&EPA
          United States
          Environmental Protection
          Agency
           Industrial Environmental Research  EPA-600/7-79-1 55
           Laboratory          July 1979
           Research Triangle Park NC 27711
Total  Particulate Mass
Emission Sampling Errors

Interagency
Energy/Environment
R&D Program Report

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                  RESEARCH REPORTING SERIES


Research reports of the Office of Research and Development, U.S. Environmental
Protection Agency, have been grouped into nine series. These nine broad cate-
gories were established to facilitate further development and application of en-
vironmental technology. Elimination of traditional  grouping  was consciously
planned to foster technology transfer and a maximum interface in related fields.
The nine series are:

    1. Environmental Health Effects Research

    2. Environmental Protection Technology

    3. Ecological Research

    4. Environmental Monitoring

    5. Socioeconomic Environmental Studies

    6. Scientific and Technical Assessment Reports (STAR)

    7. Interagency Energy-Environment Research and Development

    8. "Special" Reports

    9. Miscellaneous Reports

This report has been assigned to the INTERAGENCY ENERGY-ENVIRONMENT
RESEARCH AND DEVELOPMENT series. Reports in this series result from the
effort funded  under the  17-agency  Federal  Energy/Environment Research and
Development Program. These studies relate to EPA's mission to protect the public
health and welfare from adverse effects of pollutants associated with energy sys-
tems. The goal of the Program is to assure the rapid development of domestic
energy supplies in an environmentally-compatible manner by providing the nec-
essary environmental data and control technology Investigations include analy-
ses of the  transport of energy-related pollutants and their health and ecological
effects; assessments  of,  and development of, control technologies for energy
systems; and integrated assessments of a wide range of energy-related environ-
mental issues.



                        EPA REVIEW NOTICE
This report has been reviewed by the participating Federal Agencies, and approved
for  publication. Approval does not signify that the contents necessarily reflect
the views and policies of the Government, nor does mention of trade names or
commercial products constitute endorsement or recommendation for use.

This document is available to the public through the National Technical Informa-
tion Service, Springfield, Virginia 22161.

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                                        EPA-600/7-79-155

                                                  July 1979
Total  Participate  Mass  Emission
             Sampling  Errors
                         by

                      E. F. Brooks

                  TRW Systems and Energy
                     One Space Park
               Redondo Beach, California 90278
                  Contract No. 68-02-2165
                      Task No. 104
                 Program Element No. INE624
               EPA Project Officer: Robert M. Statnick

           Industrial Environmental Research Laboratory
             Office of Energy, Minerals, and Industry
               Research Triangle Park, NC 27711
                      Prepared for

           U.S. ENVIRONMENTAL PROTECTION AGENCY
              Office of Research and Development
                  Washington, DC 20460

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                                CONTENTS



                                                                    Page




Foreword                                                             iii



List of Tables                                                        iv



Sections



   1 .   Conclusions                                                     1



   2.   Recommendations                                                 2



   3.   Introduction                                                    3



   4.   Particulate Mass Transport                                      4



   5.   Error Analysis                                                  6



   6.   Evaluation of Error Sources                                     9



   7.   Summary and Discussion of Results                              15



References                                                            17



Glossary                                                              18



Appendices



   A.   Derivation of Mass Transport Equations                         20



   B.   Error Source Evaluation                                        24



   C.   Comments on Data and Error Analyses                            42
                                    ii

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                                FOREWORD

     This report is an analysis of sampling errors in the determination of
total participate mass emissions from stationary sources.   In particular
it examines the accuracy which is obtainable with EPA-IERL Level  1  assess-
ment procedures and hardware.  It was prepared under Task 26 of EPA Contract
68-02-2165, "Sampling and Analysis of 'Reduced1  and 'Oxidized1  Species in
Process Streams".
     This work was conducted under the direction of Dr.  R.  M.  Statnick,
Environmental Research Center, Research Triangle Park,  North Carolina.
The Fluid Physics Department and Applied Chemistry Department,  Applied
Technology Division, TRW Systems and Energy, Redondo Beach, California,
were responsible for the work performed on this  task.   Dr.  C.  A.  Flegal,
Applied Chemistry Department, was Program Manager, and  the Task Manager
was E.  F. Brooks.  The author wishes to thank Southern  Research Institute
for stratification background data and discussions on sampling  techniques.
                                   m

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                             List of Tables

