshop
                   Durham, NC
                  May 12-14, 1998

-------
                                                 RMetfvtty OV12/VC
               EPA/On-Site CMAQ SCIENCE TEAM
    Science Team Leader: Daewon Byun
                                      Motivation
K)
    MM5/MCIP
        Al Bourgeois
        Hao Jin
        Jon Pleim
        Tanya Spero
        Ruen Tang
    MEPPS
        Bill Benjey
        Chris Maxwell
        Nick Moghari
        Tom Pierce
    Project Management
        Jason Ching
        Robin Dennis
        Joan Novak
        Ken Schere
CMAQ
    Frank Binkowski
    Jerry Gipson
    Jim Godowitch
    Sharon LeDuc
    Sang-MiLee
    Shawn Rose lie
    Jeff Young
                                          The complexity of environmental or air quality
                                          prediction has increased because we must deal with
                                          secondary pollutants, as well as primary ones.
The multi-pollutant nature of the atmosphere is being
recognized, also increasing prediction complexity.
Multi-pollutant interactions tell us that we should be
thinking and modeling increasingly from a one
atmosphere perspective.  They also tell us that we need
to be thinking multi-scale.
                                         There is greater dependency on the realism of the
                                         simulations. We recognize that we need to predict
                                         outside today's mix of chemical species to future, very
                                         different mixes under conditions of complexity and
                                         nonlinearity.
                                          Our Modeling Should Have:

                                             Increased Reliability Entailing Improved Realism in
                                             an Expanded Scope, a One Atmosphere Scope

-------
K)
         We Came to the conclusion that this necessitated
         models that:

            •    Are as first principles as possible or feasible

            •    Include a full set of interconnected physical
                 and chemical process descriptions

            •    Incorporate a full marriage with prognostic
                 meteorological modeling
We also came to the conclusion that:

    Current Systems Not Expected to Cope

    Incrementalism Not Expected to "Get Us There"

    No Single Group Can Do It All (Nor should be
    expected to)
Three Pillars of Requirements for a 3rd Generation Modeling
System

        Science
            Increased realism and adaptability

        System Framework
            Increased Modeling capability

        Computing Infrastructure
            Increased compute power and flexibility

    Umbrella Concept of Community Modeling Is To
    Permeate
    Our Response:  Develop a 3rd Generation Modeling System.

             This new modeling system is composed of a 3rd
             Generation Modeling Framework, termed Models-3,
             and a 3rd Generation Air Quality Model, termed the
             Community Multi-scale Air Quality Model, CMAQ or
             Models-3/CMAQ.

-------
IJ

•     Up to date science with better or easier integration
         of new science
             (Keep up with the best)

  >     More complete multldisciplinarity; One atmosphere
         scope
             (Integration of "complete" set of physical and
             chemical processes)

  >     Better evaluation
             (Diagnosis of model processes; diagnostic
             evaluation)

  >•     More robust and adaptable model structure
             (CTM adaptable to different dynamic driver
             configurations)

  >•     Better modularity to support community modeling
Increased Modeling Capability (SYSTEM FRAMEWORK)

  4      Support for the different levels of modularity.

  •      Full system available to dispersed scientific
         community for process study, model/module
         development, and incorporation of advances.
         (Support community modeling at the science level.)

  +      Full system available to operational user
         community for assessment, "easy," controlled
         execution.

  >      Support for levels of interoperability and
         intercommunication needed to support community
         modeling.

  4-      Full execution analysis:  verification, visualization,
         output analysis, process analysis, model
         evaluation.

-------
                                              RMctMty O5/12/W)
 SCIENCE

 Set of Three Models: CMAQ/ MM5v2/ MEPPS

     Designed to be Multi-pollutant and Multi-scale

       O     Ozone, Acidic Deposition (S and N), Nutrients
             (N), Fine Particles (primary and secondary:
             sulfate, nitrate, organics), and Visibility

       O     From Continental to Urban, with embedded
             Plume-in-Grid
Annual Releases of the Model Set Are Expected for the Next
Several Years.

    Public Release of CMAQvl.O
             June 1998

    Major Update and Expansion of Selected Science
    Options (Given Below) of all Three Models, With a
    Focus on CMAQ
            June 1999 Release
    Subsequent Release Dates to be Determined
       MCIP
      Emission
     Processor
     (MEPPS)
                      Meteorology
                        (MM5)
                    Data Flow
         Principal Non-framework Components
Models-3 Interfaces
Analysis Tools
               System Instructions

-------
                                                  R**ctMty 05/12/90
                                                                                                                  Ructivfcy 05/12/98
NJ
    Meteorological Model: MM5v2
Basic Pedigree

    Penn State/NCAR Mesoscale Model Version 5

    State-of-the-science prognostic meteorological
    model

    Started in 1970's; on-going development today;
    MM5 is contributed to extensively by the scientific
    community

    National and international use for operations and
    research
MM5 Operation
    We are using MM5 Version2, the latest release

    It is non-hydrostatic (to be able to go down to small
    grid sizes)

    Tested, most applicable set of physics options
    invoked

    One-way nesting (we were first to debug this
    option) at 108-, 36-, 12-, and 4-km resolutions

    4-Dimensional data assimilation (Analysis Nudging)
    to recreate past meteorology as closely as possible
    for 108-36-12 resolution

    Augmented, adapted output to better serve air
    quality modeling
                                                                        MM5 Future Development by Our Group
                                                                            Higher resolution land-use and soil data (Vegeland)

                                                                            More advanced PBL, microphysics, radiation
                                                                            (Pleim-Xiu with Vegeland)
                                                                            Implementation on workstations and massively
                                                                            parallel computer - CrayTSE
                                                                                              10

-------
Daewon W. Byun
Chemical Transport Model: CMAQ
       Model design
                             MEPSE
            CMAQ  Adaptability
                Chemistry - Transport model
           Chemistry      _ Advection      Diffusion
                         2-48

-------
                                               RudMty OS/12/M
NJ
Science Features - CMAQvl.O for June 1998 Release

    Generalized coordinate system internal to CTM (to
    work with any map projection and meteorological
    driver)

    Generalized chemical mechanism reader

    Gas-phase chemical mechanisms and solvers
         RADM-2+ (Carter isoprene)
         CB-IV
             QSSA for workstation
             SMVGEAR for Cray (vector machine)

    Piecewise Parabolic Method (PBM) for advection

    Vertical diffusion: Kv (eddy dlffuslvity)

    Horizontal diffusion: KH (resolution dependent)

    Clouds (and precipitation)
         Large-scale: grid-resolved at all1 resolutions
         Convective: sub-grid parameterizations at 36-
         and 12-km
                 Precipitating
                 Non-precipitating
         Aqueous chemistry (RADM)
CMAQvl.O for June 1998 Release (cont.)

    Particulate Matter
        Modal dynamics
        3 size ranges
             PM-fine      Secondary (S, N, Organics)
                         Primary (emissions
                         inventory)
             PM-Coarse   Primary (emissions
                         inventory)
        Chemical speciation tracked
        Size dependent dry deposition

    Regional Haze:  Light extinction; Deciviews

    Plume in Grid

    Photolysis rates:  Look-up table, with cloud
                     attenuation
                                                                        Implemented on PC/NT; Sun Ultra, Dec Alpha, and
                                                                        SGI (close); and Cray vector supercomputer
                            12
                                                                                          13

-------
                                                                                                            Hn • «| asnvm
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Additional Science Features Expected - CMAQ, June
1999 Release

    Chemistry:   SAPRC

    Advection:   Bott, ASD (spectral), YAM

    Diffusion:     Asymmetric Convective Model (ACM)

    Surface PBL: Vegeland Pleim-Xiu (PX)

    PM:          Improved production of organics
                 Incorporation of sea salt

    IC/BC:       Stratospheric background (top)

    Photolysis:   4-D implementation
          Implementation on massively parallel computer -
          CrayT3E
MCIP, Meteorology-Chemistry Interface Processor

    Features - MCIP for June 1998 Release

        Generate coordinate dependent meteorological
        data (Jacobian) for generalized CTM simulation
        (traditionally treated in CTM)
          >     Maintains modularity of CMAQ regardless
                 of coordinates

          >•     Allows consistent links to many
                 meteorological models

          >•     Provides meteorologically consistent
                 interpolation methods

        Process meteorological data
          >•     Window to CMAQ domain

          >•     Compute or pass through surface and
                 PBL parameters

          >•     Diagnose cloud parameters

          >     Compute species-specific dry deposition
                 velocities (gases)

          >•     Output meteorological data in Models-3
                 I/O API format
                            14
                                                                                         15

-------
NJ
    Additional Features Expected - MCIP, June 1999
    Release
        Link with RAMS (by end of Calendar 1998)

        Deposition:   CMAQ method (linked to
                     Vegeland_PX land-surface model)
Plans for Future Improvements: CMAQ and MCIP
    Morphecule Chemical Mechanism

    Links to other meteorological models (ETA, RUC,
    ARPS, WRF)

    Additional diffusion options: Hybrid (local/non-
    local), Transilient

    Greater option consistency between MM5 and CTM

    Explicit simulation of aqueous phase chemistry in
    clouds

    Particulate modeling: External particle mixtures
    (particles with same size but different chemistry);
    better representation of blowing dust.

    Improved methods for mass conservation (mass vs
    mixing ratio)
        Deal with mass tracking, source
        apportionment

    Sensitivity analysis packages incorporated
Emissions Model: MEPPS
Models-3 Emissions Processing and Projection System

    INPRO/IDA (Inventory Data Analyzer)
        QC of source/emissions inventory emissions data

        Format conversion to Models-3 I/O API

    EMPRO
        Modified GEMAP/EMS-95 for point and area
        sources
            SAS-based system, incorporating ARC/lnfo
            geographic information system to accomplish
            spatial allocation of emissions data.

        MobileSa mobile source emissions model

        BEIS2 biogenic emissions  model

        Speciated emissions for RADM-2 and CB-IV
        mechanisms
                                                                ECIP
                                                                    Linked to MCIP for meteorological data

                                                                    Calculate plume rise for major point sources

                                                                    Linked with Plume-in-Grid
                          16
                                                                                      17

-------
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                                               70
                                               !
MEPRO
    Project base year emission data using source-
    category-specific Economic Growth Analysis
    System (EGAS) factors for input to EMPRO
                  Additional Features Expected - MEPPS June 1999
                  Release
                      MobileSa with PM-fine emissions

                      BEIS3 biogenic emissions model

                      Speciation for SAPRC (fixed stochiometry)
              Future Improvements for Emissions
                      SMOKE emissions processor

                      Generalized speciation

                      Link to Morphecule chemical mechanism
                                                                                         18

-------
                                                  RwctMty W12»«
to
   Modeling Scales

        Horizontal
             Nests of 108-km, 36-km, 12-km, and 4-km

             Windowing to subdomains from continental to
             regional
                layers from the surface to the top of the free
             troposphere
             30 layers collapsed to 21 layers, converting the top
             18 layers to 9 layers
                     predictions for 24-hour simulation
              segments; typically for 5-day simulation penods
                         meteorological inputs at 36- and 12-km
                   15 minute meteorological inputs at 4-km

              Aggregation (statistically weighted average) of 44
              synoptic flow patterns for seasonal and annual
              averages at the continental scale
MO If    130 W   120 If  HOW  100 y  BOW  BO If  70 If  60 IT   60 If    40
                                                                 30 N
        110 W ir
                  too w
                                     60 W
                                               70 W
                                                         IT
                                                         SO N
                                                         40 N
                                                         20 H
                                  19

-------
                                                          121
                                                                                        RADM VERTICAL DOMAIN
   .40*    130 W   120 y   110 W 100 W  90 W  BOW  70 W   00 W   60 ₯    40 W
K)
   i  .
                                                             50 N
           110
                      100 W
                               90 IT
                                         60 W
                                                  70 W
                                                                                          200  220  240  260   280
                                                                                                Temperature (K)

-------
                                              R.KItvtty OS-1MH
               CMAQ MODEL EVALUATION
                       Near Term
Purpose: Acceptance by Regulatory Community

  • Traditional Operational Evaluation - NARSTO NE '95
    >• O, predicted versus measured
    >• Daily bias & gross error aggregated over all sites
    >• Accuracy of peak predictions
    Time-Space Disaggregated O, Statistics - NARSTO NE
    '95
    >•  Space: type of grid cell based on photochemical
        Processes
    >•  Time:
        * early morning: titration & inversion breakup
        # daytime: mixing height & dilution;  O3 production
        # nighttime: deposition, surface layer loss
                           20
                                                                                                             RuctKHty-OS'12/M
               CMAQ MODEL EVALUATION
                       Long Term
Purpose: Acceptance by Scientific Community
  • Process understanding and scientific uncertainties
  • Determine best model configuration to reduce
    uncertainties
  • Assess value of new measurement information
    Diagnostic Evaluation - Nashville SOS '95
    >•  Insight into processes generating O3
        *   OH & NOX cycle Interactions with resulting O,
             production
        *   Integrated reaction rate/ mass balance
        *   Indicator species
    >•  Sensitivity : CB4 versus RADM2+ chemistry

    Sensitivity Analysis - Nashville SOS '95
    >•  Characterize importance of process differences
    >•  Interpretive analysis related to appropriate use of
        CMAQ
                                                                                         21

-------
SYSTEM FRAMEWORK


Enhanced Modeling Capability

  *     Support for the different levels of modularity

  *     Full system available to dispersed scientific
        community for process study, model/module
        development, and incorporation of advances.
        (Support community modeling at the science level)

  •:•     Full system available to operational user
        community for assessment, "easy," controlled
        execution.

  <•     Support for levels of interoperability and
        intercommunication needed to facilitate community
        modeling

  *     Full execution analysis: verification, visualization,
        output analysis, process analysis, model
        evaluation.
An Advanced Computer-based Problem Solving and
Modeling Environment or Framework With An Effective
Human-Computer Interface for Environmental Modeling and
Assessment That is Adaptable to a Changing Computing
Infrastructure.
Assist Environmental Analysis and Model Development

  >    Facilitate execution of air quality simulation
        modeling systems, especially air quality models,
        and the visualization and analysis of their results.

  >    Minimize the tedium and chance of error
        associated with modification of rigid model
        execution scripts.

  >•    Provide comprehensive data management to assist
        in storing, accessing, tracking, identifying, and
        capturing processing history of numerous datasets
        associated with modeling studies.

  >    Manage and organize large collections of model
        executions and associated data.

  >•    Provide cross-platform (a variety of computing
        platforms) computing of complex modeling studies
        with distributed data management.
                          22
                                                                                        23

-------
                                                    R««c«vty 05/12/90
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       Assist Environmental Analysis and Model Development
       (cont.)

         >    Aid the assembly, testing, and evaluation of
               science process components by facilitating the
               interchange of process modules and minimizing
               the chance of incompatible assumptions.

         >•    Facilitate the tailored execution of the modeling
               system, including customized process analysis.

         >    Provide the flexibility to change key "global" model
               specifications such as grid resolution, map
               projection, or chemical mechanism without
               rewriting code, thus minimizing error.
Functionality Achieved Via the Following Management
Components Incorporated in the Modeling Framework:

    Science Manager

    Model Builder

    Program Manager

    Data Manager

    Strategy Manager

    Study Planner

    Tool Manager

    Source Code Manager

    Framework Administrator
                                                                    Flexibility for Future Change Achieved by Architectural
                                                                    Layering
                                 24
                                                                                              25

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   ARCHITECTURAL LAYERING:
FLEXIBILITY FOR FUTURE CHANGE

USER
INTERFACE
USER INTERFACE
Management Layer:
Data Manager Science Manager
Study Planner Model Builder
Strategy Manager Source Code Manager
Tool Manaaer Framework Administrator
Environment Layer: OS, System "Personality"
Computational Layer: Programs: models, analysis, visualization,...
Data Access Layer: I/O Applications Programming Interface
Data Structure/Representation: netCDF, XDR
Data Storage: File systems & databases
Physical Device Layer: Disks, networks, printers, machines
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       CMAQ   Adaptability
            Chemistry - Transport model


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                                                                                                               R««c«vtty O5/12JW
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       MODELS-3 FRAMEWORK CAPABILITIES (cont.)


 Data Manager
  •  Data access from any networked system
  •  No need to convert data between computers
  •  Manage dataset history information
  •  Uses Federal Geospatial Metadata Standard

Strategy Manager
  • Evaluate alternative emissions control options and
    future years


Study Planner
  • Automated multiple-platform execution of a series of
    interlinked programs/ model/ independent modules
  • User control over input parameters
                                                                        MODELS-3 FRAMEWORK CAPABILITIES (cont.-2)

                                                                  Tool Manager
                                                                    •  Prepare emission inputs compatible with selected
                                                                       model
                                                                    •  Invoke visualization & analysis tools
                                                                        >  VIS5D -  3-D analysis & animation
                                                                        >  PAVE -  2-D analysis & remote viewing
                                                                        >  IBM DX - specialized analysis tools
                                                                        V  SAS
                                                                  Source Code Manager
                                                                    • Version control of science code ensures documented
                                                                      software evolution & replication of previous executions
                                                                    • Facilitates automated building of models from
                                                                      components
                                                                  Framework Administrator
                                                                    •  Controls integrity of official model versions
                                                                    •  Controls security & access to data/ code
                                                                    •  Provides system maintenance capabilities
                                27
                                                                                             28

-------
     Seamless Computing & Data Management

       From PC to Scalable Parallel Computer
State/Regional Offices
      Public Access
                     Jylaster
                            Metadata
                            & Global Info
                         Object Oriented DBMS
   Federal Agencies
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                                                RtcclMly 03/17/M
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         KEY MANAGEMENT LAYER COMPONENT DETAIL

                       STUDY PLANNER
      • Automated multiple-platform execution of a series of
        interlinked programs / models
        Automatic registration of generated output files
Execution "History" information written on each output
file

 >• Link to compile time information
     *   science module versions
     *   configuration file, compile environment & date
         >•  Runtime control information
             *  environmental variables, namelist input,
                command line
             *  study/plan identification
             *  link to input/output file metadata
SOME FEATURES OF THE MODELS-3/CMAQ SYSTEM THAT
SHOULD AID THE SUPPORT OF REACTIVITY
CALCULATIONS


        Chemical Mechanism Reader

        Customizable Process Analysis

        Study Planner

        Data Manager

        Multi-pollutant CTM

        Responsibility for Evaluation, Including Diagnostic
        Evaluation

        Meteorological Case Variety and Availability
        Expected to be Extensive
         >  runtime environment
             * execution date & time
             * hardware platform, OS version
                              30
                                                                                         31

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                Establishing a Community Modeling Capability
                                Kenneth Galluppi
                       Univeristy of North Carolina at Chapel Hill

    Taken From: Air Quality Community Modeling and Analysis System
                            Attributes and Implementation
                                    Draft 09/15/97
 I.     Introduction

 Over the past four years, there has been a tremendous growth in the community's utilization
 of air quality models in the development of emission strategies related to Clean Air Act
 compliance.  For example, the Ozone Transport Assessment Group, OTAG, witnessed model
 applications growing beyond the four "official" centers to extend to many States, private
 industries, consulting engineers, and environmental groups. With this, exposure, came
 concerns of public access and consistency in model evaluation, analysis, interpretation, and
 scientific integrity of the systems and their application. One approach to reducing these
 concerns is to implement a community modeling and analysis system.

 From August 27-29, 1997, a workshop was held in Research Triangle Park to discuss the
 purposes and needs for models, the benefits of a community modeling approach, and the
 attributes of and obstacles to developing and implementing; such a system.  The workshop
 had fifty participants whp represented federal and state governments, industry, and university
 researchers.  This paper is a summary of the background, findings and recommendations
 from the workshop.
 II. Models, Analysis, and Their Applications

 There are many approaches to modeling ranging from statistical to comprehensive models
 based on governing equations of physics and chemistry. Each approach has its strengths and
 weaknesses in terms of reliability, predictability, and cost. A diversity of modeling
 approaches serves to check our models for consistency resulting in greater confidence in their
 application for emission strategy development.
— -
^Untangling the physical-chemical relationships required to understand the cause-effects of
f pollution problems is a daunting task. Over the past decade, the air quality community has
 been engaged in various developments and applications of comprehensive models in
 conjunction with complex analysis of observations. Each model or analysis improvement
 has opened the door to new sets of unexplained observations and hypotheses.  Improving our
 scientific understanding is, and always will be a dynamic process, but remains at the pinnacle
 of developing sound environmental practices.

 It is assumed that the community is committed to the development of scientifically credible
 models and in building skill in their use for guidance, to discern probable cause-effects and in
                                         2-63

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develop mitigation and prevention strategies of air quality problems.  This commitment
stems from the increasing costs of assigning culpability for pollution abatement and
-prevention.  Policies are establishing who pays and how much which opens questions to how
reliable is the scientific guidance used for this judgement. The question remains, how does
the community develop the best simulation tools for use by both scientists and managers
whose common purpose is achieving a sustainable environment?

While the scientific community is  engaged in developing new insights into science, the
management community is engaged in making decisions based upon the best available
science.  Most would agree that these are complementary objectives.  However, history has
shown us that scientific knowledge and new analysis methods are difficult to transfer to a
large, diverse, and often an divided management community whose time and funding
constraints may inhibit the use of "best" science or its proper application and interpretation.

The development of numerical models and their application to real world  problems has
enabled mediocre transfers of scientific knowledge and technology utilization. Howeyer, the
rising costs of environmental protection demands the quicker development of better models
and their transfer for use in scientific and management practices. In order to develop low-
cost, equitable policies, that the community has confidence in, we need to capitalize on a
shared goal to develop the best scientific formulations and learn to apply models in a
consistent manner.

The question explored in the workshop is whether the community can enhance these efforts
through common, integrated development and application efforts. If so, does this warrant the
defining, development afod implementation of a community-based modeling and analysis
system?
 HI. What is a Community Modeling and Analysis System (CMAS)?

 A Community Modeling and Analysis System (CMAS) is an approach to model
 development, application and analysis that leverages the community's complementary talents
 and resources in order to set new standards for quality of science and reliability of
 application of air quality models.  The resulting comprehensive system forms the foundation
 which the community, including governments, industry, academia and other stakeholders,
 participates in the examination of issues and the subsequent development of strategies that
 meet societal challenges of environmental protection.

 A community modeling system is a computerized framework and intellectual process that
 integrates the research and development findings, and application experiences into a common
 set of tools and knowledge base. The information and tools in the CMAS are open and
 readily accessible to everyone.  It is called a system because the integration is organized into
 a wide range of computerized information modules. It is the desire of the CMAS approach to
 increase productivity and reduce the cost of examining issues and developing alternate
 scenarios. The cornerstone for accomplishing this is.the framework that enables quicker
 integration of science and techniques and for easier transfer of knowledge and experiences to

                                         2-64

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the community.  The result is peer reviewed, process of providing the best simulation and
analysis tools for use in a regulatory setting.

A CMAS is not a single "mother of all models", but an integrated collection of science
modules which can be linked together to form multiple model configurations. The
underlying premise is that there is no single group of modules that can claim to be the "best"
model.  Rather, by changing specific modules one can gain insight into the validity of
modeled results. This does not preclude the regulatory community from assigning and
locking a prescribed set of modules into being the "regulatory model" for consistency
purposes. In fact, there is an advantage to having several "regulatory" models for routine
scientific comparisons.

For example, the National Weather Service in its earlier days of weather forecasting, utilized
three models for daily comparison of predictions: the complex Limited Fine Mesh (LFM),
the 2 variable Baroclinic, and the 1 variable Barotropic models. Although formulated
differently, they were compared for consistency. The "simpler" models aided the
meteorologist to get a feel for the numerical forecast generated by theJLFM, the model of
choice. The models are more sophisticated now, but are still cross-checked against models of
similar complexity.

How does this freedom of module use potentially impact the regulatory process?  Which
modules can be utilized and when? Are we adding more confusion to the analysis than
before?  How can do we know when we are getting a "better" simulation".  How do we
prevent model "calibration"? These are but a few of the more imposing questions that will
inevitably arise and many of which were addressed at the workshop.
 IV.  Benefits of a Community Modeling System

 Increasing productivity, raising confidence in results, interpretation and use, increasing
 stakeholder buy-in, and reducing costs are all worthy goals of any modeling approach. The
 CMAS is intended to maximize these benefits through the reduction of overlapping
 developments, peer review, and ease of development and application.  Given a robust and
 streamlined system design and a peer review process by which the CMAS can be used for
 development and application, the benefits of a CMAS.  The benefits should easily justify the
 focusing of resources and change in process by  which models, tools and techniques are
 currently developed in the community.  There are many benefits to the community. These
 include:

 a)  Implementing scientific advancements into  models  can be difficult. A modular
    community system allows for process and formulation changes easier and with less
    resource. This will enable the community to take advantage of new approaches sooner
    than  ever before.
 b)  Model versions and revision levels can be more readily controlled. Further, time to create
    new revisions will be significantly reduced. A CMAS inherently will have far better
                                        2-65

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   quality assurance procedures when many more are involved in establishing a new
   version.
c) With a common framework, model formulations and their applications will be far easier
   to compare.
d) New scientists and engineers can be trained in specific areas of expertise since only one
   framework needs to be learned. Further, over time, there will be a cadre of experts who
   can share their knowledge with new personnel. This will lead to a dramatic reduction in
   costs associated with training and continuing education.
e) Scientists and computer scientists will complement one another without having to learn
   the other's field. Development groups will be able to better utilize the skills and training
   of its personnel.
f) The science and application talents and knowledge will be added to a common base and
   made available to all. This will enable all problems to be addressed at the best available
   skill level.
g) Databases that are utilized by the models and for analysis will be more easily shared
   which should lead to more thorough quality control, analysis and consistent
   interpretation.
h) Analysis techniques and methods can be more readily transferred to the community. This
   should enable more revealing techniques to be utilized and understood by a larger pool of
   experts.
i) A common system will have several levels of use including the management decision
   maker, scientist/engineer, and model practitioner.  A robust CMAS enables each of these
   specialists to maintain the appropriate level of detail needed to keep their understanding
   within context, and while at the same time enable each group  to communicate more
   effectively to one another.
j) User groups and other transfer methods would be implemented to develop a knowledge
   base.
k) A peer review process will assure that quality science, application, and analysis are being
   implemented and put to best use by the community.
V.  Attributes of a CMAS

The workshop breakout groups looked at six areas of attributes and implementation issues:
science, environmental management, education, support and maintenance, intellectual
property, and model application and evaluation. In this draft, each group's listing of
attributes is given. In later drafts, the groups' replication of comments will be eliminated.
The attributes are characteristics that describe a community modeling and analysis system.
In other words, what must a CMAS be able to do to meet the specific perspectives of
modeling support?

Group A - Science Workgroup
a)  General enough to minimally integrate the processes required to simulate regional and
    urban scaled problems.
b)  Incorporates the physical-chemical processes to enable utility for examination of multiple
    pollutant (ozone, aerosol, acid deposition), air quality problems.  Eventually, it must

                                        2-66

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   extend to cross-media where chemical transport crosses media types, for example to
   water.
c) Able to produce three dimensional concentration and deposition fields of key chemical
   and physical species that enable a diagnosis of the cause-effects relationships.
d) Must be usable by scientists, environmental managers, and stakeholders within the
   effected communities and regulated industries.
e) Brings together a working community to examine issues such as the NAAQS, NSR, and
   deposition.
f) The science modules must be peer reviewed, relevant processes required for multi-
   pollutant assessments.  Further, the CMAS must be extensible to include alternate
   formulations of known processes and the inclusion of new science when it becomes
   available.

Group B - Environmental Management Workgroup
a) Able to assist the managers by modeling input variations consistent with varying
   environmental strategies.
b) Have a high level of quality control to raise confidence of use.
c) Should be linked to and assist in risk assessment and decision making techniques
   including social-economics and health risk.
d) Be able to expose and explain sensitivities and uncertainties in the formulation and their
   impacts on results, interpretations and utilities.
e) Responsive to time constraints and adjust formulation accordingly
f) Must be able to facilitate communication to multiple levels of users from managers,
   practitioners and public.
g) Must be a ble to summarize and explain input scenarios and impacts on results through
   the use of multiple analysis techniques.
h) Must be well documented and understandable by multiple levels of users.
i) Must be reasonable cost to not be prohibitive for any stakeholder to utilize.
j) The CMAS must be open for all participants to examine. The process to include new
   modules must be open, peer-reviewed, and well understood.

Group C - Education Workgroup
a) The community requires a diverse set of expertise to be available to educate and be
   trained in. This includes: emission engineering, meteorology, computer science,
   atmospheric chemistry and physics, data analysis, and program and operations
   management.
b) Additionally, the community needs to be educated into the impacts on economics, control
;  technologies, risk assessment, population exposure, community and industrial planning,
?!  and other environmental concerns.
c) Good practices in computer science need to be brought to the training program. This
   includes: systems engineering, database management, programming,
   graphics/visualization, and system administration.
d) A thorough program management training must be undertaken that includes: planning
   and scheduling, science and technology appreciation, resource allocation,
   communications, and negotiation skill. J>


                                        2-67

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e) Multiple education and training methods must be deployed. Examples include:  hands-
   on, internships, web-based, print, video, satellite, workshops, user groups, and chat
   rooms.
f) Various sectors within the community must have better dialog and cross training. These
   include the scientific, management and practitioner groups, as well as government,
   industry, environmental, and academia groups.
g) Guidelines are needed to help establish consistency in personnel skill and training.
h) Education programs need to be able to expand quickly and be effective to train many
   users in a relatively short time period.

Group D - Support and Maintenance Workgroup
a) The CMAS is a common platform for model development and application for both the
   scientific and regulatory communities.
b) The system automates as many of the computer operations as practical and makes it easy
   for code  compatibility and code re-use. To the extent possible, CMAS is modular and
   standardized.
c) The CMAS is self-documenting and readily available
d) Acceptability criteriaTor any change to CMAS will be established. This includes new
   modules as well as for using in scientific and official regulatory studies.
e) The CMAS will be supported by a core maintenance group. This group also has
   responsible for maintaining key databases and datasets that are utilized by the
   community.
f) The CMAS and data are open and readily available through several distribution channels.
g) The core group assigned to maintain the CMAS, implements the procedures for updates,
   testing and distribution. This include science and computer updates.
h) The support group is established and overseen by a governing board.  The Governing
   Board is responsible for establishing official policies regarding CMAS and establishing
   funding support.
i) Procedures are established by the Board for creating updates to the system and releasing
   versions for scientific and regulatory use. A proposed schematic linking the institutions
   involved with CMAS and the procedures that they follow is shown in Figure  1.

Group E - Intellectual Property Workgroup
a) There are three approaches to making software available that need to be considered: It is
   accepted that public domain or shareware concept are acceptable only if the code is fully
   open and accessible.
   •   Public Domain: Creator relinquishes all rights to intellectual property and makes
       software freely available. The code is open.
   •   Shareware: Author maintains a copyright on the intellectual property and code but
       makes it available free or at low cost to promote sharing. The  code may be open or
       closed.
   •   Proprietary:  The author retains all rights and generally charges a fee for use. The
       code is usually closed.
b) The source code for software that affects model results should be available for free. This
   promotes understanding, review, and trust of the^science and its implementation. Related
   components, such as interfaces and graphical tools, that do not affect the model or

                                        2-68

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   analysis results must be readily available for free or low cost but do not necessarily have
   to be open.
c) CMAS tools could also include third party software, such as SAS or Arc/Info, which
   would remain proprietary. However, regulatory procedures should give a low cost, low
   resource, alternative.
d) Value added modules for analysis, graphics, etc. can have license fees, but must be open
   to scrutiny.
e) Most credit will be given by reputation and publishing. However, contributed modules
   should be documented for credit and given proper credit by the users.
f) There may be liability issues related to deficiencies in best science, bad science, and
   coding errors. The Governing Board will need to establish procedures for investigating
   these issues and establishing limits to liability, if any.

Group F - Model Application and Evaluation
a) The CMAS is managed by a central organization and overseen by a Board of Governors
   that represents the air quality community stakeholders.
b) The CMAS center supports, facilitates and maintains the development of a low-cost, open
   modeling and analysis system. The center does not apply the system.
c) The CMAS does not preclude outside model developments but serves to promote more
   involvement in development.
d) Research intersts should be linked to regulatory needs, including time and funding
   schedules.
e) All aspects  of CMAS must be peer reviewed.
f) CMAS must be linked to data bases that are readily available, quality  controlled and
   documented.  The CMAS management organization can act as a data clearinghouse.
g) The management center must have sustained support,  remain viable, reliable and growing
   in competence.
h) In order for applications to be successful, CMAS must provide the following types of
   tools: a flexible framework, analysis tools, tutorials, technical guidance, and transfer
   mechanisms such as workshops.
i) In order for management practices to be improved via a CMAS the following needs must
   be met: assurance of the best tools, sanctioned regulatory configurations, detailed
   guidance for use and interpretation, and technical support for all levels.
j) To improve model evaluation, the CMAS must provide a range of open diagnostic tools
   that facilitate collaboration. The data and modeled results must be easy to access and
   with proper guidance, easy to analyze and interpret. Performance evaluation should be
   understood.

rVI.    Issues With Implementing  a CMAS

There are many obstacles that would prohibit an effective community approach from being
implemented, the most obvious being funding support. However, there are many other
pressing issues, each of which could inhibit the benefits of a Community  Modeling and
Analysis System. Whereas, the workshop groups were able to define attributes along six
different sets of attributes, the implementation obstacles were much more ubiquitous during


                                       2-69

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the breakout and plenary discussions. Because of overlap of issues, a consolidated view of
the workshops can be presented.

a) A sustainable funding is critical to achieving a CMAS. To this end, the benefits of a
   CMAS must be clear and communicated to stakeholders in government, industry,a nd the
   public sector. Long term commitments to funding must be identified and put in place.
   This will be difficult due to funding mechanisms, mix or public and private dollars, and
   accountability.
b) A consensus view of the attributes needs to be developed. This will not be straight
   forward as funding constraints will prevent all attributes from receiving the same
   attention.
c) Defining and promoting standards within the community will be difficult. This covers
   coding and module integration standards.
d) An agreed upon management structure must be put in place.  This includes a Governing
   Board as well as the CMAS center administration and technical staff.
e) Guidance and modeling protocols need to be established as to how to utilize a CMAS.
   This includes guidance for modeling evaluation and peer reviewed acceptance of
   modules and science.
f) Setting up a CMAS, management structure, databases, and codes will take time.
   Additionally, the community will need to change how it performs modeling  currently.
   These changes will take time as well as funds.  It is questionable to some whether this
   resource cost is justified.
g) The community is accustomed to using certain models and analysis techniques.
   Establishing credibility for a flexible system will be difficult. The community would
   need to establish an evaluation program that meets a concensus view of acceptance.
 VII.   Recommendations

 There is general agreement that the benefits of a community modeling system are significant
 enough to warrant further study and defining. The main recommendation is to form a group
 of writers to put together a first proposal.  This initial draft proposal needs to be outline how
 a Community Modeling and Analysis System can be funded, managed, and leads to
 improved science and decision practices.  The proposal needs to clarify the following points.

 a)  Clearly define the CMAS for all to understand.
 b)  Clarify the benefits to the various stakeholder groups.
 c)  Propose a detailed funding proposal that shows costs to implement and sustain a CMAS
    Center and future developments. This includes the number and type of positions required
    and their reporting structure.
 d)  Clarify how the development cycles of the regulatory and scientific versions of the
    community system will work together to assure the best science availability on regulatory
    timeframes.
 e)  Outline how the CMAS would be applied within guidelines, peer reviewed procedures,
    that enable the best application practices.


                                       2-70

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f)  Clarify the peer review checks for the science, the CMAS developments, regulatory
   recommendations, and application guidance.
g) Clarify potential legal issues involving intellectual property and liability.

It is highly recommended that progress towards defining a CMAS be made quickly and
systematically.  To this end, the following recommendation are made:

(a) Groups that have responsibility for achieving progress with Clean Air Act compliance
   must be briefed about the CMAS proposal. Their buy-in to the concept is extremely
   important. These institutions include the EPA's Office of Air Quality Planning and
   Standards (OAQPS), industry and other stakeholder communities, State environmental
   groups, consultant groups, and academia.  These groups must be made aware of the
   benefits of a community approach and how it would work.
(b) The Federal Advisory Committee (FACA) looking at new approaches to  achieving
   national air quality standards needs to be briefed about CMAS.  FACA should provide
   guidance as to the  needs for a CMAS.
(c) An outline of the CMAS proposal needs to be circulated as soon a§ practical to get a
   wider acceptance to the proposal needs of the community. Accompanying this outline
   should be a proposal for gaining community buy-in.
(d) A full  proposal outlined above must to be circulated within a wide community audience.
   The community should have time to comment to the proposal whereby and final proposal
   to establish a CMAS be written.
(e) A workshop should be considered for the spring of 1998 that will examine and debate
   the merits of a CMAS, its feasibility, and funding.  The outcome of the workshop would
   be targeted at gaining a community go or no-go decision and commitments.
                                        2-71

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            Establishing a Community
               Modeling Capability
                   Kenneth Galluppi
         University of North Carolina at Chapel Hill

              Summary of the Air Quality Community
              Modeling and Analyze System Workshop
                    August 27-29. 1997
What is a Community Model and
    Analysis System (CMAS)?
•  Leverage community-wide talents for
  development and application of modeling
  and analysis.
•  CMAS is computes-framework for
  integrating "best" tools and knowledge.
•  Available to all for operational and research
  needs.
        Benefits of CMAS

  Less resources to develop and maintain and
  evaluate.
  Regulatory and research needs are satisfied
  and complement one another.
  Operational needs for maintenance and
  training are a priority.
  Consistency.
  Peer reviewed for all purposes.
K)
           CMAS Workshop Groups

        Science
        Environmental Management
        Education and Training
        Support and Maintenance
        Intellectual Property
        Model Applications and Evaluation
        Science Workgroup

 Regional and urban scaled problems, for
 multiple pollutant (O3, aerosol, acid dep.)
 Usable by science, management and
 stakeholders.
 Peer reviewed.
 Processes that get to the causes.
 Accommodates robust analysis and
 alternate formulations.
   Environmental Management

• Consistency of formulation and use.
• Decision enhancing analysis.
• High level of quality control.
• Linked to risk-assessment, and other
  decision making parameters.
• Responsive to regulatory time constraints.
• Facilitate communications.
• Documented, open, no (low)-cost.

-------
            Education Workgroup

       Diverse levels of education/training needed:
       management to practitioner, cross-
       disciplines including computers.
       Many forms of training to meet all needs.
       Guidelines for training to establish
       consistency in knowledge and application.
       Timely and affordable.
       Education to link to decisions and impacts.
 Intellectual Property Workgroup

• Give proper credit where credit is due.
• Open, peer reviewed and
• Free if it impacts science results, may
  charge for value added modules, but open.
• If community "owned," are there liability
  issues?
    Support and Maintenance

Modular, standardized, oriented for code re-
use. This includes inputs and analysis tools.
Well maintained and documented.
Procedures for making changes and
acceptance for scientific and regulatory use.
Core support group is maintained and
overseen by a board.
to
         Application and Evaluation

       Central organization overseen by a Board.
       Maintenance, QA, and training are critical.
       Peer review everything in appli. and eval.
       Facilitate application and developments of
       an open system but remain neutral.
       Assure best tools, sanctioned versions,
       guidance for use and interpretation.
       Good set of tools and facilitated collab.
           Difficult Issues

  Sustainable funding for support and maint.
  Consesus view of attributes given funding.
  Design and promoting standards is hard.
  Management structure.
  Guidance and modeling protocols a MUST.
  Setting up CMAS takes time and money.
  Establish credibility for flexible approach.
 Recommendation for CMAS

Clarify CMAS and its benefits.
Detail funding requirements.
Clarify development and "locking" of
science and regulatory versions.
Guidance procedures for application, peer
review, and evaluation.
Clarify legal issues of a "community"
model

-------
                              ABSTRACT

Emissions Modeling Issues for Reactivity Calculations: State and Status of
    the Sparse Matrix Operator Kernel Emissions (SMOKE) Modeling
                                  System.

                                Neil Wheeler
                            Environmental Programs
                      North Carolina Supercomputing Center

There are a number of scientific and operational criteria for emissions modeling systems
to support the use of photochemical grid models to calculate VOC reactivity. These
include:

    1.  The flexibility to support high-resolution chemical mechanisms that are
       continually changing.
    2.  The ability to validate that the emissions modeling system is the same as used by
       other parties.
    3.  The ability to validate that new mechanisms are properly represented in the
       emissions modeling system.
    4.  Sufficient processing speed to allow for the development of multiple emission
       scenarios, fortaioderate to long  episodes, and potentially complex (large)
       chemical mechanisms.
    5.  Designed to be integrated with state-of-the-science meteorological models,
       photochemical grid models, and analysis tools.
    6.  Be reasonably easy to use and have a base of technical support for maintenance,
       technology transfer, and user training.