                                                                     Page

1.   Values for Minor Error Sources                                   10

2.   Values for Velocity Measurement Parameter Errors                 11

3.   Values for Collected Particulate Mass Error                      13

4.   Values for Mapping Error                                         14

5.   Single Point and System Errors for Total Particulate Mass
     Sampling                                                         15
                                     iv

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                    1.  CONCLUSIONS

Level  1  total participate mass emission assessments:
•   A SASS train operated in accordance with "IERL-RTP Procedures
    Manual,  Level  1  Environmental  Assessment"  sampling at  a  single
    point will have  a sampling accuracy of a factor of ±2  or better
    in most locations such as stacks  or control  device inlets.
    Under worst case conditions,  such as at an ESP outlet,  it will
    have an accuracy of about a factor of ±3.
•   The degree of anisokinetic sampling induced by the SASS  train
    design and operation has a negligible effect on system accuracy.
•   In single point  sampling, the mapping error (non-representative-
    ness of the selected point) will be the largest individual error
    in the system.
•   Sampling accuracy using the SASS train could be improved to
    about ±25% by using a 16 point traverse rather than sampling
    at a single point.
General
•   For traverse sampling, the largest individual error will normal-
    ly be in collected particulate mass, due to anisokinetic sampling
    and flow/probe misalignment.
•   System accuracies of ±10% to ±16% can be achieved using com-
    mercially available equipment and a 16 point traverse.  These
    accuracy levels, while not required for environmental  assessment,
    indicate potential accuracies for control device evaluation
    testing.

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                   2.   RECOMMENDATIONS

 The  SASS train  in  its present state is recommended for Level 1
 assessment work, using single point sampling.  A modified traverse
 (along a single line) should be considered for places such as ESP
 outlets to minimize errors due to stratification.
 Additional stratification data should be obtained at sites such
 as full scale coal fired power plants for the three general  types
 of most important  locations:  control device inlets, control device
 outlets, and stacks.  Such data should be obtained with a single
 (or  identical) train(s) to isolate the stratification data.
 Development of methodology to optimize single point sampling
 accuracy through judicious selection of the sampling point should
 be pursued through analysis of stratification data and proof of
 principal  source testing for proposed techniques.
 There is a need for lightweight,  high volumetric flow sampling
 hardware and associated procedures to perform quick (1-2 hour)
 surveys to determine particulate stratification in sources so
 that appropriate techniques can be used for longer term source
 assessment testing.
Additional error analysis work should be performed for size
 fractionating sampling techniques.  The present analysis applies
 only to the total  particulate mass determination.
Although this report does not deal specifically with Method  5
 hardware and procedures,  results  suggest that for hardware of a
 given accuracy, there will exist specific procedures to optimize
 system performance (achieve close to maximum accuracy while
 minimizing manpower requirements  and sampling times).  Work
 should be continued to prepare an IERL-RTP Procedures Manual in
 this area.

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                            3.   INTRODUCTION
     The purpose of this report is to present a "first cut"  estimate of
sampling errors in the measurement of total  particulate mass emissions
from stationary sources.  In "IERL-RTP Procedures Manual:   Level  1
Environmental Assessment" (Reference 1),  the desire is expressed  to per-
form measurements which are accurate "to within a factor of ±2 to 3."
Measurement errors are divided into two general categories:   sampling
errors and analysis errors.  This report deals with evaluation of total
particulate mass sampling errors, within the framework of a  system error
analysis.  A mass transport expression is developed in terms of measured
parameters to serve as the basis for the analysis.   A standard explicit
error analysis is performed on the derived expression for mass transport.
Since there are also important non-explicit error sources, terms  are added
to the explicit equation to handle them.   The individual error terms are
then evaluated on the basis of previous analyses, available empirical data,
and, where no data are available, guesses.  The evaluation leads  to a
ranking of individual error sources and estimates of total system error.
     For   single point sampling, which is recommended in Level 1  work,
the analysis shows that accuracies within a factor  of two to three should
normally be achieved.  This conclusion is, however, tentative at  present
due to a shortage of quantitative data on particulate stratification.
Results of this study show that particulate stratification causes the
greatest individual error in the system.   For traverses using sixteen or
more sampling points, it can be said with reasonable certainty that the
system error should be less than ±25% when proper hardware and techniques
are used.  For traverses, the largest error will usually be due to velocity
measurement and collected mass uncertainties.
     Conclusions are that single point sampling will usually be acceptable
for a Level 1 assessment, but additional mapping error work is needed to
provide better justification.  In addition, methodology development should
be pursued to optimize single point sampling techniques — the present method
of sampling at a point of average velocity is a step in the right direction,
but further refinements are needed.

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                       4.  PARTICULATE MASS TRANSPORT
      For cases of current interest,  it  is  reasonable to describe the flow
 stream as consisting  primarily  of  a  gas, with small amounts of entrained
 solid and/or liquid aerosol.  The  mass  transport of the gas is given by
 (Reference 2):
                           ""G  =  //PG "G  '  " dA                        0)
                                A
 where
      trig = total  gaseous mass  flow  rate, g/s
      PQ = local  gas density,  g/cm3
      UG = local  gas velocity  vector, m/s
       n = unit  vector normal  to measurement plane, dimensionless
       A = area  of measurement plane, m2

 Aerosol  mass  transport can be handled in a number of ways.   The most exact
 would be to  consider the  particles individually, and use statistical methods
 dealing with  single particle  mass and velocity.   Since the  sampling hardware
 operates on  the  particle  as being entrained in a gas flow,  it is most appro-
 priate from an engineering standpoint to use an entrainment model.   This
 allows us  to  represent aerosol mass  transport in a manner analogous to
 gaseous  mass  transport:
                          "A" //cAa "G  • "dA
                                A
 where
      mA  =  total aerosol  (liquid and solid)  mass  flow rate,  g/s
      C.  =  local aerosol  concentration, g/cm3
       <*  =  correction factor to account for  local difference
           between mass mean aerosol velocity and gas velocity
           (i.e., particle slip velocity).

 Equation  (2)-can be considered an  exact representation  of aerosol mass
 transport  if the proper value of «  is selected for each application.
 For particles of diameter 10 microns or less,  we can expect 0.99 <  <* < l
 in most  streams.  The  correction factor « is more fully discussed in
Appendix B.

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     The transformation of equation (2) into measured engineering parameters
is performed in Appendix A.   This transformation is needed to perform a
meaningful error analysis.  We are presently concerned with two cases:
single point sampling and traverse sampling.  For these cases,  the engineer-
ing representations are:
                              mA          /2Ap R  ~
Single point:        m. = « A g- k cos e */	——                   (3)
                                  N  m.
                                     "A          /^prrrco
Traverse:        m^ = « k\/2lT^  >^ ^— cos 6 -t/— • _""• •             (4)
                                 n=l  9n           °°n  n

where
     k = calibration factor for S probe, dimensionless
     e = angle between local velocity vector and the vector
         normal to the measurement plane
    Ap = measured differential  pressure, torr
                                                2
     R = universal gas constant, 8314.32 —? ' ? 6|/
                                         mole s2  K
    T^ = local static temperature, °K
    p^ = local static pressure, torr
     M = local average molecular weight (of the gas), g/mole
    m,, = mass of collected aerosol, g
    V  = volume of withdrawn gas at stream temperature, pressure
     9   and gas composition, cm3
  ( )  = value of parameters at traverse point n
     N = total number of traverse points

These relations are in terms of parameters which are measured directly
with the sampling hardware or for which values are established through
prior calibration or assumption.  The forms of the relations, as is shown
in the next section, determine the relative contributions of the individual
parameters to total system error.

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                            5.  ERROR ANALYSIS
      The  function of this error analysis is to identify individual  sources
 which contribute to total system error, and to quantify their relative
 contributions  to that error.  The value of the analysis lies in two areas —
 the  estimate of total error reflects reliability of the data and can be used
 to accept or reject individual data points; the estimates of individual
 errors  identify leading error sources, thus indicating where resources
 should  be allocated to improve system accuracy.
      The  following error analysis is carried out under the assumption of a
 normal  distribution of random errors.  This assumption will be valid for
 most, but not  all, of the parameters involved.  Reference 3, "The Analysis
 of Physical Measurements" is a recommended text for appropriate background.
 The  logic of the analysis below is identical  to that of error analyses for
 total volumetric flow and gaseous emissions presented in detail  in  Reference
 2.   Consider the general relation (Reference 3);

                         G = f (Hr  H2, H3 — Hr)                    (5)
 where
      G  =  dependent variable (quantity to be calculated)
      H  =  independent variable (parameter to be measured)
      f  =  functional  relationship