In this presentation these criteria are discussed in further detail in the context of the
Sparse Matrix Operator Kernel Emissions (SMOKE) modeling  system. SMOKE was
developed as a research prototype for high performance emissions processing under a
USEPA cooperative agreement. It has evolved into an operational emissions modeling
system under funding from various state and federal agencies. The current state of
SMOKE and other currently used emissions modeling/processing systems, and what is
needed for each of these systems to support reactivity calculation will be discussed.
                                    2-74

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                              . Environmental Programs
 Emissions Modeling Issues for
      Reactivity Calculations

  State and Status of the Sparse Matrix
  Operator Kernel Emissions (SMOKE)
           Modeling System

             Neil Wheeler
    North Carolina Supercomputing Center
         Environmental Programs
         Research Triangle Park, NC
	North Carolina Supercomputlng Center
   Emissions Modeling Issues

• Flexibility
• Validation
• Speed
• Integration
• Ease of Use
• Technical Support
                              . Environmental Programs
                         North Carolina Supercomputlng Center
                 2-75

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                               . Environmental Programs
            Flexibility
The flexibility to support high-resolution
      chemical mechanisms that are
          continually changing
                       . North Carolina Supercomputing Center
                               . Environmental Programs
      System Validation
The ability to validate that the emissions
 modeling system being used is the same
         as used by other parties
               	North Carolina Supercomputing Center


                2-76

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                             . Environmental Programs
   Mechanism Validation
     The ability to validate that new
 mechanisms are properly represented in
     the emissions modeling system
                      . North Carolina Supercomputing Center
                              . Environmental Programs
      Processing Speed
The need for sufficient processing speed
 to allow for the development of multiple
     scenarios, for moderate to long
    episodes, and potentially complex
      (large) chemical mechanisms
               	North Carolina Supercomputing Center


               2-77

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                             . Environmental Programs
          Integration
Designed to be integrated with state-of-
   the-science meteorological models,
    photochemical grid models, and
            analysis tools
                       North Carolina Supercomputlng Center
                             . Environmental Programs
 Ease of Use and Support
The system must be reasonably easy to
    use and have a base of technical
  support for maintenance, technology
       transfer, and user training
                    	North Carolina Supercomputlng Center


               2-78

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                                  . Environmental Programs
  Sparse Matrix Operator Kernel
         Emissions (SMOKE)
           Modeling System
                           . North Carolina Supercomputlng Center
                                  . Environmental Programs
         SMOKE - Concepts

 • Traditional Emissions Processing Paradigms
   - Self-contained records describing sources
   - Admirably suited to 1970's-vlntage machines with
     minuscule available memories and tape-only storage
   - Passing of redundant data
   - No exposed parallelism
 • Factor based tasks - linear matrix operations
 • Sparse matrices
 • Re-arrange the order of multiplications to
  avoid redundant  computations
 • Uses the Models-3/EDSS I/O API
 • Integrated within EDSS

	^	North Carolina Supercomputlng Center

                     2-79

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                                          . Environmental Programs
           SMOKE Sparse Matrices
Transformed
 Emissions
   OUTi
   OUTa
   OUTE
      Each column =
one model species, one grid  Inventory
 cell, or one control factor   Emissions
                           Si

                           Sa
                           SN
                                  North Carolina Supercomputing Center
                                          . Environmental Programs
              EPS 2.0 Processing Paradigm
             SMOKE Processing Paradigm
                                  North Carolina Supercomputing Center
                         2-80

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En
SMOKE Submodels and Dataf
A
?v:ONC
Land Use
Data

Meteorology
Data

Emissions
Inventories

L

Biogenic :
Submodel
/
MoMe /
Submodel ^
L
Area M
Submodeti /
//
Submodel J
	 I Time-Stepped
yfl Emissions \
( \
fe Matrices -^
7, 7
Time-Stepped ^
Layer Fractions
vironmental Programs
lows
Merge
•oeesscir::::
\
Model-Ready
Emissions
North Carolina Supercomputing Center
        Structure of SMOKE Submodels
                                        . Environmental Programs
Inventory
Data


Ifet*
Structuring

/

Vleteorology
Data

Profiles &
Xrefs

Source 1
Database |
MC.fJC
                                 North Carolina Supercomputing Center
                         2-81

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                                       Environmental Programs
            SMOKE Features

• Inputs: EPS 2.0 or EMS-95
• Outputs:
   - Models-3 (CMAQ) / EDSS (MAQSIP)
   - UAM-IV / UAM-V / CAMx
   - SAQM with converter
• Machine Independent I/O API (M-3/EDSS)
• Multi-day runs
• Approximately 30 times faster than EPS or
  EMS-95
• 70% less disk space than EMS-95
                             __ North Carolina Supercomputing Center
                                      . Environmental Programs
                  SMOKE
      Speed
  Disk Space
  SMOKE vs. EMS-95 on OTAG 1890
  IBM RS-6000 CPU and Wan-dock Time,
I
SMOKE vs. EMS-95 on OTAG 1990
      Disk Storage
                         CD
                         o
                                            •EMS-95
                                            OSMOKE
                               P«   PMdl)   604J
                              KWwrio        efts*
                              . North Carolina Supercomputing Center
                       2-82

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                                    . Environmental Programs
           Status of SMOKE
• Operational Prototype
• Validation
   - EMS-95(OTAG)
     EPS 2.0 (North Carolina)
     BEIS2
• Current Applications
     Season Model for Regional Air Quality (SMRAQ)
     North Carolina Regional and Urban Modeling
• Availability
     Publicly released February 1998
     http://envpro.ncsc.org/products/smoke
                             North Carolina Supercomputing Center
                                     Environmental Programs
       SMOKE - Future Needs
• Enhanced support for new species
• Enhanced sorting of profiles/cross references
• Run-Time Dimensioning
• Control-Related Enhancements
• Enhanced Error Handling
• Integration with a Chemical Mechansim
  Reader
• Enhanced Quality Assurance
• Improved User Interface
• Improved input format
• Integration with inventory development
                             . North Carolina Supetvomputlng Center
                     2-83

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                                 . Environmental Programs
Work Plans and Level of Effort
                          . North Carolina Supercomputlng Center
                                 . Environmental Programs
        Further Information

               Neil Wheeler
              (919)248-1819
            wheeler ©ncsc.org

           http://envpro.ncsc.org
        http://envpro.ncsc.org/EDSS/
   http://envpro.ncsc.org/products/smoke/

                           North Carolina Supercomputlng Center

                  2-84

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  Scientific and Operational Criteria
                   for the
 Use of Eulerian Models to Compute
                Reactivities
                    May 12, 1998

                     U.S. EPA
              Photochemical Reactivity Workshop
                 Regal University Hotel
                    Durham. NC
Harvey Jeffries
Environmental Sciences and Engineering
University of North Carolina
Chapel Hill, NC
 	-•< Operational Ov.-v;

Background
"Reactivity" is a sensitivity, or change in a system's
state relative to a change in the system's input.

It has been clearly established from theory and
experimental evidence that:
  The reactivity of an organic compound in the
  atmosphere is a strong function of both the
  compound's unique properties and the
  conditions of the ambient environment in which
  it is reacting.
Therefore, there is not a single reactivity per
compound, but instead a continuum of reactivities.
This same phenomenon prevents the direct
application of "smog chamber" reactivities to the
atmosphere.
                    2-85

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    Peak Ozone Sensitivity
11.2-H


| m

I 0.8
TJ
«3
00.6
Q.
Q.
«0.4-
o

I 0.2
 TO
        6 to 1 HC to NOx

        4 to 1 HC to NOx
    ni'«priki
      PAR
      ETH
              OLE  TOL  XYL  FORM  ALD2  MIX
                CB4 Model Species
                                   Harvey Jeffries
All VOCs Contribute To Os
   o
   £
   Q.
    Q.
    Q.
   O
   I
0.11

0.10

0.09

0.08

0.07

0.06

0.05

0.04

0.03

0.02

0.01

0.00

-0.01

-0.02
       | 6 to 1 HC to NQ,

       g3 4 to 1 HC to NQ,

       Trajectory Simulation
        jcoi
                       For 2% change in TOL
 \  •• ' Incr. Reactivity
Sum all  of TOL
organic   i ^~-
chemistry   :
                TOL
           ': PAR
         CO | PAR I OLE I XYL I ALD
          CH4  EtH  T^L HCHO
                      I Iriit | Dil"~|
                     Inor Emis Loss
                                   Harvey Jeffries
                  2-86

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 Cf.-v. •-<*•: .md Operational Cnu>n.-

Background, cont.

Such understanding raises questions about the use of
a "bright-line" test or about a "national exemption".
Basil Dimitriades described this problem as,
  All these methods of using the reactivity
  concept in regulatory organic emissions
  programs have varying merits and difficulties.
  Scientific issues associated with obtaining a
  valid, acceptably accurate measure of an
  organic compound's reactivity presents a
  common difficulty.
 -, .< :«?;-•- .jrto Operational CHU . >.*

 Background, cont.

 Given the newest national standards and goals,
 focusing only on role of VOCs in ozone formation is
 not acceptable.

 Instead, VOC reactivity needs to be expaned to
 include the atmospheric compositional effects that a
 VOC would have on:
 • Peak one-hour ozone and 8-hour ozone
 • PM2 5 formation
 • Regional Haze
 • HAPS formation
 • Nitrate deposition

 Conceptual Model of VOC reactivity shows complexity
                       2-87

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             Ci !••

Background, cont.
Previous efforts to deal with this complexity have
centered around trying to find "standard conditions"
which would ideally produce a "universal reactivity
scale", for example, manipulate ambient NOX
conditions, to produce maximum ozone response (the
MIR scale). To use these scales for policy, one must
argue their relevance to natural-use environments.

An alternative method  is to assess all impacts of a
real-world VOC emissions change scenario for a set
of well-simulated regional and urban conditions and
to include the VOC's projected use conditions.

Modern, community-based Eulerian Air Quality
Models can meet these requirements.
       Different Mechanisms.
        i^*^->—	 *  f\.		*_»•   *•»
             toluene IR Compared by Mecli

                 CB4 TOLD
               [  I CAL86 TOLD

               •• SAPRC90 ARO1
          E •'
                                         Harvey Jeffries
                       2-i

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       M85  Less Reactive
   Than lnd.Avg.Gaso5ine
    0.50
                                    0.50
oo
04-Sep-91 .
            8  9  10 11 12 13 14  15  16  17 18 19
        L.L.I.', I . I . I , I . I  , I , I , I . I . I .
        6  7  8  9  10 11 12 13 14 15  16  17  18 19

                HOURS,EOT

                                Harvey Jeffries
                ...But, Not
                                              o.so
                                              0.40
                £ °'30


                5
                £ 0.20
                                             b
                                              0.10
                                              0.00
                                                                         I I I I I
                                                       I ' I ' I ' I ' I ' I ' I ' I
                                                      . 2.04 ppmC SynUrb+HCHO / SynM85 03-Sep-91
                                                                              ,0.50
                                                 —........2.04 ppmC SynUrb+HCHO / SynlAG
                                                - J.40
                                                — NO
                                                                              0.00
                                                567
                             10 11 12 13 14  15  16  17 18 19

                             HOURS, EOT
                                              100
                                             E
                                             >-,
                                             sf
                                             I
                                                S  6  7  8 9 10 11 12  13  14  15 16 17 18 19
                             HOURS, EOT
                                             Harvey Jeffries

-------
Conceptual Model of Organic Trace Gas Reactivity
             -' time •'
                                               /••**-, •-
                                               C Property/
                  / Xsect
                  X Q Yield
       Organic Trace Gases

       Abstract Property

       Process Rates

       Concentrations
                                   .'Property,'
   Purpose
   To identify and describe the attributes of a modeling
   system that can compute a VOC's (or a mixture of
   VOCs') impacts on atmospheric composition.

   To compare these attributes with those of existing
   modeling systems.

   To identify significant work that needs to be done to
   use this modeling system to evaluate possible
   strategies that incorporate VOC reactivity.
                           2-90

-------
     im! Operational Criirna
Components

     Simulate Target VOC's Chemistry

     Simulate Target VOC's Emissions
          (also Replaced VOC's Emissions)

     Simulate Environments including
          Target VOC

     Evaluate Atm. Compositional
          Changes

I will discuss each of these in detail.
 !••;!(' six! Operational Criteria

Simulate VOC Chemistry

Ail reactivity calculations require the use a chemical
simulation model to establish the radical and
chemical environment in which the VOC reacts.

If the reaction mechanism and reaction parameters for
the target VOC are not available, a kinetics and
chamber study must be undertaken to produce these
items. This would be the responsibility of the party
wanting to assess the reactivity of the target VOC.

This target VOC chemistry must be integrated with a
chemical reaction mechanism for the regional and
urban atmospheric environment.

Particle and HAPS formation are new data
requirements.
     - -.'.! ' ietr-t-jit
                    2-91

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  • :JM-', anil Operational Cniet ia

Simulate VOC Emissions

To have accurate estimates of a target VOC's effects
on atmospheric composition, we must have a
accurate simulation of the emissions of the VOC,
resolved in both space and time within the test
domains. This would also be the responsibility of the
party wanting to assess the reactivity of the target
VOC.

Further, the expected growth in emissions over the
requested deferment  period must be provided. In
addition, the decrease in any displaced emissions
already in the existing base and future case model
inventories must be specified.
'. H-jstiJft. and Operational Crilrrta

Simulate Environments

Eulerian models permit our most advanced and most
accurate simulations of urban, regional, and global
atmospheric chemical environments.

For reactivity assessments, we want to perform "best
operational practice" model simulations of 3 to 5
"well-simulated" and "well-understood" regional and
urban domain test cases. Ideally, a test case that
represents a significant market for the target VOC
would be included.

The responsibility for the creation and maintenance of
these test cases rests with the EPA and the States.
States and industries share responsibility to run tests.
                      2-92

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         rational C>
Evaluate Simulation Results

A variety of ways exist to assess atmospheric
compositional impacts.  I prefer those that indicate
the entire range of results, e.g., changes in frequency
of predicted concentrations. (Need some example
results to test meaningful ways of analysis).

The impact could be classified as:
   always negative impact outcomes
   non-detectable outcomes
   always positive impact outcomes, and
   mixture of outcomes.
      UAM Surface Cell Os Frequency Distribution

                       One-hour at Os peak, 625 total cells
                    100% Std Gasoline Vehicles
  o o o  o o
             0000
                              9CDCMIDO900CMI0O
                                SO) O O. »-»-»- CM  CM O
                                P T T *"^ *"!*";
                           oooooo'ooo'ooo
                    '? Ozone interval, ppm
                       2-93

-------
         UAM Surface Cell Oa Frequency Distribution
  eo     	JB       One-hour at O3peak7625 total cells
                                    100% Nat Gas Vehicles
                                          100% Std Gasoline Vehicles
                  ooooooooooo
                              Ozone Interval, ppm
nj

0)
£
C

-------
          •;.(:• attona! C- •< >
  Evaluate Results, cont.

  For always negative outcomes, the "proposed use"
  should not be permitted and the VOC should be
  controlled.

  For non-detectable and always positive outcomes, the
  "proposed use" should be permitted for a renewable,
  fixed-time period.

  For a mixture of outcomes, the "proposed use" might
  be permitted for a renewable, fixed-time period, if the
  adverse effects are "tolerably small" compared to the
  costs and other societal benefits.
Community Modeling System for Reactivity
EPA/States
                                             Research


                                           EPA/Slates
                   onirounify
                   Modeling's
                   ISystem
                            cnemlcal
                            reaction
                            echanism, uses
                                     chemistry ( EPA/StateS
                                     mechanism
                                       Research
                Results
                          2-95

-------
 •   ! .  an,!- Operalional


Work  Needed

Major Research Topics

   Fundamental VOC chemistry, target VOC chemistry, analytical
   methods, synthesis of products for further testing, better
   coordinated observations for challenging models, ambient
   measurement of VOC products.

Major Modeling System Improvements
   Rapid emissions processing system, sensitivity computational
   subsystem, reactivity results display and analysis system.

Major Modeling Data Set Needs
   Nested-grid, regional and urban emissions inventories, nested-grid
   regional and urban meteorological scenarios.

Education and Technology Transfer Needs
   Full educational and reactivity modeling technology transfer
   package,  support for a Community Modeling User's Group.
•£
o
MSIS-I^U-SI  >
*amjji2jiij
« —  
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"INCREMENTAL REACTIVITY FOR THE PAINT
                 INDUSTRY"
                PRESENTATION TO
EPA PHOTOCHEMICAL REACTIVITY WORKSHOP
                  May 12-14, 1998

               Durham, North Carolina
                       By

              Fdward D Edwards. Ownership

         Robert Wendoll. Director of Environmental A/fairs

          DUNN-EDWARDS CORPORATION
                CLEAN AIR ACT 1990

                    SECTION 183(e)

    (2)  STUDY AND REPORT —

         (A) STUDY.—The Administrator shall conduct a
study of the emissions of volatile organic compounds into the
ambient air from consumer and commercial products (or any
combination thereof) in order to—

         (i)  determine their potential to contribute to ozone
levels which violate the  national ambient air quality standard
for ozone; and...
                                                               REQUIREMENTS OF 183(e

                                                                   1.   Ambient air validity
        2.   Contribution to ozone levels that violate the
            iNAAQS

                 A. Includes from 80 ppbv O3 and up

                 B. Includes ambient availability, not just
                    content

        3.   Determine potential

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         (3)
                     CLEAN AIR ACT 1990
                         SECTION 183(e)
         REGULATIONS TO REQUIRE EMISSION
         REDUCTIONS —
to
         (A) IN.GENERAL.—Upon submission of the final
report under paragraph (2), the Administrator shall list those
categories of consumer or commercial products that the
Administrator determines, based on the study, account for at
least 80 percent of the VOC emissions, on a reactivity-adjusted
basis, from consumer or commercial products in areas that
violate the NAAQS for ozone.
         COMMENTS:

             This section requires analysis of regulations on the
     same reactivity adjusted basis that matches the study.
       OZONE FORMATION POTENTIAL OF
                   VARIOUS VOCs


A useful definition of reactivity is that of incremental reactivity,
defined as the amount of ozone formed per unit amount (as
carbon) of VOC added to a VOC mixture representative of
conditions in urban and rural areas in a given air mass (Dodge,
1984; Carter and Atkinson, 1987, 1989b; Carter, 1991),
                                                                            Incremental reactivity  =   &[ozone]
                                                                                                       AfVOCJ
where Afozone] is the change in the amount of ozone formed as
a result of the change in the amount of organic present, A[VOC]
(note that Carter and Atkinson [1989b] used the quantity
A[ozone]-[NO]) rather than A[ozone] under conditions where
the maximum ozone was not attained and NO was not fully
consumed). This concept of incremental reactivity corresponds
closely to control strategy conditions, in that the effects of
reducing the emission of a VOC or group of VOCs, or of
replacing a VOC or group of VOCs with other VOCs, on the
ozone-forming potential of complex mixture of VOC emissions
are simulated.
                                                                    —Source: Rethinking the Ozone Problem in Urban and Regional Air Pollution,
                                                                            A Report to Congress, 1992, The National Academy of Sciences, pps.
                                                                            153-154

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 ATMOSPHERIC CHEMISTRY
                                                            155
TABLE 5-4  Calculated Incremental Reactivities of CO and Selected VOCs
   as a Function of the VOC/NO, Ratio for an Eight-Component VOC Mix
   and Low-Dilution Conditions
+ 11.0-,
VOC/NO,, ppbC/ppb
Compound
Carbon monoxide
Ethane
n-Butane
/i-Octane
Ethene
Propene
omj-2-Butene
Benzene
Toluene
m-Xylene
Formaldehyde
Acetaldehyde
Benzaldehyde
Methanol
Ethanol
Urban mix*
4
0.011
0.024
0.10
0.063
0.85
1.23
1.42
0.033
0.26
0.98
2.42
134
-0.11
0.12
0.18
0.41
8
0.022
0.041
0.16
0.12
0.90
1.03
0.97
0.033
0.16
0.63
1.20
0.33
-0.27
0.17
0.22
032
16
0.012
0.013
0.069
0.027
0.33
0.39
031
-0.002
-0.036
0.091
032
0.29
-0.40
0.066
0.065
0.08S
40
0.005
0.007
0.019
-0.031
0.14
0.14
0054
-0.002
-0.051
-0.025
0.051
0.098
-0.40
0.029
0.006
0.011
  "Eight-component VOC mix used to simulate VOC emissions in an urban
area in the calculations. Surrogate composition, in units of ppb compound per
ppbC surrogate, was ethcne, 0.025; propene, 0.0167; /i-butane, 0.0375; n-pcn-
tane, 0.0400; isooctane, 0.01S8; toluene, 0.0179; m-xylene, 0.0156; formalde-
hyde, 0.0375; and inert constituents, 0.113.
  Source:  Adapted from Carter and Atkinson (1989b).
                                                                        fl—
                                                                        7-
                                                                        .6-
                                                                  AVOC
                                                                        .3-
                                                                        2-
          Calculated  Incremental  Reactivities
                       AO,
                      AVOC
                               at 40 ppbV NOX  (in mole units)
                                           Ethene     — • — • —

                                           Toluene    ------

                                           m-Xylene   —=—

                                           Ethanol    	

                                           Urban mix  ————
                10
                            20
                                 VOC
                                 NOX

                Source Adapted from Carter and Atkinson (1989)
                From Rethinking the Ozone Problem in Urban and Regional Air Pollution

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                                                                                         Isopleth Lines - Ozone Production Rate In ppbv/nr
            Production of O3 as function of Nox for 3 levels of VOC's

            Slaflelbach and Neflel [1997]
            >s adapted from StUlmtn el aJ [1990]
U)
          0
     10
NOx [ppbV]
15
20
            For Incremental Reactivity,

            We need to look at both slopes and the transition area

            Species data must be from ambient air shed chamber work

            This yields production and loss as incremental reactivity,
            not mechanistic reactivity
                                                                                     0.01
                                                                                                    1            10

                                                                                                          Propy-Equiv (ppbC)
                                                                                                                                           1.0CO
                                 Fig.  16.  Summary of hydrocarbon/NO^ regimes. The four rect-
                               angles indicate the typical total [Propy-Equiv]surf and NO, concen-
                               tration  ranges observed at I. urban/suburban sites; II, rural sites in
                               the eastern United States; III. remote sites in the tropical forests of
                               Brazil;  and IV, remote sites in the marine boundary layer. Isopleth
                               lines are used to indicate model-calculated  net rates  of ozone
                               photochemical production (in units of ppbv per hour) at midday as a
                               function of assumed NO, and propylene concentrations. The cal-
                               culations were carried out using the photochemical box model and
                               methodology described by  Chameides tl al. [1987] with rate con-
                               stants from Gery el al. [1989] and DeMore et al. [1990]. The model
                               adopted a temperature of 290 K, a dew point of 285 K, a solar zenith
                               angle of 30°, a CO concentration of 85 ppbv, a CH4 concentration of
                               1.85 ppmv, and an Oj concentration of 25 ppbv. The shaded area in
                               the figure denotes  the concentration regions for which photochem-
                               ical processes were calculated to produce a net loss of ozone.

-------
 Suggested NOX levels for Incremental Reactivities
      Chamber  Studies Simulating Ambient Air
001
  0.00
             050
                                   1.50
                                              2 00
                                                         250
                         VOC (ppmC)
   1 The dotted lines indicate the following NO, levels: .001, 005. 01. 02, & 04
            INCREMENTAL REACTIVITY
 1.   Can reasonably simulate ambient air with appropriate
     chamber work.

 2.   Is based upon measured ozone forming potential of VOCs
     in simulated ambient air.

 3.   Determines a VOC's "contribution to levels that violate the
     NAAQS" for all ozone levels required by NAAQS starting
     at 80 ppbv (8-hour average).

4.   Is speciated.

5.   Can validate the slopes of ozone isopleths generated by SIP
     model.

6.   Can be used to validate a SIP modeling process that
     simulates attainment at two points rather than the current
     one point method.

7.   Can distinguish between naturally clean air  and ozone
     attainment that results from VOC reductions only
     (important to determining ozone  transport potential).

8.   Provides BRIGHT LINE regulatory distinction by VOC
     species by air shed.
   Source FW. Lurmann. Sonoma Technology. Santa Rosa. Calif. (1990)
   From Rethinking the Ozone Problem in Urban and Regional Air Pollution. Figure 6-2 page 171

-------
o\
 9.   Provides PALE LINE regulatory distinction by VOC
     species by air shed to reduce overall reactivity.

 10.  Provides improved graphical basis for decision between
     VOC + NOX controls vs. NOX only controls.

 11.  Can be validated for all air sheds.

 12.  Provides for seasonal control strategies through
     temperature and sunlight variables.

 13.  Provides for speciated VOC regulation that declines as
     reactivities reach zero or become negative.

 14.  Reduces the discrepancy between container VOC content
     and reactive emissions to allow one adjustment factor by
     product type.

15.  Fits into a CTG framework.

16.  Is better than a preemptive Federal approach.
        PROPOSAL AND REQUIREMENTS

1.   Requires a new large chamber available to
    Government, Industry and Academia

2.   Chamber to be built that meets the requirements of the
    CAA of 1990 Section 183(e)

3.   A reactivity engine and a peak 1 hr/ 8 hr simulator that
    are in public domain and the best currently available

4.   Support by one or more major regional or local Air
    Management Districts

5.   Support by Paint Companies affected by the District(s)

6.   A peer reviewed process developed under NARSTO

7.   Joint Funding by Districts, Government and Industry

8.   EPA incorporate Incremental Reactivity into the SIP
    process

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                CLEAN AIR ACT 1990

                    SECTION 183(e)
    (3)  REGULATIONS TO REQUIRE EMISSION
         REDUCTIONS.—
         (C) USE OF CTGS.—For any consumer or
commercial product the Administer may issue control
techniques guidelines under this Act in lieu of regulations
required under subparagraph (A) if the Administrator
determines that such guidance will be  substantially as effective
as regulations in reducing emissions of volatile organic
compounds which contribute to ozone levels in areas which
violate the national ambient air quality standard for ozone.
    COMMENTS:

         Incremental reactivity, with a CTG is far more
effective in reducing ozone for each air shed than a national
mass-based regulation.

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                        EPA Photochemical Reactivity Workshop
                                   May 12-14, 1998
                                Durham, North Carolina
Presenter
The Solvents Council of the Chemical Manufacturers Association. Jonathan Kurland of
Union Carbide Corporation will make the presentation on behalf of the Solvents Council.

Title of Presentation

CMA Research Initiatives

Abstract

The Chemical Manufacturers Association (CMA) is a Washington D.C. based trade
association with over 200 member companies that collectively produce approximately 90
percent of the basic industrial chemicals produced in the United States.  The CMA Solvents
Council represents the major U.S. manufacturers of hydrocarbon and oxygenated organic
sol vents. -

The Solvents Council recognizes (1) the need to better understand the role that individual
ozone precursors  (including solvents) play in forming ground-level ozone and (2) the
potential benefits  of designing regulatory systems that take into account differences in the
ozone-forming potential of different precursors.  For this reason, the Council has been
involved in both research and public policy discussions about the concept of photochemical
reactivity.

This presentation will briefly summarize the activities of the Council in both the research and
public policy arenas, including the following:

•      The work being sponsored by the CMA Ethylene Glycol Ether and Propylene Glycol
       Ether Panels to examine the kinetics and photochemical oxidation mechanism of
       glycol ethers.

•      The Council's support for the HONO work being conducted by Dr. William Carter.

•      The Council's perspective on the Reactivity Research Advisory Committee (RRAC)
       established by the California Air Resources Board (CARB).

•      The approach developed by the Council and submitted to CARB for taking uncertainty
       into account in reactivity-based programs.
       The following companies are members of the Solvents Council: ARCO Chemical
       Company; BP Chemicals, Inc.; Celanese Ltd;  The Dow Chemical Company; Eastman
       Chemical Company; Exxon Chemical Company; Phillips Chemical Company; Shell
       Chemical Company; Sun Company; Union Carbide Corporation.
                                        3-8

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    CMA Research Initiatives
              Barbara Francis
      Chemical Manufacturers Association
             Jonathan Kurland
          Union Carbide Corporation

      EPA Photochemical Reactivity Workshop
                May 13, 1998
Chemical Manufacturers Association
                (CMA)
  Trade Association
  Over 200 member companies
  • Collectively produce approximately 90% of
    the basic industrial chemicals produced in
    the U.S.
                   3-9

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        Solvents Council

Represents the major U. S. producers of
hydrocarbon and oxygenated solvents
Addresses environmental issues that
affect both users and producers
  Solvents Council Members
ARCO Chemical Company
BP Chemicals, Inc.
Celanese Ltd.
Dow Chemical Company
Eastman Chemical Company
Exxon Chemical Company
Phillips Petroleum Company
Shell Chemical Company
Sun Company
Union Carbide Corporation
                  3-10

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Atmospheric Reactivity Task Group
 Includes both scientists and policy
 specialists
 Active in:
  • Policy issues
  • Research
          Policy Activities
                                 *

 Participates in developing a regulatory
 framework for reactivity
 Provided comments  to CARB for dealing
 with the uncertainty in MIR values in
 regulations
 Presented an alternative model for
 categorizing complex hydrocarbons, such as
 mineral spirits, naphthas, Stoddard Solvent,
 etc.
                   3-11

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         Research Interests
  GARB Reactivity Research Advisory
  Committee
  Chemical Mechanism Studies
  • Reactivity studies on glycol ethers
  • Support for better reactivity estimation
    methods
  Environmental fate
Reactivity Research Advisory Committee
  Participation on RRAC of the California EPA Air
  Resources Board (CARB)
  • Choice of significant compounds for MIR
    determination by Dr. Carter under his
    contract with CARB
  • Advice on prioritization of CARB research
  • Support for MONO work by Dr. Carter
                  3-12

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  Ethylene Glycol Ether and Propylene Glycol Ether Panels
                    Research Activity
Kinetics and Mechanism of Photochemical Oxidation
of Glycol Ethers
   • 2-Butoxyethanol and 1-Methoxy-2-propanol
   • Work by Dr. Roger Atkinson
       - Kinetics and products of oxidation
       - koH and products of the reaction of the ethers with HO- in
        air with NOx
       - Soon to be published
   • Work by Dr. William P. L Carter
       - Smog chamber runs
       - Mechanism and kinetics derived from Atkinson's studies
       - Calculation of MIRs
  Principal Factors Determining the MIR
   The rate of reaction with HO-
   •  If the compound is unreactive this is the dominant term. Very
      reactive compounds will be completely consumed.
   Direct reactivity
   •  The more oxidations of NO to NO2 by peroxy radicals, the
      more ozone production
   Effect on HO- concentration
   •  Compounds that generate free radicals by photolysis will
      increase the concentration.
   •  Reactions of alkylperoxy radicals with NO to make alkyl
      nitrates instead of NO2 and RO- reduce the  concentration.
   The effect on NOx concentration
   •  Formation of alkyl nitrates removes NOx
                         3-13

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  Ethylene Glycol Ether and Propylene Glycol Ether Panels
                    Research Activity
  Determination of Nitrate Yields in Photo oxidation
  Work to be done by Dr. Paul Shepson at Purdue University
  Oxidation of ppm levels of glycol ethers in air with NOx
   • PTFE-coated chamber
   • Controlled hydroxyl radical source by photochemical initiation
  Determination of nitrate yields by
   •  gas chromatography
   •  pyrolysis of RONO2 to RO and NO2
   •  determination of N02 by chemiluminescence
      - no calibration needed to quantify molar yield of nitrate
      - speciation requires further work
          •  GC/MS or synthesis of authentic samples
HONO Work by Dr.  William P. L. Carter
  Purpose:  To support better estimation of MIRs when direct
  experimental data is lacking, and avoid use of arbitrary
  default values
  Objective:  Obtain direct reactivities to make possible a
  scheme for estimating MIR values that considers by SAR
  or other means koH, direct reactivity and  indirect reactivity.
   • Direct reactivity is the NO to NO2 conversions during
     oxidation of a compound.  The current Carter scheme for
     upper limit MIRs lumps the direct and indirect reactivity.
   • HONO yields HO  and NO  upon photolysis.
   • In a flow system, radical generation loses its importance and
     the direct reactivity can be determined.
                         3-14

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          Related Work
Other CMA Panels
 • sponsor chemical-specific work
Individual members of CMA acting
independently
 • atmospheric chemistry and kinetics of
  specific chemicals
  Other Interests Areas of CMA
          Environmental Fate
Low-vapor-pressure (LVP) Compounds
 • Volatility as well as reactivity influences
  ozone formation.
Down-the-drain Factor
 • The EPA inventory of consumer product
  emissions recognizes that some VOC
  largely go into wastewater and are
  biodegraded at a POTW.
                3-15

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            Summary
CMA is committed to involvement in these
issues.
CMA is active in reactivity research and
policy development.
CMA is interested in related issues.
We want to play an active role in future
activities.
       Acknowledgments
             CMA Staff

  Atmospheric Reactivity Task Group
                3-16

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        CSMA Position on  the
        Importance of Relative
        Reactivity

                     D. Douglas Fratz
               Director of Scientific Affairs
                   Chemical Specialties
                Manufacturers Association
                     Washington, DC
                       Presented at (lie
      EPA Photochemical Reactivity Workshop
                    May 12-14,1998
               Durham, North Carolina
Good morning. I am Doug Fratz, Director of Scientific Affairs for the Chemical
Specialties Manufacturers Association in Washington. DC. CSMA represents
manufacturers of formulated chemical products for household, institutional.
commercial and industrial consumers. These products include cleaners.
disinfectants, pesticides, polishes, automotive products, and aerosols of all types
I'd like to talk to you today about CSMA's positions on the importance ol
relative reactivity to ozone attainment strategies.
                                                                         Importance of Reactivity
       «••  History of CMSA Support
       **•  Importance to Ozone Attainment
        Strategies
       >••  CSMA Research on Reactivity
       **•  Future Research Needs
In presenting our current positions. I'll also review the history of our industry's
support tor reactivity: the many ways in which reactivity is important to cost-
effective ozone attainment; some studies CSMA has sponsored over the past 10
years, and some concepts for future research that we believe is still needed

-------
oo
                History of CSMA Support

                ?•-  1988 - CARB Consumer Products
                  Program
                »*•  1990 - 183(e) of Clean Air Act
                »•  1991 - CARB/South Coast Conference,
                 Irvine
               >*-  1993 - Support for VOC Exemptions
               >*•  1994 - California SIP Hearings
       We began urging the consideration of reactivity in 19X8 in relation to ihe
       California ARB regulations on consumer products, which began wnh underarm
       products. We also helped develop Section I83(e) of the Clean Air Act of I WO
       on Consumer & Commercial Products, a section which contains requirements lor
       EPA lo consider reactivity in relation to those products. 1 gave  a talk at the 1991
       Irvine conference on reactivity, supporting the consideration of reactivity for
       consumer products. Around 1993, we began supporting EPA exemptions for
       negligibly reactive VOCs. urging that standard criteria and protocols be
       promulgated. In 1994, we were successful in getting the California Air
       Resources Board to include the potential to consider reactivity in the consumer
       products element of the State Implementation Plan.
       History of CSMA Support

       »  1995 - EPA Report to Congress -
         Chapter 3
       »•  1996 - Reactivity Principles to CARB
       »  1997 - Proposed CARB Reactivity-
         Based Compliance
       »•  1998 - Proposed CARB Regulatory
         Language
In 1995. EPA's Report to congress on Consumer & Commercial Products was
finally completed. We worked closely with EPA to assure that they met their
statutory requirements lo consider reactivity under IK3(e). Chapter 3 of the
report and the regulatory prioritization process EPA conducted met those
mandates. By 1996. we were working again with California on reactivity.
putting forth the principles we believed were essential to establishing reactivity-
based compliance options for consumer products, as allowed in the SIP. Since
1997, we have also participated in ARB's Reactivity Research Advisory
Committee. In 1997. we outlined the specific elements of a consumer products
reactivity program, and this year  we have developed specific draft regulatory
language upon which a voluntary reactivity compliance option can be based.

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         CSMA Policy Positions
             »-EPA VOC Exemptions Program
                •   Ethane Criteria
                •   Mass-Based Criteria
                •   Standard Criteria & Procedures
                •   Expeditious Review
Now. I'd like in review our current positions on leaciivnv related r,sues  VW
support retaining ethane as the standard lor exernritm;' VOCs as /i<-i'li;ribly
reactive There is no need to reproduce the 1977 exprimii'iii ih.it  (iiovides iln-
basis lor choosing ethane  We may need to inventory some i-.vm|iii-d \'()('•> loi
use in modeling, bui there is no need in.subject idem toconiiols  Wi- lavoi
ma.vs-ba.sed, as opposed  to mole-based, comparisons lor VfX' exemptions  All
ozone attainment inventories, controls and strategies to date have  hern mass-
based. We support EPA developing standard criteria and procedures lor
exemptions. And we support expeditious reviews of exemption pennons  Our
industry ha.s relied on these exemptions to meet regulatory siandanlv and they
arr i-ssential to our meeting the o/.onr ri-diK non goals brmj' pl.i> >-il upon us
        CSMA Policy Positions
        <*•  Consideration of Relative Reactivity in
          Ozone Attainment
           •  Alternative to Mass-Reduction
           •  Regulatory Prioritization
           •  Increased Cost-Effectiveness
           •  Tost Effectiveness Based on Cost Per
             Ozone Reduction Benefits
We- belirvr ili.n consideration ol relative reactivity is essential in mjny other
aspects .is well  In particular, u is an important alternative 10 simple mass basic
V(K' rrdui nons We support allowing regulated parties to use reactivity
reductions in painally or lully meet their VOC mass reduction goals  Tins
would result in increased cusi-ettectiveness in moving toward ozone reduction
goals  Finally, we .support all regulatory analyses of ozone attainment options
being based on cost per ozone reductions, not precursor reductions  This would
[mi all V(X.' controls, and even NOx controls, on an even playing lield

-------
u>
rO
O
CSMA Policy Positions
  Reactivity Positions for
 Consumer Products
 .  Principles
       -  Optional
       - Sound Science/Stable/Flexible
       - Cost Effective/Efficacy
        Maintained
       - Existing Provisions/Enforceable
     These are the principles we proposed in California in 1996. Reactivity
     considerations must be optional, to allow companies to determine whether
     reactivity or mass-reductions are more cost-effective.  Our VOOs already are of
     low reactivity. Mandatory reductions would not make sense.  The reactivity
     values assigned to VOCs must be based on sound science, and be both stable (so
     manufacturers will use them) and flexible (to encourage continued research).
     The program must encourage cost-effectiveness, and allow manufacturers to
     make products that are both safe and effective. We believe that all of the
     provisions related to the mass-based standards, such as the various exemptions.
     must be maintained. Obviously, the program must also be enforceable.
CSMA Policy Positions

>•- Reactivity Positions for
  Consumer Products
   • Policy Position
      •  Optional
      •  Product-By-Product Ozone Equivalence
      •  Maintain Exemptions
      •  Scientifically Determined MIRs
      •  All Products
                                                                   We reiierated these same positions in our updated policy positions over the past
                                                                   year, and added a few more specific ones. In particular, we believe the most
                                                                   sound program would assure product-by-product equivalence of ozone impact.
                                                                   or equivalence by groups of products. We would like to see a program that
                                                                   could benefit all consumer products, and be adapted for other industries as well.

-------
to
              CSMA Consumer Products
                -  Reactivity-Based Compliance Option
                and Credit Program
                 •   Equivalent Ozone Impact on Product-By-
                   Product Basis
                 •   Official List of Reliable Ml Rs
                 •   Over-Reduction Credits Transferable
                   between Products
       This year, we developed a specific proposal tor a reactiviiy-based. voluniary
       compliance option for consumer products in California. Our program is a
       relatively simple one. It is designed to assure ozone equivalence on a product-
       by-product basis.  It would be based on a list of VOCs with reliable MIR
       values.  VOCs without reliable MIRs would not be allowed to be traded, and
       have to meet mass-reduction goals. We are proposing, however, that excess
       reductions credits for one product be usable for products which can't meet their
       reduction goals. This adds further flexibility. We are not proposing any
       complex schemes to address uncertainty. Only reliable MIRs would be used.
       What is often overlooked is that mass-based reductions also demonstrate high
       uncertainties regarding ozone reduction.  In consumer products, we already have
       generally minimized VOC content for cost reasons. Mass reduction
       reformulations usually require different VOCs. These might be 3 times more
       reactive, or 3 times less reactive, than those they replace. The We uncertainix
       for reactivity is small when compared to this 3(X)"r level nt uncertainty. Bui
       even the.se larte uncertainties will even out over Hills ot products.
         CSMA Research on Reactivity
          •  1988 - UAM Study on Underarm
          Products in California
          -  1993 - UAM Study on Pesticides,
          Disinfectants, Air Fresheners in New
          York
          1997 - Impact of Consumer Products on
          California Air Quality
Now. I'd like to review some of the reactivity studies we've done over the past
decade  All have been modeling studies on the effects of consumer product
emissions on ozone formation. The three studies are: a  19X8 study on underarm
products in California; a 1993 study on pesticides, disinfectants and air fresheners
in New York: and. a study completed just last year entitled. "Impact of Consumer
Products on California Air Quality"  All of the modeling in these studies was
done by Dr. Gary Whitten.

-------
UJ
K)
ro
 1988 UAM Study


»•• Underarm Products in
  California South Coast AQMD
   .   0.06% VOC Inventory
   •  No Measurable Impact
   •  0.2ppb
   •  One Third as Reactive
       The first study, way back in I98X, looked a! the impact of underarm
       untiperspirants and deodorants in the Los Angeles basin. These products
       represent only about 0.06% of their VOC inventory, and are mostly composed ol
       ethanol. simple hydrocarbons, and other low-reactivity VOCs. The modeling
       showed that even eliminating all emissions would have no measurable impact on
       peak ozone—less than 0.2ppb, primarily because of their low reactivity.  This
       study may have been done before its time.  It was spectacularly unsuccessful in
       convincing California not to regulate. Underarm products remain targeted for an
       80%  reduction that our industry still hasn't figured out how to meet.
                                                                                    1993 UAM Study

                                                                                    >*•  Pesticides, Disinfectants, Air Fresheners
                                                                                      New York City Metropolitan Area
.  0.1% Ozone-1990
.  0.25% Ozone -1997
•  No Measurable Impact
•  One Third as Reactive
                                                              We are not un industry that gives up. however, and our second study was more
                                                              successful with similar findings. This time, we looked at household pesticides.
                                                              disinfectant and air fresheners in New York City. The ozone contribution here
                                                              was O.\c'f in 1990.  0.25% in 2(X)7. Again, the low reactivity contributed to the
                                                              unmeasurable ozone impact. This study convinced New York to promulgate
                                                              only reasonable standards for these products.

-------
U)
NJ
1997 Study - Sierra Research

'•-"Impact of Consumer Products on
  California's Air Quality"

   •  Inventory

   •  MIR-Weighted Inventory

   •  UAM Sensitivity Runs
      Our final study, completed last year by Sierra Research, was a multi-phase study
      looking at the inventories and reduction goals of the IW4 C.ililorma SIP The
      study included correcting the VOC emissions inventory tor consumer products;
      creating a reactivity-weighted inventory for aj] VOC sources: and. dome Urban
      Airshed Modeling to determine the ozone benefits of the additional VOC
      reductions for which consumer products were targeted in the SIP. Both South
      Coast and Sacramento UAM runs were done.
1997 Sierra Research Study

>•• Consumer Products Inventory
  corrections

   .   Non-emitted VOCs

   •   Survey Errors

   •   Industrial/Agricultural Products
                                                                 The inventory corrections for consumer products included removing non-
                                                                 emitted VOCs. most of which were those biodegraded in waste water treatment.
                                                                 This correction was made by EPA in its consumer and commercial products
                                                                 inventory, but has never been made by California. The study also corrected
                                                                 errors in consumer products survey data, mostly non-VOC ingredients that were
                                                                 misreported as VOCs. And, products that were industrial, agricultural, or
                                                                 otherwise double-counted in other VOC inventories were removed. The result
                                                                 was a change in the totaJ VOC emissions inventory for consumer products in
                                                                 California from 265 tons/day to less than 215 tons/day.

-------
       1997 Sierra Research Study

       >•• MIR-Weighting of Inventory

          •  Specialization of Inventory

          •  MIR Estimates

          •  Less Than One Half as Reactive
      MIR Values for Consumer
      Products and Other VOC
      Sources
                        2.6  1.3
                                     D AitraKt fur
                                       SutTumtniti H/II
                                       Consumer Products
                                     DAifr»K« for South
                                       Coast »/« Consumer
                                       Products
                                     QSitrra Kstinmlr
                                       Consumer Products
The reactivity-weighting was done tor all VOC .sources in the IW-4 SIP
inventory. MIR estimates were used to create an MIR-wea'hied inventory. The
consumer products VOC inventory was found to be less than halt'as reactive as
the overall inventory.
This slide shows how consumer product reactivity compares to the overall 1990
VOC inventory in California. Consumer products emissions average an MIR ot
1.3. The average for other emissions was found to be 2.6 in South Coast and 3.0
in Sacramento.

-------
        1990  Sacramento VOC
        Emission Inventory
A3
45
40
22
li
12
II
10
J

4'
* ',..



'. -A


&..
«# ,
->•'
Toul - 2 1 y loru/diy

• On-RMdExhuut
D On-Rued Ev»por»»k
•$o)<*MUn
• OffRtmd
• OUIYodAMktf
OCeaimiHQo
OCoMQnMr Product*
QMlKProtnc

This slide, which I hope you can read, shows the 1990 Sacramento inventory by
VOC tonnage. The emissions inventory is dominated by on-mad exluust. on-
road evaporation, solvent use. and off-road emissions.  Smaller, but still
seemingly significant contributions occur form oil production, combustion.
consumer products, miscellaneous processes, and industrial processes
       1990 Sacramento Ozone
       Forming Potential Inventory
                                                                        273

                                                                         HX

                                                                         X4

                                                                         71

                                                                         54

                                                                         32

                                                                         IK
                                                                         15

                                                                          5
                                       lOn-Koid
































odl c 648 lons/diy
aorr-Raid
• On-Koid EMporilion
• Sohf nl I ir
Q M he Proctisri
OOil Prod & Mkle
OConsumrr Products
Dlndo>lri.l I'rncr"








Here is lhat same Sacramento inventory that is MIR-weighted On-road exhaust
now dominates the ozone production inventory, with oft-road also increasing its
contribution All of the other sources, including consumer products, now
represent a much  smaller portion of the inventory, and can be seen to be
makjng a much smaller contribution to ozone formation.

-------
u>
to
        1990  South Coast VOC
        Emissions Inventory
         43V
         293
         261
         ISO
         110

         84
         84
         S3
         19






•
^™























• On-Koud KxhmiM
• On-Roiicl Kvuporutioii
• OfTKuttd
QMiw: TrtHTt-ss
DCoiviunter I'ruducLs
OlnHiisirUIIViHirxs
D C!omhiistiiin

                   TuUl« 1493 lons/d.y
Here is the same inventory, this time for South Coast.  Once again, on a VOC
tonnage basis, on-road exhaust is closely followed by solvent use. on-roud
evaporation, and off-road, with others making smaller contributions to VOC
emissions.
                                                                                        1990 South Coast Ozone
                                                                                        Forming Potential Inventory
                                                                                         1710

                                                                                         MO

                                                                                         5(13

                                                                                         441

                                                                                         12V

                                                                                         111

                                                                                         102

                                                                                          HO

                                                                                          A3
• On-Rimd Klh.uil
OOffRo.d
• On-Rowi Ev.purL.llon
 Solvrnl U«r
• Oil Prod 4 Mkm
B Curnumrr Product*
D Mlsc Protrrsscs
D Indu*lri»l Procev.
D ComhiBlion
                                                                                           Toul - 3749 lons/d.y
                                                                                 And. once again, in the MIR-weighted inventory, we see the actual ozone
                                                                                 contribution of on-road exhaust and off-road increase significantly, while the
                                                                                 contributions of other sources, including consumer products, go down
                                                                                 proportionately.  Consumer products here contributed only less than 3% of
                                                                                 ozone formed. We believe that this type of analysis could provide a valuable
                                                                                 tool in prioritizing ozone precursor reductions.  The MIR-weighting technique.
                                                                                 however, can only look at VOCs; the use of airshed modeling could allow this
                                                                                 consideration to include NOx as well.

-------
u>
to
               1997 Sierra Research Study

               »••  UAM Sensitivity Runs

                 •  SCAQMD and Sacramento

                 •  30% and 85%/38% Reductions
•  Peak Ozone Remained within 1-Hour
  Standard
                                                                  UAM Runs
                                                                  Effects of Consumer Product Controls
                                                                  South Coast - 2010
                                                                  »•  85% Controls
                                                                  >« 30% Controls
One-Hour Peak Ozone

 *  122.3


 *•  124.9
                                                                                   >»  One-Hour Standard   »»   125
       Our study also included UAM sensitivity runs by Dr. Whitten. These runs were
       using the uncorrccted VOC inventories in the SIP. even though we knew
       consumer product emissions were overestimated. Both South Coasi and
       Sacramento runs were done, with the base case being the 30<7
-------
to
oo
              UAM Runs
              Effects of Consumer Product Controls
              Sacramento - 2005
              '»  38% Controls
              '•30% Controls
 One-Hour Peak Ozone

>»   124.2


*   124.5
              '»  One-Hour Standard  »•  125
       Likewise, here are the data on peak ozone in the Sacramento run.  In this ca.se.
       the additional consumer product reductions in 2••  UAM Sensitivity Runs

   •  Reasons for Low Peak Ozone Impact

      •  Low Reactivity

      •  Emissions Geography
                                       So in both South Coast and Sacramento, no additional controls on consumer
                                       prodycts still result in levels less than 125ppb in 2010 and 2005. respectively, if
                                       all other VOC and NOx reductions in the SIP are made. The two reasons why
                                       this result occurred were determined to be that, first, the low reactivity of the
                                       consumer product emissions, and. second, where the emissions occur
                                       geographically. They are distributed in the grids of the model by population.
                                       which does not allow them to contribute ozone formation proportionally in the
                                       areas of peak ozone formation.

-------
to
              Reactivity - Future Directions
                 Continued VOC Exemptions
                 Reactivity-Weighted Trading
             •••  Cost-Effectiveness on Ozone Basis
      These are our recommendations for future directions in ozone attainment policy.
      First, we support continued exemptions for negligibly reactive VOCs. Second,
      we support the establishment of broad-based reactivity-weighted trading
      programs.  Finally, we support the use of cost-effectiveness analyses based on
      ozone reductions instead of precursor reductions in looking at regulatory
      options.
         Future  Research Needs

         >*• Identification of Negligibly Reactive VOC
         »»  Improved Precursor Inventories
               •  Tonnage
               •  Speciatfon
         >•- Chamber Studies to Establish Additional,
           Reliable MIRs
         '*  Chemical Mechanisms Studies
         •»  Reactivity Estimation Protocols
         »»  UAM Sensitivity Runs
         '»  UAM Cost-Effectiveness Optimization Runs
Right now our scientific knowledge is many years ahead of our regulatory
policies, but we do have suggestions for further research. Research is needed for
identifying more negligibly-reactive VOCs. Research is needed to improve
precursor inventories, both in terms of tonnage and speciation.  Chamber studies
are needed to establish additional MIR values. Chemical mechanisms studies are
needed to improve both MIR determinations and the computer models.
Sensitivitity runs, like those we did in the Sierra Research study: could help to
evaluate regulatory options. In addition, similar computer modeling of regulatory
options  should be run routinely to optimize the cost-effectiveness of the
regulatory options being considered for ozone controls, both those for VOCs and
NOx.

-------
        Conclusions

        >*-  Reactivity Consideration Essential

        ?*  CSMA Supports Reactivity-Based
         Compliance Options for Consumer
         Products

        >•  Additional Research Needed
In conclusion, CSMA and the consumer products industry continue to believe
that the consideration of reactivity is essential to ozone attainment policy. We
support continued VOC exemptions as well as cost-effective, voluntary.
reactivity-based, compliance options. We also believe that continued research is
needed. The best incentive for encouraging our industry to fund research,
however, would be to see ozone attainment policies change in response to the
many years of research that has already been accomplished.  Thank you.

-------
        Reactivity Concerns


         Philip J. Ostrowski
        Occidental Chemical

 Photochemical Reactivity Workshop
           May 13, 1998
5/11/98
             Summary

  Regulations based on multiple day
  reactivity should be used for the best
  long term scientific approach
  More data is needed to properly
  implement reactivity regulations
5/11/98
                 3-31

-------
             Summary


• For the interim
  - Old VOC exemptions must continue to
    be used
  - No new exemptions of marginally
    reactive compounds
  - Use the reactivity of methane as a cut
    off for new exemptions to avoid long
    term mistakes
5/11/98
             Summary

  There are practical concerns on the
  enforcement side of reactivity
  regulations
5/11/98
                 3-32

-------
  Current Two Tier VOC System


 VOCs are treated equally
  - VOCs differ significantly in O3 formation
   potential
  - Sources are not encouraged to use
   VOCs with low reactivity
  Current Two Tier VOC System


  Exempt compounds are treated
  equally
  - Exempt compounds differ significantly
    in O3 formation potential
  - Sources are not encouraged to use
    exempt compounds with low reactivity
5/11/98
                3-33

-------
       Reactivity Regulations

  Reactivity based VOC regulations
  make sense for the long term
  - Sources will be encouraged to use
    materials which have low reactivity
  - Reactivity must be based on weight
    since most emissions are measured by
    weight
  - Air quality should improve
       Reactivity Regulations

  Reactivity regulations must be
  flexible.
  - Relative ranking for the one day box
    model has in some cases changed
    significantly over time
  - Need flexibility to accommodate better
    data (up or down)
5/11/98
                  3-34

-------
       Reactivity Regulations

  Reactivity regulations must have
  scientific input
  - Need scientific community consensus
    for values of reactivity
  - Uncertainty must be addressed
  - Need periodic review as more
    information becomes available
5/11/98
    Current Reactivity Thinking

• Box model
• One day episodes
• Absolute reactivity differs in different
  air shed
• Relative ranking is about the same in
  all airsheds so regulations are
  possible

5/11/98                                  10
                 3-35

-------
    Current Reactivity Thinking

• What makes sense in California may
  not work for other parts of the
  country
  - LA has little influence from upwind
    sources
  - LA has unusual weather and geography
    • Weather includes lots of sunshine and a
     persistent high that causes inversions
    • Mountains add to the trapping of pollutants
5/11/98                                   11
  National Reactivity Regulations

• Need regional models East of
  Mississippi
• Cities in the Northeast corridor are
  affected by transport of ozone and
  precursors from upwind sources
5/11/98                                  12
                 3-36

-------
  National Reactivity Regulations


1  Use multiple day reactivity,
  compared on an integrated O3 scale
  -The relative reactivity ranking of some
    compounds in multiple day episodes
    shows significant differences versus
    the one day box model
  - Incorrect reactivity could encourage
    use of the wrong chemical

•/11/98                                 13
  National Reactivity Regulations

• Second highest one hour average O3
  is not reliable for measuring trends
  - Compounds should be compared on an
    integrated O3 scale
• Relative reactivity scales must be
  developed for multiday events using
  an integrated O3 scale

• More Data is Needed
5/11/98                                14
               3-37

-------
           For the Interim

• Old VOC exemptions must continue
  to be used
  -Without the old VOC exemptions non
   compliance would soar
  - Sources may revert back to old highly
   reactive compounds
  -Time must be allocated to switch from
   two tier to reactivity systems

5/11/98                                  15
           For the Interim

  No new exemptions of marginally
  reactive compounds
  - Mistakes could be made with excess
    use of the wrong compound
  - Multiday reactivity will increase or
    decrease the relative reactivity of
    compounds
5/11/98                                  16
                3-38

-------
           For the Interim


  No new exemptions continued
  - Compounds in the EPA VOC exemption
    petition queue may have different
    relative rankings in multiday reactivity
    evaluations
  - Some of these compounds will have
    increased relative reactivity
                                    17
           For the Interim


  No new exemptions continued
  - More VOC exemptions could encourage
    widespread emissions of a compound
    which may adversely impact air quality
  - Marginally reactive exempt compounds
    can be used to replace exempt
    compounds with much lower reactivity
5/11/98
                                     18
                3-39

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           For the Interim

  Use the reactivity of methane as a
  cut off
  -This approach should eliminate
    mistakes since methane has very low
    reactivity
5/M/9S                                  19
        Enforcement Policy

  Complex analytical issues must be
  dealt with
  - Laboratory Methods
  - GC Mass Spec
  - Method 24
  -Variability issues
  -Theoretical composition versus actual
  Production Records  use
5/11/98
                                    20
                 3-40

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                  Categorization of Low Reactivity Compounds

                                 John G. Owens
                                 3M Chemicals
                               St. Paul, MN USA
It is recognized that all organic compounds which volatilize into the atmosphere do not
contribute to the formation of tropospheric smog. Some compounds have low reactivity
with respect to common atmospheric removal mechanisms such as photolysis and reaction
with hydroxyl radicals. These low reactivity compounds are stable enough to become well
dispersed throughout the troposphere prior to the onset of their decomposition. As a
result, these organic materials are incapable of contributing to the production of ground
level ozone.

As compounds are considered for exemption from VOC regulations, it would be useful to
first categorize them based upon their reactivity.  Those which are shown to have low
reactivity will not contribute significantly to ground level ozone regardless of their ozone
yield during decomposition. These materials could be considered for exemption from
VOC regulations without need for further information. Compounds of higher reactivity
have the potential to add to ground level ozone during their decomposition.  These higher
reactivity compounds could be selected for further study to determine the ozone
production from their atmospheric oxidation.  Such categorization could streamline the
exemption process and focus resources on the study of compounds which have  the
greatest potential to impact smog formation.
                                      3-41

-------
 Categorization of Low Reactivity
               Compounds
               John G. Owens
               3M Chemicals
        Criterion for VOC Exemption

      (x) < kOH (C2H6)
  (compound x is atmospherically longer lived than ethane)

> k OH (C2H6) - 0.24 x 10-12 cm3/molecule-s
  which translates into an atmospheric lifetime of
  approximately 0.24 years

> Additional criteria being being developed such as
  ozone production during tropospheric decomposition

> Reactivity of compounds in recent exemption requests
  have been very close to and in some cases higher
  than ethane
                    3-42

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       Very Low Reactivity Compounds

 >  Some compounds are very low in reactivity
    koH (x)  « koH  (C2H6)
    and do not photolyze in the lower atmosphere
    e.g. saturated, halogenated compounds

 >  Compounds with sufficiently low reactivity will
    be well dispersed throughout troposphere during
    decomposition

 >  Oxidation of these compounds does not
    contribute measurably to ground level smog
    regardless of O3 yield.
Categorization of Low Reactivity Compounds
> Useful to establish a criterion which distinguishes
  between :
I. Compounds with
  reactivity relatively close
  to ethane

   i.e. more likely to
   contribute to smog
   formation and smog
   chamber studies
   necessary	
Vs.
II. Compounds which are
   significantly less
   reactive than ethane

   i.e. clearly will not
   contribute to smog
   formation and k0H
   and photolysis data is
   sufficient
                        3-43

-------
              Transport Times for

     Chemical Species in the Atmosphere

    The longer a compound survives in the atmosphere, the greater the
    proportion transported to high altitudes by diffusion and convection.
      30km
1 to 3 years into stratosphere
       10km
       1km
days to weeks to reach tropopause
hours to reach planetary boundary layer
Categorization of Low Reactivity Compounds
 > further clarify VOC definitions


 > focus resources on evaluation of compounds which
   are more likely to be contributors to smog formation


 > streamline exemption process


 > provide benefit to chemical users
                    3-44

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EPA Photochemical Reactivity Workshop, May 12-14, 1998, Durham, NC

Presenter:

Daniel B. Pourreau, Ph.D., Coatings Development Manager, ARCO Chemical
Company.

Title of Presentation:

Impact of a Molar Ethane Standard on the Number and Type of VOC-Exemptible
Compounds; Practical and Environmental Implications.

Abstract:

Since  1977, the USEPA has granted several industry petitions to exempt specific
organic compounds on the grounds of "negligible photochemical reactivity". Most of the
early exemptions were granted on the basis of kinetic reactivity data, that is the rate of
hydrogen abstraction by atmospheric OH radicals.  The compound's hydrogen-
abstraction rate constant, kOH, expressed in molar units was typically compared to that
of ethane.  Compounds with kOH constants lower than ethane were considered
"negligibly reactive" and appropriately exempted from VOC regulations.

More recent petitions have been granted on the basis of both kinetic and mechanistic
data.  The reason for relying on mechanistic reactivity was the realization that several
compounds with negligible kinetic reactivity had significant ozone yields when irradiated
in the  presence of other more reactive gases and NOx pollutants. Mechanistic reactivity
is defined as the incremental amount of ozone formed when a compound is added to a
polluted atmosphere under well defined conditions.

The compounds' maximum incremental reactivity, or MIR, expressed on a  weight basis
has been the published standard since the EPA's  Report to Congress in 1995 and was
the basis for the exemption of Acetone from VOC  regulations.  Here, the "cutoff
 between reactive  and "negligibly reactive" compounds was the  MIR of ethane on a per
gram basis.

 Since then, the EPA has received several petitions from industry to exempt other
-compounds based on MIR data.  Because of this and concerns about possible future
.petitions, EPA is now considering a tightening of the MIR standard by requiring that
^compounds be less reactive than ethane on a per mole basis.

We will present evidence that shows that the number of useful  compounds that meet
the current gram-based MIR standard is limited and that the proposed mole-based
standard would severely limit the number of useful VOC-exempt compounds available
to industry.  The  impact this policy change would  have on the industry's ability to meet
current and future VOC regulations wilPalso be discussed.
                                    3-45

-------
Introduction - Title Slide

Good Morning.  First, I'd like to thank the EPA for calling this workshop and giving
Industry the opportunity to participate. ARCO Chemical also has a petition before the
EPA to exempt a new solvent from VOC regulations. I will, however, not discuss this
petition oday, only to the extent that it illustrates how such low reactivity materials can
provide immediate and substantial environmental benefits by replacing more reactive
VOCs still in use today.

The main thesis of my presentation is that the EPA's proposal to adopt a new, stricter
standard based on  the photochemical reactivity of ethane on a per mole basis would
virtually eliminate all viable substitution candidates.  The impact of such a decision
would be two-lold:

1. It would strengthen the Industry's opposition to further mass-based VOC limitations
and,

2. it would favor substitution to environmentally persistent halocarbons.

Neither would achieve anywhere near the environmental benefits which would result
from the exemption of a handful of solvents which meet the EPA's current gram-based
exemption criterion.

Slide 1
                    t
Let me start by illustrating the magnitude of the challenge we face today.  Based on
recent Industry analyses, the US Coatings, inks, and adhesives industries alone
consume close to 5 billion pounds of solvent  per year, despite all the regulatory efforts
to decrease their usage.  As you'll see later on, there are many reasons why solvents
continue to be popular tools in these industries.

Slide 2

Low VOC technologies such as water and powder have made significant strides in the
past few years but  are still  not suitable for many applications and often lag in
performance compared to solvent-based systems. For example, you still cannot
powder coat a bridge nor can you repaint it with water in cold and damp weather. These
are realities we have to deal with.

Abatement technologies have also been very helpful in reducing the amount of solvent
emitted into the atmosphere. But solvent recovery is not often practical and incineration
generates NOx.

For these reasons, the EPA should continue to encourage the development of low
reactivity solvents and their use in place of many of the more reactive and toxic solvents
still in use today.
                                     3-46

-------
Slide 3

By far the most popular solvents in these industries are aliphatic and aromatics
hydrocarbons and oxygenated solvents such as esters, ketones, and alcohols.
Halogenated solvents,  which are still popular in the cleaning industries because of their
high solvency and low flammability account for less than 1% of solvent usage in the
coatings industry.
Slide 4

The reasons for choosing hydrocarbon and oxygenated solvents are numerous.

The best solvents have intermediate solvency.  Strong enough that they reduce resin
viscosities effectively but not so strong that they strip primer coatings or attack the
substrate. This is one of the reasons strong solvents such as methylene chloride are
almost never used in the coatings industry.

Waterborne coatings also require solvents to stabilize the paint formulation and improve
film formation.  Here, the best solvents are oxygenated solvents such as glycol ethers
and N-Methyl-pyrrolidone. Hydrocarbons and halogenated solvents are not useful here
because they are essentially insoluble in water.

Different coating operations also require different drying or evaporation rates.  Fast
solvents are used in ak-dried systems, slower solvents under bake conditions. Most
often, blends of solvents are used to tailor the dry time to the specific operation and
optimize the performance and appearance of the coating.

Another reason for choosing solvent-borne systems is that their dry times are
independent of environmental conditions.  This is not the case with waterborne systems
that dry much slower under cold and damp conditions.

Most solvents used today have  relatively low toxicities. Solvents such as benzene are
no longer used and those solvents listed as Hazardous Air Pollutants are strictly
regulated by OSHA in the workplace and by State and Federal Environmental
Protection Agencies. Many companies have already reformulated their products with
non-HAP solvents such  as Cypars, P-series glycol ethers, alcohols, and esters.

These solvents are also inexpensive.  Because paint is sold by the gallon and solvents by the
pound, low density is a distinct benefit. Halogenated solvents, in contrast, have high densities
and are relatively expensive on a volume basis.

Another advantage of non-halogenated solvents is that emissions can be incinerated.
They typically have good fuel value and no corrosion issues related to halo-acid
formation.  The coil coating industry, for example, is effectively using solvent
incineration as  an abatement and energy producing tool.

                                      3-47

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Finally, non-halogenated solvents typically have low environmental persistence. Since
they do not contain halogens, they have zero ozone depleting potential and low acid
rain contributions. They rapidly oxidize in the atmosphere to water and carbon dioxide
which has relatively low global warming potential.

Slide 5

I'd like to expand a little more on this point with this table which compares the ozone
depleting and global warming potentials of the major halogenated solvents and the
average of several halogenated and non-halogenated solvents.  As you can see, the
atmospheric lifetimes of halogenated solvents are typically measured in months
whereas non-halogenated solvents typically oxidize in the matter of days.

Since the global warming potential of a solvent is a function of its atmospheric lifetime,
its ozone depleting potential, and its total infrared absorbance relative to carbon dioxide
it is easy to see why halogenated solvents are likely to have a greater impact on global
warmr.g than their non-halogenated counterparts.

Slide 6

Which brings me back to the challenge we face today:

Replacing close to 5 billion pounds of solvent per year with  substitutes that generate
less tropospheric ozone yet do not have a lot of health and  environmental baggage
attached to them.    v

This graph provides a clue as to how we might achieve that. Of the top 20 solvents
used  in the coatings industry today, only a handful contribute significantly more than
their actual emissions to tropospheric ozone formation.  These are the aromatics, and
to a lesser extent, some of the higher members of the ketone, alcohol, and glycol ether
families.

Clearly, one way to significantly reduce ozone formation would be to develop policies
that encourage substitution of these highly reactive VOCs with less reactive ones.  And
to a certain extent, the EPA's current policy does that.

Slide 7

By exempting VOCs with incremental reactivities less than ethane on a per gram basis,
the EPA has given Industry the incentive to develop and use low reactivity solvents
such  as acetone and PCBTF. Petitions for several other solvents with similar or lower
reactivities are before the EPA today. Granting these petitions could result in
immediate and substantial environmental benefits which are illustrated here.

With additional exempt solvents, current ozone Jevels could potentially, with time, be
reduced by 88%,  assuming that all exempt solvents had reactivities equal to ethane on

                                     3-48

-------
a per gram basis. In fact, some of the petitioned solvents have reactivities less than
half that of ethane so ozone reduction opportunities of over 90% are conceivable.

Which brings us to this key question:

If such substantial benefits are achievable using ethane on a per gram basis as the
cutoff between exempt solvents and VOCs, why not make the standard stricter? Why
not go to ethane on a per mole basis?

Slide 8

The reason you do not benefit from using a molar ethane cutoff is that you drastically
reduce the number of viable exempt substitutes for more reactive VOCs. As this graph
illustrates, the number of practical non-halogenated solvents which  meet the current
MIR standard on a per gram basis is approximately ten. Going to a mole standard
reduces this number to one.
Given the wide range of properties required from today's coating formulations, having
10 viable substitutes for high reactivity VOCs is a minimum.  Having one is essentially
useless.

Another potential impact of this new proposed  standard is that it would favor
halogenated solvents.  As I illustrated earlier, halocarbons have limited use today in
coatings, inks, and adhesives and have relatively high atmospheric persistence.  A
stricter ethane standard would have relatively little impact on the number of exemptible
halogenated solvents and could drive Industry to turn to these solvents to  meet the new
and more stringent mass-based VOC limits.  This could have a negative impact on
worker health, acid rain, global warming, and stratospheric ozone depletion.

Slide 9

I'd like to leave you with a real life example of how low reactivity solvents can be used
to replace more reactive and toxic ones. What we have done here, and for several
other coating formulations, is taken a conventional high solids formulation and replaced
the solvents with lower reactivity and non-HAP alternatives.  We then calculated the
.ozone impact of each formulation on a pounds ozone per pound of solids  applied basis.
Finally, we compared these solvent-based formulations to a standard waterborne
formulation.

Slide 10

This slide graphically illustrates that reformulating conventional solvent-borne systems
with low reactivity and non-HAP solvents can significantly reduce the  ozone impact and
toxicity of these formulations. In this particular case, we were even able to lower the
ozone yield and HAP content of the solvent-borne system below that  of the waterborne

                                     3-49

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system.

You will notice, however, that the low ozone formulation has the same solvent content
as the conventional system. Without VOC exemptions, there would be  no incentive for
industry to go to this type of formulation.

Worse yet, if the EPA goes to a mole based ethane standard or suspends further
exemptions,  Industry will have the incentive but no tools to reformulate with.

Slide 11

In conclusion, we urge the EPA to continue exempting VOCs based on their reactivity
relative to ethane on a per gram basis. The status of exempt solvents can always be
revisited at a later date in light of newer and better science.  It would counterproductive,
however, to wait for the outcome of what will likely be a lengthy and complicated
process to reap the benefits that can be achieved today, with the current policy.

Thank you for your time.
                                    3-50

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     Impact of a Molar Ethane Standard
         on the Number and Type of
       VOC-Exemptible Compounds;
         Practical and  Environmental
                 Implications.
        EPA Photochemical Reactivity Workshop
                  May 12-14, 1998
                    Durham, NC
                                Daniel B. Pourreau, Ph.D.
                                Coatings Development Manager
                                ARCO Chemical Company
    1996 US Solvent Usage in Coatings by End Use
                          Special Purpose
           OEM
                            Architectural
                  3.2 Billion Ibs
 Kusumgar, Nerfli & Growney. 1&97
. Powder limited to larger volume OEM operations
. Waterborne coatings have performance limitations
. Abatement not practical in architectural & special purpose sectors
. Incineration generates NOx
                                                                                          1997 US Solvent Usage by the
                                                                                      Coatings, Inks, and Adhesives Markets
   Million Pounds
   4000 ,	
   3000
                                                                                 2000
   1000
            3,240
                                                                                         Coatings
                                                                                                        Inks
                                       BOO
                                                                                                                   Adhesives
        . Solvents continue to be widely used
    Hydrocarbons and Oxygenated Solvents Popular
                                                                                   ,l!   Aromatics23%
                                                                                         Ketones 14%
                                                                                                            Aliphatics 32%
                                 Glycol ethers7%

                              Esters 11%
                Alcohols 11%
                     3.2 Billion Ibs
    Kusumgaf. Nerfli A Growney. 1997
, Hydrocarbons and oxygenated solvents account for >99% of usage
, Halogenated solvents account for <1% of coating solvent usage

-------
                   Reasons Why Hydrocarbon and Oxygenated
                      Solvents are Popular Coating Solvents
                         . Physical and Solubility Properties
                           . Intermediate solvency for coating resins
                           . Some can stabilize resins in water
                           . Range of evaporation rales
                           • Dry times independent of conditions
                           . Low cost per gallon

                         . Environmental, Health, & Safety
                           . Can be incinerated
                           . Relatively low toxicities
                           . Low environmental persistence
                           . No ozone depleting potential
                           . Low acid rain contribution
                           . Low global warming potential
to
                        Top 20 Coating Solvents: Volume &
                            Tropospheric Ozone Impact
Mineral Spirits
Xyiene
VMiP naphta
Toluen*
MEK
Butyl Acetate
Higher aromatic*
Acetone
EB
Butanola
Propunolt
Ethanol
Lacquer solvents
Ethyl acetate
MIBK
Ethylene Glycol
, PM Acetate
1 PM
OB
Methanol
Billions of Pounds
) 05 1 15 2 25 3
' ^
• 	 •
—
!=3
5=>
i
b | Solvent Used Q Ozone Equivalents

                   . Top 20 coating solvents account for 92% of usage
                   . Aromatics generate the most tropospheric ozone
        Based on Cartel MIR data & KN&G Solvent study
Impact of Atmospheric Lifetime
on the Global Warming and
Ozone Depleting Potential of Solvents

















Major Halocarbon Solvents
Methylene Chloride
Chloroform
Carbon Tetrachloride
1,1,1-Trlchloroethane
Perchloroethylene (PERC)
Other Halocarbon Solvents
(Avg. of 24)
Non-halocarbon (Avg. of 13)
References
Average
Atmospheric
Lifetime,
days

131
200
50 years
6 years
130
229
26

Pounds
CO2 per
Pound
Solvent

0.53
0.37
0.29
0.66
0.53
0.84
2.60


Ozone
Depletion
vs. CFC-11

> 0
> 0
1.1
0.1
>0
>0
none

Global
Warming
Relative
to CO2

28
15
> 2,000
> 360
unknown
>15I
~K5

1 1994 Report of the Scientific Assessment Wonting Group of Intergovernmental Panel on Climate Change
2 Kirk Othmer Encyclopedia of Science and Technology. 4th Ed
'Based on Ihe relative lifetime and CO2 equivalents ot chloroform
               Potential Environmental Benefits with
                  Ethane Cutoff on a Weight Basis
                                                                                                                          Today
                                          w/ Exempt solvents
                . >88% reduction in ozone possible

                . Major HAP reductions also achievable

Assumes replacement of lop 20 solvents with noo-HAP solvents with MIRs equal to ethane on • wofcht basis

-------
          Impact of a Molar Ethane MIR Cutoff on the Type
             and Number of Available Exempt Solvents
                                               150         200
       Halocarbon
   Non-Halocarbon
                                     Q Meet Molar standard
                                     H Meet Weight standard
                                     • Solvents Evaluated
                                                148
          > Stricter standard would drastically limit the number of
           exempt hydrocarbon and oxygenated solvents

          . Substitutions would be limited to exempt halocarbons
Based on Cartel MIR data
                         Wood Coatings
      Two-component Urethanes vs Waterborne Lacquer

      Ibs/lbs solids
      onventional 2K PU
                           TBAc-Based 2K PU
        L30.3
        mm.
Waterborne Lacquer
        . Ozone Impact of TBAc-based wood coatings lower than water-borne

        . HAP content lower than waterbome & conventional

        . Ease of use and durability superior to waterbome
                                                                  Wood Clearcoats
                                                                                                                               •Rohm & Han CL-204 Wood Clear Formulation
                                                         Potential Environmental Benefits of
                                                                 Current EPA Policy
                                                                                                             Today
                                                                                  w/ Exempt solvents
                                                         . >88% reduction in ozone possible

                                                         . Major HAP reductions also achievable

                                          Assumes replacement of top 20 solvents with non-HAP solvents with MIRs equal to ethane on a weight basis

-------
                      General Industry Concerns With the Process
                              Remarks by Donna Carvalho
                              Pennzoil Products Company

Good Morning, my name is Donna Carvalho. I am here representing Pennzoil Products Company.
I am here today to offer an industry perspective on the need for further photochemical reactivity
research.  Pennzoil Products  Company, through its subsidiary, Magie Brothers Oil Company,
currently has a delisting petition before the Agency. I will not be discussing that petition except as
it relates to why clear science is needed.

Pennzoil applauds this EPA effort to identify research needs and partners. We also welcome the
opportunity to have this forum for policy discussions. As EPA seeks to determine what research is
necessary, we offer the following suggestions:

First, we ask EPA to focus whatever process is adopted for photochemical reactivity decisions to that
purpose only.  This process does not need to be a  substitute program for new source review,
prever ion of significant deterioration, global warming or the hazardous air pollution program. We
recognize that the final process may impact each of these other programs; however, we believe that
any negative impact will be very small while the positive impact could be significant as state and
federal agencies  and industry  rightfully focus on controlling those VOC emissions that are most
volatile and reactive.

Second, we  suggest that EPA recognize that it  does not have to have 100% surety to delist a
chemical. Whatever scientific  approach is adopted should combine scientific excellence with
realistic and timely policy making. States inherently recognize the tension between what knowledge
is available and what can and should be controlled when they exempt certain materials from control
requirements.  Your counterparts in EPA will be doing the same when they finalize the VOC
consumer product rule.  As proposed, this rule exempts materials with a particular vapor pressure,
or where the vapor pressure  is not known, with a carbon-number cutoff.  These various rules
combine what the regulator knows about the materials being regulated with what can be realistically
and cost-effectively controlled.

Third, as members of  industry, we suggest that EPA develop and adopt an easily understood
"cookbook" type of approach to making photochemical reactivity decisions.  As discussed in more
detail later, our preference is that this approach would include giving deference to volatility issues.
Other alternatives might include a carbon number  cutoff, use constraints, and/or magnitude or
volume of use considerations.

Finally, Pennzoil offers the following specific comments. First, we would prefer that photochemical
assessments be made on a per-gram basis rather than a per-mole basis.  Second, we would also
recommend a reactivity scale that looks at ozone formation over a period of time.

I will now discuss each of these suggestions and recommendations in more detail. As noted initially,
the research and  final decision-making process that is developed out of these workshops should be
focused solely  on defining photochemical  reactivity.    The final method  for  determining
photochemical reactivity should be consistent with other programs to the greatest extent possible,

                                          3-54

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but should not replace other programs.  Trying to address other pollution concerns with a process
for determining whether a chemical is photochemically reactive or not will only make an already
complicated process more complex and time-consuming. There are already numerous other EPA
programs which have been developed to control hazardous and non-hazardous VOC emissions. The
goal of the research coming out of the workshop should be to determine which chemicals participate
in ozone formation and which do not. Once this group has established the process that answers that
question and that question only, then other EPA programs fill the gap to determine what and how
emissions are to be controlled.

Having an overly broad process is a real concern for us. I  mentioned earlier that Pennzoil has a
delisting petition before the Agency. This petition is the culmination of nearly 20 years of tests and
research. One of the initial tests done in 1982 indicated that the product which is the subject of the
petition had essentially the same photochemical  reactivity as ethane. However, at that time, EPA
expressed to us reluctance to act on the findings because of the uncertainty regarding what Congress
would be doing with hazardous air pollutants within the context of the then proposed Clean Air Act.
That question took another eight years  to answer.  Recently, EPA has said in its perc  delisting
whether the product is hazardous  or not is not  a factor to  be considered when making its VOC
delisting decisions.  Even though EPA's current position would not help or hinder  our petition, we
think this position is the correct one and should be maintained.  Other air pollution concerns should
not play a role in determining if the material is photochemically reactive or not. Rather,  the other
EPA programs in place will address other concerns.

As noted earlier, we do not believe that limiting the scope .of the program will negatively impact
these other programs.  Instead, controls can be directed to those VOCs which actually merit control.

Pennzoil also believes that the Agency should identify realistic research goals and decision-making
frameworks. This is what combining scientific excellence with realistic and timely policy making
means.  The Agency must decide what method or methods will reasonably satisfy it. As part of this
decision-making, EPA should determine which method or methods get the best information it can
have for the most reasonable  cost.  Pennzoil has tested its materials several different ways.  Other
companies who do not have our resources may  not be able to make a twenty-year investment in
evaluating their products under changing tests or reactivity scales.

Our preference is that EPA adopt a relatively simple, easy to  understand, "cookbook"  method. Our
history with the Agency shows that we have tested our materials in various manners and conditions.
^When it became apparent that the Agency preferred one scale over another, we ensured that  our
testing results  included those  scales. However, industry should not have to continue to try and hit
a moving target. One company should  not be evaluated under  one set assumptions one day and
another company evaluated under different assumptions the next. The Agency's goal today should
be to develop  a simple method that can be understood and easily performed.