 Define  the error in the measurement  of variable Hr as er-   The standard
 deviation of the measurement of Hr is then given  by
                                       N
                                        V
                              •    ».   •**                         w
where
    ar = standard  deviation of Hr
     N = number of measurements
By derivation,  the standard deviation of G is  then given as
                2    /af    \\/3f    v2          '-'    v2
               «< *•  -^ i __	 f^ i^i   -  r\

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For the present case,  it is  convenient  to  analyze  the  single  point  relation,
equation (3),  and then generalize  to  the traverse  case.
     Applying  equation (7) we obtain:
               2                    22
               m.    a    a.    a.     m.     V
              "A
                           2
                      1  / c
                           (/      ^    a       a-r
                          ^*-£*-
                          AP2    M2    p2      T2
Equation (8) is presented in a non-dimensional  form which  will  allow us  to
speak of dimension!ess errors rather than the actual  standard deviations,
which are usually dimensional (e.g., we can  consider a  temperature  error
OT /T^ in percent rather than a-r in °K).
  00  °°                          <»
     The individual  error terms in equation  (8)  correspond to errors which
will occur at each point in the stream where a  sample is obtained.   They
are explicit errors  in that they are due to  identifiable performance
aspects of the sampling hardware itself.   In addition to these  error sources
there will also be non-explicit errors due to limitations  of the methodology
employed.  Whenever  possible, it is desirable to separate  hardware  errors
from methodology errors so that appropriate  hardware and technique  can be
selected separately  to achieve optimum accuracy in any given sampling
situation.  To accomplish this in the present analysis, we will  consider
the hardware related  errors in equation (8) as those which occur at a
given  point in the  stream.  Methodology error terms, introduced below,
basically deal with  distinctions between the sample obtained at a single
point or points and  the true total particulate mass emission rate.   By
definition, then, let a-  in equation (8) be the sampling  uncertainty
occurring at a point in the stream.
                                       x 100%                         (9)
                          °SPE -

where
     °SPE =  P°int error,  percent
                                    7

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 We can then define a system error as

                       °SE = °SPE + °ME + °TE + °AE
 where
      a^c = total  system uncertainty, percent
      OJ,.E = mapping uncertainty,  percent
      a,-r = temporal  uncertainty, percent
      o.r = assumption uncertainty,  percent

Significance of the  individual  terms is as follows:
     °SPE ~~ as exPlained above>  tni's  represents  the system's capability
            to extract a representative sample  at any one point  in  the
            stream, and is  determined by the accuracy of the hardware.
     OME  — the mapping uncertainty  is  associated with stratification in
            the sample plane.   If all  other errors  are zero, o.,E is a
            measure of how  accurately the  sample point or points represent
            the total  aerosol  emission.
     o,.,:  — temporal  uncertainty  is that due to changes in stream condi-
            tions during  the sampling  period, and applies to traverses.
     aAE  — the assumption  error  accounts  for inaccuracies in the math-
            ematical model  used in a  given  situation.  For example, if
            the temperature is assumed  constant during a traverse when
            in  fact it varies  by  a few  percent  in the sample plane, the
            resulting  error will  show up in  a^ by definition.
     aSE — this represents the total system error, and is the final
            desired quantity.

Equations  (8),  (9), and  (10)  specifically  identify thirteen separate error
sources which  occur during total particulate mass emission sampling.  Of
the  thirteen,  ten are hardware related, and three are methodology related.
In the following section,  the individual  terms are quantitatively evaluated
and  the  leading sources  of error are specifically  identified.

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                     6.  EVALUATION OF ERROR SOURCES
     This section deals with quantitative evaluation of the thirteen error
terms identified in Section 5,  with the objective of producing realistic
estimates of total system error.   Emphasis is  placed on a summary of evalu-
ations and comments on leading  error sources.   A more detailed evaluation
of individual terms is presented  in Appendix B.   Two points should be kept
in mind when considering the data presented below:   (1) The errors, presented
in terms of standard deviations,  are random errors,  rather than systematic
errors due to causes such as instrument calibration  shifts or mistakes due
to operator error.  (2) For normally distributed errors, the standard 95%
engineering confidence interval is represented by a  ± 2o interval.  Most,
but not all, of the errors can  be reasonably represented by a normal dis-
tribution.  For non-normally distributed errors, emphasis is placed on the
"95% confidence" aspects rather than on trying to determine the appropriate
type of distribution.
     Of the thirteen error sources, seven are generally rather small and
well understood.  These are treated briefly as a group.  Following that is
commentary on the three terms related to velocity measurement, which are
well understood but are not always small.  The section concludes with indi-
vidual discussion of the temporal error, collected particulate mass error,
and mapping error.
6.1  Generally Small, Well Understood Error Sources
     Errors  in static pressure and temperature, duct cross-sectional area,
and average molecular weight of the gas are usually small because the
parameters are not difficult to measure in most applications.  When sig-
nificant  errors do  occur, they are usually systematic  in nature and are
due to such  things as improper calibration practices,  unaccounted for wall
deposits  which reduce the  flow area, and other procedural errors.  The
error due to particle slip velocity is typically small due  to  the particle
size distribution and density encountered  in most process streams.  The
slip velocity, represented by «,  is treated further  in Appendix  B.  The
other terms mentioned above are discussed  at length  in  Reference  2.