In this light, Pennzoil would  urge the Agency to reconsider looking at volatility as a surrogate for
photochemical reactivity and/or as an initial screening measure.  After all, you are determining if
something is a "volatile organic compound".  It seems counterintuitive that non-volatile or negligibly
volatile chemicals are nonetheless "volatile organic compounds"

                                           3-55

-------
Unlike reactivity scales which are developed after time-consuming and sometimes costly chamber
tests are performed, volatility is easy to determine.  Further, there  is already  substantial EPA
precedence  for using volatility to determine control  requirements.  As noted  earlier, your
counterparts in EPA are expected to issue any day now a consumer products rule that will exempt
products with a volatility of less than 0.1 mm/Hg at 20 degrees C. Where vapor pressure is unknown
the Agency will exempt products with more than 12 carbons.  Similarly, most states exempt the
storage and/or use of low volatility products from control requirements in EPA-approved SIPs.
Given the industry familiarity with these types of tests and controls, EPA should determine whether
it can build and/or improve upon a process which uses volatility. Neither EPA nor industry should
have to spend time and effort determining if something is "photochemically reactive" when in some
cases, the emissions will be exempted from control requirements  anyway. Unfortunately, even if
there are no control requirements, there are costs associated with identifying and quantifying the low
volatility emissions.  Further, the facilities may be unnecessarily  paying to obtain and maintain a
Title V permit.

Another option for EPA to consider is using volatility as the screening tool.  Other easily understood,
uniform tests (whether chamber tests or modeling) could be required if one cannot pass the screen.

Finally, to the extent that EPA adopts a uniform process where chamber tests are conducted and
results are modeled, we offer the following specific recommendations.  First, such tests should
compare the tested material with ethane on a per-gram basis. The basic reason for determining if
a compound is photochemically reactive is to determine if it is a "volatile organic compound" which
must be controlled. Under all the regulatory programs of which we are aware, VOC emissions are
controlled on a weight basis (usually pounds per hour or tons per year). For paints,  coatings, and
consumer products, where solvent  substitution is often the most  effective approach for reducing
VOC emissions, VOC limits are set on a grams per liter basis. Where solvent substitution is used
as a control strategy, the substitutions are made  on a volume basis,  which is fairly close to a weight
basis and has nothing to do with the molecular weight of the compounds. The VOC control program
and the process for determining if a compound is or is not a VOC should be consistent. EPA has
publicly announced that, in making  decisions about VOC exemptions, it will compare compounds
to ethane on a gram-basis. EPA should continue to follow this policy.

Similarly, whatever reactivity scale is finally decided to  be  appropriate should  model ozone
formation over a period of time and not just look to peak occurrences.  Again,  we suggest this for
consistency with the new  ozone  control requirements.  The systems for  determining ozone
attainment now take into account the fact that ozone develops over a period of time and is affected
by weather and other local conditions. When comparing tested materials to ethane, one should look
to see what happens to both materials over time and differing conditions. If the results are basically
the same, the material should be exempted.

Pennzoil hopes that these remarks will give you an  industry perspective on these issues.  We too
want to see  a  process developed  where all the players will  know what is  expected to  make
enlightened and accurate photochemical reactivity decisions. Thank you for  this opportunity to
speak.
                                           3-56

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TITLE:             A GLOBAL 3-D RADIATIVE-DYNAMICAL-CHEMICAL
                    MODEL FOR DETERMINING LARGE-SCALE IMPACTS
                    OF ATMOSPHERIC OZONE PRECURSORS

PRESENTER:      Dr. Eduardo P. Olaguer
                    The Dow Chemical Co.
                                 ABSTRACT



The Dow Chemistry-Climate Model (DOWCCM) is a new 3-D modeling tool that utilizes

sophisticated methods for simulating radiative transfer, photochemistry, and geophysical

fluid dynamics in order to compute large-scale atmospheric impacts of ozone precursors.

These large-scale impacts include global and regional ozone formation potentials, global

warming potentials, ultraviolet actinic flux changes, tropospheric oxidation capacity

changes, and changes in global atmospheric circulation. DOWCCM combines an 11-

wave, spectral meteorological model with a grid, chemical transport model to enable the

simultaneous prediction of the general circulation and chemical composition of the

atmosphere from 0 to 79 km.  The current photochemical scheme incorporates up to 136

gas phase and heterogeneous reactions involving about 40 species, including those

pertaining to methane oxidation.  Work is now in progress to expand the tropospheric

chemical mechanism to include non-methane hydrocarbons and oxygenated species such

as acetone. The DOWCCM employs a fourth-order, positive-definite Bott scheme similar

to that used in Models-3 to simulate tracer advection. Also incorporated in the model is a

parameterization for convective venting of tracers from the boundary  layer to the free

troposphere. The DOWCCM is very computationally efficient (approximately 1 CPU

minute is  required per model day on a Cray T90), yet it successfully simulates the basic

features of the general circulation and of total column ozone, and precisely predicts the

atmospheric lifetime of methyl chloroform.  Future versions of DOWCCM may contain

nested regional models within a global framework.

                                   4-1

-------
              Reactivity  Calculations  with  the
    Regional  Atmospheric Chemistry  Mechanism
                          William R. Stockwell
Fraunhofer Institute for Atmospheric Environmental Research (IFU), Kreuzeckbahnstr.
19, D-82467 Garmisch-Partenkirchen, Germany, e-mail: stockwel@ifu.fhg.de

The gas-phase chemical mechanism is one of the most important components of an air
quality model.  The Regional Acid Deposition  Mechanism, version 2  (RADM2)
(Stockwell et al.,  1990) is used in a number of air quality  models including the
MODELS3/CMAQ modeling system.  Many new measurements  of mechanism
parameters have become available after the RACM2 mechanism  was completed 8 years
ago. We have used these measurements to create a successor to the RADM2 mechanism,
the Regional Atmospheric Chemistry Mechanism (RACM) (Stockwell et al., 1997).
The RACM mechanism has a reasonably complete set of explicit inorganic reactions that
include 21 chemical species. The revisions to the RADM2 inorganic chemistry for the
RACM mechanism were relatively small. The RACM organic chemistry was highly
revised from RADM2.  The most important revisions included a reevaluation of the yields
of aldehydes and ketones from alkanes, the yield of HO from the ozonolysis  of alkenes,
revised branching ratios for the reactions of acetyl peroxy radicals with  NO and NO2, a
revised aromatic oxidation scheme, new oxidation schemes for isoprene and terpenes and
the addition of thd reactions of NO3 radical with organic peroxy radicals. The reactions
of organic peroxy  radicals with  NOs radical  and the revised branching ratios for the
reactions of acetyl peroxy radicals  with  NO  and NO2 lead to predicted PAN
concentrations by RACM that nearly 40% lower than those predicted by RADM2 under
similar conditions.  The RADM and  RACM mechanisms have been tested  against
environmental chamber data and the agreement is good for 03, NOX and hydrocarbons.
We have applied the RACM mechanism to ozone reactivity calculations for biogenic
emissions and highly oxygenated compounds for rural European conditions. We believe
that the new scientific data included in the RACM mechanism make it a better mechanism
for the determination of incremental reactivities than the RADM2 mechanism. The new
RACM mechanism should replace the RADM2 mechanism in any future development of
comprehensive Eulerian air quality models.
References
Stockwell, W.R.,  F. Kirchner,  M. Kuhn, and S. Seefeld,  A New Mechanism for
     Regional Atmospheric Chemistry Modeling, J. Geophys. Res., 102, 25847-25879,
Stockwell, W.R.,  P. Middleton, J.S.  Chang and X. Tang, The Second Generation
     Regional Acid Deposition Model Chemical Mechanism for Regional Air Quality
     Modeling, J. Geophys. Res., 95,  16343-16367, 1990.
                                   4-2

-------
-fx

OJ
          Requirements for Chemical
                Mechanisms for
             Eulerian 3-D Regional
        Atmospheric Chemistry Models
1. Predict  concentrations  of
   H2O2, ROOM, PAN, HNO3, H2SO4..

2. Mechanism must give accurate
   predictions   over   chemical
   concentrations  ranging  from
   clean to moderately polluted.

   •   Peroxy radical reactions are
      important

3. Mechanisms  must be valid for
   multiday simulations.

   •   Nighttime chemical species
      such as NOa are important.

   •   Less reactive species which
      are subject to  long range
      transport are important.
                                                      The Regional Atmospheric
                                                    Chemistry Mechanism (RACM)
                                                   A completely revised version of the RADM2
                                                      mechanism of Stockwell et al. [1990]
Mechanism Includes:

     • 237 reactions

     • 17 stable inorganic species

     • 4 inorganic intermediates

     • 32 stable organic species
       (4 are primarily of biogenic origin)

     • 24 organic Intermediates
     William R Stockwell

     Reactivity Calculations with the Regional Atmospheric Chemistry Mechanism
     Fraunholer Institute for Atmosphenc Environmental Research (IFU)
                                            William R Stockwell

                                            Reactivity Calculations wuh the Regional Atmosphenc Chemistry Mechanism
                                            Fraunhofer Institute for Atmosphenc Environmental Research I IFU)

-------
      The Regional Atmospheric
        Chemistry Mechanism
                  1996
Includes:
• Detailed and  explicit inorganic
  chemistry

• Lumped organic chemistry
Type
Number
Alkanes
Alkenes (including biogenics)
Aromatics
Carbonyls
Organic Peroxides
Organic Acids
Organic Nitrate and PANs
    5
    7
    3
    9
    3
    2
    3
William R. Slockwell

Reacliviiy Calculations with 
-------
Statewide  Air  Pollution  Research Center
Smog  Chamber Experiments  for
Testing  of RADM Mechanism
Description

Propane

n-Butane

Ethene

Acetaldehyde

Toluene

Toluene + n-Butane

m-Xylene

Multi-Component
Identification  Numbers

    EC216

    EC178, EC305,  EC306

    EC142, EC143

    EC254

    EC340

    EC331

    EC344, EC345

    EC231, EC232, EC233,
    EC237, EC238,  EC241,
    EC242, EC243, EC245,
    EC246
Statewide Air Pollution  Research Center
Multi-Component Smog  Chamber
Experiments
                 Components

                    NOX
                  n-Butane
              2,3 Dimethylbutane
                   Ethene
                  Propene
                 t-2-Butene
                  Toluene
                 m-Xylene
                   HCHO
                    CO
  William R. Stockwell

  Reactivity Calculations with the Regional Atmospheric Chemistry Mechanism
  Fraunhofer Institute for Atmospheric Environmental Research (IFU|
                                      William R Stockwell

                                      Reactivity Calculations with the Regional Atmospheric Chemistry Mechanism
                                      Fraunhofer Institute for Atmospheric Environmental Research lIFU)

-------
                           NO.
                SAPRC environmental chamber

                      experiment EC-237
o\
      o.
      O.
      2
      •**
      c
      Ol
      u
      c
      o
      U
           0
0
                      100       200


                         Time, Min
300
400
                 O Experimental values of NO2

                 A Experimental values of NO

                   RACM simulations; dotted lines

                   RADM2 simulations
      William R. Stockwell


      Reaciivity Calculations with the Regional Atmospheric Chemistry Mechanism

      Fraunhofer Institute for Atmospheric Environmental Research (IFU)
                               Ozone
                      SAPRC environmental chamber

                            experiment EC-237
            E
            o.
            o.
            C
            o»
            u


            o

           U
                 0
                   0
                                                                     400
                       O Experimental values of 03


                          RACM simulations; dotted lines

                          RADM2 simulations
             William R. Stockwell



             Reactivity Calculations with the Regional Atmospheric Chemistry Mechanism

             Fraunhofer Insmuie for Almosphenc Environmental Research (ffTJ)

-------
Comparison  of Simulation and Smog-Chamber  Run  for Isoprene
                                                                                      Comparison of Simulation and Smog-Chamber Run for d-Limonene
  I  °H
  *
  S  o.4H
  i
                 OJ (expcmncMil dau)
                 03 (KADM2)

                 O3 (»cw mcduniun)
                03 (eipcrimonl dm)
                03 (RADM2)
                O3 (a«w mcrtartm)
                       ; «•!•>
                             s       §
                                                     i     §.,_..> a     §     §
    a»-
 5  04-
 ?
           Q    O3 (u^rimal dju)
          	  O3 (RADMJ)
          	  O3 (ne" meditniim)
       0      8       § i,miB)  §       |
       William R~ Siockwell
           1     §     §     I     §
                                                                l(min)
       Reactivity Calculations with the Regional Atmospheric Chemistry Mechanism
       Fraunhofer Institute for Aimosphenc Environmental Research (CFU)
                                                                                          i(min)
the experimental data are given by the following symbols: squares represent
ozone, circles NO and triangles the sume of NO2 and nitrates
the lines represent the simulation results for the corresponding species but
the NO2 line represents only NO2 (without nitrates)

     WiUiam R. Siockwell

     Reacuvity CoJculauon.s with the Regional Atmospheric Cherrustry Mechanism
     Fraunhofer Institute for Atmospheric Environmental Research (IFTJi

-------
Comparison of Simulation and Smog-Chamber Run for a-Pinene
  the experimental data are given by the following symbols: squares represent
  ozone, circles NO and triangles (he sume of NO2 and nitrates
  the lines represent the simulation results for the corresponding species bui
  the NO2 line represents only NO2 (without nitrates)
                                                                 Maximum ozone concentrations
                                                                 predicted by RACM and RADM2
                                                                   mechanisms plotted against
                                                                   SAPRC experimental values.
                                                                                                *   RADM2

                                                                                                O   RACM
                                                                0.0
    William R. Slockwell
                                                                    0.0     0.2    0.4    0.6     0.8     1.0     1.2

                                                                         Experimental Maximum Ozone, ppm
William R. Slockwell

Reactivity Calculations with ihe Regional Atmospheric Chemistry Mechanism
Fraunhofer Institute for Atmospheric Environmental Research I [FU)
     Reactivity Calculations with the Regional Alnmphenc CnemiMry Mechanism
     Fraunholer Institute for Atmospheric Environmental Research lll-lh

-------
   Time of the maximum of the ozone
      concentrations predicted by
    RACM and RADM2 mechanisms
             plotted against
      SAPRC experimental values.
    600
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500-



400-



300-



200-



100-
      0
                             X  RADM2

                             O  RACM
0    100   200   300   400   500   600

 Experimental Time of Ozone Maximum, Min
                                               Maximum NO2 concentrations
                                              predicted by RACM and RADM2
                                                mechanisms plotted against
                                                SAPRC experimental values.
                                                                      X  RADM2

                                                                      O  RACM
                                                       0.0    0.2     0.4     0.6    0.8     1.0

                                                            Experimental Maximum NO2, ppm
William R. Stockwell

Reactivity Calculations with the Regional Atmospheric Chemistry Mechanism
Fraunhofer Institute for Atmospheric Environmental Research I [FU)
                                          William R Stockwell

                                          Reactivity Calculations with the Regional Atmospheric Chemistry Mechanism
                                          Fraunhofer Institute for Atmospheric Environmental Research (IFU)

-------
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       Effect of Revisions on
       Ozone and PAN
         40
                 234
                   Time, days
                                            —i—i—i—i—r
                                            234
                                             Time, days
                               4-10

-------
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                                       E3 RCO3*NO
                                          [Villenave etal., submitted]
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-------
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              Initial Conditions for
  Incremental  Reactivity Calculations
            Start Time (Local Hour)         3:00
            End Time (Local Hour)         22:00
            Temperature (K)             298.15
            Pressure (mbar)            1013.25
            Photolysis Frequencies  July 01, Latitude 45*
Initial Concentrations
Species  (ppb)
O3       50
        2.0
        0.2
        0.5
        0.1
        1.0
        200
       1700
        500
H202
NO
NO2
HN03
HCHO
CO
CH4
H2
      H20
      02
      N2
         1.0
        20.9
        78.1
                          Emission Rates
                          Species
                          NOX
                          SO2
                          CO
                          Ethane
                          Low Reactive Alkane
                          Medium Reactive Alkane
                          Highly Reactive Alkane
                          Ethene
                          Internal Alkene
                          Terminal Alkene
                          Toluene
                          Xylene
                          HCHO
                          Aldehyde
                          Ketone
                                                      Emissions
                                                      (ppb mln'1)
                                                        Varied
                                                      5.18 x1(H
                                                      5.65 x 10-3
                                                      2.41 x 10-4
                                                      2.94 x 10-3
                                                      7.70 x 10-4
                                                      4.52 x 1(H
                                                      4.56 x 10-»
                                                       1.88x10-*
                                                       2.19 x
                                                       5.72 x
                                                       5.19 x1(H
                                                       1.39X10-4
                                                       3.62 X10-5
                                                       5.02 x1(H
                        4-12

-------
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                           RACM Mechanism
                 NOX Variation for PLUME/2 Case, Day 1
                            EBIR
                                   MOIR
                                             \
                                                 MIR
                        5          10         15

                        Initial + Emitted NOX (ppb)
                                                           7.5

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                                                                   	 Max O3 (ppb)


                                                                   	 IR NOX


                                                                   	 IR VOC * 10


                                                                   	 IR VOC





                                                                    July 01 Latitude 45


                                                                    Start Time = 3:00


                                                                    Stop Time = 22:00


                                                                    Total Time = 19 h
                                                           -2.5  S

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                                        4-13

-------
      Maximum  Incremental
      Reactivity  (MIR) vs kHO
  10
DC
 0.1-
                 HCHO
                   Terminal
                    Alkene
                                 Internal
                                 Alkene
          Ethenex.
                •__^_«
            Aldehyde /£>   \ Isoprene
       Toluene	0   / Xylene «  K
     Low
   Reactive
    Alkane \
/
     Ketone
Ethane
     CO
             .SO
           d-Limonene
      cc-Pinene
*—Middle Reactive Alkane
   *\
    Highly Reactive Alkane
0.01
 1.0E-13
     1.0E-12    1.0E-11   1.0E-10

           (cm^molecule"1s"1)
                 1.0E-09
            Conclusions

• We  strongly  recommend  the
  RACM  mechanism  for  use  in
  atmospheric  chemistry  models
  over  the  RADM2  because  the
  RACM chemistry is  based upon
  more  recent and  reliable data.

• Compared with the  RADM2 the
  RACM predicts concentrations:

    - somewhat greater for  03,
      H2SO4 and HNO3
    - almost the same H2O2
    - significantly less PAN.

• The extended  RACM has been
  applied  to ozone   incremental
  reactivity calculations for rural
  European conditions.

• We have estimated  incremental
  reactivities of isoprene, terpenes
  and dimethoxymethane.
   William R. Siockwell

   Reactivity Calculations wilh ihe Regional Atmospheric Chemistry Mechanis
   Fraunhofer Institute for Atmospheric Environmental Research (IFU)
                                          William R. Stockwell
                                          Reactivity Calculations with the Regional Atmospheric Chemistry Mechanism
                                          Fraunhofet Institute for Atmospheric Environmental Research (UFU)

-------
    Hydrocarbon reactivity and ozone production in urban pollution according to the

                       Stockwell et al., (1990) reaction mechanism


                                     Chris J. Walcek
                          State University of New York at Albany


Abstract- A method for ranking the ozone production potential for various classes of reactive

hydrocarbons is presented. Using the Stockwell et al.,(1990) chemical reaction mechanism

("RADM2"), ozone production efficiencies for 14 classes of emitted hydrocarbons included in

the mechanism are quantified over a wide range of background NOX and hydrocarbon

concentration regimes. 63 production efficiencies are calculated by running a box model

initialized with specified concentrations for a 2-day period under fixed sunlight and

meteorological conditions, after which NOX is oxidized and ozone production ceases. Individual

organic compound concentrations are then perturbed by 1 ppb, and the resulting changes in 63

after 2 days are compared with the base  simulation. For some ranges of NOX and organic

compound concentrations, the additional ppb of 03 produced  from each additional ppb of organic

compound is somewhat constant, but there are  some compounds under some chemical conditions

for which the additional ozone production potential is highly variable. Despite these variations,

net ozone production from each class of organics is approximately correlated with the

corresponding reactivity of the organic compound with HO radical, although there are some

broad violations of this correlation. HO  reactivity may only crudely be an indicator of ozone

production potential under many conditions for some classes of organic compounds.
                                           4-15

-------
o\
                Hydrocarbon reactivity and ozone production in

                        urban pollution according to the

                  Stockwell et al., (1990) reaction mechanism
                                     Chris Walcek
                             Slate University o( New York at Albany
1. Simple method for calculating
    "ozone productionefficiency"
                       2. Detailed description of a couple "cases"
                       3. Generalized results for wide range of
                           NOx and hydrocarbon concentrations
                       4. Conclusions
                                                                  Ozone concentration change in
                                                                    air parcel, calculated using
                                                                      Stockwelletal., (1990)
                                                                            mechanism
                                                                                          33.0
                                                                                            11.40 1145 11:50 11:55 1200 12:05 12:10
                                                                                                   Local 11m* (hrmln)
                                                                      noon conditions,
                                                                      50% clear-sky photolysis rates
                                                                      20 'C, 50% Rh; 1.8 ppb isoprene

-------
  Ozone formation rates vs
 concentrations of NOx and
hydrocarbon concentrations
                                                                 Ozone concentration (ppb) vs time
 0.1     1     10    100    1000   10000
 non mathana, r»actlv* organic concentration (ppb C)
          noon conditions
          April, 40'north
    50% clear-sky photolysis rates
              20'C
             50% Rh
          1.8 ppb isoprene
                                                       a
                                                       Q.
                                                       a.
                                                       c
                                                       o
                                                                 Initial N0x=   10 ppb
                                                                     NMHC=100ppbC
Base Case
+ 1 ppb Acetaldehyde
  Initial NOx=   1 ppb
      NMHC= 10ppbC
                                                                                time (hours)

-------
oo
              NOx and Organic concentration vs. time
                   Q.
                   a.
                   c
                   o
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                  2
                   
-------
               (qdd) uojjejjuaouoD auozo
 Perturbation ozone concentration induced by 1
      ppb increase in various hydrocarbon
'.    Initial NOx=10ppb; Initial NMHC-100ppbC
                                                          Carbonyls
                                                           Alkanes
                                                                  ETH
                                                                  HC3
                                                                  HC5
                                                                  HC8
                                                           Alkenes
                                                           Aromatics
                                                                    TOL
                                                                    XYL
                                                                    CSL

-------

Aromatics    Change in accumulated ozone (ppb) after
                 two days due to change in initial specified
                               organic by 1 ppb
Toluene
(& less reactive)
TOL
                001 -
                  0.1     1      10    100    1000  10000

                  non methane, reactive organic concentration (ppb C)
              >' 10OO
                0.01
                  0.1     1      10    1OO    10OO   10000

                  non methane, reecllve organk concentretlon (ppb C)
               1000
                   $ 100

                   I
Cresol              |  10
(& other             Z
  hydroxy-substituted)  g  ,
CSL
                o.oi
                  0.1     1     10    100    1000   10000

                  non methane, reactive organic concentration (ppb C)
             Olefins (Alkenes)

Change in accumulated ozone (ppb) after
two days due to change in initial specified
              organic by 1 ppb
                                                                         Ethene OL2
                                                                                                                Terminal alkenes OLT
                                                                        01     1     10    100    1000   10000     0.1     1      10     100    IOOO   10000

                                                                        non methane, reactive organic concentration (ppb C)     non methane, reactive organic concentretlon (ppb C)
                                                                          Internal alkenes OLI
                             Isoprene ISO
                                                                        0.1     1      10    100    1000  10000

                                                                        non methane, reactive organic concentration (ppb C)
                                                                                                               	_!_//£__
                           0.1     1      10    100    1000   100OO

                           non methane, reactive organic concentration (ppb C)

-------
Carbobvls
/aldehydes)
v  ueiiyue*/
                   Change in Accumulated ozone (ppb) after
                   two days due to Cnan9e in initial specified
                                  organic by 1 ppb
                     1000
       Formaldehyde
       HCHO
                     0.01
                        0.1     1      10     tOO    1000  10000
                        non methane, reactive organic concentration (ppb C)
                      100
_^     Acetaldehyde |   10
'      (& higher aid) |
I-     ALD         I   ,
                      o.i
                        0.1     1      10     1OO    1000  10000
                        non methane, reactive orgenic concentration (ppb C)
          Ketones
          KET
                               1      10     100    1000  10000

                        non methane, reactive organic concentration {ppb C)
                   Alkanes
Change in accumulated ozone (ppb) after
two days due to change in initial specified
               organic by 1 ppb
                                                                                Ethane ETH
                                                                                                                         Slow reactive HC3
                                                                                           10    100    1000   10000
                                                                              non methane, reecllve orgenic concentration (ppb C)
                                                                                Intermediate reactive HC5
                                                                                                                                                   _J
                                                                                                                      0.1     1      10     100    1000   10000
                                                                                                                      non methane, reactive organic concentration {ppb C)
                                                                                                                        Fast reactive HC8
                                                                                                                   o.oi
                                                                               0.1      1      10    100   10OO   10000      0.1      1      10     100    1000  10000
                                                                               non methane, reactlva organic concentration (ppb C)      non methane, reactive organic concentration (ppb C)

-------
                    Change in Accumulated ozone (ppb) after
                   two days due to 1 ppb change in initial NOx
Ozone "production efficiency" from hydrocarbons
    in the Stockwell et al., (1990) mechanism
initial conditions: 10 ppb NOx, 100 ppb(C) organic
   after 48 hours, continuous noon conditions
        NOx
        (NO + NO,)
to
S)
                          0.01
                             0.1     1      10     100    100O  10000

                             non m«lh«n«, rucllv* orginlc concentration (ppb C)
        y - 2076.7 * 10*(0.94024x) • R*2 - 0.7«S

                                -T—~-_

                                 1 ISO
                                                                                                     v-r-v?;-'.-•Tway
                                                                                             -05
                                                                                                       00        0.5       1.0       1.S        2.0

                                                                                                            ppbO3 produced p«r MtdNlonil ppb orginlc «dd*d

-------
              Correlation coefficient (r) between

           (a) change in accumulated ozone (ppb)
               due to 1 ppb change in all organics
                            vs.
           (b) log (rate coefficient for reaction of
                     each organic with HO)
to
                  0.01
                    0.1     1      10    100    1000  10OOO
                    non m»th«n«, rwctlv* organic concentration (ppb C)
          Joint probability distribution:
 NO» and nonmethane hydrocarbon concentrations
% probability of observing concentration per 1/3 logio
            concentration range
  900 - 950 mb. Northeast U. S.. 21-24 April 1981
            (RADM 35x38 domain)
                                                                                 1000
        i       10      100      1000
             Non mathan* organlca (ppb)
                                     10000

-------
  MULTI-DAY OZONE FROM
  LOW-REACTIVITY VOC's
              by
       Gary Z. Whitten
       Systems Applications International
Overview

I Concern for downwind areas
I New technique based on UAM
I Compares candidate VOC to ethane
I Provides incremental impacts
              4-24

-------
UAM-BASED TECHNIQUE
  VOC increment added to upwind cells
  Uses "back" trajectory from final peak cell
  100 tons ethane for base case
  Spread over 9 cells over 1 hour
  Use explicit chemistry for ethane and
  candidate VOC
Example Candidate VOC

I l-bromopropane
  I Same k^ by weight as ethane
  I Molecular koH 4 times faster
I Chemistry assumed to be like propane
  I Molecular k^ same as propane
                4-25

-------
UAM  Results
I 1st day both nearly 14 ppb impact
   I  Not at main peak (cloud not there yet)
I 2nd day impacts differ
   I  ethane 4 ppb (on peak of 190)
   I  candidate only 2.3 ppb
I 2nd (off peak impacts)
   I  ethane 7.8 ppb
   I  candidate 4.8 ppb
      LEVEL I Ozon* (ppb)
      Time 4-2
-------
   LEVEL I  Oioni (ppb)

   Time  0-2400 August 27. 1987
                                                                 UAXIUl'M   1.1 9 pj.h

                                                                 UINIUUU «  04 ppl.
 275	325	375	425	475	525         575
401  i i i i  i i i i  | | ii i I I  I i I I  | I i I I  I I I  I i | i i  i i i i i  i i | i i  i i i i i I I | I  I i I M II i| i l-r'1
                                                                                     7JO
                                                                                    3670
   Difference in Maximum Simulated Ozone Concentrations

   August 27,  1967  (Simulation   100 ton ethane  minus base)
LEVEL 1 Ozone (ppb)
Time .0-2-100 August 27  1987


75	325         375
  I  I I I I  I I I  I I I I I  I I I  I I I I  I
30
20
10
                                                                  * MAXIUl M . 139 pph

                                                                   MINIMUM   -0 fl pph
                                       425
                                                   475	525	575      _,D_
                                                   i I i i i  i i i i  i i [ i i  i i i i  i i i I  i i i i j 38 i I)
                                                                                   3770
                                                                                   3720
              10
                          20
                                       30
                                                   40
                                                               50
                                                                           60
                                                                                   3670
   Difference  in Maximum Simulated  Ozone Concentrations

   August  27. 1987   (Simulation  100 ton bromopropane minus base)
                                      4-27

-------
  LEVEL I Otone (ppb)
  Tim. 0-2400 AugUJl 28.  1967
                              MAXIMUM  • 7 6 ppli

                              MINIMUM • -0 J pph
                                                                           575
                                                                                r r 3H70
                                                                            60
  Difference in Maximum Simulated Ozone Concentrations
  August ZB. 1967  (Simulation   100 ton ethane  minus base)
   LEVEL 1  Ozon* (ppb)
   Tim^ 0-2JOO August  28  1987


.275	325	375
•JUi i ' ' i i  i i i  i I i '  i i i i  i i i i i  i
20
10
                             *  MAXIMUM   < 8 ppb

                               MINIMUM   -0 I  pph
 425         475
I I |  I I I I 1  I I I I  | T I
                          525
575
 Q1 '  ' ' ' '  ' ' ' ' ' ' '  ' ' ' ' '  • I I 1 I  ' I I I  I I ' I	Nil
              10
                          30
                                      30
                                                   40
                                                               50
  Difference  in Maximum Simulated Ozone Concentrations

  August 26. 1987  (Simulation   100 ton bromopropane minus base)
                                                                                   < 38 .'I I
                                                                                   \
                                                                           60
                                                                                    3770
                                                                                    3720
                                                                                   3670
                                  4-28

-------
                                       Abstract
          Computing Volatile Organic Compound Reactivities with a 3-D AQM
                                      Zion Wang
                              University of North Carolina
                                     at Chapel Hill
In many urban areas, selective VOC control on reactive VOCs is much more advantageous over
indiscriminate control.  This raises the need for identifying reactive VOCs.  One of the currently
used methods to quantify VOC reactivity is by measuring how changes in VOC emissions in an
airshed affect ozone formation in the same airshed with the EKMA modeling method. However,
due to simplifications in the dispersion component of the model and in the ambient conditions and
emissions inputs, the use of three-dimensional photochemical models to obtain reactivity data is
desirable. This study attempts to use a three-dimensional photochemical model to compute the
reactivity data for a few VOC species. The study also examines how different parameterization
techniques impact reactivity calculations.
                                      4-29

-------
   Box Modelling of NOx and VOCs to Determine Emission Reduction Strategies

                                  PA. Makar
                        Atmospheric Environment Service
                    Environment Canada, 4905 Dufferin Street
                     Downsview, Ontario, Canada, M3H 5T4
                              paul.makar@ec.gc.ca
                                   T.Dann
                   Environment Canada, River Road Lab, Ottawa
                                   D. Albin
                               MYDA Consulting

                                 May 25, 1998
Abstract:
      Measurement  data from  the  Canadian National Air  Pollution  Surveillance
monitoring network was used to provide initial conditions for a series of sensitivity runs
of a box model of local  chemistry.  The sensitivity runs were used to determine the
factors having the greatest impact on ozone concentrations at 15 sites in urban centres in
Canada.   Sensitivities  to NOX  were either  zero  or negative,  indicating  that  the
measurement sites  were likely VOC limited and subject to NOX titration of ozone.
Decreases in model Nox at these sites led to increases in ozone production by the model.
Sensitivities  to total  VOC and  ten major  unoxygenated  VOC classes  were positive,
indicating that reductions in VOCS would result in decreases in ozone concentrations.
Specific VOC classes had a much greater effect than others, with internal-bond alkenes
and higher aromatics having the greatest impact on ozone production.

Model Description:
      The photochemical model employed had three main components:
(1) A gas-phase chemical mechanism (Makar et al, 1998) used as input for the model
   chemical calculations. The mechanism employed has been under development for
   several years at AES, and is intended as a replacement for the regional model
   mechanism of ADOM. The major revisions to the species of the previous mechanism
   include:
      the inclusion of three additional PAN-like species
      the inclusion of CO and C2H6 as advected, non-constant variables of the system
      the separation of higher alkanes into C4-C5 and C6-C8 species
      the separation of higher alkenes into terminal and internal double bond species
      the separation of higher aromatics into di and tri substituted species
      the inclusion of species-specific RO2s and R(O)O2s
      the inclusion of six (previously one) higher carbonyls
      the inclusion of formic  acid, acetic acid, and C1-C3 alcohols
      the inclusion of HNO4  as an advected species.

      The new mechanism has 251  reactions, compared to  the ADOM mechanism's
114. Some of the more important revisions include:

                                     4-30

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•      All  reactions retained  from the ADOM model have rate constants  updated
       according to the most recent data for those reactions.
•      Inclusion of specific RO2+RO2 reactions and their products
•      NO3 + RO2, NO3 + R(O)O2 reactions included
•      Much greater detail in  the formation of oxygenated products from the original
       nonoxygenated VOCs.     Aside from the greater speciation, the formation of
       products of higher alkanes, alkenes, and aromatics has been altered to incorporate
       recent laboratory studies on these species. The aromatic mechanism now includes
       the highly reactive broken ring  products and dicarbonyls known to form after the
       initial oxidation by OH, O3 and NO3.
•      A more detailed isoprene  mechanism,  including the formation of MACR and
       MVK and MPAN has been included.
•      Higher Terpenes have been included as a separate species.
•      All photolysis rates  have been updated according to the most recent information
       available.
(2) A one-dimensional radiative transfer subroutine.  This model (Yung, 1976) was
    used to calculate the intensities of light as a function of wavelength at each site for
    which the model was applied. The radiative transfer model made use of the US
    Standard Atmosphere (1976) for ozone and total column number density information.
    Solar zenith angles were calculated using the latitude, longitude, local time and time
    zone of each  site  for  which  calculations were performed.   The resulting solar
    intensities were used to calculate photolysis rates for the chemical model.
(3) A numerical solver to  solve the system of differential equations resulting from the
    chemical mechanism.   The solver used here was  that of Kahaner et al (1989),  a
    variation on the predictor-corrector code of Gear (1971). The same solver was set up
    by the  author  of  the current work for  use  as the numerical driver in the AES
    CREAMS box  model.

    As input data, the model  made use of the  NAPS database.   The National  Air
Pollution Surveillance database includes time coincident NOX and VOC measurements
made at several sites across  Canada, from 1986 until the  present. A subset of 15 sites was
used in the current study. VOC measurements include standard testing for 175 different
species.  These were lumped into  the model speciation using the reactivity weighting
method of Middleton et al, (1990).
       Unfortunately, until  1996, the NOX data was usually only  reported  to the nearest
10 ppbv. In addition, the records contain only a total NOX  expressed as NOi.   The lack
of more detailed NOX data presents an important confounding factor to the conclusions of
the study, as is noted below.
                                      4-31

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Methodology:

       A model run  of an  individual record would take place  through  the following
stages:

(1) A  measurement   record,  consisting  of  the  site  latitude,   longitude,   time
   (year,month,day, start hour, end hour, time zone), NO2, NO, NOX, O3,  CO, SO2, and
   VOCs was read in by the model.
(2) Most of the NAPS records did not have NO reported as a separate variable, and the
   NOx and NO2 concentrations were usually equal.  Initial concentrations of NO2 and
   NO were calculated using the following stages:
       (a) If NOx was reported, and NOx=NO2 in the record, then it was assumed that
          the NO concentrations were less than the 5 ppbv, and the model mechanism
          was used to generate an initial NO concentration by assuming  a steady state
          with the other model variables. The same process was used if  only NO, was
          reported (a smaller number of stations reported NOX, and zero NO2 and NO).
       (b) If both NO2 and  NO values were reported, those values were used as  initial
          conditions.
(3) Following initialization of NOX, the model was run forward in time for one hour to
   initialize the other variables.  If the site was located in  a city, the concentrations of
   NO, NOa, CO, SOa  and the unoxygenated VOCs were held constant during this
   initialization, simulating the replenishment of these variables by emissions. If the site
   was considered to be rural, then all variables aside from methane,  water vapour,
   oxygen and the tqtal number density were allowed to vary with time. Table 1 gives a
   listing of the stations, and their categorization  as rural or urban.  This  procedure
   allowed the  generation  of initial concentrations for the  other model species (eg.
   oxygenated  hydrocarbons,  organic  peroxides, hydrogen peroxides, radicals,  etc.).
   These were used as initial values these species in the sensitivity runs which followed.
   The idea here was to allow the chemical model to "spin up" slightly, to avoid the
   sensitivity calculations being  affected by the initial conditions for the unmeasured
   species.
(4) Twenty-five sensitivity runs were then performed on each record.  For urban runs, the
   concentrations of NO and the ten unoxygenated VOCs {ethane  (C2H6),  propane
   (C3H8), C4-5 alkanes (C4AK), C6-8 alkanes (C7AK), ethene  (C2H4),  terminal bond
   alkenes (as  propene; PRPE),  internally bonded  alkenes (as trans-2-butene; BUTE),
   toluene (TOLU),  di-substituted  aromatics  (DARO) and  tri-substituted  aromatics
   (TARO)} were held constant at the measured (or calculated, as was often the case for
   NO) values, once again in an attempt to mimic the emissions dominated regions. For
   rural runs, all species were allowed to vary with time, the above species having their
   initial concentrations taken from the measurements.
       The twenty-five runs consisted of
           •  A Base run:  1 hour integration as described above.
           •  Two NOx runs:  NO increased and decreased by 25%, relative to the base
             run.

                                      4-32

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          •  Two Total  VOC runs:  the hydrocarbons  listed above all increased or
              decreased by 25%, relative to the base run.
          •  Two individual VOC  runs for each of the ten VOCs listed above,  with
              increases and decreases of 25%, relative to the Base run.
(5) The output  data  from  the  runs were used  to calculate sensitivities  of ozone
   concentrations to the given perturbation by fitting the three data points (+25%, base, -
   25%) values to a  parabola, then calculating the resulting derivative of ozone  with
   respect to percent change in the particular variable).
       The concentrations of biogenic hydrocarbons were not affected by the sensitivity
runs; isoprene and alpha-pinene were treated like the other unoxygenated VOCs, but no
sensitivities  were calculated.
       The  resulting output was a  list of sensitivities of ozone towards each of the
perturbed variables, in units of change of ozone concentration per percent change in the
parameter from its measured concentration (AO3 / A variable; units (ppbv/%)).  Positive
sensitivities  indicate that a decrease in the variable will result in a decrease in ambient
ozone concentrations.  Negative sensitivities indicate that a decrease in the variable will
result in an increase in ozone concentrations.

       Results:
       The records were analyzed in two groups:  cases for which ozone concentrations
were greater than 70 ppbv (G70) and cases for which ozone concentrations were less than
50 ppbv (L50).   Here, only the summer (July and August) O3 > 70  ppbv cases will be
examined in detail.

       The  results for these records are shown in Figures 1 to 7.  Figure 1 shows the
sensitivity of model ozone towards changes in NO. Regional differences are apparent in
these stations. Stations in Windsor, Toronto, Hamilton and Sarnia all show that decreases
in local NO concentrations  would  lead to increases in ozone concentrations.   This
probably indicates  the effects of local ozone titration;  if the NO  concentration was
decreased, then ozone concentrations close to the emissions sources would increase due
to a reduction in importance of the NO +  Os  removal pathway.  In Simcoe  and
Stouffville,  this effect is  less apparent.  In the three west coast stations (Coquitlam,
Surrey, Langley), changes in the  NO concentration had little  effect on the ozone
concentration.
       Figure 2 shows the effect of changes in total VOCs.   For all sites, sensitivities
are positive; VOC reductions result in  ozone decreases.  The greatest reductions  as  a
function of percent change in the local VOC concentration are for Coquitlam, Sarnia and
Windsor (note:  the Coquitlam value is the result of only three  records, and must be
considered less statistically significant than the other cases).  Figure 2 shows that a 25%
reduction  in total VOCs  would result in a reduction in  ozone concentrations during
episodes of about 15 ppbv (0.6 ppbv/% x 25%).
       Figures 3 and 4 show die sensitivities towards the two VOCs which  had the
greatest impact on ozone concentrations  out of  the ten for  which  sensitivities  were
calculated. They show the effects of targeting particular VOCs for emissions reduction.

                                       4-33

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       Figure 3 shows the sensitivity to BUTE; the internally bonded alkenes.  Urban
Ontario values are between 0.05 and 0.25 ppbv/%.   Simcoe, Stouffville, Surrey and
Langley have virtually no change.  Coquitlam values are very sensitive to changes in
BUTE.
       Figure 4 shows Tri-subsituted aromatics, with sensitivities of about 0.03 ppbv/%
being typical.
       The  remaining  species  have  progressively  smaller  effects  on  the  ozone
concentration.   In decreasing order of importance, they are:  Toluene, Di-substituted
aromatics,  C6-8  Alkanes, terminal-bond alkenes,  ethene,  C4-5 Alkanes, Propane and
Ethane.
       These results suggest that targeted reductions of internal-bond alkenes, followed
by higher aromatics would have the biggest effect on local ozone concentrations in  most
of  southern  Ontario.  Certain   VOCs (those  with both  high  reactivity  and  high
concentrations) result in much of the ROi formation  leading to ozone production.

       Figures 5  -  7 show the  sensitivities grouped according to region and plotted
rel uive to each other. The greatest impacts of VOC  controls are  seen in the urban regions
of Ontario, Sarnia and Windsor in particular, followed by Toronto. Impacts of reductions
are smaller in Simcoe, Stouffville and the Vancouver sites other than Coquitlam.  The
latter has a high sensitivity to BUTE as in the Ontario sites, but  this may be due to small
sample size (three records).

       In addition to the summer ozone episode cases, sensitivities were also calculated
for spring episodes ^April to May).  The relative  results were similar to  the summer
episodes for most stations, but the magnitudes of the  sensitivities were smaller.   For
example, the Junction Triangle station's  sensitivity to total VOCs  was  about 0.075
ppbv/% in the spring versus 0.25 ppbv/% in  the summer.   NO sensitivities at the same
site were also lower in spring versus summer, -0.25 ppbv/% versus  -0.4 ppbv/%. The
same pattern of sensitivities for individual VOCs was noted as for the summer cases;
sensitivities tend to be highest for internally bonded alkenes, with aromatics following in
importance.
       The spring data included a single record from Edmonton. Although statistically
insignificant, it is interesting to note that the NO sensitivity was still  negative, and that
the pattern of VOC  sensitivities has changed.  Di-substituted aromatics have the greatest
impact on ozone  concentrations, followed by toluene,  propene and the C6-C8 alkanes.
Further episode measurements would be required to determined  whether this reflects true
regional differences in the ozone production due to hydrocarbons.
       A large number of records with ozone less than 50 ppbv were examined to see if
the sensitivities  of ozone  production due to NOX or  VOCs  differed  between ozone
episodes and non-episode scenarios.  The sites show the same pattern  as for the summer
cases, with negative NO sensitivities, positive VOC  sensitivities, with butene followed by
the higher  aromatics leading the  VOC sensitivity magnitudes.  The magnitudes are
smaller than for ozone (>70 ppbv) episodes (eg. Windsor VOC sensitivity 0.25 versus 0.5
ppbv/%); VOC controls will have a smaller impact on non-episode situations than during
episodes.  Figure  22 shows the  sensitivities for  the Rocky Point site at Coquitlam, BC,
                                     4-34

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with negative NO sensitivities and positive VOC sensitivities, internally bonded alkenes
(BUTE) being the most important of the latter.

       Discussion:

       The results from these tests suggest the following:

       (1) At the sites for which ozone episode data was available, decreasing local NO
          concentrations would lead to increases in ozone.  Provided that this was not a
          result of model setup (see  below), this would  suggest that  NOX reduction
          strategies in the vicinity of urban areas would actually lead to local increases in
          the ozone concentrations.
       (2) At all sites, reductions in the  total VOC loading resulted in immediate local
          ozone decreases.  These reductions in ozone concentrations were greatest for a
          total, across the board VOC cut, but more detailed work showed that specific
          VOCs  (in  order of precedence: internally bonded  alkenes, tri-substituted
          aromatics, di-substituted aromatics, and toluene) probably make up most of the
          VOC effects. These VOCs are both sufficiently reactive and have sufficiently
          high concentrations to have a significant local impact on ozone production.
       (3) The direction (if not the magnitude) of the sensitivities was the same for cases
          in which the ozone concentration was less than 50 ppbv.   This would suggest
          that a strategy in which different components of the reactive mix are targeted
          for reductions at different times seems unnecessary.  The same VOC reduction
          strategy m#y be used regardless of whether an ozone  episode is taking place;
          VOC reductions during low ozone days will not have adverse effects.
              Two confounding factors should be noted at this point.
              NOX concentrations,  and NOX sensitivities. As  was mentioned above, the
       NO2 and NO concentrations in  the NAPS database were  usually reported only to
       the nearest 10 ppbv, and usually total NO* was reported as NO2. The strategy of
       determining NO concentrations  from the use of steady-state may have led to errors
       in the sensitivities  in  two  ways; through lack of  accuracy in  the original
       measurements, and through the  use of steady-state to generate NO concentrations,
       followed by perturbations from  that steady-state to generate sensitivities.
              Assumption  of local emissions via constant NO and  VOCs.   Another
       source of uncertainty (for the urban sites) is the assumption of a local emission
       source (ie.  the concentrations of NO  and  unoxygenated VOCs  being  held
       constant; the level being changed for sensitivity calculations). The effect of these
       uncertainties  can only be resolved with more accurate measurement data and
       further model runs, as discussed below.

              Conclusions and Plans for Future Work:

       The  work performed here indicates that the  NAPS sites  studied have positive
sensitivities of ozone  production with respect to VOCs, and  negative sensitivities with
respect to NOX.   NOX  reductions  at the given sites could lead to increases in local ozone.

                                      4-35

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VOC reductions will reduce local ozone, and specific VOCs (internally bonded alkenes,
followed by aromatic compounds) can be targeted as having the greatest local impact on
ozone production.

       It should be noted that significant uncertainties exist in the NOX conclusions, due
to the limitations on the measurement accuracy and  the assumptions in the use of the
measurements.  The following steps are recommended for future work to resolve these
uncertainties:
   (1) The use of more accurate NOX data (ie. both NO and NO2 resolved, with ppbv or
      better accuracy) from measurement intensives (eg. Pacific 93, NARSTO). These
      can be used to test the effect of the NAPS data being reported in lOppbv intervals;
      the intensive data can be degraded in the same  fashion as the NAPS data, and the
      resulting model  output compared  to  that resulting from  the  true  NOX initial
      conditions.
   (2) The effect  of the "emissions" boundary condition can easily be tested with the
      current  data set and model;  all  species can be  made time variables with the
      measurement data providing an initial condition only.

   References
Gear, C.W.,   1971:   Numerical  Methods  for Initial  Value Problems  in  Ordinary
   Differential Equations. Prentice-Hall, Englewood Cliffs, New Jersey.
Kahaner, D., C. Moler, and S. Nash, 1989: Numerical Methods and Software, Prentice-
   Hill, Englewood Cliffs, New Jersey.
Makar, P.A., S-M. U, P.B.  Shepson and J. Bottenheim,  1998:   The AES Gas-Phase
   Mechanism for Tropospheric Chemistry:   Theoretical  Formulation:  AES Internal
   Report, Atmospheric Environment Service, Downsview, Ontario (In preparation).
Middleton, P., W.R. Stockwell, and W.P.L.  Carter, 1990:  Aggregation and analysis of
   volatile organic compound emissions for  regional modelling.   Atm.  Env., 24A, pp
   1107-1133.
Yung,  Y.L.,  1976:  Numerical  Method  for   Calculating  mean intensity  in  an
   inhomogeneous Rayleigh-scattering atmosphere. J. Quant. Spec. 16, pp755-761.

Tables:
1. NAPS stations included in this study.

Figures:
1. Sensitivity of model ozone with respect to changes in NO, Summer O3 > 70 ppbv episodes.
2. Sensitivity of model ozone with respect to changes in Total VOCs, Summer Oj > 70 ppbv
   episodes.
3. Sensitivity of model ozone  with respect to changes in BUTE; internally bonded alkenes,
   Summer Os > 70 ppbv episodes.
4. Sensitivity of model ozone with  respect to changes in  TARO;  tri-substituted  aromatics,
   Summer Os > 70 ppbv episodes.
5. Sensitivities of model ozone with respect to NOx and VOCs, Southern Ontario Stations
   outside Toronto, Summer O3 > 70 ppbv episodes.

                                     4-36

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6.   Sensitivities of model ozone with respect to NOx and VOCs, Toronto stations, Summer O3 >
    70 ppbv episodes.
7.   Sensitivities of model ozone with respect to NOx and VOCs, West Coast Stations, Summer
    O3 > 70 ppbv episodes.
                                      Table 1.
NAPS#
30118
60204
60403
60413
60418
60422
60424
60512
61004
62601
63201
90130
100111
100127
101301
ST. NAME
Roy Building
UIC Building
Evans & Arnold
Elmcrest Rd.
Junction Triangle
33 Edgar Ave.
Bay and Grosvenor
Beasley Park
Centennial Park
Experimental Farm
Hwy 47 & Hwy 48
10255-104* st.
Rocky Pt. Park
Surrey East
Langley Central
NEAREST
CITY
Dartmouth
Windsor
Toronto
Toronto
Toronto
Toronto
Toronto
Hamilton
Sarnia
Simcoe
Stouffville
Edmonton
Coquitlam
Surrey
Langley
PROV.
N. Scotia
Ontario
Ontario
Ontario
Ontario
Ontario
Ontario
Ontario
Ontario
Ontario
Ontario
Alberta
B.C.
B.C.
B.C.
CITY/
RURAL
(OR)
C
C
C
C
C
C
C
C
C
R
R
R
C
R
C
                                     4-37

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                                                 Figure 1.
                     Sensitivity of Model O3 to NO vs Collection Station
                              Summer Ozone Episodes Greater Than 70 ppbv
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               Toronto        Toronto         Toronto         Sana         Stoutfville        Surrey
                                                STATION
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                         Sensitivity of Model O3 to VOC vs Collection Station
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                    Toronto         Toronto        Toronto         Samia        StouffviBe         Surrey
                                                    STATION
                                                    4-38

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                                    Figure 3.

            Sensitivity of Model O3 to BUTE vs Collection Station
                     Summer Ozone Episodes Greater Than 70 ppbv

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                                    Figure 4.

            Sensitivity of Model O3 to TARO vs Collection Station
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                                       STATION
                                       4-39

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                      Figure 5.
Sensitivities of OS Production to NOx and VOC
     Summer Ozone Episodes Greater Than 70 ppbv
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Figure 6.
Sensitivities of O3 Production to NOx and VOC
V
Summer Ozone Episodes Greater Than 70 ppbv
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                        4-40

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Comparing the full time series	
                Correlation between
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-------
               And the synoptic perturbation
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                                 Conclusions

                                     [••   Shows promise as an approach for developing a
                                         "modeled ozone  climatology"
                                             *••   applications in weight-of-evidence
                                                  component in SIP
.fx
^                                   r*   Model performance seems good
00                                           *»   need to ensure that we're not "getting
                                                  the right answers for the wrong
                                                  reasons"
                                         Demonstrates the importance of modeling the
                                         time dependence of biogenic VOC emissions
                                             *»  gives an indication of the temperature
                                                 dependence that is well known for
                                                 ozone in the Northeast

-------
                                        Abstract
                   TVA's Research In Tropospheric Ozone Mitigation
              and Contribution of Natural Hydrocarbons to VOC Reactivity
                                 Roger L. Tanner, Ph.D.
                    Atmospheric Sciences & Environmental Assessments
                           Environmental Research and Services
                               Tennessee Valley Authority
                              Muscle Shoals, AL 35662-1010
The Tennessee Valley Authority has, through its partnerships with OtNr federal and state agencies,
universities, and private  sector participants, Contributed substantially to the knowledge base
concerning tropospheric ozone. Particularly through participation in the Southern Oxidants Study
(SOS), ;ts field studies and related modeling efforts, new information concerning the formation of
ozone in plumes from urban areas and point sources of precursor NOX and VOC emissions has been
developed. This information is critical in diagnosing whether reductions in NOX emissions, VOC
emissions, or both are most effective in reducing the likelihood of exceedances of the NAAQS for
ozone. These efforts have also provided new insight on whether emissions of NO, from all sources
                      v
produce ozone at the same efficiency when mixed with VOCs found in ambient air. TVA and its
SOS collaborators have also found that, in the Southeast during the "high ozone" season, natural
hydrocarbons and specifically isoprene are the major source of VOC reactivity in ozone formation
processes in non-urban areas. Urban area VOC emissions are clearly important for ozone mitigation
in populated areas, but different strategies may be required for urban and rural areas especially in
light of the new 8-hour NAAQS for ozone.
                                        4-69

-------
  Computational Studies of Oxidant Reactions of Volatile Organic Compounds Relevant to the
  Formation of TropOSpheric Ozone: David A. Dixon. Thorn H. Dunning, Jr., Mloh«l Dupuls

        • Volatile organic compounds or VOCe play a key  role in the global carbon cycle
            - the direct formation of carbon monoxide CO from their oxidation by
        radicals and ozone.
            - primary seed  compounds leading to the formation of aerosols which
        provide reaction sites and act as carriers of condensed  active species

        • Develop a fundamental molecular understanding of the oxidation of VOC's by
        using advanced computational electronic structure methods on  high performance
        computing systems.

        • Calculate the thermodynamio and kinetic information needed to predict
        degradation mechanisms. Provide both novel insights and chemically accurate
        data. Provide spectrosooplo information for identifying  key intermediates.

        • Develop a base capability in the  modeling of rates and mechanisms of oxidation
        processes of importance to the Atmospheric Chemistry  Program.  Such  a
        capability can be used to help guide further experiments and to extend limited
        experimental data into new domains.

        • Reactions of oxidants such as OH. Cl, NOa, and Os with key VOCs
                                                    /,
                                              HC	C.
                                             //    \\
                                            H,C       CH,
                                                             CH38CH3
                    1            2                3
                 a-pinene     {3-plnene         ieoprene


TM&-9  Capabilities and Interest Relative to Atmospheric  Chemistry

 • Reliable predictions of thermodynamic properties of atmospheric compounds
 and intermediates including radical species, including predicting molecular
 structures.

 • Reliable prediction of kinetics of important atmospheric chemistry reactions
 (rate constants from ab initio molecular theory, variational transition state  theory,
 tunneling effects).

 • Models of reaction mechanisms and pathways.

 • Thermodynamics of cluster formation.

 • Global warming potentials (infrared  intensity calculations).

 • Predtotions of exerted state chemistry.

 • Focus on aerosol formation from natural and anthropogenic sources.

 • Expertise In stratospheric chemistry, tropospheric degradation processes,
 cluster formation, and global warming potential predictions.

 • Expertise In algorithm development  end software implementation on massively
 parallel computers for development of high performance, portable, and scaleable
 software.

                                     4-70

-------
   EMSL Molecular Science Computing Facility

      A DOE National Scientific User Facility
                                        ZVNWChem
                Experimental Computing Graphic* &• Visualization
                   Laboratory   _^^^   Laboratory
                      Applied Mathematics
                       Computer Science
Molecular Science
   High Performaqce Computing
                     r'acility
   Pacific Northwest National Laboratory
 Multidisciplinary Teams for
 HPC8I Software Development
Computer
Science
                       Applied
                  Mathematics
Application Discipline

  - theories
  - approaches

Applied Mathematics

  - numerical analysis
  - mathematical algorithms

Computer Science

  - software methodolgy
  - software tools
                           4-71

-------
    Molecular Science Software Distributed Computing Model
Molecular Science Computing facility

             ///con/, Mdi/i'lui1^ 
-------
Environmental Molecular Sciences laboratory
      Pacific Northwest National
                Current  NWChem Functionality
      Quantum Mechanical Capabilities:
      •  Hartree-Fock energies, gradients, and second derivatives.
      •  Multiconfiguration self consistent field (MCSCF) energies and gradients.
      •  Density functional theory at the local and nonlocal levels (with N3 and N4 formul scaling)
        energies and gradients.
      •  Many-body perturbation theory (MP2-MP4) energies plus MP2 gradients.
      •  Coupled cluster [CCSD and CCSD(T)] energies.
      •  Single and multireference configuration interaction energies.
      •  Segmented and generally contracted basis sets including the correlation-consistent hasis
        sets under development at EMSL.
      •  Effective core potential energies, gradients, and second derivatives.
      Classical Mechanical Capabilities:
      •  Energy minimization
      •  Molecular dynamics simulation
      •  Free energy calculation
      •  Supports variations such as: multiconfiguration thermodynamic integration or multiple-
        step thermodynamic perturbation, first order or self consistent electronic polari/.ation,
        simple reaction field or particle mesh Ewald, and quantum dynamics
 i.it\ ironnit niul \}i>lt'ciiltir .S
High Performance Computational Chemistry

      I'a i if 1C So rill* < vf .\\ilin/i ill I iil>i-tti!iir\
           Current NWChem Functionality  Targets
                   1F^Classical to Highly Correlated
                              (KT  HF  MP(2-4)   MCSCF   CCSD(T)  MKSDCI  ...
                                        Staling

                                               F
                                                                       »  0.1 kcal


                                                              	     ^  10 atoms
                                                        1 000 bf           500 hf
                                                        100 atoms    5 000 000 CSFs
                                                                      10 - 20 atoms
                                      4-73
                                                 High f'crformance Computational Chemistry

-------
Environmental Molecular Sciences Laboratory
Pacific Northwest National laboratory
      Measured Parallel Efficiency for NWChem -  DFT on IBM-SP;
           Wall Times to Solution for Full SCF Convergence
     32    64    66    126    ISO    182

                Number of Nodes
                                      224
                                           256
Zeolite
Fragment
SflH,
Wi
w»
Wi
Basis AQCD (Number of
Nodes
347/832 64
mm I2X
1199/2X18 256
I6S?H 256
Wall Tire to
Solution
238s
364s
1137s
2766s
                                             High Performance Computational Chemistry

                   Theory, Modeling iV Sinnilnliiin  ^^s=^~=ss=^^^=s=^=
                Required Accuracies for Chemical Qystems:

                 Qeparafions and Catalysts


      •  Absolute Rates (Speedup for Catalysts): Impact on Rates


          - Factor of 10 @ 25°C is AEa = 1.4 kcal/mol


      •  Relative Rates/Equilibrium Constants (Selectivity for Catalysts and Separations):
        Impact on Selectivity


          - Change from a 50:50 mixture to a 99:1 mixture @ 25°C
            Keq =1 changes from Keq = 100

            AO = 0 to AG = 2.8 kcal/mol

      •  There is a dear requirement for accuracy in the computational results.  How is
        this accomplished?
                           i Environmental Molecular Sciences Laboratory/    _

                                    4-74

-------
    Expansion of the Many-Electron Wave Function :
           Methods of Electron Correlation
     MP/i
     (MBPT)
                            Molecular Orbital
                             Wave Functions
             SCF(RHI-VUHF)
                   ^^H
                CISD
                C/SDTO
           CCSO
           CCSD(T)
           CCSDT
                                  MCSCF (CASSCF)
                                                        T
                                    CASPT2
                                                     MRCI
       How to best represent the molecular orbitals:
              Correlation Consistent Basis Sets
     How important are different types
         of Gaussian functions?
  100.0
_  10.0
ui
    i.o
    0.1
                       Oxygen atom
\
                 (g)   (0
            1234

             Number of Functions
                                  4-75
                         Functions are added in correlation
                                consistent shells
                                          cc-pVDZ
                                         cc-pVTZ
                                        cc-pVQZ
                                      cc-pV5Z

-------
                                  CH4


• ID.ICHJ = 419.60 kcal/mol

• ID.(CH4) = 420.71 kcal/mol including core correlation and spin orbit effects?

• ZPE = 27.09 kcal/mol.

• AHf (CHJ = -17.1 kcal/mol at 0 K
• Experimental value of -16.0 _+ 0.1 kcal/mol

• Use of larger A2PE =  27.71 kcal/mol (Grev et.al.): AHr(CH4) = -16.5 kcal/mol


• LD.(CH4) = 419.2 kcal/mol by exponential extrapolation.

• AH,(CH4) = -15.6 kcal/mol based on AZPE = 0.5IV,

 • Use of the Grev value  for AZPE gives AH^CHJ = -15.0 kcal/mol.
                       Organic Thermochemistry & Kinetics

  • Estimates of computer time required for CCSD(T) calculations with cc-pVQZ basis
  sets. Estimates are based on an algorithm that scales as Ne,  rather than the N7
  formal  scaling.

          Molecule     Time (1 TFlop)     Time (100 Tflop)

          CeHe            1 min            0.6 sec
          C8H18            40 min          25 sec
          C,eH34           40 hr            25 min
          C24H6o           600 hr          6 hr

  • Kinetics: Probably requires augmented cc basis sets:  —10 x per point at the
  aug-cc-pVQZ  level
                                    4-76

-------
            Organic oxidation reactions: Thermodynamics
                          ,MI?/DZ+P level and final •wtfes calculated at the
              in projected) level.
 CH3OOH -> CH300' + H'             AHca,c = 86.2 kcal/mol
                                        AHexpt = 87.4 kcal/mol

 CH3OH -> CH30* + H*                AHcalc = 104.0 kcal/mol
                                        AHexpt = 104.2 kcal/mol

 CH4 -> CH3« + H*                    AHcalc = ,03.5 kcal/mol
                                        AHext = 104.8 kcal/mol
                Organic oxidation reactions: Kinetics

• Calculate for the following prototypical reactions
  - the barrier heights, AE*(0), and activation energies.
  - Ea, from transition state theory with a Wigner tunneling correction

• Geometries optimized at the MP2/DZ+P level and final energies calculated at the
PMP4/TZ2PF (spin projected) level.

  CH4 + *OCH3 — > CH3 OH -I- CH3*      AE'(O) =  12.0 kcal/mol
                                         Ea  = 10.2 koal/mol
  CH4 + CHs* — > CHs* 4- CH4          AE*(0) =  19.3 kcal/mol
                                        Ea = 17.9 kcal/mol
  CH4 + *OOCH3 — > CHs* + CHs OOH  AE»(0) = 23.8 kcal/mol
                                        Ea = 21.2 kcal/mol
                              4-77

-------
                   Isoprene Chemistry: 1
  //
    HC — C
          /
            CH,
CH,
          OH       CH3

+ OH —*~    HC— C         +


       •CH2        CH2


             4a
                                      HC'	 C

                                                           CH,
                                      \
                                              CH,
                                                   OH

                                                     4b
                           CH,                 /CH3

                   H     '               , ,,-. 	 /-*
                   C — C — OH    +    HC — C-
                CH,


                      4c
                                 OH

                                4d
                                                                   (6)
                      Isoprene Chemistry: 2
  4a to4d+ O-,-
    OH

     HC
    /
•OOCH,
                         — C
                              CH,
                              CH2
                                        OO'
                            HC — C
                           /
                                      \
                                   ,CH3
                                   CH,
                                                                 CH,
                                                     H2C
                         5a
                            OH

                              5b
HC==C
/



 OH

 5c (c/t)
                                                               \
                                               CH,


                                               OO-
                                                            ,CH,
 HC—C— OH

CH2      CH2


         OO-

    5d
                 HC^~ COO'
                S    \
              CH2        CH2

                      HO

                   Se
                                                    HC= C
                                                   oo.
                                                          \
                                                            C

                                                          OH
                                                                 (7)
                                                      5f (c/t)
                               4-78

-------
                        Isoprene Chemisfry: 3
                     P"    .CH,     O.       CHJ                CH,
5ato5f+NO— *-     HC — C       +   HC — C       +     //    \
                  /      %        /     ^           //    ^>
               •OCH2       CH2   HOCH;      CH2     HOCH2    H:CO-

                     6a               6b                  6c (c/t)


                        CH3                 CHj                  CH,

         +     HC - COH      +     HC — CO-       +      HC^=C
              S     \            -/    \             /      \
            CH.         H2CO-    H^C      H:COH      -OCH^     H:COH
                       Isoprene Chemistry: 4

•OCH:      CH2                    H      H

        6a                             7
                                   O     CH3
                                                                       (K)
                   6d                  6e                   6f(c/t)
   \     /         „                 II                \       /
   HC— C          P-sc'SSIQrV          C         +       wr— r         (9a>
   /    ^                         / \                -
                                   C     C        +      >OOH      (9h)
                                 / \  /  ^
                                H    CH    CH:


                                     OH

                                     9

                                 OH        CH,
                                  \     /
                    1.5-H Shift^       HC — C                         (90

                                   /     ^
                                HOCH2      CH;

                                       10
                                4-79

-------
              9(CH3)2 Chemistry
CH39(OH)'CH3 + 02      ->  CH39(0)CH3  +  H02<

                         -> CH390H + CH302-

                         -> (CH3)2902 + »OH
               N03 (Nighttime) Chemistry
                         CH.i

                         V         l°:l       \
          +   NO3 	^     «CH— CH2   	^       CH	CH:


                               ONO-.       -O	0        ONO
                        CHj H

                                              NO     (20)

                      H  V  H
                         0
O
II
/\ + N02 ^
H H
•CH2 ?i
	 | + II ^
°N°= H/XCH3
0
                                     CH3
                                        CH — CH2


                                              ONO2
                            C    ON02    I [Oa]


                         H    CH2
                        4-80

-------
                        Ozonolysis
                    XW             { V              /-\.        O



                   \  /            \  /             \           y v
               Criegee Intermediate Reactions

CH200'   + R02*     -»     HCHO +  RO- + 02
•OCH20-  -H  02      ->     HC02- + H02-
•OCH20-  +  HCHO ->    HOCH2-0-CHO
          Theory, Modeling & Simulation
        Unimolecular Decomposition of CH3CH20

 Method            AE
 MPO/TZ2PF         10.93      7.1     23.17      20.§
 PMP2/"            11.16       7.3    16.32      13.7
 MP49DQ/"          14.80      11.0    24.19      21.6
 PMP49DQ/"         14.98      11.1     19.35      16.8
 MP49DTQ/"         13.18       9.3    22.90      20.3
 PMP49DTQ/"        13.35      9.5    18.21       15.6
 QCI9D/"            15.78       11.9    22.04      19.5
 QCI9D(T)/"          15.50      11.7    20.54      17.7
 CC9D/"            16.13       12.3    22.40      19.8
 CC9D(T)/"          16.68      11.7    20.85      18.3
 CC9D(T)/aug-ooTZVP  16.61       11.6    19.53      17.0

 BP/DZVP2          20.63      18.1    20.71      18.1
 B31YP/DZP         17.87       14.6    19.96      16.8
 B3LYP/TZ2PF        15.13       11.7    18.13       14.9

 Expt                          13.1(NA8A/JPl/94)    21.e(Batt)

 Energies in kcal/mol, Geometry at MP2/TZ2P level except for NLDFT

                 ! Environmental Molecular Sciences Laboratory ss
                            4-81

-------
              Theory, Modeling & Simulation
           Unimolecular Decomposition of

                               Rafes

RRKM. High Pressure limit, 298K, N2 collision pertner.s = 4.2 A, • = 260 K

    Method              Ea(koel/mol)     log A(«-l)        k(n-l)

QC18D/TZ2PF             18.3            13.7             1.2
QCI9D(T)AZ2PF           20.3           13.7             0.041
CC8D(T)/TZ2PF           18.9            13.7             0.46
CCSD(T)/8ug-oo-VTZ       17.7             13.7             3.2

Expt                     21.6            15.0             0.14

Tunneling estimate for an imaginary frequency of 642i with a Wigner correction
booed on the reverse reaction: 1.4 @ 298 K, 1.46 @ 277 K

BsH, M. J. Ch«n. Kinei. //, 977 (1979)
                •*••••• Environmental Molecular Sciences Laboratory \

                     Benchmark  Calculations
                 for  Abstraction of H from CH4
      CH4 + OH'	> CH3* + H2O

      - Model for hydroxyl radical decomposition of alkanes in troposphere

                       RH + OH*	> R* + H2O

      - Reactions have low activation energies leading to alkanes having
        short atomospheric lifetimes.

      CH4 + Cl*	> CH3' + HC1

      - Atmospheric sink for Cl atoms which participate in the destruction
        of ozone.

      CH4 + H*	> CH3f + H:

      - Simplest reaction of a radical with  a hydrocarbon.

      - Potential importance in the combustion mechanism of simple
        hydrocarbons.

                                4-82

-------
                 Computational   Model


Abstraction of H from CH4


                    [H3C-H-X]'*
    CH  + X
                                             CH3* + HX
  What does the TS structure look like?


  What is the  overall reaction enthalpy, A//298?


  What is the barrier height, A£a*?
    Kinetic Parameters From Transition State Theory
rigid rotor, harmonic oscillator
1 free internal rotor
Wigner tunneling correction
    E. - 4.32 kcal/mol
    A - 1.47 x 10-11 cc/moleoule - s

    E. - 5.56 kcal/mol
    A - 1.16 x 10-10 cnrvVmolecgte - s

Experimental values

    E, - 3.6 kcal/mol
    A - 2.9 x 10'12 crrvVmolecUe - s
200<;T<;420K


200 ^ T i 3000 K
                         4-83

-------
        -20-
        -24-
        -28-
        -32-
        -36-
       -40
             O
      D ln[k(calc)]

      O ln[k(expt)]
                  8
 0
               D
             CH4 + OH —> CH3 +
         0.0   1.0   2.0   3.0   4.0   5.0
                   1/T (x 100
HFC-23 and HFC-236fa Reactions with OH
  HFC-23 = CF3H   & HFC-236fa = CF3CH2CF3
   Molecule
   exot
       calc
     HFC-23
     HFC-236fa
2.4x10-16
3.4x10-16
6.9x10"16
6.1
   Experimental values from DeMore's work at JPL
        Rate constants in cm3/molecule-sec
                     4-84

-------
ATMOSPHERIC CHEMISTRY OF ORGANIC COMPOUNDS
                   Roger Atkinson
          Photochemical Reactivity Workshop




                  May 12-14, 1998
          Tropospheric VOC Removal Processes









The tropospheric removal or transformation processes for




VOCs are:








Physical Removal Processes




         Dry deposition




         Wet deposition








Chemical Removal Processes




        Photolysis




        Reaction with ozone (O3)




        Reaction with the hydroxyl (OH) radical




        Reaction with the nitrate (NO3) radical

-------
    VOC
    ROOH
 R

 I0'
      NO2
RO2  ^   *"   ROON02
          ROj
carbonyl
  +
alcohol
                         NO
             RONO2
                  RO-
                 products
 Net photochemical formation of O3 versus net photochemical

 loss of O3 in the troposphere depends on the rate of


    HO2 + NO -» OH +  NO2

 versus

    HO2 + HO2 -* H2O2 +  O2

and

    HO2 + 03 -» OH + 2O2


and also by the rate of
                                                        RO2 + NO - RO + NO2

                                                    versus

                                                        RO2 + HO2 -* ROOH  + O2

-------
           Organic Reactions (genera!)
                                                                   Peroxy Radical Reactions
         voc  — -»-
ROOM   —^  R02'
    carbonyl
       +
    alcoliol
                                T   ROON02
                           RONO7
                       ROT
                     products


Reactions of organic peroxy radicals

Organic nitrate formation.

Reactions of alkoxy radicals.

Wet and dry deposition of VOCs and of their reaction

     products.
                                                               RO, + NO
                                                                                   RONO2
                                                                                   RO  + NO,
                                                      RO2 + NO2 ** ROONO2
                                                               RO,  + HO, -» ROOH  + O,
RCH(OO)R -f

                                                                              RCH(O)R + RCH(6)R  + O2

                                                                              RCH(OH)R  + RC(O)R  -f O2
                                                      RO2  + NO3 -* RO + NO2 + O2 (or other products)



                                                      There is a need for kinetic and product data for the

                                                      reactions of a wide variety of organic peroxy radicals

                                                      with NO, HO2 radicals and NO3  radicals.

-------
     R02 +  NO
Organic Nitrate Formation

         RONO2
         RO + NO2
•    The nitrate yields  increase with increasing pressure and
     with decreasing temperature.

•    Data are available for 18 secondary alkyl radicals formed
     from alkanes and for 4 other alkyl and /3-hydroxyalkyl
     radicals formed from alkanes and alkenes (mainly at
    room temperature and atmospheric pressure).
    decomposition
        x-"
|+  CH,CH2CH2
     Jo,

 NO —I—»- NO2

 CH,CH2CH26
                                                    (  CH,CH;CHo] .
                                                                                            CHjCH(O)CH2CH2CH,
                                                                                                               isomen nation
                                                                                         HO2 + CH,C(O)CH2CH2CH,
H'     CH-CH,

                                                                                                                          CH2
                                                                                                           1
                                                                                                   CH,CH(OII)CII2CH1CH2
                                                                                                           I"   '
                                                                                                      NO --— *• NO;

                                                                                                   CH3CH(OH)CU2CH2CH2b
                                                                                                            isomcrizanon

                                                                                                  CH,C(OH)OI2CH2CH2OH

                                                                                               	I0-
                                                                                                CH,C(O)CH2CH2CH2OH I + HO2

-------
OH and NO3 Radical Reactions with Alkanes and Alkencs
    The initial reactions lead to the formation of alkyl or



    substituted-alkyl (R) radicals, which then add O2 to form



    RO2 radicals.







    The present knowledge and uncertainties in the OH



    radical-initiated reactions of alkanes and alkenes are:



    •   RONO2 formation from RO2 + NO



    •   RO2 + RO2,  RO2 +  HO2 and  RO2 +  NO, reactions



    •   Reactions of alkoxy and hydroxyalkoxy radicals:



        •    Reaction with O2 (if a-H atom present)



        •    Decomposition



        •    Isomerization through a 6-membered transition



             state
      isomenzation
CH3CHCH2CH(OH)CH2OH
CH3CH2CH2CH(OH)CH2O



       \-
       H02 +
                                              decomposition
                       CH3CH2CH2CH(OH)CHO
                         CH3CH2CH2CHOH
CH3CH(OO)CH2CH(OH)CH2OH



  NO—j—*- NO2






Cl I,CH(O)CH2CH(OH)CH2OH




        isomcnzalion
OI3CH(OH)CH2Cll(OH)CHOH




        02
 CH3CH(OH)CH2CH(OH)CHO  +•  HO2
                                        M02

-------
OS
 •   Isomerization reaction has been observed from alkane


     and alkene reactions; quantification of the resulting


     hydroxycarbonyl and dihydroxycarbonyl products is now


     required.





•    The products and mechanisms of the NO3 radical


     reactions are  not well understood;  in part because these


     reactions occur in the essential absence of NO and hence


     RO2 + HO2 and RO2 + RO2 reactions are important and,


     especially in laboratory systems, ROONO2 are important


     intermediate reservoir species.
                                                                            R.       B
                                                                      o3 +    )c=c(
                                                                            T» /      •
                                                                                                 R!-
                                                                                                            f

                                                                                                            R4
                                                                               R,C(O)R2  +  (RjR4COOJ*
                                                                    followed by reactions of the biradicals
                 R3C(O)R4  »  [R:R2CO6p
                                                                      [R,CH2C(R2)OO]' + M
                                                                      [R,CH2C(R2)00]'
                                                                                                 R,CH2C(R2)OO  + M
                                                                                                                -   [R,CH2C(0)OR2]'


                                                                                                                         decomposition




                                                                                                                    PRODUCTS

                                                                                                                 (including R]CH3 if R2 = H)
                                                                       [R,CH2C(R2)00]'
[R,CH=C(OOH)R2]'
                                                                                                                     R|CHC(0)R2  f  OH

-------
Areas of uncertainty:




•   Reactions of the thermalized biradicals.




    •    Appear to be with water vapor under atmospheric




         conditions.




    •    The CH2OO biradical reacts with H2O to form




         HOCHjOOH which (heterogeneously?) decomposes




         to HC(0)OH + H2O.




    •    Certain more complex biradicals appear to react




         with water vapor to form the carbonyl (plus H2O2).








         R,C(O6)R2 +  H2O - R,C(0)R2 + H2O2








•   Reactions of the organic radical co-product to OH; e.g.,




    CH3C(O)CH2  radical from the [(CH,)2CO6l* biradical.
             AROMATIC HYDROCARBONS









 •   For benzene and the alkyl-substiruted benzenes, the major




     atmospheric reactions are with OH radicals (major) and




     NO3 radicals (minor).








•    NO3 radical reactions proceed by overall H-atom




     abstraction from the alkyl substituent groups.








•    OH radical reactions  proceed by overall H-alOm




    abstraction from the alkyl substituent groups (< 10%)




    and by OH radical addition to the aromatic ring to form a




    hydroxycyclohexadienyl radical  (^90%).

-------
                   CH3
      OH
oo
                   CHj
                                        H20
•   Under tropospheric conditions, the




    hydroxycyclohexadienyl radicals (OH-aromatic adducts)




    react with O2; at elevated NO2 concentrations




    encountered in some laboratory studies the OH-aromatic




    adduct reactions  with NO2 may be important.








•   The products and mechanisms of the reactions of the OH-




    aromatic adducts with O2 and NO2 are not presently




    understood in any detail, although product data



    (sometimes contradictory) are available from a number of




    laboratory product studies.
                                                                        Formation of ring-opened unsaturated dicarbonyls




                                                                        [-C(O)C=CC(O)-] and di-unsaturated dicarbonyls




                                                                        [-C(O)C=CC=CC(O)-] have been observed and may be




                                                                        very important.

-------
,OH


 II
  1



 H
                            OH
                               +  HO2
                          ,OH
                           OH
                           00
These radicals formed after O2 addition to the OH-benzene


adduct react further to (potentially) form:






    HC(O)CHO + HC(O)CH = CHCHO




    HC(O)CH =CHCH—CHCHO


    HC(O)CH=CHCH = CHCHO
                                                      Additionally benzene oxide/oxepin reacts to form



                                                      HC(O)CH = CHCH = CHCHO

-------
Tropospheric Chemistry of Oxygen-Containing Compounds
                                                                            Aliphatic aldehydes,  ketones and a-dicarbonyls
     •   Aliphatic aldehydes, ketones and a-dicarbonyls.


     •   Alcohols.


     •   Ethers and glycol ethers.


     •   a,|8-Unsaturated carbonyl compounds.
<^>
i
5   •   Unsaturated dicarbonyls.


     •   Esters.


     •   Hydroperoxides.


     •   Other oxygenated compounds.
                                                                      These react with OH radicals and (to a lesser extent) with


                                                                      NO3 radicals, and also photoiyze.





                                                                      Need absorption cross-sections and photolysis quantum


                                                                      yields as a function of wavelength [apparently reliable


                                                                      cross-section and quantum yield data arc available only


                                                                      for HCHO, CH3CHO and (CHO)2].





                                                                      The OH radical and NO3 radical reactions with  >C2


                                                                      aldehydes lead to peroxyacyl nitrate (PAN) formation.

-------
      Esters
       •   Reaction of RC(O)OCH(6)R radicals:









               RC(O)OCH(6)R -» RC(O)OH + RCO








j_    Ethers and Glycol Ethers








       •   Decomposition of > COC(6)RR radicals appears to be a




           factor of ~ 103 faster than expected by analogy with tlic




           alkoxy radicals formed from alkanes and alkenes.
         NITROGEN-CONTAINING ORGANICS









•   Organic nitrates (RONO2) and peroxyacyl nitrates




    (RC(O)OONO2) appear to be the most important N-




    containing compounds.








•   Rate constants for the OH radical reactions are available




    for alkyl nitrates; product data are needed.








•   For RC(0)OONO2 compounds (apart  from PAN), data




    are needed for photolysis and thermal decomposition.
                 COC(6)RR - > C(O)OR + R

-------
to
                      CONCLUSIONS




 •   Much progress has been made over the past 2 decades:




     •    Importance of NO3 radical reactions.




     •    Kinetics of OH and NO3 radical and O3 reactions




          with VOCs.




     •    Studies of RO2  radical reactions.