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      The assumption error will  be small  as  long as  adequate attention  is
 paid to sampling details.  This means  that  each of  the  parameters  in
 equation (3) should be measured at each  sampling point.   The  form  of
 equation (3) is sufficiently exact and inclusive that assumption errors
 will be relatively small.  Assumption  errors  are also treated at greater
 length in Reference 2.
      The error in the volume of withdrawn gas will  be small when adequately
 calibrated equipment is used and it is acknowledged that  V  is based upon
 stack temperature,  pressure,  and composition, which usually means  that the
 instrument reading  (e.g.,  from  a dry test meter)  must be  properly  corrected
 for  temperature and pressure, and condensible and volatile stream  components
 must be accounted for.
      Achievable errors  for  the  above parameters  are presented below in
 Table 1.   The  listed accuracies  are not difficult to obtain with generally
 available equipment as  long  as  adequate care  is  taken to avoid systematic
 errors.
                 Table 1.  Values  for Minor  Error  Sources
Parameter
M
Poo
T
A
oc
V9
Assumption
Error
2a (95% Confidence Interval)
Error, Percent
±2
±2
±2
±2
±2
±2
±2
6.2  Velocity Measurement Parameter Errors
     These are errors associated with the parameters k,  9,  and Ap.   They
are discussed at considerable length in References 2 and 4.  Errors  for
various types of hardware and flow conditions are given  in  Appendix  B,
and summarized in Table 2.
                                   10

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                Table 2.   Values  for Velocity Measurement
                          Parameter Errors
     Parameter
Related Component
          Error
                      Pi tot-static  probe
                      S-type probe
                            x 100% = ±0.5%
                            x 100% = ±156
 a.  near flow
     disturbance
 b.  far from flow
     disturbance
Pitot-static
                      S-type
Pitot-static
                      S-type
2(tan e) a0 x 100% = ±1.3%
          y
2(tan e) a. x 100% = ±8%
          t>
2(tan e) aQ x 100% = ±0.5%

2(tan e) CTQ x 100% = ±2%
        AP
U-tube manometer
                      SASS train1
                      Baratron
2aAp = ±0.065 Torr
                            x 100% = ±14%
                                              Ap
                              100% = ±0.16%3
IAP read on 0-.5 or 0-4 in ^0 Magnehelic gage
2nominal velocity range 6-40 m/s
3nominal velocity range 1.7-55 m/s

The SASS train, selected for Level 1  assessments,  employs an S-type pi tot
probe and two Magnehelic differential pressure gages.   These components
comprise a low cost, reasonable accuracy system.   The  high accuracy
Baratron/pitot-static probe combination has been  used  in the field by TRW
without handling problems (Reference 4), and is recommended, especially
for very low flow velocities (< 5 m/s), in situations  where accuracy takes
precedence over hardware cost.
                                   11

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6.3  Temporal Variation  Errors
     The temporal error, OT^, is difficult if not impossible to evaluate
when significant changes occur during the period of traverse.  The best
way to handle the problem is the standard approach of being sure that
plant operating conditions are held constant during the sampling period,
and discarding the data  if they are not.  Concurrently, it is also
desirable to minimize the sampling time by maximizing the sample flow
rate, as is done with the SASS train.  The constant attention of the
sampling team is required during the sampling period to detect variations
in flow or other critical parameters.  The estimated value for 2aTE in
sources such as power plants is ±4%.
6.4  Collected Particulate Mass Errors
     The term am. gives the accuracy with which the sampling probe obtains
an aerosol  sample representative of the point at which the probe is placed.
The major error contributions result from anisokinetic sampling and from
sample loss or gain within the collection system.  Anisokinetic errors,  due
to improper sampling rate and/or probe misalignment, are treated at length
in Appendix B.  Sample gain or loss is usually due to improper hardware
design or procedures.  The appropriateness of condensing some types of
vapors and considering  the result as particulate is a philosophical
battleground which will  not be trod upon here.   A 2o error of ±4% in  col-
lected mass due to aerosol  gain or loss is considered reasonable for  a
sampling system such as  the SASS train.
     Isokinetic sampling is achieved for different gas velocities  through
variation of the sampling rate,  the nozzle orifice diameter,  or both.
Size fractionating devices like the SASS train require a constant,  fixed
flow rate so that adjustments to approximate isokinecity must be done  by
varying the nozzle I.D.   Nozzle diameters are typically available in  .32 cm
(.125 in.)  intervals, which allows maximum deviation from isokinetic  sam-
pling to be calculated,  as is done in Appendix B.
     The magnitude of achievable isokinetic sampling errors depends on the
type of hardware used (e.g., fixed or variable sample rate),  component
                                   12

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accuracy, and stream conditions (particle size distribution  and  local  flow
direction).  Collected mass errors,  as  determined in  Appendix B,  are sum-
marized below in Table 3 for several  general  cases.

         Table 3.   Values  for  Collected  Particulate Mass  Error
    Sampling Location
                                                       m.
                                Collected Mass  Error, 2—- x  100%
                             SASS  Train
               Maximum Accuracy Train*
  Control  device inlet

  Control  device outlet

  In stack, z 8 diameters
  above breeching
±20%
±16%
±10%
±8%
±6%
Hypothetical  train using best readily  available  hardware components.

6.5  Mapping Errors

     In the case of   single point sampling, which is the method recom-
mended for Level 1 assessments, the mapping error will  usually be the
largest single error in the system.   Consequently,  the  mapping error
deserves considerable attention.   The major problem encountered so far
has been a shortage of particulate stratification data, which is essen-
tial in evaluation of mapping techniques.   The bulk of  the  data examined
to date has been comparisons of single  point impactor measurements and
Method 5 type traverses.  Due to significant differences between the
types of sampling trains, it is difficult to isolate the differences in
output which are due solely to stratification.  Data examined and discus-
sion thereof are presented in Appendices B and C, respectively.  Mapping
error estimates for single point sampling and 16 point  traverses are
presented in Table 4 for various types  of conditions.
                                   13

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                   Table 4.  Values for Mapping Error
Sampling Location
Control device inlet
Control device outlet
In stack, *8 diameters
above breeching
Mapping Error, 2oME
Single Point
+60%, -40%
+150%, -60%
+50%, -33%
16 Point Traverse
±8%
±12%
±5%
As Table 4 shows, maximum mapping errors tend to occur  at  a  control device
outlet, especially for electrostatic precipitators,  meaning  that  stratifi-
cation is increased by the control device.   Just as  it  is  a  general rule
for velocity measurement to avoid working immediately downstream  of a  large
flow disturbance, it is wise in particulate sampling to avoid  sampling
immediately downstream of a stratification  source.   When sampling is done
near such a source, such as an ESP outlet,  knowledge of the  ductwork and
characteristics of the source can be used to select  a single sampling
point which would be more representative than a  randomly selected point.
                                   14

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                 7.   SUMMARY AND DISCUSSION  OF  RESULTS
     Error values in Tables  1-4 were  substituted  into equations 8-10  to
obtain single point  and system errors,  which are  shown  in  Table 5.  The
 point error, OSPE;» is indicative of. hardware accuracy,    while the
system error, ar, indicates the combined  hardware  and  procedure  accuracy.
           Table 5.   Single Point and  System  Errors  for  Total
                     Parti culate Mass  Sampling

Sampling
Train


.^•— • "~
SASS





Maximum
Accuracy





Sampling
Location


Control device
inlet
Control device
outlet
Stack, * 8 dia.
above breeching
Control device
inlet

Control device
outlet
Stack, > 8 dia.
above breeching
Error



20SPE
*Jl L.
±23%

±20%

±13%

±9%

±9%
±7%


2°SE


Single Point
+64%, -46%

+150%, -64%

+52%, -36%

+60%, -42%

+150%, -60%
+50%, -34%


16 Point
±24%

±24%

±15%

±13%

±16%
±10%

Largest Error
Source



Single
Point
aMF
ric.
a

Oijr-
ME
aME

aME
OK • ^
ME


16
Point

mft
a
mA
a
mA
CTME,
a
mA
aME
a
mA
Hypothetical train using best readily available hardware components.