     •    Alkoxy radical reactions (isomerization)




     •    Fate of hydroxycyclohexadienyl radicals, including




         formation of ring-opened unsaturated dicarbonyls




         from aromatic hydrocarbons




     •   Product and mechanism studies of O3 +  alkenes;




         formation of OH radicals from these reactions.








•   Still many details to deal with!
                 Needed Research




 Quantitative knowledge of the rate constants and




 mechanisms of the reactions of organic peroxy (RO2)




 radicals with NO, HO2 radicals, NO3 radicals and other




 RO2 radicals (the latter mainly to allow accurate




 modeling  of irradiated NO, - VOC - air mixtures.








 Additional data concerning the organic nitrates yields




 from the reactions of organic peroxy radicals with NO,




 preferably as a function of temperature and pressure.








The reaction rates of alkoxy radicals for decomposition,




 isomerization and reaction with O2, especially of alkoxy




radicals other than those  formed from alkanes and




alkenes (for example, from hydroxy-compounds, ethers,




glycol  ethers and esters).

-------
 •   Detailed mechanisms of the reactions of O3 with alkenes




     and VOCs containing  >C = C< bonds.  This involves




     understanding the reactions of the initially energy-rich




     biradicals, and thermalized biradicals, formed in these




     reactions.









•    Mechanisms and products of the reactions of




     OH-aromatic  adducts with O2 and NO2.








•    Tropospheric  chemistry of many oxygenated VOCs




     formed as first-generation products of VOC




     photooxidations,  including (but not limited to) carbonyls




     (including unsaturated dicarbonyls, di-unsaturated




     dicarbonyls, and  unsaturated epoxy-carbonyls),




     hydroperoxides, and esters.

-------
     Atmospheric Chemistry of Oxygenated Organic

                              Compounds


                                Ray Wells

                               AFRL/MLQR
                              139 Barnes Drive
                        Tyndall AFB, FL 32403-5323
                               (850)283-6087
                     ray.wells@ccmail.aleq.tyndall.af.mil


      Uncharacterized volatile organic compound (VOC) emissions from complex

formulations (coatings, coating strippers, cleaners) are involved in the production of

tropospheric ozone (63), a regulated pollutant. Since the detailed atmospheric chemistry

of several of these chemicals has never been investigated, experimental atmospheric

research coupled with incremental reactivity calculations is useful  to more accurately

assess the atmospheric impact of coatings emissions. The atmospheric impact of the

coating systems was determined, using individual VOC incremental reactivity

calculations, coupled with a detailed description of coating system emissions. The

concentrations and identification of VOCs in the coating emissions were determined by

combining gas chromatography, mass spectroscopy  and Fourier transform infrared

spectroscopy (GC/MS/FTIR) techniques. The OH rate constant for ethyl 3-

ethoxypropionate was determined using the relative  rate technique. The products of the

OH + ethyl 3-ethoxypropionate reaction were determined and an atmospheric reaction

mechanism for ethyl 3-ethoxypropionate was proposed.
                                  5-14

-------
    AIR FORCE RESEARCH
        LABORATORY
 ATMOSPHERIC CHEMISTRY
 OF OXYGENATED ORGANIC
        COMPOUNDS
           Ray Wells
           AFRL/MLQR
            Air Team
         (850)283-6087
     ray.wells@ccmail.aleq.tyndall.af.mil
         AIR TEAM
       Lt. Leon Perkowski
         Dr. Ray Wells
         Darrell Winner
        Stewart Markgraf
         Steve Baxley
         Sheryl Wyatt
          Bill  Bradley
We determine impact on air quality.
             5-15

-------
           URGENCY
          -1990 Clean Air Act-

           200 new regulations
         and guidance documents
       They impact our missions!
           DoD Releases by
             Media, 1994
             Land    Water
             1.31%   1.25%
                              Air
                              97.44%
From: 1994 Toxics Release Inventory for the DoD Publie Data Report, March 7, 1996
                  5-16

-------
            Of That 97%...
                     Metals - 6%
          Acids - 4%
 Chlorinated
  organics
    and
  chlorine
    55%
    Impacts
  Stratospheric
    ozone
  Volatile
  Organic
Compounds
   35%

   Impacts
 Ground level
   ozone
   Compromise ozone formation and depletion
          Sources of Pollution
       Paints
            Thinners
                Solvents
                     Combustion
                         Exhausts
New replacements affect these sources
                    5-17

-------
                      Purpose
GOAL: Prevent pollution intelligently while maintaining performance


                  Achieved by addressing:

        1. What is being emitted?

        2. What happens to emitted chemicals?

        Tech Need: 1940 -  Replacement of chlorinated
        cleaners for engines  (High)
             Experimental Apparatus


    Reaction Chamber
                      Sample Loop
                                      Analysis System
                         5-18

-------
Pertinent Radical Formation
        Reactions
        OH Radical
O  + hv
O(1D) + H2O
RH + OH —
               0(1D) + O2
                2 OH
               R +H2O
        NO3 Radical
 NO2 + O3
 NO2 + NO:
 RH + NO3
               NO3 + O2
                N205
                R + HNO3
O Atmospheric Transformation llSRi
v , Processes ^bss3^
DU -I- OU-
KM + \Jr\
• + o2
|—)/^S . k 1 S-\
RO2 + NO
NO2 + hv
01 /^i i R It
+ O2 + M
RLJ + OH- + 9O
r\n ^ \j\\ • ^w2
R. + u n
^ n2v/
» i~^k /*\
RO2
> M/^\ _L D/^
NU2 + KU
k hi /"^i . /^"X
NO + O
«• /^\ i iv yi
Oq + M
o
PO + u n+ o
' r\w ~ n2\_/^ v^3
           5-19

-------
         Experimental  Methods
I.  Relative Rate Technique:
Compare unknown hydroxyl reaction rate to one that is
known:
1)
2)
      Reference + OH-
      Unknown + OH'
Products
Products
Dividing differential equations to remove OH concentration
and time and integrating yields:
 In
[Unknown],,

[Unknown],
i\Unknown i
n
M i
K Reference
[Reference ]0
[Reference],
     Hydroxyl Radical Rate Constant for EEP
         CH3CH2OCH2CH2C(=0)OCH2CH3
        1.2
         0.00   0.01    0.02    0.03    0.04    0.05

             {ln([Ref]0/[Ref]|)/kRe,}*10'12cm3molec"1 s'1
                      5-20

-------
     Hydroxyl Radical Rate Constants
 Rate constants and chemical structures are variable
 Compound/Structure
kOH(10-12cm3molecule-1s-1)/lifetime(hr)
Ethyl 3-ethoxypropionate
CH3CH2OCH2CH2C(=0)OCH2CH3

Hexyl Acetate
CH3(CH2)5OC(=0)CH3

Isobutyl Acetate
(CH3)2CHCH2OC(=O)CH3

2-Butoxyethanol
CH3(CH2)3OCH2CH2(OH)

2-Butanol
CH3CH2CH(OH)CH3
             23/12


             9.3/30


             6.5/43


             22.5/12


             8.1/34
                            5-21

-------
           Experimental Methods
II. Product Identification and Yields:
         Unknown  + OH	> Products
Must correct for transformation product/OH reaction to
determine yield:
                            [Unknown],
    P  _ k-...... ~ k.......           [Unknown],
           k°'"-     f  [Unknown] V	  [Unknown],
                   V [Unknown] )     [Unknown],
                        5-22

-------
            CH,-CH9-O-CH
                        2-CH2-C(=O)O-CH2-CH3 + OH
CH3-CH-O-CH2-CH2-C(=O)O-CH2-CH3
           - "NO,
           *  decompose
HC(=O)-O-CH2-CH2-C(=O)O-CH2-CH3
Ethyl (3-formvloxv) propionate (EFP)
    CH3-CH2-O-CH-CH2-C(=O)O-CH2-CH3
      O2. NO  -
                                     CH,-CHrO-CH2-CH-C(=O)O-CHrCH3
                      decompose
                                    O2, NO
HC(=0)-CH2-C(=0)0-CH2-CH3
Ethyl (2-formyl) acetate (EFA)
     CH3-C(=0)H
    Acetaldehvde
                                              decompose
                                                     I
                                           CH(=0)-C(=O)O-CH2-CH3
                                           Ethyl Glyoxatc (EG)
                                CH3-CH2-O-C(=O)H
                                Ethyl Formate (EF)
                      CH3-CH2-0-C(=O)-CH2-C(=O)0-CH2-CH3
                          Diethvl Malonate (DM)
                          2-Butanol
CH3CH2CH(OH)CH3 +  OH
                                          CH3CH2C(=0)CH3
   ? Where did oxygen come from in methyl ethyl ketone product?

   ?Is this major transformation pathway a source of ozone?

                 Experiment to reveal mechanism:

   CH3CH2CH(18OH)CH3 +  OH  — f - » - * CH3CH2C(=180)CH3

     Experiment reveals that major transformation pathway is not
                        a source of ozone.
                              5-23

-------
   Reaction Product Identification
V)
'£

.a
-2-

I
TO

o
JD
   Experimental Spectrum
Pure 1,2 Ethanediol acetate formate
          3000           2000
                 Wavenumbers (crrr1)
                                            1000
   Corrected Ethyl Formate Product Yield
          0123

             EEP Reacted (ppmv)
                    5-24

-------
            Reactivity of Emissions
•Reactivity(ozone forming potential) of individual chemicals requires
knowledge of atmospheric kinetics and mechanisms.
•Reactivity of emissions is based on summation of reactivity of
individual chemicals.
•Reactivity values for each formulation are used to assess impact
on air quality and minimize regulatory impact.
          EMISSIONS - The Real Problem
    Evaporation!
                              Emissions NOT content!
                          5-25

-------
   8
   ro
              TIC for MIL-P-23377F
                           Methyl benzene
    IBA
             4-methyl-2-pentanone
            MEK
             1,3 DMe benzene
                                           1,4 DMBZ
                                 Ethyl benzene
Time (Minutes)->
            10.00 11.00 12.00 13.00 14.00 15.00 16.00 17.00 18.00
             Air Quality Impact
    Coating A
=  0.27 g O3/g paint
    Coating B
=  0.27 g O3/g paint
    MIL-P-23377F    =  0.75 g O3/g paint
   jram O/gram paint = £ (gram emitted VOC/gram paint}* Factor,
                                           voc
                       5-26

-------
Materials Benefits
 Meet pollution prevention goals.
 Formulation flexibility.
          5-27

-------
            Multicomponent Aerosol Generation System (MAGS)  for the
        Study of Fine Particulates on Photochemical  Reactivity of Organu
                     nics
        5 V. Kulkarni. KulTech Incorporated
        Research Tnangle Park, North Carolina
M. B Ranade. Particle Technology Inc
Beltsville, Maryland
      Considering the relative merits of using individual VOC species reactivities versus
VOC-group ratings (S Question/Issue 4 ) may address the effects of synergism within the
VOCs present in an organics  emission  source,  but  it does not consider the  chemical
reactions that may affect photochemically active VOC species  Mixed oxides and  salts
such as SiO2/TiO2 are known photocatalysts in  oxidation  of ethylene  In the  study of
binary metal oxides as photocatalysts, it has been noted that there is a strong correlation
between  surface acidity and reactivity   Other reactions between gaseous  species and
VOCs are also  likely to affected  The fine particles in industrial emissions may contain
metal oxides and sulfates and nitrates and may  enhance or reduce the photochemical
reactivity depending upon the organics present in the emissions.  We propose to study the
role of  atmospheric  fine  particulates  on  the  photochemistry of   volatile  organic
compoundsCVOCs).
       We have developed a compact and portable multicomponent aerosol generation
system(MAGS) which produces a paniculate composition closely mimicking the ambient
and stack particulates The system  has  the ability  to produce  representative  aerosols
containing  inorganic oxides(and Ca, Al silicates), sulfates, ammonium nitrate, organics -
hygroscopic, solid and Hquid, volatile components  in appropriate size ranges
       MAGS, shown in the Figure below, can combine several types of particulates  such
as mixed oxides, mixed salts and  other species such  as carbonaceous compounds  each
type may be produced  by  nebulization and  chemical conversion of precursor solution
droplets  Particle size distribution of each  component  may be varied from submicrometer
to 10 micrometers
                                                           hotochemical Reactor
                                            Aerosol Conversion
                                            Reactors
                    Nebulizers
                                             precursor Solutions
                                     5-28

-------
Numerical  Study of the Development  of  an  Ozone Episode in
Germany: Relation of Anthropogenic and Biogenic Hydrocarbons
F. Fiedler, H. Vogel, B. Vogel
Institut fur Meteorologie und Klimaforschung
Forschungszentrum Karlsruhe / Universitat Karlsruhe
Postfach 3640, 76021 Karlsruhe, Germany
 Abstract

 A mesoscale numerical model  is used to study the development of ozone concentrations
 within the atmospheric boundary layer for different emission scenarios of anthropogenic and
 biogenic emissions. The major results are:
 •  In the reference case the maximum ozone concentrations are in the order of 100 ppb.
- •  When all anthropogenic emissions are switched of the maximum ozone concentrations are
    in the order of 60 ppb.
 •  When  the anthropogenic  emissions of the four most reactive hydrocarbons within the
    RADM2 gas phase mechanism are switched off the ozone concentrations are reduced up
    to 15 ppb.        i
'. •  When all anthropogenic hydrocarbon emissions are switched of the ozone concentrations
    are reduced up to 50 ppb.
 1 The problem

 The atmosphere is a huge deposit for gaseous waste from a large variety of anthropogenic and
 biogenic sources. Due to the complex interaction of the chemical and physical processes in the
 atmosphere a clear determination of the importance of individual substances for the develop-
 ment e.g. of photooxidants like ozone is very difficult.

 In  this paper a comprehensive model  system including the most relevant atmospheric and
 chemical processes is used to estimate the influence of man made nitrogen oxides and hydro-
 carbons  on the development of maximum ozone concentrations during an ozone episode.
 Especially four cases will be studied:

 •  The reference case where both the anthropogenic and the biogenic emissions are included.
                                      5-29

-------
   The background case where all anthropogenic sources are switched off and only natural
   emissions  of  nitrogen  from  soil and  of hydrocarbons  from  biogenic  sources  are
   considered.
   The case where all anthropogenic emissions of hydrocarbons are switched off.
   The case where the anthropogenic emissions  of the four most  reactive hydrocarbons
   within the RADM2 chemical mechanism are switched off.
2 The model system and the data base

For this study the non-hydrostatic mesoscale model system KAMM (KAMM = Karlsruhe
Atmospheric Mesoscale Model) together with the gas phase mechanism RADM2 (Stockwell
et al., 1990) is used. The model system is driven by a basic state which is derived from the
larger scale observations. It is documented in more detail in Adrian and Fiedler (1991), Vogel
et al., (1995) and Fiedler (1993). As a result the model provides all important meteorological
variables and the concentrations of chemical species for episodes of several days.

Emission data of the most important anthropogenic emissions have been compiled in hourly
time steps  and for an area of 177  km x 177 km with a horizontal  resolution of  3  km.
Additional data like terrain height, land use and soil data have also been provided as close to
reality as possible. Those  data  are especially  important for  the  parameterization of the
turbulent fluxes of momentum, energy, water vapour but also for the parameterization of the
emission and the dry deposition  of chemical species  at the surface. In  addition with the
temperature and  the  photo synthetic active radiation  calculated by KAMM the  natural
emissions of nitrogen oxides from soil surfaces and of hydrocarbons  from vegetation are
determined online by the model system.
3 Results

A situation for south-west Germany is selected, where high ozone concentrations have been
observed. It was  accompanied by  high air temperatures (-34 °C) and therefore enhanced
biogenic emissions. For the simulations with the model system a day at the beginning of
August 1990 has  been chosen. On that day ozone concentrations have been observed up to
about 100 ppb in the early afternoon. Winds were rather weak and showed a dominant easterly
component in most of the of the area.

The dominant emission area for the anthropogenic emissions is within and in the surroundings
of the city of Stuttgart (Fig.l) which  is located in  the centre of the model domain. Fig. 2
shows the simulated ozone (O3) concentration for the reference case at about  18  m above
                                      5-30

-------
ground. Areas of maximum ozone concentration appear in the west and south-west of the city
and approximately 30 to 40 km downstream. The highest concentrations reached are at about
100 ppb. They are comparable to the observations.
An extreme situation  is a  case where no anthropogenic  emissions  would  be available.
Therefore only natural  emission from soil and from biogenic source have been included. In
this case the maximum ozone concentration is around 60 ppb. This value gives  the lowest
level which can be achieved by abatement strategies. The reductions in ozone at the same time
as for the reference case (Fig. 2) are given in Fig. 3.  Maximum reduction areas are in the
range of 50  km downstream of the city complex.
The more realistic procedure would be the reduction of the most reactive species. In order to
estimate the  level  of  reduction  by  eliminating the  four  most  reactive groups  of the
hydrocarbons, a  scenario has been used, where  emissions of propene, butene, toluene, and
xylene were switched off. Compared to the total anthropogenic emissions for the whole model
domain, about 20 to 25 percent of the hydrocarbons have been extracted by this  procedure.
The ozone  reduction in this case  is shown in Fig. 4, where again the difference in ozone
concentration compared to the reference case (Fig. 2) is presented.  Significant reductions in
, ozone concentration are confined to rather small  areas in the west of the city of Stuttgart and
to the south-west of Heilbronn. Therefore Fig. 4 gives also those areas  where the ozone
production  is limited by the availability of hydrocarbons.

5 Conclusions        '»

Numerical  models are capable to study the effects of emission reductions but only according
to the state  of the art of the understanding physical and chemical processes in the atmosphere.
 However they provide the possibility to study quite realistic cases comparable to observations.
 It is therefore possible to quantify the effects of different abatement strategies.
 For the episode and the area of interest we focused on the ozone level is decreased by 30 to
 50 % when all anthropogenic emissions are switched off.
 When the emissions of the  four most reactive groups of hydrocarbons are switched off the
 ozone reduction reaches only about 15 % and the reduction is also confined to rather small
 areas compared to the case with total reduction of anthropogenic emissions.
 5 References

 Adrian, G., F. Fiedler (1991): Simulation of unstationary wind and temperature fields over complex terrain and
 comparison with observations - Contr. Phys. Atmos., 64, 27-48.
 Fiedler, F. (1993): Development of meteorological computer models
 Interdisciplinary Science Reviews, 18, 192-198.
 Stockwell B.W., P. Middleton, J.S. Chang, X. Tang (1990): The second generation regional acid deposition
 model chemical mechanism for regional air quality modeling, ]. Geophys. Res., 95, 16343-16368.
                                       5-31

-------
Vosel. B., F Fiedler, H. Vogel (1995): Influence of topography and biogenic volatile organic compounds
emission in the state of Baden-Wuerttemberg on ozone concentrations during episodes of high air temperatures,
J. Geophys. Res., 100, 22907-22928.
                                          75     100    125    150     175
                                                                                     >   IOD.O
                                                                                  so.o - ioa.0
                                                                                  es.c - 6
                                                                                  £0.0 - 2G.O
                                                                                  1.5.0 - 20.0
                                                                                  10.0 - 15.0
                                                                                   7,5 - 10,0!
                                                                                   s.c -  7.5!
                                                                                   3,3 -  6,0
                                                                             I   I   L.O -  E,6
                                                                             I   I     <    l.o'
Figure 1: Horizontal distribution of the anthropogenic VOC emissions at 0800 CEST.
                           25
50
                                           75     100    125    150
                                          	x in km	
                                       175
Figure 2: Horizontal distribution of ozone at  1400 CEST (18 m above ground).

                                               5-32

-------
                          25
 50      75     100
	Y in km
125
150
Figure 3: Simulated ozone concentrations without anthropogenic emissions, minus simulated ozone
concentration with all emissions at 1400 CEST (18m above ground).
              175
                                                                              14:00 CIST
                                                                              40, in ppb
                                                                              HI     >    -I.E.
                                                                              Hi   -30-  -1.6
                                                                              |H   -46 -  -a.0
                                                                                    B-8 0 -  -*•.&
                                                                                    -T.5 -  -5.0
                                                                                    -9.0 -  -7.5
                                                                                   -10.6 -  -B.O
                                                                                   -13.0	10.&
                                                                                   -13.6 - -1S.O
                                                                              I   I  -16.0	13.&
                                                                              I   |     <;   -16,0
                                           75      100
                                          	x  in  km	
                         125
         150
         175
 Figure 4: Simulated ozone concentrations without anthropogenic emissions of propene, butene, toluene, and
 xylene, minus simulated ozone concentration with all emissions at 1400 CEST (18 m above eround).
                                                5-33

-------
    European Studies on the  Photooxidation Mechanisms of Aromatic
           Hydrocarbons and Oxygenates: Reactivity Implications

                     I. Barnes, K.H. Becker, B. Klotz and H. Geiger

    Physikalische Chemie/FB 9, Bergische Unix ersitat - Gesamthochschulke Wuppertal.
                     GauBstraBe 20, D-42097 Wuppertal, Germany

Within the  framework of the  German Tropospheric Research Programme (TFS) in Germany
and the Chemical Mechanisms Development (CMD) subproject of EUROTRAC 2 research is
currently in progress in Europe to  elucidate the  photooxidation mechanisms of VOCs,  in
particular aromatic hydrocarbons and oxygenates  (e.g. dicarbonyls, ethers and acetals).  The
aim of these efforts is the development of chemical mechanisms for inclusion in CT models to
better predict photoooxidation formation.
Since  model calculations indicate that aromatic  hydrocarbons mainly BTX (benzene, toluene
and the xylene isomers) can contribute up to as much as 40% to the formation of O3  and other
photooxidants in urban areas over Europe (Derwent  el a!., 1996, 1998) substantial efforts
have been expended on investigating aromatic hydrocarbon oxidation mechanisms.  However,
the accuracy of these predictions depends on the mechanism incorporated into the model and
thus model validation is required. The types of work performed embrace:
•  investigations on the atmospheric chemistry of benzene oxide and toluene oxide, possible
   primary  oxidation products for benzene and toluene, respectively (Klotz et al. 1997,1998).
•  detailed   product  and  kinetic  studies  including  verification/identification of  carbonyl
   products by GC/MS  detection by their  O-(2.3,4,5,6-pentafluroobenzyl)-hydroxylamine
   (PFBHA) derivatives (Yu et al.. 1997; Kwok et al.. 1997).
•  measurement of photolysis frequencies of glyoxal. methylglyoxyl. biacetyl, butenedial and
   3-he\ene-2.5-dione.
In the area of ethers and acetals  (diethers) detailed chemical mechanisms are being developed.
Particular attention has been  given to diethers and cyclic  ethers, which in Europe  are under
discussion  for the use as fuel additives or alternative  solvents.  The  developed  chemical
mechanisms  are tested  against  experimental  data  obtained in the  outdoor  EUPHORE
photoreactor in Valencia, Spain as well as in several  indoor photoreactors.  In collaboration
with  the  Fraunhofer  Institute,  Garmisch-Partenkirchen, FRG, the  influence  of these
oxygenates  on tropospheric  ozone formation is estimated by  integration  of the  obtained
chemical degradation schemes into the ozone prognosis model RACM (Stockwell et al. 1997)
and application of the model to well  defined scenarios.
The efforts in the area of aromatic  hydrocarbon and oxygenates research within Europe will be
briefly summarised and the results  discussed  in  terms of ranking these  VOC  classes with
regard to their reactivity.

References
Derwent, R.G., M.E. Jenkin, S.M. Saunders, Atmos.  Em-iron. 30 (1996) 181-199.
Derwent, R.G., M.E. Jenkin, S.M. Saunders and M.J. Pilling Atmos. Environ. 32 (1998) in press.
Klotz, B., 1. Barnes, K.H. Becker, B.T. Golding, J. Chem. Soc. Faraday Trans,, 93 (1997) 1507-1516.
Klotz, B., 1. Barnes, K.H. Becker, accepted Chem. Phys., (1998).
Kwok, E.S.C., S.M. Aschmann, R. Atkinson and J. Arey, J. Chem.  Soc., Faraday Trans. 93 (1997) 2847-
Stockwell, W.R., F. Kirchner, M. Kuhn  and S. Seefeld, J. Geophys. Res. 102 (1997) 25847-25879.
Yu, J., H.E. Jeffries, K.G. Sexton, Atmos. Environ. 31 (1997) 2261-2280; Yu, J., H.E. Jeffries, Atmos. Environ.
31 (1997)2281-2287
                                        5-34

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Experimental (symbols) and simulated (lines) concentration-time profile
in a toluene/NO photooxidation experiment
 (730 ppb toluene /115 ppb NO).
O): toluene, left scale; (*): benzaldehyde; (•): o-cresol; (T): m-cresol;
(A): p-cresol, right scale.
     1.8 10
    1.3 10°
             12:00       13:00       14:00       15:00
                          time of day [hh:mm]
16:00
                                                                                  1200  1300 1400  1500  1600
                                                                                     time of day [hh-mm]
                                                          II 20  1200  12 40 13 20  14 00
                                                                limt of day [hh:mm)
                                                                                 I 00  II 20 II 40  12.00  12 20
                                                                                     lime of day (hhtmm)
                                                          10 JO 1045 II 00 II 15 11.30 II 45
                                                               limr of  day [hhrmm)
                                                                                                                                      000 S-
                     Bcrgische Universitat Wuppertal
                          Universitat Heidelberg
                          LT3 - Projekt D.I / D.2
                                         Bergische Universitat Wuppertal
                                                 LT3 - Projekt D.I

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UJ
os
              Untersuchung an ungesattigtenl,4-Dicarbonylen
                       im Europaischcn Photoreaktor
            J(Dicarbonyl)
                J(N02)

          (40°N. Mittag.  I Juli)
           Lebensdauer T.
    Hauplprodukte:

    3H-2-Furanon

5-Methyl-3H-2-furanon

 Maleinsa urea nhyd rid
                                   Z-Butendial
                           l,62x 10' s"
                                    9x 10 V
                                    10 Minuten
                                     30,1
                                     3 1,0 %
                              I
                k(OH)

        (Bierbach et  al. 1994)
           Lebensdauer TO,,

           [OH]= 1,6-10'cm'

           [OH1 = 3,5 10'cm'
                          5,2 10" cm' s1
                             200 min

                              9 min
                                           Z-4-Oxo-2-pentcnal
                                                      1.98 x 10's'
                                               9x 10 V
                                               8,4 Minulen
   31,9 %

   13.6 V


5.6-10" cm' s '
   186 min

    8 min
                                                                                              cis-butcncdial: product yields

2-3H-furanone
maleic anhydride
glyoxal
acrolein
carbon monoxide
(%perC)

sum of products
Photolysis
(Valencia)
30%
31 •/.
6V.
3 •/,
<3%

70-73 %
OH radicals
(CH3ONO/NO)
< 2 %
40-50 %
15-20%
observed
< 13 %

55-85 %
OH radicals
(H2O2)
not observed
6-12 %
20-45 %
not observed
(<27 %)

26-60 %
                          Bcrgische Uiiivcrsitat Wuppertal
                                 LT3 - Projekt D.I

-------
                          cis-butenedial
U)
       •o-..    -"-
        3H-2-funnon
o     o
                             o     o
                            O,/NO
                             Oi-U
                            Milfic (n
                               j\ *
     The numben we product yields obiam«t in photolysis
     c.penmenu made in EUPHORE in Aprile I997
                                          O,/NO
                                                             C=0
                                                   Acroleln
                                                    5 %
                                                    o     o
                         O,
                         NO
                          O,
                          NO
Abhangigkeit der Diacetyl-Photolysefrequenz von J(NO2)

V
T
C
,*—
I
4.
c.
4,5
3.5
3
2.5
->
1.5
03
Q 1 -


0,5
0 -
C
X



x^
_/*•
S









2 4 6 8 10 12 14
,T(N02)[10-Js-']
2»0 Bergische Universitat Wuppertal
"jfffff LT3 - Projekt D.I
                                         GlTO.ml
                                          C V,

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QUESTION/DISCUSSION SUMMARIES

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PRESENTATION SUMMARIES
Session I Summary of Questions and Discussions

Current EPA Regulatory Viewpoint on Reactivity
       Bill Johnson, Ozone Policy and Strategies Group, EPA

       Mr. Johnson was asked how to get a copy of Rule 66 and vapor pressure cutoffs. He
responded that inquiries on this rule, now referred to as Rule 442, can be made through Los
Angeles County (i.e., South Coast Air Quality Management District).  Mr. Johnson was also
asked about obtaining a list of the 14 pending petitions.  Mr. Johnson said that he will make this
list available.

       William Carter (University of California) commented that this workshop group  should
look at other scales in addition to the maximum incremental reactivity (MIR) scale. He added
that for compounds with low vapor pressure, the equilibrium vapor pressure should be
considered.

       Robert Hamilton (Amway Corporation) asked about the mole versus mass based
reactivity and what the advantage would be if the standards are weight based. Mr. Johnson
commented that reactivity comparisons made on the mole basis would be more scientifically
sound. The regulation of emissions is still done on a weight-basis. A question was asked
concerning the basis for exempting compounds and what goal was trying to be accomplished.
Mr. Johnson responded that the goal is ozone reduction, but that other collateral effects are being
considered as well.

       Brian Keen (Union Carbide) commented about the  wide range of compound
concentrations and reactivities, and about the pit falls of using bright line cutoffs. Mr. Johnson
responded by stating that this is one of the issues he hopes  will be discussed at this workshop. At
the present time, bright line  cutoffs work well from a regulatory perspective. Dr. Keen also
commented on the problem of the uncertainty of the information.

Current EPA Research Viewpoint on Reactivity
       Basil Dimitriades, National Exposure Research Laboratory, EPA

       Alan Hansen (EPRI) asked about the difference between relative versus absolute
reactivity.  He stated that the question of gram-based versus mole-based reactivity shouldn't be
important since the two are related by  a proportionality constant.  Dr. Dimitriades responded by
stating that the problem depends on how the data are used. The differences between cases
depends on the applications or how the material is used. For example, comparing paint solvents
with ethane on a per-gram basis is affected by the problem; but intercomparing solvents on a per-
gallon basis is not. John Festa (American Forest and Paper Association) asked if Dr. Dimitriades
had stated that there was no basis for excluding any VOC.  Dr. Dimitriades responded that he
was referring to an exclusion from the inventory requirements.  Another question was asked
about the distinction made between VOCs and non-VOCs.  Dr. Dimitriades and William Carter

                                           6-1

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(University of California) clarified this issue. The distinction is a legal or regulatory one; EPA
has defined compounds as being VOCs or non-VOCs and this information is provided by means
of a table.

       Dr. Carter also commented that there are several issues that will drive the science. The
first issue is what type of policy is going to be used. If the policy continues to be the exemption
policy, then the question is whether ethane is the appropriate dividing line and, if not, what
substance should be used. One area of research is to determine what is the best dividing line or
bright line.  The second issue, once the bright line has been determined, is to determine where
other compounds fall relative to the bright line.  Dr. Carter commented that the most appropriate
comparison is on a mass  basis, because this is how the VOCs are emitted.  Dr. Dimitriades
responded by stating that the question of which basis to use is one that needs further discussion.

       Dave Morgort (Eastman Kodak Company) asked if MOIR has been considered over MIR
as the basis for a reactivity scale.  Dr. Carter commented that exemption decisions were based on
a number of reactivity scales (e.g. EBIR or MOIR) and not on just the MIR scale.
Dr. Dimitriades commented that the discussion  on the reactivity scales is still an open one.
Jake Hales (ENVAIR) suggested that this workshop group try to develop a good definition for
the term reactivity.

California's Hydrocarbon Reactivity Program
       Randy Pasek, California Air Resources Board

       Can Roque (Naval Aviation Depot) asked if California was integrating their research
with those from other states. She continued by  asking if there would be a shift from air pollution
to water pollution when changing over to material using water-based chemistry. Dr. Pasek
responded by stating that they are seeking opportunities to share studies. He also stated that
California doesn't plan to shift from air to water pollution. An addition, a comment was made
concerning the need to recognize instances where multimedia consideration must be made.

       Bemie Zysman (Occidental Chemical Corporation) asked about other research facilities
doing work on MIR.  William Carter (University of California) stated that he was not aware of
others doing reactivity research, except Harvey  Jeffries's group (University of North Carolina).
Mr. Zysman add that he would like to see more research and development to clarify Dr. Carter's
work.

       Bob Kozak (Atlantic Biomass Conversions, Inc.) asked if CARB was considering in-use
vehicle speciation testing for possible upgrading of smog check equipment.  Dr. Pasek stated that
these types of measurements are not being done on a routine basis, but there is a need for this
type of information. Mr. Kozak also asked if tropospheric ozone production work might
interfere with any stratospheric ozone depletion work being done by CARB. Dr. Pasek stated
that they have taken this into account by considering the effects compounds might have on
stratospheric  ozone and global warming, as well as its toxicity.
                                          6-2

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VOC Reactivity - Beyond Ozone
       Alan Hansen, EPRI

       Dave Golden (SRI/Stanford) stated that no one knows the chemical mechanism of the
SO2 to sulfuric acid reaction.  There is a lot of the chemistry in the models that may not be
correct, but care must be taken when jumping to the complexity of the model.  Mr. Hansen
agreed with these comments.

       Jake Hales (ENVAIR) asked about the counter-intuitive findings that result when you
increase NOX, the nitrate aerosol decreases. He asked if there was a mechanistic explanation for
this occurrence.  Mr. Hansen responded that he didn't know the mechanistic reason why this
occurred. Ted Russell (Georgia Institute of Technology) commented that since you're decreasing
N02, you're increasing the OH radical pool. This allows for faster oxidation of VOCs, the ozone
concentration increases, and, with more ozone, there is more OH. The presence of more ozone
also causes faster nighttime conversion of NO2 to nitric acid.
Session II Summary of Questions and Discussions

Comparison ofPOCP and MIR Scales
       Richard Derwent, Meteorological Office, United Kingdom

       Eduardo Olaguer (The Dow Chemical Company) asked if by moving from the MIR scale
to a regional reactivity scale, there would be as much of an advantage in moving from highly
reactive to moderately reactive compounds. Dr. Derwent responded by stating that the best
benefit is from changing from a high reactive compound to a low reactive compound. He stated
that the MIR scale underestimates the impact of controlling the middle reactive compounds.
Dr. Olaguer also asked if there would be any significant impact on reactivity values if fast
vertical motions associated with convective activity, such as precedes thunderstorms, were
accounted for in models used to derive reactivity scales. Dr. Derwent stated that this has not
been considered, because ozone is not produced in thunderstorms.

       Donna Carvalho (Pennzoil) asked if Dr. Derwent had made any assumptions about the
reactivity of C-13 or greater compounds. Dr. Derwent responded that he had not. These
compound were not included in his calculations, because they are not included in the emission
inventory.

       Dr. Derwent was asked about why formaldehyde was not photolyzed.  He responded that
it was, but whether or not to photolyze formaldehyde is not a user's choice, but is determined by
the hydroxyl radical concentration. In Dr. Carter's MIR scale, because of the high NO* levels
used, much of the formaldehyde is photolysed and so it appears to be highly reactive. In the
regional POCP scale, because NOX levels are lower, much of the formaldehyde reacts with
hydroxyl radicals and its reactivity appears lower.
                                          6-3

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Session III Summary of Questions and Discussions

Dunn-Edwards Proposed NARSTO Research on Ozone Formation Potential ofVOC Emissions
from Architectural Coatings
       Edward Edwards, Dunn-Edwards Corporation

       Jeff Gaffney (Argonne National Laboratory) commented that by investigating lowNOx
chemistry, a great deal can be learned about regional scale reactivity.  He also commented that on
a regional scale, consideration must be given to the formation of species other than ozone, such
as organic peroxides and the conversion of SO2 to sulfate. These species have impacts on other
environmental concerns such as regional haze.

       Harvey Jeffries (University of North Carolina) commented on the importance of reactivity
in low NOX conditions.  In  low NOX environments, the VOCs determine the fate of the NOX; the
loss of NOX limits the formation of ozone.  These effects can cause increases in ozone downwind
of urban areas. As illustrated by an SAI study, changes in solvent content from a more reactive
solvent based on toluene to a less reactive solvent based on paraffins can cause increases in
ozone concentrations in a downwind NOx-limited environment. Dr. Jeffries concluded by stating
that some of Dr. Edwards'  concerns are legitimate and the issues of nitrate yields and nitrate
formation in these mechanisms are important pieces of information.

       William Carter (University of California) commented about his chamber study that was
used to evaluate the isoprene mechanism. The changes made to the model were based on better
fundamental chemistry, but the predictive capability of the model was not evaluated. Dr. Carter
continued by stating that the current regional models are not designed to handle organic reactions
under low NOX conditions, with the exception of the RADM mechanism.  He stated that the data
have not been adequate to evaluate these models and to gather the necessary data would require
the use of advanced analytical equipment to analyzes for other species.

       Edward Edwards (Dunn-Edwards Corporation) added a comment about the need to do
full circle analysis: model, chamber, and ambient air.

CMA Research Initiatives
       Jonathan Kurland, Union Carbide Corporation

       Following Dr. Kurland's presentation, William Carter (University of California)
discussed the different factors that affect reactivity and the ways to evaluate whether a model can
adequately predict them all.  In systems with VOC reacting in the presence of excess nitrous acid
and where the nitrous acid is forming all of the OH radicals, the amount of ozone or NO formed
is very sensitive to how fast the VOC reacts and the NO is converted to NO2. There is almost no
sensitivity to radical initiation or inhibition effects. This provides a way of testing that aspect of
the model independent of the other uncertainties. This method could potentially be used for very
low volatility compounds that cannot be done practically in environmental chambers. Dr. Carter
commented on his new program with the California Air Resources Board to develop more
generally applicable methods of measuring reactivity to replace the more expensive chamber
experiments.

                                          6-4

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CSMA Position on the Importance of Relative Reactivity
       Doug Fratz, Chemical Specialties Manufacturers Association

       Harvey Jeffries (University of North Carolina) commented that the ozone formation in an
urban area cannot be determined by multiplying an inventory by the MIR; a whole airshed model
has to be used. He reiterated that nearly half of the ozone is produced by low reactivity
chemicals.  Mr. Fratz responded by stating that they found very good agreement between the
MIR-weighted inventory approach and the urban airshed model approach. Both approaches
predicted very small amounts of ozone formed considering the VOC controls targeted. Both the
MIR-weighted approach and the modeling approach were being used to assess the effects of
marginal changes in VOC emissions on marginal ozone formation.  William Carter (University
of California) commented that he agreed with the way Mr. Fratz had used the MIR to look at how
to prioritize controls and not to look at what caused ozone formation.

Reactivity Concerns
       Phil Ostrowski, Occidental Chemical Corporation

       John Festa (American Forest and Paper Association) commented that the branch  of EPA
administering TRI requires the air program to declare a chemical as a negligibly reactive VOC
before it  can be removed from TRI. Mr. Ostrowski responded that maybe there would be a
rethinking of the TRI exemption in the new policy.

       Bob Avery (Eastman Chemical Company) commented that the cutoff for exemptions
should be raised in the short term, rather than lowered, in order to get more useful chemicals in
the 'tool  box.' Mr. Ostrowski expressed his concern that this approach may end up impacting air
quality in a negative way. Mr. Avery  continued by stating that there may be some local  adverse
impacts,  but overall, the substitution of low reactivity compounds would be directionally correct,
and, overall, an improvement.

Categorization of Low Reactivity Compounds
       John Owens, 3M Company

       William Carter (University of California) commented that there are procedures to
estimate  upper limits of reactivity that could be used to establish the cutoff.

       Harvey Jeffries (University of North Carolina) stated that, although compounds with a
low kOH must be looked at closely, he is not calling for compounds with lifetimes on the order
of months or years being studies in the smog chamber.

       Richard Derwent (Meteorological Office, United Kingdom) stated that this is not so
simple for theoretical studies. When working on CFC replacements, they looked at long-lived
VOCs.  It is important to have information about the degradation products and to consider the
by-products from the production of these low reactive VOCs. This will require more than just a
theoretical study, because there are a whole range of other problems. Mr. Owens responded by
stating that 3M does sponsor these studies of degradation products and does a life cycle analysis
of byproducts and products.

                                           6-5

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Impact of a Molar Ethane Standard on the Number and Type of VOC-Exemptible Compounds:
Practical and Environmental Implications
       Daniel Pourreau, ARCO Chemical Company

       Harvey Jeffries (University of North Carolina) proposed a deferred control system of five
years with possible renewal based on further analysis. Dr. Pourreau responded by stating that
industry would be reluctant to use an alternative that might not be available in the future. He
proposed that the new reactivity-based policy revisit the exemptions, but he thinks the
exemptions granted now for the low-reactivity materials would still benefit under a reactivity
based policy. Dr. Jeffries continued by commenting that it would be necessary to inventory the
exempt products.  He stated that it is necessary to know where and when and in what quantities
the VOCs are emitted to know the impact on the environment.  Dr. Pourreau stated that, although
they are trying to replace highly reactive compounds to reduce ozone, there are practical
limitations on how they can do this.