The  "Maximum Accuracy" train in Table 5 is a train which would consist of
the  highest accuracy components readily available commercially.  For example,
it would  include a high accuracy differential pressure transducer.  The
purpose  in showing the "Maximum Accuracy" train error estimates is only to
illustrate the  best state of the art capabilities.
                                   15

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      A  comparison  of  relative accuracies of  hardware and procedures is
 given by  aspE  and  o^.   For  single  point sampling, OSE is invariably large
 compared  with  aspE, due  to the  single  point  mapping error.  Thus hardware
 improvements in  the SASS train  would not improve the system accuracy when
 single  point sampling  is used.  For traverses, the situation is different.
 The  SASS  train system  accuracy  is limited by the hardware rather than by
 procedure, while for  the Maximum Accuracy train, the respective hardware
 and  procedure  errors are about  equal.
      There has been a  twofold reason for performing the above analyses.
 The  first has  been to  determine whether hardware and procedures recommended
 for  Level 1 assessments  are adequate to produce the desired "factor of
± 2  to  3" accuracy.  The second has been to determine optimum accuracy
 capabilities and to show where  future efforts should be devoted to optimize
 system  accuracy.   Results of the analyses show that a Level  1  assessment
 should  have a  sampling accuracy of better than a factor of i 2 except at
 a control device outlet, where  the accuracy  is more likely to be a
factor  of 3,  especially  if the control  device is an ESP.   It is likely
 true  that the  error at a control device outlet can be reduced by making
 use  of  known device characteristics in selecting a sample point.  This
type  of methodology should be pursued.   For very high accuracy work,
Table 5 indicates that there is a good match between the accuracies of
currently available hardware and traverse sampling procedures.   Future
work  in this area would  involve integration of high accuracy components
 into a  viable  system for efficient traverse sampling.
      In conclusion on the matter of Level  1  assessments,  it is  recommended
that  sampling after a control device be done in a stack whenever feasible-
rather  than directly at  the control  device outlet.   This  will  be the best
way to  optimize accuracy.  In addition, development of methodology for
single  point sampling and/or modified traverse sampling (along  a single
line  to minimize  moving of equipment) directly at a control  device outlet
should be pursued to minimize the error due to particulate stratification.
                                  16

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                               REFERENCES
1.  "IERL-RTP Procedures Manual:   Level  1  Environmental  Assessment,"
    EPA-600/2-76-160a,  Hamersma,  Reynolds,  and Maddalone,  June 1976.

2.  "Flow and Gas Sampling Manual," EPA-600/2-76-203,  Brooks and Williams,
    July 1976.

3.  The Analysis of Physical  Measurements,  E.  Pugh and G.  Winslow;
    Addison-Wesley, 1966.

4.  "Continuous Measurement of Total  Gas Flowrate from Stationary Sources,"
    EPA-650/2-75-020, Brooks, et al.,  February 1975.


    (See Appendices for additional  references.)
                                   17

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                                 GLOSSARY

SYMBOL                                     USAGE
    A           flow cross-sectional area, m2
   C.           true aerosol concentration in the stream ahead of the
                probe,  g/cm3
   C            aerosol  concentration inside probe entry,  g/cm3
   D            particle diameter,  cm
   D            sample  probe orifice diameter,  cm
    f           empirical  functional relationship;  functional  relationship
    G           dependent  variable  (quantity to be calculated)
    H           independent variable (parameter to be measured)
    k           pi tot probe calibration factor, dimensionless
   mA           mass  of  collected aerosol,  g
   m            total aerosol  (liquid and solid)  mass flow rate,  g/s
   ITU           total gaseous  mass  flow rate, g/s
   M           local gas  average molecular weight,  g/mole
    n           unit  vector normal  to measurement plane, dimensionless
    N           number of  measurements;  total number of  sampling  points
   D            local static pressure,  torr
   roo
   p             local stagnation pressure,  torr
   Ap           P   ~  POO  '  tfie  Pressure differential  between  the local
                stagnation and static pressures,  torr
                                                      g-m2
               universal gas constant, 8314.32
                                  mole S2 °K
                              }K
local  gas velocity vector, m/s
               local gas static temperature, °K
  UG           true gas velocity ahead of the probe, cm/s
  U            mean velocity at probe inlet, cm/s
                                   18

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SYMBOL                                     USAGE

   V            volume of withdrawn gas  at stream temperature,  pressure,
    9           and gas composition,  cm3

 ( )            value of parameter at sample point n

                correction factor to  account for  local  difference  between
                mass mean aerosol velocity and  gas veloctity (i.e.,
                particle slip velocity).