       Jim Berry  (Berry Environmental) commented on a specific slide referring to 37% solids
from water-based solvents.  He stated that for the comparison to be appropriate, the water must
be removed. Dr. Pourreau stated that the information was in pounds/ VOC and pounds/solids
and, therefore, water was not an issue.  The weight percent solids was included as an illustration
to show that the non-water coating applies more solids per application.
Session IV Summary of Questions and Discussions

Computing Volatile Organic Compound Reactivities with a 3-D AQM
       Zion Wang, University of North Carolina at Chapel Hill

       Jake Hales (ENVAIR) commented that there are many choices: use kOH, use sensitivity
coefficient, use MIR or MOIR, etc or use 3-D models over EKMA. It needs to be remembered
that MIR isn't all that simple; even with the one-dimensional EKMA model, many parameters
need to be specified such as the different ways to titrate the NOX, how peak ozone is used in the
numerator of the equation, and what domain is used. Dr. Hales concluded by soliciting
comments from the 3-D modelers.

       Ted Russell (Georgia Institute of Technology) commented that many of these are policy
questions. It needs to be asked: what is the metric for the policy makers.  Once that decision is
made, then the modelers can react. There is a need to get away from boundary conditions and
initial conditions and to look at how these emissions are added. When looking at the impact of
change in fuel composition, the emissions change needs to linked to the fuel. For a solvent, the
solvent emission distribution used would be different. It is necessary to normalize the results to a
mixture of compounds and different people might have different ideas on this normalization
process.  It will also be necessary to compare the 3-D models results to the box model  results.

       Gary Whitten (Systems Applications International, Inc.) agreed with Dr. Russell's
comments about policy. A policy decision is needed. Currently, xylene and ethane are treated
equally, but clearly they are not.  He commented that there needs to be a methodology for trading

                                          6-6

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solvents with lower reactivities. He proposed a 4-tier reactivity scheme in place of the 1-tier
scheme currently in place. Compounds in the highest tier (e.g. xylene) would be counted twice
as much; lower reactive compounds would be counted half as much. This would encourage
switching from solvents like xylene to paraffins and would be beneficial even if the alternative
was still somewhat reactive. In this way, industry can be a big credit for making the switch and
for making improvements in the reactivity in the atmosphere. Dr. Russell responded to this
proposal by stating that more bright lines don't help, especially there aren't huge gaps in the
reactivity spectrum where these different classes would divide.  Dr. Russell believes that this is
defeating the purpose of reactivity and he would prefer the policy to be driven by the best
science.

       William Carter (University of California) agreed that the policy will drive the approach.
He continued by stating that there are two main ways of looking at policy: (1) reactivity scale
which is generalized and  (2) assessment or specific substitution scenario where  replacement
should be handled in detail  with a detailed model. There is also a need for a generalized scale to
be used for prioritizing, but the reactivity scale poses different modeling problems in trying to
answer the question: what is the optimum scale to use.  The scale would need to be representative
of the criteria and to represent  a distribution of conditions (set of scenarios). Lastly, Dr. Carter is
not convinced that an EKMA model is not adequate for the purposes of developing a scale.

       Chris Walcek (State University of NY at Albany) commented that, because the scale can't
be made to be a simple one, this doesn't mean that it is impossible to have a scale. The scale
won't be simple and there will be a great deal of controversy about its development. Dr. Carter
added that it is important to have a standardized protocol for the scale; it is important not to vary
the metrics.

       Barbara Francis (CMA) commented that CMA has not yet developed positions on the
issues raised in yesterday's  or today's discussions and noted that the positions expressed here by
CMA member companies are company specific  and not necessarily industry consensus positions.
She continued by saying  that CMA is conducting research on specific chemicals and that CMA
believes that research programs should, wherever possible, be policy relevant.

Temperature Dependence of Ozone Chemilwninescent Reactions with Organics: Potential
Screening Method for VOC Reactivities
       Jeffrey  Gaffney, Argonne National Laboratory

       Chris Walcek (State University of NY at Albany) asked about the cost of the
chemiluminescence system. Dr.  Gaffney stated that the system costs between $6,000 and $7,000
which is cheaper than the NOX system and  it could also be used to look at reduced sulfur gases.

 VOC Receptor Modeling as an Aid to Evaluating the Effect of Reactivity Changes on Ozone
Formation
       Donna Kenski, US Environmental Protection Agency

       Alan Hansen (EPRI) asked about the reconstruction of the emissions mix at  the
monitoring stations and the complicating factor of emissions in between the monitoring sites.

                                           6-7

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Ms. Kenski responded by stating that the model a very simple, screening-level model and does
not include any reinforcement or deposition.  Mr. Hansen continued by asking about the lack of
impact from refineries being an artifact of the location of intermediate sources.  Ms. Kenski
answered that they tried to account for this issue with the trajectory, and by comparing the
upwind trajectories.

Computational Studies ofOxidant Reactions of Volatile  Organic Compounds Relevant to the
Formation ofTropospheric Ozone
       David Dixon, Pacific NW National Laboratory

       Eduardo Olaguer (The Dow Chemical Company) asked all the presenters if neural
network techniques had been applied. Dr. Dixon responded that he was not sure if neural nets
are being used in the field of VOC  reactivity. Neural nets are a data analysis tool and could
probably be used effectively to correlate a range of experimental measurements. Dr. Dixon was
not aware of any reasons why neural nets can not be used in this area and research on their use
and applicability would be appropriate.

       It was asked if Dr. Dixon was going to look at the reaction between the hydroxyl radical
and NO2 and he answered affirmatively. Dave  Golden (SRI) commented that the potential
energy surfaces for the hydroxyl radical and NQ reaction are inaccurate. There are two groups
that have estimated this, the IUPAC estimate is wrong and the JPL estimate is correct. It has
been measured to 5%, but could it be calculated better. Dr. Dixon responded by stating that
temperature and pressure corrections  could be included in the calculations. A question was also
asked concerning the impact of water on this reaction. Dr. Dixon responded by stating that there
would be no effect from water, unless the reaction was taking place in a droplet, but because
these reactions are fundamental gas-phase processes, this would not be expected.
Session V Summary of Questions and Discussions

Oxygenates: Reactivity Implications
       Ian Barnes, Bergische University at Wuppertal, Germany

       Eduardo Olaguer (The Dow Chemical Company) commented that the ideal approach
would be to learn all that could be learned about reactivity options, then decide how to design the
reactivity strategy.  It seems that currently, all the money goes into designing a policy index, and
the science is done to make that convenient.  Dr. Olaguer would prefer to do the science first.
                                          6-8

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FREE FORUM SUMMARY

       Howard Feldman (Moderator) described this portion of the workshop as the opportunity
for any attendee to express their 'two cents worth.' There were many experts in the audience, not
all of whom made a presentation, and many others with opinions or points of view. The free
forum was their opportunity to make whatever presentation they wished to make.

       S. Kent Hoekman (Chevron Products Company) began his comments by observing that
there had been talk about how desirable it was to separate policy and science issues.  He
expressed his opinion that, in the case of reactivity, this is impossible, and that policy is actually
required to define reactivity.  He continued by stating that science has been stymied by the lack
of policy or, at least, a broad policy outline.  In California, there is a policy definition of
reactivity, but it's limited to the certification of new vehicles with respect to exhaust emissions.
It was not designed to result in an ozone benefit, but only to achieve an equivalent ozone impact.
Therefore, the absence of the  automobile industry from this meeting is conspicuous, with the
exception of Honda.  This is perhaps because the California system is complex and burdensome
and it does not achieve an air quality benefit.  Therefore, automobile companies haven't taken
advantage of the opportunity to develop their own reactivity factors, but have relied on the
default values developed by CARB. Establishing the default values is a every expensive process;
CARB has spent hundreds of thousands of dollars to establish and maintain their ability to
determine reactivity adjustment factors.
       When reactivity is applied to stationary sources and consumer products, there are some
simplifications and some additional complexities. The first simplification is the absence of
simultaneous emissions of VOC and NOX from stationary sources or consumer products. This is
very important when dealing with automobile exhaust. Another simplification is that, for
automobiles, the VOC's are changed during the combustion processes within the car. Therefore,
the fuel put into the car is not what is emitted in the exhaust. Thirdly, there is a great variability
between the vehicles, between operating conditions, and between technology classes whereas this
complication is not present for the stationary sources.
       The first complication for stationary sources and consumer products over the mobile
sources is the great diversity of chemical structures and classes of solvents. In addition, the
atmospheric chemistry is not understood well. Secondly, it will be much more difficult to trade,
and trade fairly, for consumer products, because the materials being traded are very dissimilar.
For mobile sources, we are trading one gasoline emission mixture for another and these mixtures
are very much like one another. For consumer products and stationary sources, this will require
greater quantification and certainty in the  reactivity of materials.
       Dr. Hoekman continued by discussing two associated issues for which reactivity
arguments are being used, but that he believes must remain separate: (1) to reduce the ambient
ozone  levels and (2) the exemption of specific VOCs.  For the issue of exempting VOCs, the
focus is on establishing a bright line by looking at the  least reactive VOCs. For the issue of
reducing the ambient ozone levels, the focus is on what materials should  be controlled (VOCs,
which VOCs, or NOJ by looking at the most reactive  VOCs.  The attainment of the standard is a
broader, more urgent issue, but a VOC reactivity policy must be developed to encompass the full
spectrum of issues. It can also be asked whether or not there is any real justification for
exempting anything if it contributes to ozone.
                                           6-9

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       Dr. Hoekman summarized his remarks by stating that there are two main concerns for
industry. The first concern deals with all of the different decisions which must be made on
defining conditions, setting the scale, and measuring reactivity. There is a great deal of
arbitrariness in any policy, and although this is not good, instability is worse.  It is very difficult
for industry to deal with changes in the rules. The second concern of industry is that reactivity
may become an attractive control measure, that appeals to different states (and districts) to
different extents.  Dr. Hoekman encouraged EPA to be sure, when developing its policy, that it
can be applied generally and fairly to the whole country and not as a patchwork of different
requirements.

       Anne Giesecke (American Bakers Association) discussed the  concerns of the baking
industry. Yeast fermentation releases ethanol, which is released to the air. In addition, they
operate the third largest trucking fleet in the nation. Dr. Giesecke stated that this industry is
encouraged by these discussions.  This industry has spent about $30,000,000 turning ethanol into
CO2 and increasing the NOX emissions through catalytic oxidation. The modeling discussions
were interesting and this work needs to move forward. Although access to the models is
important, Dr. Giesecke believes that not every state and industry  needs to operate the model.
The resources of many states are strained as are many industries and she suggested that modeling
work could be out-sourced.  Dr. Giesecke is encouraged by the work  on relative or incremental
reactivity or the potential for ozone formation and the shifting  of the emphasis away from the
'yes or no' system currently in place for evaluating VOC emissions.  She  expressed the need for
more sophisticated tools such as the baking industry's interest  in the holistic or life cycle
approach.  The baking industry also recommends looking at emissions trading and how to change
from the current system where all VOCs are considered equal to one where a more reactive VOC
can be replaced by a less reactive VOC. This industry would like to see more effort put into the
study of more reactive chemicals and those that have other complications. They would also like
to see more of their money going into fleet conversion instead  of ethanol control. The baking
industry operates at a 2% profit margin and, therefore, they don't have a surplus of money to do
both.

       Leslie Ritts (Hogan & Hartson), who represents a large number of stationary source
categories, commented that for 20 years billions of dollars have been spent on control strategies
and on decisions that have led to moving business offshore.  She expressed her concern about
how the discussions held at this workshop will feed into regulations and whether or not there is a
time line for such regulations.

       Barbara Francis (CMA) commented that the consensus among the solvents producers is
that the models  are not really ready for the regulatory community  to use.  They believe that there
is enough information available now, especially on the incremental reactivity, to implement
reactivity-based regulations.

       Neil Wheeler (MCNC-NC Supercomputing Center) began his comments by reminding
the audience that establishing a reactivity policy was not going to be  easy and that the issue of
reactivity can not  be simplified.  It will take a great deal of work to apply the policy fairly and
effectively.
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       Mr. Wheeler stressed the need for this to be a community effort and that people need to
participate and to share information. He commented that there is a wide range of possibilities of
how to use reactivity in the regulatory process: from setting exemptions with a bright-line (or
not) to reactivity-weighted emissions. He also commented that models do not make decisions.
There will be external information (scientific or policy) that will affect the decision making
process and consideration must be given to other environmental issues as well.
       He expressed the need for multiple metrics to help the policy makers and the need for the
scientific community to clearly describe the meaning of these metrics. Consideration should be
given to the range of conditions from the current time out into the future. It is important to
monitor an exempt VOC both in the inventory and in the ambient environment into the future to
be certain that a poor decision has not been made. He agrees that stability is important in a
regulatory process but noted that we cannot have absolute stability, especially in light of possibly
making a bad decision. There needs to be a systematic process for dealing with necessary change
based on new information.
       Mr. Wheeler discussed the range of metrics needed such as metrics to  assess exposure,
various meteorological conditions, multiple locations, multiple pollutants, and total risk. He
emphasized the need to develop metrics using photochemical models with the best science
available. He feels that it may be possible to use simpler models, such as EKMA, for developing
a reactivity scale but they must first be evaluated against state-of-the-science models.

       Roger Tanner (TVA) commented that the data shows clearly that ozone formation is NOX-
limited in some areas and is VOC-limited in others and that these conditions vary greatly by
location and by season, depending on the sources of VOCs and NOX. He believes that a metric is
needed that scales with the actual conditions within an airshed. In order to predict ozone
reduction in particular locations and at the times necessary get below the standard, a sliding
airshed-specific metric in needed.  Dr. Tanner believes that this type of metric can be  devised
with our current scientific knowledge.

       Ken Schere (EPA/ORD) discussed the differences between developing assessment tools
and procedures and screening tools for implementation.  Between these two ends of the
spectrum, there are many possibilities. The scientific tools are available to do a full scale
assessment to describe reactivity as a function of various environmental variables.  Dr. Schere
commented that Dr. Russell showed that a sophisticated tool can be reduced down to  a simple
screening tool. In order to decide where on the spectrum we need to be, it is  necessary to know
what the policy makers need.

       Randy Pasek (CARB) expressed his agreement with comments made previously about
California's reactivity regulation. The regulation is limited and complex.  But California has
been moving ahead since the regulation was developed.  From a regulatory perspective,
Dr. Pasek believes that the policy must be based on good science and that the complexity should
be understood. And it is very important that the policy be constant. He echoed Dr. Wheeler's
suggestion to build into the policy a process for change in order to make the policy more stable.
CARB has a policy based on the MIR scale, because it is a good complement to the NOX
controls.  Lastly,  Dr. Pasek expressed his agreement with the comment of Ms. Francis that the
science is adequate to develop regulations, as has been done  in California.
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       Dave Golden (SRI and Stanford University) believes that good models are needed to
understand any complex process.  He continued by commenting that although the science has
advanced very far and the models are reasonable, there are a lot of things we don't know. He
warned that we shouldn't think that because we can model something that the models are
necessarily correct. He expressed his inability to believe in  a model that predicts PM2 5.  He
concluded by urging that the scientific work and the funding be continued

       George Brown (National Aerosol Association) discussed the problems caused by the huge
variability in VOCs and the fact that the current regulations  treat them as being equal. This
situation severely inhibits the use of certain substances and outlaws the use of others. As an
example, on January 1,1999, CARD will implement a rule that allows zero VOCs in one
product. Mr.  Brown believed this is ludicrous.  The National Aerosol Association (NAA) has
supported several reactivity studies over the last ten years and, based in these studies, they are
committed to the regulatory use of relative reactivity. The NAA realizes that some substances or
products will  have difficulty operating under that system and they don't, as yet, have the
solutions to these problems. At the present time in California, the NAA believes that relative
reactivity ought to be used on an optional basis by sources having trouble meeting a mass-based
standard.  Lastly, Mr. Brown believes we should stop thinking hi terms of cutting down the mass
of precursors  of ozone and begin thinking in terms of ozone limitation itself.

       Phil Ostrowski (Occidental Chemical Corporation) commented about the economic
benefits of reactivity regulations.  Properly designed reactivity regulations should provide a tool
whereby small solvent users can avoid installing costly control equipment. This will provide
good environmental benefit at a low cost.

       JeffGaffney (Argonne National Laboratory) echoed some of Dr. Golden's preceding
comments. He urged the group not to forget about VOC chemistry  and not limit the discussion
to only the ozone-driven aspects.  It should be remembered that VOCs form fine aerosols and
other products such as nitro-phenols that are very toxic and water soluble. Wet deposition, cloud
condensation, climate effect, and radiative properties (UV and IR absorption) of VOCs should
also be considered. He made a plea for the science and the sum-level support of the science. He
believes that by understanding the science better, the scientific community will be able to provide
a knowledge base to allow the policy markers and the modelers to do a better job.

       Tun Lawrence (Georgia Pacific and American Paper and Forestry Association)
commented that, although the science has been fascinating,  we must recognize the need for
pragmatic regulatory tool development in parallel with the existing  scientific research. At this
time, EPA is moving forward with implementation  plans for a national ambient air quality
standard for fine particulates, ozone, and regional haze; VOC and NOX are all listed for controls
under these programs. By November 2000,170 different industrial categories will receive
MACT standards.  For organic HAPs, many of the MACT floors are being set based on existing
VOC controls. There is also implementation of the Kyoto Treaty that needs to be considered.
Mr. Lawrence feels that there need to be two parallel tracks: (1) one track moving forward very
quickly because  of pending regulatory decision that have to be made and (2) the other track
continuing to understand the details of the science.  Regulatory tools such as those described by
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Donna Kenski (EPA, Region 5) are important in the near term to assess the effectiveness of
proposed regulatory action.

       Praveen Amar (NESCAUM) stressed the need to look at aerosol forming potential of
VOCs which might be exempted, in addition to the ozone forming potential. As an example,
between 33% and 40% of the fine particles in the Northeast are organics.  Consideration should
also be given to wet deposition, dry deposition, and toxicity.

       Doug Fratz (Chemical Specialties Manufacturers Association) made comments
comparing the use of regional or local reactivity scales versus the use of a linear national scale.
There are a number of control types that could be controlled locally. For other sources, such as
consumer products, it would not be practical to have a different product for every local region.
Therefore,  to use reactivity, there must be a single national scale based on a single metric.
Mr. Fratz also commented on the funding of research as compared to the  cost of controls. He
feels that research is still under-funded and that the ratio of money spent on controls to money
spent on research is far to high.

       Jeffrey Holmstead (Latham & Watkins) stated that in the regulatory arena, we operate in a
legal  framework that doesn't offer much flexibility. He hopes that in the long term, the
framework can be changed to allow flexibility. But in the near term, there are things that can be
done. Mr.  Holmstead reminded that group that they already have a reactivity scale where
everything is either a 0 or a 1, and he believed that it would be hard for this group to do worse
than that.  In the near term, he believes that the current knowledge can be used to help people
move from using highly reactive compounds to using lower reactive compounds.  In the long
term, the scientific research needs to continue.  Mr. Holmstead urged the group not to let the
perfect be the enemy of the good in the  short term.

       William Carter (University of California) wanted to echo what Mr. Holmstead said about
the near term problems. There are three approaches to using reactivity: the two currently used
reactivity scales (the binary national scale and the California MIR scale)  and airshed/scenario
specific assessment.  The scientific basis of the ethane exemption standard is not good.  This is
why the EPA has frozen the exemption  petitions, but these can't stay frozen for long. Dr. Carter
suggested that in the near term the EPA do a modeling assessment to recertify the ethane
standard or identify another standard. This would then allow the present method to continue
while alternative methods are being developed. In California, the regulations they are developing
require a scale which, if nothing else is put forward, is going to be the MIR scale. With the
demand for stability, if the MIR scale is implemented (later in the year), it will be difficult to
change. Therefore, this is the time to provide an alternative. Dr. Carter strongly emphasized the
urgency of this problem.

       Bob Avery (Eastman Chemical Company) recommended two tracks be followed in the
future. Although the modelers are improving our understanding, the necessary results will not be
available for three to five years, optimistically. A more realistic time frame is  between five and
ten years.  The current system is bad and, therefore, a better interim system is needed for the next
two to five years. Mr. Avery suggested that a few dozen individuals should be able to sit down
in a room and improve on the current binary policy.

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       Cyril Durrenburger (Texas Natural Resource Conservation Commission) discussed the
Control Measure Catalog developed for the last SIP submitted by Texas.  It is a metric that ranks
the VOC controls based on the tons reduced, toxicity, and the reactivity using Dr. Carter's MIR
scale.

       Robert Wendoll (Dunn- Edwards Corporation) discussed two approaches to the
policy/science issue first raised by Mr. Hokeman. The scaling approach is used to rank VOCs by
some reactivity metric for regulatory purposes.  There are policy decisions that have to be made
and some of these will be arbitrary, by necessity. Other decisions would be arbitrary only
because of the lack of scientific information. The complementary approach is the systemic
approach which is the study of actual emissions into ambient air to determine their potential to
contribute to high ozone levels across the full range of environmental conditions. Mr. Wendoll
believes that the systemic approach is important because it is the area of research that will
develop the policy-relative science or the science that links actions with outcomes.  This allows
the policy makers to choose action intelligently.  Mr. Wendoll believes that both the scaling
approach and the systemic approach should be pursued simultaneously. The policy makers must
realize that both of these approaches together are embedded in the total ecological impacts.
There will be other factors that affect the regulatory decisions being made, such as the impact of
the regulations, including material resource and energy consumption, waste disposal, and water
quality. Mr. Wendoll echoed the comment made by Mr. Fratz about the ratio of research
spending to compliance spending. He believed that the amount of money that needs to be spent
on the research necessary to provide a better basis for sound regulations is minuscule compared
to the cost of compliance.  Lastly, Mr. Wendoll  reminded the group that control costs also have
indirect health impacts by reducing available income.

       Dave Morgott (Eastman Kodak Company) commented that in order to assess the intrinsic
impact of VOCs on the environment, the more appropriate scale is the MOIR scale and not the
MIR scale. The MOIR scale provides information about the peak amount of ozone that can be
formed when a quantity of VOC is introduced into the environment.
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POLICY AND SCIENCE QUESTIONS SUMMARIES


       Howard Feldman (Moderator) introduced this segment of the workshop by asking the
group to consider what needs to be done next.  A review of these policy and science questions
will be a form of guidance. This is a genesis workshop and a group will be formed as a result of
this workshop and will continue these discussions. Mr. Feldman reviewed the policy questions
listed below and asked the group if these are the right policy questions.  He also asked the group
if there are other questions that should be added to this list.

POLICY QUESTIONS

1.     How should reactivity policy account for interaction with other air-pollution problems?
2.     How should the reactivity concept be used to both maximize environmental benefit and
       encourage environmentally superior product development? "Exemption" vs.
       "substitution"?
3.     What is the maximum uncertainty level that can be tolerated for reactivity-related
       decision making?
4.     Exemption policies:
       ° Bright line vs. bright band?
       o Environmental cofactors?
       o Where, ethane?
       ° Molar or mass basis?
5.     Exemption protocols:
       o Cookbook?
       o Maintenance and tracking?
       ° Automatic testing criteria?
6.     Procedures  for modifying exemption criteria? Grandfathering?  Grace periods?
7.     Substitution protocols and guidelines?
8.     How should vapor pressure be incorporated into the decision process?


       Bob Avery  (Eastman  Chemical Company) raised the issue of national standards versus
regional standards, and he believes that this question needs to be added to the list.

       Edward Edwards (Dunn-Edwards Corporation)  was concerned about availability and
whether availability will be considered when making policy decisions.  Availability is the issue
of the difference between what's in the can and what's in the air.  He was also concerned about
looking at the time domain used to assess the ozone impact. For example, a paint may last from
between two to fifteen years, depending on how it is formulated.  The question is will the ozone
impact be assessed only for the one-time application or for the full life cycle of the product.
These are both very critical policy decisions in analyzing how to- determine whether the VOC
life cycle is important for ozone forming potential.

       Jonathan Kurland (Union Carbide) made comments on question 8 that deals with vapor
pressure. He stated that the issue of volatility  is a subset of the general issue on how much of the

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content becomes emissions. There are other environmental non-evaporative fates (e.g. down the
drain). Dr. Kurland believes that this question should be expanded to include consideration of
whether the policy can properly determine the actual emissions released into the atmosphere as
opposed to other estimates such as gross sales.

       John Durkee (Creative Enterprizes) commented that an additional policy question is
needed that deals with the issue of communication of the policy to the affected community.
Policy which can't be communicated may not be good policy. As the policy is developed,
consideration should be given to how the policy will be communicated, because, regardless of the
quality of the science, the end-user won't buy it if they don't understand it.

       Howard Feldman (Moderator) reviewed the science questions listed below and asked the
group if these are the right science questions. He also asked the group if there are other questions
that should be added to this list or it any of these questions should  be taken off the list.

SCIENCE QUESTIONS

1.     Is a reactivity-based policy practical, feasible, and beneficial?
2.     How do we best factor long-range transport into a reactivity-based strategy? How about
       co-dependencies with  PM?
3.     What are the uncertainties of the various possible reactivity scales?
4.     What are the advantages/disadvantages of using MODELS3 for estimating reactivity?
5.     What are the merits of using speciated VOC reactivities, as opposed to lumped VOC
       reactivities?

       William Carter (University of California) commented that several of these questions are
actually policy questions.  The questions on the practicality and feasibility of a reactivity-based
policy are policy issues. Although the question on the benefits of a reactivity policy is a
scientific issue, it would require a policy on how to measure the benefit. Also, the question on
using MODELS3 (question 4) has both a policy and a science component.  Whether or not
photochemical grid models can be trusted  is a science question, but the advantage or
disadvantage to using one is a policy question.

       Anne Giesecke (American Bakers Association) commented that it is difficult to divide
science and policy issues. From an industry perspective, they are looking for regulatory
baselines: predictability, long-term planning, and basic functionality. Baking companies
currently work with a very high level of uncertainty on their emissions (+/- 30%). This is
acceptable, because it provides a regulatory baseline that tells them if they are in or out of an
EPA threshold for clear air requirements.  For this reactivity-based policy, the same level of
science and policy would be acceptable, if it establishes a regulatory baseline.

       Jason Ching (EPA) pointed out that a powerful system framework such as Models-3,
together with its Community Multiscale Air Quality (CMAQ) model provides a modeling
capability for estimating model reactivity.  The Models-3/CMAQ  system ability to provide a plug
and play capability allows the substitution or replacement of various science process options
including the means to modify (edit) existing chemical mechanisms or by exchanging and

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studying alternative chemical mechanisms. This capability and the other unique suite of
modeling capabilities and features in this system provide a powerful means to perform the
various model experiments and sensitivity tests needed to evaluate model response to changes in
reactivities.  Further, because this is a publicly available system, it provides a means for the
entire community of interested parties to become involved and to contribute to the research,
development and assessment of reactivity models, and ultimately, to improved air quality
models.

       Jake Hales (ENVAIR) commented that Question 4 was intended to be more generic than
just MODELS3. He suggested that MODELS3 be replace with 3-D or Eulerian models. Howard
Feldman (API) suggested that a Question 4a be added: how do you use one of these models to
determine a relative or incremental reactivity for substitution purposes. Other related questions
are:  how many simulations are needed, how good do the databases need to be for a given urban
area to do these calculations on a national level, or, if a scale is used, was the modeling used to
develop the  scale adequate.

       Jim Vickery (EPA/ORD) would like to add a question about timing. He asked the
scientists what could they produce in the next two to three years that  could help guide the policy.
This would allow the policy maker to decide if they should develop an interim policy or if they
should wait  for a permanent answer.

       William Carter (University of California) wanted to add to Question 4:  What is the
distribution  of conditions where ozone is a problem and where VOC  control is relevant.

       Howard Feldman (API) commented about the time period of a scale:  1-hour or 8-hour or
some other time period.

       Ed Edwards (Dunn-Edwards Corporation) was concerned about the sensitivity of the
models and their ability to measure small changes in product formulations and how these small
changes are expanded into a airshed which contain only fractional percentage of VOCs.

       Jim Berry (Berry Environmental) made several comments concerning the change in 1976
from Rule 66 to the beginning of the federal program. Rule 66 was based on reactivity
measurement for one solar day.  Subsequent work based on multi-day exposures, recognized that
many of the compounds that Rule 66 exempted actually reacted over the longer term. In earlier
discussions, Dr. Jeffries stated that half of the ozone formation was the result of slower reacting
materials. Mr. Berry continued by discussing the impact that Rule 66 and, subsequently the
change to the federal program, had on various industries.  He commented on the resources spent
on reformation to comply with Rule 66 and then again to  comply with the federal program. He
urged that the lessons learned in 1976 not be forgotten, and that changes be made to the federal
program only after there is a longer term vision.

       Paul Makar (Atmospheric Environment Service) asked if it would be possible to create a
hierarchy of methods for measuring reactivity that agree with one another. Many methods of
dealing with reactivity had been presented; his concern was that the use of more than one method
for regulatory purposes may necessitate intercomparison to ensure that the methods do not give

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conflicting results. For example, before using 3D models for regulatory purposes, their results
should be compared to the current ethane standard and/or MIR indicies. Any differences should
be fully understood in advance of implementation of regulations, to avoid undermining their
scientific credibility.

       Jeffrey Gaffney (Argonne National Laboratory) suggested that a question be added about
the reactivity of secondary products of the primary emitted VOCs. The chemistry of these
secondary products needs to be understood, because they will play a role in the long-range
transport issue.
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PUBLIC/PRIVATE PARTNERSHIP DISCUSSION SUMMARY

       Jake Hales (Moderator) began this portion of the workshop by describing NARSTO. Dr.
Hales then asked the group if it is appropriate to go into a public/private partnership to pursue the
reactivity issue, either within NARSTO or separate from NARSTO.  Dr. Hales described his
views on the function of this committee as follows: (1) to establish the forum for communication
among interested participants, including the policy community and (2) to design a plan for the
future strategy for reactivity research and to provide a time table for the research.  He asked the
group if there were any strong feeling against forming a public/private partnership. He took the
lack of response from the group as consent.
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AD HOC OPERATIONS TASK FORCE DISCUSSION SUMMARY

       Jake Hales (Moderator) began by describing his thoughts about generally how this ad hoc
task force would operate. Anyone would be welcome to participate.  At a minimum, there would
be several meetings per year. There would be communications on a regular basis.  Travel
expenses would be the responsibility of the individuals participating.

       A question was asked about whether the ad hoc task force would necessarily function
under NARSTO. Dr. Hales responded by stating that the task force could be either independent
or it could work as a functionary group under  NARSTO. It could blend into all of the NARSTO
task activities: modeling, chemistry, observations, assessment, etc. If the group was to work
under NARSTO, it would have to adhere to the quality assurance and data management
guidelines. It would also have to adhere to the basic NARSTO principles which are to do good
research for the benefit of policy.

       Dr. Hales continued by  asking for volunteers to serve on the ad hoc task force. There was
a show of hands. Dr. Hales suggested that a sign-up list be circulated, and that the group caucus
immediately after lunch.

       Dr. Hales began the discussion by asking the group if this ad hoc group should function
under the NARSTO umbrella.  Robert Wendoll (Dunn-Edwards Corporation) asked if NARSTO
doesn't also have to agree to this association. Jake Hales described the standard procedures for
NARSTO to accept a field program under its umbrella. The Science and Resource Planning
group makes these decisions, but he expects no problem with this. William Carter (University of
California) suggested that the group encourage Europeans participation, who have made
important contributions to this work. Dr. Hales responded by saying that NARSTO has  in the
past worked with the Europeans.  EuroTrac is  an affiliate member of NARSTO and other
European efforts could be in the future.

       Bob Avery (Eastman Chemical Company) asked about alternatives to NARSTO. He
didn't feel that the workshop group had the information available to make the decision on
whether to associate with NARSTO. Mr. Avery was particularly interested in more information
about the costs associated with association with NARSTO.  He asked if the EPA could provide
the leadership as an alternative. Jim Vickery (EPA/ORD) responded by stating that the EPA is
committed to conducting and organizing all of their ozone related research through NARSTO for
two primary reasons. This has helped to coordinate all of the different aspects  of the research
and to effectively allocate the scarce resources of people and money. Dr. Vickery strongly
recommended that the ad hoc task force operate under NARSTO.

       Jeffrey Holmstead (Latham & Watkins) asked how this effort would feed into the EPA's
policy decisions.  He asked about the EPA's level of interest in pursuing these issues and
whether the EPA is in a position to accommodate the changes in the policy that this group would
recommend.  Jake Hales  expressed his observation that a simple liaison with a policy team is not
effective. There needs to be a strong presence of EPA policy people hi the partnership.  Bill
Johnson (EPA/OAQPS) responded to Mr. Holmstead's question by stating that this question is
one that EPA's management would need to answer.  Joe Paisie (EPA/OAQPS) added that as

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Sally Shaver (EPA/OAQPS) said in her introductory comments to this workshop, the EPA is here
to listen, and has been listening, but they are not prepared to say what the results will be yet.

       It was asked if this activity could enjoy equivalent status with the recent FACA process.
That is, could there be direct EPA/OAQPS participation in the process.

       Jeffrey Gaffney (Argonne National Laboratory) asked about extending invitations for
participation in the task force to people who had left or who didn't attend the workshop, such as
automobile makers. Ron Patterson (EPA/ and NARSTO) commented that several people who
are no longer here did complete the commitment forms made available at the beginning of the
workshop.  He added that many of the automakers are members of NARSTO.

       Tim Lawrence (Georgia Pacific and American Paper and Forestry Association)
commented, based on his experience with several FACA processes, that the level of interest,
participation, and commitment of resources, particularly by the regulating community, is directly
related to their sense of just how serious EPA is about moving the process forward to a useful
endpoint. He concluded that it will be very important at the beginning to see some real finite
indication of EPA's level of interest.

       Howard Feldman (API) commented that the next step is to develop a plan with a
specified time horizon. It will be important to know what time horizon EPA would be receptive
to on the policy side. On the other hand, it is important to continue to work towards the good
science, because the policy makers will use it if it is there.

       Jim Vickery (EPA/ORD) agrees with Mr. Feldman's comment about the importance of
good science and the fact that it will feed into the policy process. He described the difference
between the FACA processes and NARSTO. For the FACA process, there was a statutory driver
that required an output by a certain date.  There is no such a driver for the reactivity policy.
Reactivity research is very much like the other ozone research organized under NARSTO. Under
NARSTO, the researchers and the policy makers are brought together to organize the research in
such as way as to use the resources efficiently and  solve the most important questions for the
policy maker as quickly as possible.  The EPA policy office is committed to using good science
as soon as it is produced.

       Jake Hales (Moderator) summarized this discussion by stating that there is consensus to
form a public/private partnership on reactivity research and there are people interested in
participating in an ad hoc task force to develop the forum, the research plan and the time table.
Whether this task force operates under NARSTO is a question that will be deferred to the task
force itself.  Everyone interested in serving on the task force was asked to meet after the
conclusion of the workshop.
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APPENDICES

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                                      APPENDIX A
                           Photochemical Reactivity Workshop
                                     May 12-14,1998
                                   ATTENDEES LIST
Zac Adelman
Student
University of NC
Chapel Hill, NC 27599
919-966-1372
zac@ozone.sph.unc.edu

Robert Altenburg
Air Quality Program Specialist
PA Dept. Environmental Protection, Air Quality
400 Market St, 12th Floor
Harrisburg, PA  17105
717-787-9495  Fax 717-772-2303
altenburg.robert@al.dep.state.pa.us

Praveen Amar
Director, Science & Policy
NESCAUM
129 Portland St
Boston, MA 02114
617-367-8540  Fax 617-742-9162
pamar@nescaum.org

Viney Aneja
Research Professor
NCSU, Marine, Earth, & Atmospheric Sciences
Box 8208
Raleigh, NC 27695
919-515-7808  Fax 919-515-9802
viney_aneja@ncsu.edu

Anne Arnold
Environmental Engineer
US EPA Region I
JFK Federal Bldg
Boston, MA 02135
617-565-3166  Fax 617-565-4940
arnold.anne@epamail.epa.gov

Roger Atkinson
Air Pollution Research Center
University of California
Riverside, CA 92521
909-787-4191  Fax 909-787-5004
ratkins@mail.ucr.edu
Robert Avery
Sr. Associate, Product Issues Management
Eastman Chemical Company
PO Box 431,6-280
Kingsport, TN 37617
423-229-5409 Fax 423-224-0208
rjavery@eastman.com

Dennis Bahler
Professor
NC State University
Box 8206
Raleigh, NC  27695
919-515-3369 Fax 919-515-7896
bahler@ncsu.edu

Dan Baker
Staff Research Engineer
Shell Oil
3333Hwy6S
Houston, TX 77082
281-544-8437 Fax 281-544-8727
dcbaker@shellus.com

Ian Barnes
Bergische University Wuppertal
Gauss Str. 20
Wuppertal, D-42097 Germany
49-202-439-2510 Fax 49-202-439-2505
barnes@physchem.uni-wuppertal.de

Gary Beckstead
Environmental Protection Engineer
Illinois EPA
1340N9thSt
Springfield, IL  62702
217-524-4343  Fax 217-524-4710
epa2161 @epa.state.il.us

William Benjey
Physical Scientist
US EPA/NERL/AMD
MD-80
Research Triangle Park, NC 27711
919-541-0821  Fax 919-541-1379
benjey@hpcc.epa.gov
                                            A-l

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Howard Berman
Senior Vice President
Kessler & Associates
510 llthSt, SE
Washington, DC 20003
202-547-6808  Fax 202-546-5425

Jim Berry
Berry Environmental
PO Box 20634
Raleigh, NC  27619
919-785-9631  Fax 919-785-9631
j imberryec@aol .com

Karen Borel
Environmental Engineer
US EPA Region IV
61 Forsyth St
Atlanta, GA 30303
404-562-9029
borel.karen@epamail.epa.gov

Kim Boudreaux
Environmental Engineering Advisor
Albemarle Corporation
451 Florida St
Baton Rouge, LA 70808
504-388-7776  Fax 504-388-7046
kim_boudreaux@albemarle.com

George Brown
Executive Director
National Aerosol Association
787 Windgate Dr
Annapolis, MD 21401
410-349-8614  Fax 410-349-8616
gwbjmb@annap.infi.net

Christine Brunner
Chemical Engineer
US EPA
2000 Traverwood
Ann Arbor, MI 48105
734-214-4287  Fax 734-214-4051
brunner.christine@epa.gov
Larry Bruss
Ozone & SIP Development Section Chief
WI Dept of Natural Resources
PO Box 7921
Madison, WI 53707-7921
608-267-7543  Fax 608-267-0560
brussl@mai!01 .dnr.state.wi.us

Daewon Byun
Physical Scientist
US EPA/AMD/NERL
MD-80
Research Triangle Park, NC 27711
919-541-0732  Fax 919-541-1379
bdx@hpcc.epa.gov

William Carter
Research Chemist
University  of California
CE-CERT, University of California
Riverside, CA 92521
909-781-5797  Fax 909-781-5790
carter@cert.ucr.edu

Donna Carvalho
Pennzoil Products & Magie Brothers
PO Box 2967
Houston, TX 77252
713-546-8723  Fax 713-546-8930

Roy Carwile
Manager, Air Programs
ALCOA
1906 Alcoa Bldg
Pittsburgh, PA  15219
412-553-2680  Fax 412-553-4077
roy.carwile@alcoa.com

Janet Catanach
Environmental Planner
Exxon Chemical Company
13501 Katy Freeway
Houston, TX 77079
281-870-6959  Fax 281-588-4664
                                           A-2

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William Chameides
Regents Professor
Georgia Institute of Technology
School of Earth & Atmospheric Sciences
221 Bobby Dodd Way
Atlanta, GA  30332-0340
404-894-1749  Fax 404-894-1106
wlc@blond.eas.gatech.edu

Grish Chandra
Scientist & Technical Manager
Dow Corning Corp.
PO Box 994
Midland, MI 48640
517-496-5990  Fax 517-496-5595
gchandra@dcrn.e-mail.com

Kirit Chaudhari
Director, Office of Air Data Anal) sis
VA Dept of Environmental Quality
PO Box 10009
Richmond, VA  23240
804-698-4414  Fax 804-698-4510
kochaudhar@dea.state.va.us

Mengdawn Cheng
Research Staff Member
Oak Ridge National Laboratory
Environmental Science Division,  MS 6038
Oak Ridge, TN  37831
423-241-5918  Fax 423-576-8646
chngmd@ornl.gov

Qiao-Jung Chien
Student
University of NC - Chapel Hill
Chapel Hill, NC 27606
919-966-1372
chien@ozone.sph.unc.edu

Jason Ching
Chief, Atmospheric Model Development Branch
US EPA/AMD/NERL
MD-80
Research Triangle Park, NC  27711
919-541-4801  Fax 919-541-1379
ching.jason@epamail.epa.gov
Shao-Hang Chu
Environmental Scientist
US EPA
MD-15
Research Triangle Park, NC  27711
919-541-5382 Fax 919-541-7690
chu.shao-hang@epamail.epa.gov

Jeff Clark
Director, Policy Analyses & Communications
US EPA/OAQPS
MD-10
Research Triangle Park, NC  27711
919-541-5615 Fax 919-541-2464

John Clary
President
Bio Risk
PO Box 2326
Midland, MI 48641
517-839-8130 Fax 517-839-8130
bioriskl@aol.com

Andy Collantes
Technical Director - Chemicals
Sherwin-Williams, Diversified Brands
31500 Solon Rd
Solon, OH 44139
440-498-6092

Karla Colle
Senior Staff Chemist
Exxon Chemical Co
PO Box 4900
Baytown, TX 77520
281-834-5115  Fax 281-834-1904

Ted Creekmore
Environmental Engineer
US EPA
MD-15
Research Triangle Park, NC 27711
919-541-5699  Fax 919-541-0824
                                            A-3

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Tammy Croote
Economist
USEPA/OAQPS/ISEG
MD-15
Research Triangle Park, NC  27711
919-541-1051  Fax 919-541-0839
croote.tammy@epa.gov

Larry Cupitt
Director, Human Exp. & Atmospheric Sci. Div.
US EPA/ORD/NERL
MD-77
Research Triangle Park, NC  27711
919-541-2454 Fax 919-541-0239
cupitt.larry@epamail.epa.gov

Tom Dann
Head Air Toxics
Environment Canada
ETC, 3439 River Rd
Ottawa, Ontario  K1A OH3 Canada
613-991-9459 Fax 613-998-4032
dann.tom@etc.ec.gc.ca

Phil Davison
Issues & HSE Manager
BP Chemicals Ltd
Hull Works, Salt End
Hull, London HU12 80S  UK
44-1482-2448 Fax 44-1482-2057
davisonp@bp.com

John Dege
Manager, Air Programs
DuPont - Environmental Excellence Center
1007 Market St
Wilmington, DE 19707
302-773-0900 Fax 302-774-1361
john.a.dege@usa.dupont.com

Robin Dennis
US EPA/NERL
MD-80
Research Triangle Park, NC  27711
919-541-2870 Fax 919-541-1379
rdennis@hpcc.epa.gov
Dick Derwent
Meteorological Office
London Road
Bracknell, Berkshire  RG12 2SZ UK
44.1344854624  Fax 44-1344854493
rgderwent@meto.gov.uk

Folke Dettling
Dipl. Chem.
Umweltbundesamt
Postfach 330022
Berlin, Germany D14191
49-30-8903-3845  Fax 49-30-8903-3232
folke.dettling@uba.de

David Dewitt
Senior Engineer
Honda Research & Development
1900 Harpers Way
Torrance, CA  90501
310-781-5718 Fax 310-781-5655
ddewitt@hra.com

N. N. Dharmarajan
Senior Consultant
Central & South West Services, Inc.
1616 Woodall Rodgers Freeway
Dallas, TX 75202
214-777-1373 Fax 214-777-1320
ndharmarajan@csw.com

Basil Dimitriades
Senior Scientific Advisor
US EPA
MD-80
Research Triangle Park, NC 27711
919-541-2706 Fax 919-541 -1094
dimitriades.basil@epamail.epa.gov

David Dixon
Associate Director, Theory, Modeling &
     Simulation Env. Molecular Sciences Lab
Pacific Northwest National Laboratory
906 Battelle Blvd, MSK1-83
Richland, WA 99352
509-372-4999 Fax 509-375-6631
da_dixon@pnl.gov
                                           A-4

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Ian Dobson
External Affairs Manager, Solvents Business
BP Chemicals LTD
Pinners Hall, 105-108 Old Broad St
London, EC2N 1ER  UK
44-171 -496-2786  Fax 44-171 -496-2706
dobsoni@bp.com

Paul Dugard
Executive Director
Halogenated Solvents Industry Alliance
200lLSt,NW, Suite 506A
Washington, DC 20036
202-775-0232  Fax 202-833-0381
srisotto@hsia.org

Robin Dunkins
Environmental Engineer
US EPA/OAQPS/AQSSD
MD-15
Research Triangle Park, NC 27711
919-541-5335  Fax 919-541-5489
dunkins.robin@epamail.epa.gov

John Durkee
Owner
Creative Enterprizes
105 Anyway, Suite 209
Lake Jackson, TX  77566
409-292-0244  Fax 409-292-0440
jdurkee@brazosport.cc.tx.us

Cyril Durrenberger
Senior Engineer
TX Natural Resource Conservation Commission
PO Box 13087, MC-164
Austin, TX 78711
512-239-1482  Fax 512-239-1500
cdurrenb@tnrcc.state.tx.us

Edward Edney
Research Physical Scientist
US EPA
MD-84
Research Triangle Park, NC 27711
919-541-3905  Fax 919-541-4787
edney.edward@epamail.epa.gov
Edward Edwards
Owner
Dunn-Edwards Corp.
4885 E 52nd Place
Los Angeles, CA 90040
213-771-3330 Fax 213-771-4440

Peter Ellis
Exxon Chemical Co
5200 Bayway Dr
Baytown, TX 77058
281-834-1681 Fax 281-834-2747
peter.s.ellis@exxon.sprint.com

Ron Evans
Group Leader
US EPA/OAQPS/AQSSD/ISEG
MD-15
Research Triangle Park, NC  27711
919-541-5488 Fax 919-541-0839
evans.ron@epamail.gov

Howard Feldman
Research Program Coordinator - Air
American Petroleum Institute
1220LSt,NW
Washington, DC 20005
202-682-8340 Fax 202-682-8270
feldman@api.org

John Festa
Senior Scientist
American Forest & Paper Association
1111 19thSt,NW
Washington, DC 20036
202-463-2587 Fax 202-463-2423
john_festa@afandpa.org

Franz Fiedler
Professor
University/Research Center Karlsruhe
Kaiserstr. 12
Karlsruhe, Germany
49-721-608-3355  Fax 49-721-608-6102
f.fiedler@phys.uni-karlsruhe.de
                                           A-5

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Gary Foley
Director
US EPA/NERL
MD-75
Research Triangle Park, NC 27711
919-541-2106  Fax 919-541-0445
foley.gary@epamail.epa.gov

Yvonne Fong
Environmental Protection Specialist
EPA Region IX
75 Hawthorne St, AIR-4
San Francisco, CA 94105
415-744-1199  Fax 415-744-1076
fong.yvonnew@epamail.epa.gov

Barbara Francis
Director
Chemical Manufacturers Association
1300 Wilson Blvd
Arlington, VA 22209
703-741-5609  Fax 703-744-6091
barbara_francis@mail.cmahq.com

Douglas Fratz
Director of Scientific Affairs
Chemical Specialties Manufacturers Association
1913 Eye St, NW
Washington, DC 20006
202-872-8110  Fax 202-872-8114
dfratz@csma.org

Christopher Frey
Assistant Professor
Civil Engineering - NCSU
311 Mann Hall - CB 7908
Raleigh, NC 27695
919-515-1155  Fax 919-515-7908
frey@eos.ncsu.edu

Dawn Froning
Environmental Specialist
MO Dept of Natural Resources
PO Box 102
Jefferson City, MO 65101
573-751-4817  Fax 573-751-2706
dfroning@mo.state.us
Jeffrey Gaffney
Research Chemist
Argonne National Lab
9700 Cass Ave
Argonne, IL  60439
630-252-5178  Fax 630-252-8895
gaffney@anl.gov

Kenneth Galluppi
Senior Scientist
University of NC
107 Miller Hall, CB #1105
Chapel Hill, NC 27599
919-966-9926  Fax 919-966-9920
galluppi@unc.edu

Mark Garrison
Air Quality Meteorologist
ERM
855 Springdale Dr
Exton,PA  19341
610-524-3674  Fax 610-524-7798
mark_garrison@erm.com

Harald Geiger
Bergische University Wuppertal
Gauss Str. 20
Wuppertal, D-42097 Germany
49-202-439-3832  Fax 49-202-439-2505
geiger@physchem.uni-wuppertal.de

Nash Gerald
Environmental Engineer
US EPA/OAQPS/EMAD
MD-14
Research Triangle  Park, NC  27711
919-541-5652  Fax 919-541-1903
gerald.nash@epa.gov

Sharon Gidumal
Technical Consultant
DuPont
PO Box 80711
Wilmington, DE 19808-0711
302-999-5325  Fax 302-999-2093
                                            A-6

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Anne Giesecke
V.P., Environmental Activities
American Bakers Association
1350ISt,NW, Suite 1290
Washington, DC  20005
202-789-0300  Fax 202-898-1164
agiesecke@americanbakers.org

Gerald Gipson
Research Physical Scientist
US EPA/NERL
MD-80
Research Triangle Park, NC 27711
919-541-4181  Fax 919-541-1379
ggb@hpcc.epa.gov

David Golden
Senior Staff Scientist
SRI International
333 Ravenswood Ave
Menlo Park, CA  94025
650-859-3811  Fax 650-859-6196
golden@sri.com

Jack Goldman
Attorney at Law
Bryan Cave LLP
700 13th St,NW, Suite 600
Washington, DC  20005
202-508-6000  Fax 202-508-6200
j4g@bryancavellp.com

Joyce Graf
Director, Environmental Science
CTFA
1101 17th  StNW
Washington, DC  20036
202-331-1770  Fax 202-331-1969
grafj@ctfa.org

David Graham
Business Manager
Occidental Chemical Corp
PO Box 809050
Dallas, TX 75380
972-404-4198  Fax 972-448-6676
dave_graham @oxy. com
Ross Gustafson
Technical Director
Florida Chemical Co
401 Somerset Dr
Golden, CO 80401
303-216-9420  Fax 303-216-9425
info@floridachemical.com

Jeremy Hales
Workshop Moderator
ENVAIR
60 Eagle Reach
Pasco, WA  99301
509-546-9542  Fax 509-546-9522
jake@odysseus.owt.com

Robert  Hamilton
Research Associate
Amvvay Corp
7575 E Fulton Rd
Ada, MI  49355
616-787-7697  Fax 616-787-7941
bhamilton@amway.com

Adel Hanna
Manager, Environmental Research
MCNC - Environmental Programs
PO Box 12889
Research Triangle Park, NC  27709
919-248-9230  Fax 919-248-9245
adel@mcnc.org

Alan Hansen
Manager, Tropospheric Studies
EPRI
POBox 10412
Palo Alto, CA 94303
650-855-2738  Fax 650-855-2950
ahansen@epri.com

Madelyn Harding
Admin, Product Compliance & Registration
The Sherwin-Williams Co
101 W Prospect Ave
Cleveland, OH 44115-1075
216-556-2630  Fax 216-263-8635
mkharding@shenvin.com
                                           A-7

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Kent Hoekman
Sr. Staff Scientist
Chevron Products Co
575 Market St
San Francisco, CA 94105
415-984-3060 Fax 415-894-2075
skho@chevron.com

Jeffrey Holm stead
Partner
Latham & Watkins
1001 Pennsylvania Ave,NW, Suite 1300
Washington, DC  20002
202-637-2287 Fax 202-637-2201
jeff.holmstead@lw.com

Harvey Jeffries
Professor
University of NC
CB #7400 Rm 120 Rosenan Hall
Chapel Hill, NC  27599
919-966-7312 Fax 919-933-2393
Harvey@unc.edu

William Johnson
Environmental Engineer
US EPA
MD-15
Research Triangle Park, NC  27711
919-541-5245 Fax 919-541-0824
johnson.williaml@epamail.epa.gov

Steve Jones
AQACS
SC Air Quality Management Division
21865 E Copley  Dr
Diamond Bar, CA 91765
909-396-2094 Fax 909-396-3867
sjones@aqmd.gov

Norman Kaplan
Sr. Project Engineer
US EPA
MD-4
Research Triangle Park, NC 27711
919-541-2556  Fax 919-541-0579
nkaplan@engineer.aeerl.epa.gov
Richard Karp
US EPA, Region VI
1445 Ross Ave, 12th Fl, Suite 1200
Dallas, TX 75202-2733
karp.richard@epamail.epa.gov

Terry Keating
Harvard University - BCSIA
79 JFK St
Cambridge, MA 02138
617-495-1417  Fax 617-495-8963
terry_keating@harvard.edu

Brian Keen
Senior Technology Manager
Union Carbide Corporation
PO Box 8361
South Charleston, WV 25303
304-747-4897  Fax 304-747-4623
keenbt@ucarb.com

Gail Kelly
Project Manager
ARCO Chemical Co
3801 W Chester Pike
Newtown Square, PA  19073
610-359-6443  Fax 610-359-3155
cnsgbk@arcochem .com

Dale Kemmerick
Manager of Data &  Modeling Unit
Georgia Environmental Protection Division
4244 International Pkwy, Suite 120
Atlanta, GA 30354
404-363-7092  Fax 404-363-7100
dale_kemmerick@mail.dnr.state.ga.us

Donna Kenski
Environmental  Scientist
US EPA
77 W Jackson Blvd
Chicago, IL 60604
312-886-7894  Fax 312-886-5824
kenski.donna@epamail.epa.gov
                                           A-8

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Marc Kessler
Post Doc
University of NC
CB# 7400
Chapel Hill, NC 27599
919-966-1372
marc_kessler@unc.edu

Tad Kleindienst
Principal Scientist
Mantech Environmental Technology, Inc.
PO Box 12313
Research Triangle Park, NC 27709
919-541-2308  Fax 919-549-4665
tkleindienst@man-env.com

Kenneth Knapp
Research Chemist
US EPA
MD-46
Research Triangle Park, NC 27711
919-541-1352  Fax 919-541-0960
knapp.ken@epamail.epa.gov

Robert Kozak
President
Atlantic Biomass Conversions, Inc.
1916-16thSt,NW
Washington, DC 20009
202-387-1838  Fax 202-483-6630
kzakr@aol.com

Michael Kravetz
Director Analytical Research
Cosmair Cosmetics Corp
159 Terminal Ave
Clark, NJ 07066
732-499-2934  Fax 732-499-2978

Shri Kulkarni
President & Principal Investigator
Kultech Incorporated
1323 Mellon Ct
Cary,NC  27511
919-467-0598  Fax 919-468-8805
kultecshri@aol.com
Naresh Kumar
Senior Air Quality Analyst
Sonoma Technology, Inc.
5510SkylaneBlvd, Suite 110
Santa Rosa, CA 95403
707-527-9372 Fax 707-527-9398
naresh@sonomatech.com

Jonathan Kurland
Research Scientist
Union Carbide Corp
PO Box 8361
S. Charleston, WV 25303-0361
304-747-3816 Fax 304-747-3752
kurlanjj@ucarb.com

William Kuykendal
Senior Environmental Engineer
US EPA/OAQPS
MD-14
Research Triangle Park, NC 27711
919-541-5372 Fax 919-541-0684
kuykendal.bill@epamail.epa.gov

Brian Lamb
Professor
Washington State University
Dept of Civil & Environmental Engineering
Pullman, WA 99164-2910
509-335-5702 Fax 509-335-7632
blamb@wsu.edu

John Langstaff
Senior Analyst
EC/R, Incorporated
1129 Weaver Dairy Rd
Chapel Hill, NC 27514
919-933-9501x239  Fax 919-933-6361
jlangstaff@mindspring.com

Sang-Mi Lee
Scientist
US EPA/AMD/NERL
MD-80
Research Triangle Park, NC 27711
919-541-2368  Fax 919-541-1379
smlee@hpcc.epa.gov
                                            A-9

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Wen Li
Project Scientist
ManTech Environmental Technology, Inc.
PO Box 12313
Research Triangle Park, NC  27709
919-541-2596 Fax 919-549-4665
wli@man-env.com

Xiaoyn Lin
Student
University of NC
Chapel Hill, NC 27514
919-966-3932
xiaoyu@ozone.sph.unc.edu

Deborah Luecken
Physical Scientist
US EPA
MD-84
Research Triangle Park, NC  27711
919-541-0244 Fax 919-541-4787
luecken@geoid.rtpnc.epa.gov

James Magee
Environmental Chemical Specialist - Advanced
LA Dept of Environmental Quality
PO Box 82135
Baton Rouge, LA  70809
504-765-0146 Fax 504-765-0921
jamesm@deq. state, la.us

Paul Makar
Atmospheric Environment Service
4905 Dufferin St
Downsview, Ontario  M3H 5T4  Canada
416-739-4692 Fax 416-739-4288
paul.makar@ec.gc.ca

Deborah Mangis
US EPA/NERL
MD-77B
Research Triangle Park, NC  27711
919-541-3086 Fax 919-541-7953
mangis.deborah@epamail.epa.gov
Mike Manning
Corporate Air Specialist
BASF Corporation
Sand Hill Rd
Enka, NC 28728
704-667-7481  Fax 704-667-7718
manninj@basf.com

Robert Matejka
Environmental Manager
AKZO Nobel Coatings, Inc.
1431 Progress Ave
High Point, NC 27261
336-801-0872  Fax 336-883-9525

Rohit Mathur
Research Scientist
MCNC - Environmental Programs
POBox 12889
Research Triangle Park, NC 27709
919-248-9246  Fax 919-248-9245
mathur@mcnc.org

Carolyn Matula
Manager, Solvents Regulatory Support
Shell Chemical Co
PO Box 4320
Houston, TX 77210
713-241-0579  Fax 713-241-3325
camatula@shellus.com

Gary McAlister
Chemist
US EPA/OAQPS
MD-19
Research Triangle Park, NC 27711
919-541-1062

Jim McCabe
Sr. Environmental Engineer
The Clorox Company
PO Box 493
Pleasanton, CA 94566
510-847-6674  Fax 510-847-2496
jim.mccabe@clorox.com
                                          A-10

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Lesa McDonald
Environmental Manager
Gemini Coatings, Inc.
PO Box 699
El Reno, OK 73036
405-262-5710  Fax 405-262-9310

Mack McFarland
Principal Scientist, Environmental Programs
DuPont Fluoroproducts
PO Box 80702
Wilmington. DE  19880
302-999-2505  Fax 302-999-2816
mack.mcfarland@usa.dupont.com

Jan Meyer
Senior Environmental Engineer
US EPA/OAQPS
MD-13
Research Triangle Park, NC 27711
919-541-5254  Fax 919-541-5689
meyer.jan@epa.gov

Ned Meyer
US EPA/OAQPS
MD-14
Research Triangle Park, NC 27711
919-541-5594  Fax 919-541-0044
Meyer.Ned@epa.gov

Jana Milford
Associate Professor
University of Colorado
Dept. of Mechanical Engineering, CB# 427
Boulder, CO 80309
303-492-5542  Fax 303-492-2863
milford@spot.colorado.edu

Bruce Moore
Environmental Engineer
US EPA/ESD
MD-15
Research Triangle Park, NC 27711
919-541-5460  Fax 919-541-5689
moore.bruce@epa.gov
David Morgott
Eastman Kodak Co
1100 Ridgeway Ave
Rochester, NY  14652-6272
716-588-3704  Fax 716-722-7561
dmorgott@kodak.com

Jim Neece
Urban Airshed Modeler
TX Natural Resource Conservation Commission
POBox 13087, MC-164
Austin, TX 78711
512-239-1524  Fax 512-239-1500
jneece@tnrcc.state.tx.us

Robert Nelson
Director, Environmental Affairs
National Paint & Coatings Association
1500 Rhode Island Ave, NW
Washington, DC 20005
202-462-6272  Fax 202-462-8549
bnelson@paint.org

Monica Nichols
Principal Environmental Engineer, Flexible
Packaging Division
Reynolds Metals Company
2101 ReymetRd
Richmond, VA 23237
804-743-6154  Fax 804-285-5222
msnichol@lanmail.rmc.com

Becky Norton
Ecologist II
AR Dept of Pollution Control & Ecology
8001 National Dr
Little Rock, AR 72219
501-682-0060  Fax 501-682-0753
nortonb@adeq. state, ar.us

Joan Novak
Chief, Modeling Systems Analysis Branch
US EPA/AMD/NERL
MD-80
Research Triangle Park, NC 27711
919-541-4545  Fax 919-541-1379
novak.joan@epamail.epa.gov
                                           A-ll

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Brenda Nuite
Senior Regulatory Advisor
The Dial Corporation
15101 N ScottsdaleRd
Scottsdale, AZ  85254
602-754-6151  Fax 602-754-6180
nuite@dialcorp.com

Anne O'Donnell
Manager, Analytical Development
Safety-Kleen Corp
PO Box 92050
Elk Grove Village, 1L 60009
773-825-7053  Fax 773-825-7850
aodonnell@safety-kleen.com

Jesse O'Neal
Environmental  Science & Policy, Inc.
208 Beckley Court
Raleigh, NC 27615
919-676-1713  Fax 919-676-9056
jesoneal@pipeline.com

Eduardo Olaguer
Environmental  Science Specialist
The Dow Chemical Co
1803 Bldg, The Dow Chemical Co
Midland, MI 48674
517-636-2927  Fax 517-638-9305
epolaguer@dow.com

Philip Ostrowski
Technical Service Manager
Occidental Chemical
PO Box 344
Niagara Falls, NY  14302
716-278-7346  Fax 716-278-7297
phil_ostrowski@oxy.com

Lawrence Otwell
Senior Environmental Engineer
Georgia-Pacific
POBox 105605
Atlanta, GA 30348
404-652-5081  Fax 404-654-4695
lpotwell@gapac.com
John Owens
Research Specialist
3M
3M Center, Bldg 236-3A-03
St. Paul, MN 55125
612-736-1309  Fax 612-733-4335
jgowens@mmm.com

Prasad Pai
Senior Scientist
AER
2682 Bishop Dr, Suite 120
San Ramon, CA 94583
5 ] 0-244-7123  Fax 510-244-7129
ppai@aer.com

Joe Paisie
US EPA/OAQPS
MD-15
Research Triangle Park, NC  27711
919-541-5556

Uay Palanski
Attorney
Wilmer, Cutler & Pickering
2445 M St, NW
Washington, DC  20037
202-663-6602  Fax 202-663-6363
ipalansky@wilmer.com

Randy Pasek
Manager, Atmospheric Processes Research Sect.
CA Air Resources Board
2020 L St
Sacramento, CA  95814
916-324-8496  Fax 916-322-4357
rpasek@arb.ca.gov

Ronald Patterson
Physical Science Administrator
US EPA/NERL
MD-77
Research Triangle Park, NC  27711
919-541-3779  Fax 919-541-0329
patterson.ronald@epamail.epa.gov
                                           A-12

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John Patton
Environmental Protection Specialist 6
TN Air Pollution Control
L&C Annex, 401 Church St, 9th Floor
Nashville, TN 37243-1531
615-532-0604  Fax 615-532-0614
jpatton@mail.state.tn.us

Richard Paul
Manager, Environmental Health
American Automobile Manufacturers Assoc.
7430 2nd Ave, Suite 300
Detroit, MI 48202
313-871-5344  Fax 313-872-5400

Dib Paul
Project Manager
IT Corporation
1104CastaliaDr
Cary,NC 27513
919-233-7024  Fax 919-233-7027
dibp@mindspring.com

Rick Phelps
Technical Associate
Eastman Chemical Co
POBox431,Bldg280W
Kingsport, TN 37662
423-229-5164  Fax 423-229-4864
rcphelps@eastman.com

Daniel Pourreau
Coatings  Development Manager
ARCO Chemical Co
3801 W Chester Pike
Newtown Square, PA  19073
610-359-6837  Fax 610-359-5753
cnsdbp@arcochem .com

Gene Praschan
Manager
American Automobile Manufacturers Assoc.
1000 Park Forty Plaza, Suite 300
Durham, NC 27713
919-547-7100  Fax 919-547-7102
praschea@ix.netcom .com
Harry Quarles
Research Scientist
Oak Ridge National Laboratory
PO Box 2008
Oak Ridge, TN  37831
423-241-2412 Fax 423-576-8543
hq3@ornl.gov

M. B. Ranade
President
Particle Technology Inc.
PO Box 925
Hanover, MD 21076
301-931-1037 Fax 301-931-1038
ranade@erols.com

S. T. Rao
Asst. Commissioner, Office of Science & Tech.
NYS Dept of Environmental Conservation
50 Wolf Rd, Room 198
Albany, NY  12233-3259
518-457-3200 Fax 518-485-8410
strao@dec.state.ny.us

Doug Raymond
Director, Regulatory Affairs
Diversified Brands
31500 Solon Rd
Solon, OH 44139
440-498-6049 Fax 440-519-663 8
djraymond@sherwin.com

Leslie Ritts
Attorney
Hogan & Hartson
555 Thirteenth St,NW
Washington, DC 20004
202-637-6573 Fax 202-637-5910
Isr@dc2.hhlaw.com

Can Roque
Materials Engineer
Naval Aviation Depot, Dept. of Navy
Code 4344
Jacksonville, FL 32212
904-542-4519x127  Fax 904-542-4523
roque.psd@navair.navy.mil
                                           A-13

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Alexander Ross
Government Affairs Director
Rad Tech International, NA
400 N Cherry St
Falls Church, VA 22046
703-534-9313  Fax 703-533-1910
rossradtec@aol .com

Ted Russell
Professor
Georgia Institute of Technology
Env. Engineering, 200 Bobby Dodd Way
Atlanta, GA 30332-0512
404-894-3079  Fax 404-894-8266
trussell@pollution.ce.gatech.edu

Ron Ryan
Environmental Engineer
US EPA/OAQPS/EMAD
MD-14
Research Triangle Park, NC 27711
919-541-4330  Fax 919-541-0684
ryan.ron@epa.gov

Chris Salmi
Manager
NJ Dept of Environmental Protection
Bureau of Air Quality Planning
PO Box 418,401 E State St, 7th Fl
Trenton, NJ 08625
609-292-6722  Fax 609-633-6198
salmi@dep.state.nj.us

David Sanders
Environmental Engineer
US EPA/OAQPS/AQSSD
MD-15
Research Triangle  Park, NC 27711
919-541-3356  Fax 919-541-0824
sanders.dave@epa.gov

Ken Schere
US EPA/ORD
MD-80
Research Triangle  Park, NC 27711
919-541-3795  Fax 919-541-1379
skl@hpcc.epa.gov
Mark Schmidt
Statistician
US EPA
MD-14
Research Triangle Park, NC 27711
919-541-2416  Fax 919-541-1903,
schmidt.mark@epa.gov

John Schwind
Senior EHS Manager
Safety-Kleen
2110SYaleSt
Santa Ana, CA 92869
714-751 -0106  Fax 800-769-5841

Mohamed Serageldin
US EPA/OAQPS
MD-13
Research Triangle Park, NC 27711
919-541-2379  Fax 919-541-5689
serageldin.mohamed@epamail.epa.gov

Ken Sexton
Research Associate
University ofNC
CB#7400 School of Public Health
Chapel Hill, NC 27599
919-966-5451  Fax 919-966-7911
ken_sexton@unc.edu

Sally Shaver
Director
US EPA/AQSSD
MD-15
Research Triangle Park, NC 27711
919-541-5505  Fax 919-541-0804
shaver.sally@epamail.epa.gov

John Sherwell
Manager, Atmospheric Science
MD Dept of Natural Resources
Power Plant Assessment Division
Tawes Bldg B-3, 580 Taylor Ave
Annapolis, MD 21401
410-260-8667  Fax 410-260-8670
jsherwell@dnr.state.md.us
                                           A-14

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David Smith
Principal Scientist
ManTech Environmental Technology, Inc.
POBox 12313
Research Triangle Park, NC 27709
919-406-2147
dsmith@man-env.com

Qingyuan Song
Postdoc
US EPA/UCAE/NOAA/AMD
MD-80
Research Triangle Park, NC 27711
919-541-1949  Fax 919-541-1379
qin@hpcc.epa.gov

Donald Spellman
Manager, Clean Air Alt Compliance
Louisville Gas & Electric
POBox 32010
Louisville, KY 40232
502-627-3425  Fax 502-627-2550
don.spellman@lgeenergy.com

Charlene Spells
Environmental  Engineer
US EPA/0 AQPS/1PSG
MD-15
Research Triangle Park, NC 27711
919-541-5255  Fax 919-541-5489
spells.charlene@epamail.epa.gov

Bob Stallings
Environmental  Engineer
US EPA
MD-15
Research Triangle Park, NC 27711
919-541 -7649  Fax 919-541 -0824
stallings.bob@epa.gov

William Stockwel!
Senior Scientist
Fraunhofer  Institute D-82467
Kreuzeckbahnstrabe 19
Garmisch-Partenkirchen, Germany D-62467
011-49-8821-183262  Fax 011-49-8821-73573
stockwel@ifu.fhg.de
David Stonefield
Senior Environmental Engineer
US EPA/OAQPS/OPSG
MD-15
Research Triangle Park, NC 27711
919-541-5350 Fax 919-541-0824
stonefield.dave@epa.gov

Ron Stout
Technical Representative
Eastman Chemical Co
123 Lincoln St
Kingsport, TN 37662
423-229-3373 Fax 423-224-0414
ronstout@eastman.com

Dave Stringham
Manager, Reg & State Govt. Affairs
Safety-Kleen Corp
One Brinckman Way
Elgin, IL  60123
847-697-2221 Fax 847-468-8535
dstringham@safety-kleen.com

Gregory Suber
Ph.D. Student
Duke University
PO Box 2773
Durham, NC 27715
919-613-8054
gfs2@acpub.duke.edu

George Talbert
Assistant Director for Technology Transfer
Gulf Coast Hazardous Substance Research Cntr
POBox 10613
Beaumont, TX  77710
409-880-2183 Fax 409-880-2397
gotalbert@aol.com

Roger Tanner
Principal Scientist
TV A/Environmental Research & Services
POBox 1010, CEB2A
Muscle Shoals, AL 35662-1010
256-386-2958  Fax 256-386-2499
rltanner@tva.gov
                                           A-15

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Philip Tham
Director, Regulatory Affairs
Estee Lauder Companies
125 Pinelawn Rd
Melville, NY  11747
516-531-1624  Fax 516-531-1565
ptham@estee.com

Stanley Tong
Environmental Protection Specialist
US EPA Region IX, Air Division
75 Hawthorne St, (AIR-4)
San Francisco, CA 94105
415-744-1191  Fax 415-744-1076
tong.stanley@epamail.epa.gov

Gail Tonnesen
Visiting Scientist
US EPA
MD-84
Research Triangle Park, NC 27711
919-541-4272  Fax 919-541-4272
tonnesen@olympus.epa.gov

James Vickery
Associate Lab Director for Air
US EPA/NERL
MD-75
Research Triangle Park, NC 27711
919-541-2184  Fax 919-541-3615
vickery.james@epamail.epa.gov

Darryl von Lehmden
Principal Environmental Engineer
Midwest Research Institute
5520 Dillard Rd
Cary,NC 27511
919-851-8181 x5167  Fax 919-851-3232
dvonlehmden@mriresearch.org

Fred Vukovich
Chief Scientist
Science Applications International Corp
615 OberlinRd, Suite 300
Raleigh, NC 27605
919-836-7563  Fax 919-832-7243
fVukovich@raleigh.saic.com
Kit Wagner
Principal Scientist
Atmospheric Information Systems
PO Box 721165
Norman, OK 73070
405-329-8707  Fax 405-329-8717
kit@ionet.net

Chris Walcek
Senior Research Associate
State University of NY at Albany
ASRC, 251 Fuller Rd
Albany, NY  12203
518-437-8720  Fax 518-437-8758
walcek@contrail.asrc.cestm.albany.edu

Zion Wang
University of NC
1152 College Ave
Palo Alto, CA  94306
650-424-8301  Fax 650-424-8301
zion_wang@unc.edu

Bob Wayland
Environmental  Scientist
US EPA/OAQPS/IPSG
MD-15
Research Triangle Park, NC 27711
919-541-1045  Fax 919-541-5489
wayland.robertj@epamail.epa.gov

Ray Wells
Research Chemist
US Air Force (AFRL/MLQR)
139 Barnes Dr
Tyndall AFB, FL 32403
850-283-6087  Fax 850-283-6090
ray.wells@ccmail.aleq.tyndall.af.mil

Robert Wendoll
Director of Environmental Affairs
Dunn-Edwards Corp.
4885 E 52nd Place
Los Angeles, CA 90040
213-771-3330  Fax 213-771-4440
                                           A-16

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Kurt Werner
Product Steward Specialist
3M
3M Center, Bldg 236-IB-10
St. Paul, MN 55144
612-733-8494  Fax 612-737-9909
kt\verner@mmm.com

Neil Wheeler
Chief of Environmental Applications
MCNC-NC Supercomputing Center
PO Box 12889
Research Triangle Park. NC  27709
919-248-1819  Fax 919-248-9245
Wheeler@ncsc.org

Gary Whitten
Chief Scientist
Systems Applications International, Inc.
101 Lucas Valley Rd
San Rafael, CA '94903
415-507-7152  Fax 415-507-7177
gzw@sai.icfkaiser.com

Carolyn Wills
Manager, Regulatory Affairs
Mary Kay, Inc.
1330 Regal Row
Dallas, TX 7524^
214-905-6360  Fax 214-905-6908

William Wilson
Physical Science Administrator
US EPA/NCEA
MD-52
Research Triangle Park, NC  27711
919-541-2551  Fax 919-541-5078
wilson.william@epa.gov

Ken Woodrow
Attorney
Baker & Hostetler LLP
1050 Connecticut Ave. Suite 1100
Washington, DC  20036
202-861-1739  Fax 202-861-1783
kwoodrow@baker-hostetler.com
Albert Yezrielev
Senior Staff Chemist
Exxon Chemicals
5200 Bayway Dr
Baytown. TX 77520
281 -834-2487   Fax 281 -834-2747

Rose Zaleski
Exxon Biomedical Sciences, Inc.
Mettlers Rd, CN 2350
East Millstone, NJ 08875-2350
732-873-6053   Fax 732-873-6009
rosemary.t.zaleski@erc.exxon.sprint.com

Guang Zeng
University of NC
Dept of ESE. CB# 7400, Prosenau Hall
Chapel Hill. NC 27599
919-966-3932
guang@ozone.sph.unc.edu

Elaine Zoeller
Technical Associate
Eastman Chemical Co
POBox431,B-280W
Kingsport, TN  37662
423^229-3983   Fax 423-229-4864
ezoeller@eastman.com

Bernard Z\sman
Technical Service Specialist
Occidental Chemical Corp
PO Box 344
Niagara Falls. NY 14302
716-278-7894  Fax 716-278-7297
bernie_z\ sman@oxy.com
                                           A-17

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       During the discussion period on the last day of the Photochemical Reactivity Workshop,
moderator Jake Hales explained the NARSTO organization and asked if there was interest in
forming a group under NARSTO to explore research needs concerning reactivity. There was
tentative interest among attendees. Interested persons were asked to remain in the room after
the Workshop itself was adjourned to discuss possible formation of such a group. At this time,
participants did not identify specific research tasks to sponsor. Here are the minutes of that
meeting.

                          Ad Hoc Task Force on VOC Reactivity
                                Minutes of Initial Meeting
                                      May 14,1998

       The meeting was called to  order at around 1:00 pm by Robert Wendoll, who stated that
the first order of business was to establish the initial steps for Task-Force action.

       John Dege noted that we need to establish EPA's position on this topic, and then we need
to formulate a concept paper to establish the basis for our downstream operations. It was
emphasized that we need to set forth a list of the relevant research needs. Cyril Durrenburger
suggested that we might want to develop one or more "issue papers" that define the primary
considerations at hand. He also suggested that we consider commissioning several "critical
review" papers, similar to those for the NARSTO Ozone Assessment, as a means of codifying
salient scientific aspects.  Gary Foley stated that we need to start thinking about focusing our
scientific efforts, e.g., chamber studies, modeling efforts ..., in order to maximize relevance to
the policy community; we need to reach closure on how to produce the most definitive
information.  He also recommended parallel, evolving, and communicative efforts between the
scientific and policy communities.

       There was a general discussion of how the science/policy interface should be handled.
This arose at several points during the ensuing conversation. In particular it was asked whether
NARSTO had any direct chain-of-command linkage to EPA's Office of Air and Radiation.  Jake
Hales said definitely no. Although OAQPS is a NARSTO signatory, NARSTO tries to be
scrupulous in observing the line between policy-making, and performing policy relevant
research.  In observing this  line, NARSTO - in Jake's estimation - has been less effective than
desirable to date in getting our research products conveyed to the policy community. Currently
NARSTO is designed to make this linkage through  a Liaison Team for Policy, a standing box on
the NARSTO organization  chart.  This has been relatively ineffective, however, and because of
this, NARSTO's Executive  Steering Committee feels that in the future such liaisons need to be
hard-wired into active, functioning groups. In view of this, Jake stressed the importance of
having OAQPS staff take a strong and active role directly in this Reactivity Task Force.

       Bob Avery stated that we need to plan a meeting to formulate a mission statement
Robert Wendoll agreed, saying that we need to establish a list of meaningful scientific objectives
to go along with such a statement.


                                           B-l

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       Howard Feldman stated that it is desirable to develop an assessment of the current state of
the science associated with the reactivity issue. Is the scientific underpinning sufficiently "ripe"
for policy application? If not, when will it be?

       It was asked if this Task Force is to be considered a science group, a funding group, or
both.  If it's a funding group, what are the money sources? Basil Dimitriades responded that we
need some time after this meeting to think this over; then we should reconvene to write a
research plan.

       Referring to the question of whether this effort should be incorporated as a part of
NARSTO, Ed Edwards recommend that everyone here review NARSTO's structure and
operational process.  Jake Hales commented that the best way to do this is to visit the NARSTO
Web site on «htpp://narsto.owt.com/Narsto/>.  Robert asked for a show of hands for those
favoring incorporation into NARSTO. The response was ambivalent, mainly because of
unfamiliarity of many of the attendees with NARSTO. There was a consensus that everyone
should visit the Web site in the near future.

       There were some questions regarding alternatives to NARSTO, such as a possible FACA
[Federal Advisory Committee Act] committee or a dedicated EPA-coordinated arrangement. Jim
Vickery responded that EPA definitely prefers the NARSTO route to a dedicated EPA option, for
several reasons. First, NARSTO  was established to promote public/private communications and
offers an established resource base for operations of this sort.  Secondly, EPA desires to operate
on a multiorganizational, pooled resource basis with operations of this type, in order to
encourage all interested parties to enter in the discussion process. FACA arrangements, on the
other hand, are more suitable to short-term issues such as evaluating proposed standards and
similar concerns.

       Robert Wendoll then asked for a list of action  items for this initial meeting. These items
and their resolutions appear below:

       1. Set date and place for our follow-on meeting. It was agreed that this meeting should
be during the first week in September at RTP, NC, at EPA's conference facilities. A pilot team
will convene by conference call in early June to draft a mission strategy and design this meeting.
This team will consist of Barbara Frances, Ed Edwards/Robert Wendoll, John Dege, John
Schwind, Cyril Durrenburger, Basil Dimitriades, and Ron Patterson (or Jake Hales).

       2. Draft a Mission Strategy. This will be performed by the pilot team, as noted above.

       3. Draft an agenda for the September meeting. Basil Dimitriades will do this.

       4. Determine methods for communication.  Jake Hales suggested that, for the time-being,
at least, the group use the NARSTO home page as a primary communication medium. He will
set up a reactivity sub-page there  for that purpose.  There was also some question of how we


                                         B-2

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communicate activities of this group to individuals not present at this meeting.  Jake suggested
that, as a first measure, we put an article describing our activities to-date in the NARSTO
newsletter, the 1998 summer/fall issue of which will go into press in early June. Robert Wendoll
agreed to write this article and send it to Jake for inclusion in this issue.

       The meeting concluded at 1:40 pm.
                                             B-3

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