                Dn Pn ur
                 P  P  »
    3           -^~j;—
                lop u

    e           angle between local velocity vector and duct axis
    y           gas viscosity,  poise

   PG           gas density,  g/cm3

   p            particle density, g/cm3

  a.r           assumption uncertainty,  percent

  aME           mapping uncertainty,  percent

  OSE           total system uncertainty, percent

   a            standard deviation of H

                point error,  percent

  Oyr           temporal uncertainty, percent
                                    19

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           APPENDIX A.   DERIVATION  OF  MASS  TRANSPORT  EQUATIONS

      This  appendix deals  with  the  transformation of  t!)e participate conser-
 vation  of  mass  equation (equation  (2)  in Section 4)  into the engineering
 representations shown  in  equations  (3) and  (4) in Section 4.  The conser-
 vation  of  mass  equation is:

                          "•A  =  J[/CA «  "G '  " dA                     (A-D
                               M
 where
      m   =  total  aerosol  (liquid and solid) mass flow rate, g/s
      C.  =  local  aerosol concentration, g/cm3
      «  =  Correction factor  to account for  local difference
           between mass  mean  aerosol velocity and gas velocity
           (i.e., particle slip velocity).
      A  =  flow  cross-sectional area, m2

 Equation (A-l)  is a convection model which states that the local aerosol
 concentration is convected downstream with the gas at a speed equal
 to the gas velocity component in the axial  flow direction multiplied by
a correction factor <* which  accounts for inertial and gravitational  forces
on the particles.  As the particle mass to cross-sectional  area  ratio
 becomes  small, « goes to unity, which represents complete entrainment.
As that ratio becomes large, <* goes to zero, representing non entrainment.
For most processes of interest, <* will be very close to unity, and is  not
measured in practice.
     For purposes of the error analysis,  we need to take equation (A-l)
and put  it in terms of actual engineering parameters.  In most cases,  it
is not practical to take the entire gas stream and process  it to determine
the particulate content.  Standard techniques involve obtaining  samples
from one or more discrete points in the stream.   For these  two cases,
single point and traverse sampling, equation (A-l)  becomes
                                  20

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             Single point:   m^ % CA «  UG  •  n  A                       (A-2)
                                  N  ,             A
             Traverse:       rhA £ V* (CA  <*n  UG   •  njAAn             (A-3)
                                 n=l

where
     N = total number of sampling points
  ( )  = value of parameter at sample point n.

For a typical sampling train,  the aerosol  concentration is measured as

                               CA = r-                              (A-4)
                                     g
where
    m. = mass of collected aerosol, g
    V  = volume of withdrawn gas at stream temperature, pressure,
     9   and gas composition,  cm3

The aerosol mass mA is determined by weighing the collected samples, and
the gas volume is measured with a dry gas meter or similar device, with
correction being made for moisture removed ahead of the meter.
     The flow cross-sectional  area, A, is usually determined from blue-
prints, especially in the case of rectangular ducts.  For traverses, all
common techniques divide the area up into segments of equal size, so that

                               AAn = ff                              (A"5)

The axial component of the gas velocity is usually measured by means of
a pitot probe and differential pressure device for the primary measurement.
The transformation is as follows:

                          uG-n =  |UG| cos e                         (A-6)
where
     e = angle between local velocity vector and duct axis
                                   21

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 For notational  simplicity,  define

                                 UG  E   "G                              (A-7)

      We  will  normally  be  dealing with  incompressible gas flows, so that
                                           2Ap
                                 ur =  k
                                  6      - >G
where
     Ap  =  pQ - p^  ,  the pressure  differential between the local stagnation
           and static pressures, torr
     PG  =  gas density, g/cm3
      k  =  pi tot probe calibration factor
Substituting the equation of state,
                                     P
                                      .
                                     fT
where
     p^ = local static pressure, torr
     R  = universal gas constant, 8314.32
                                           mole S2 °K
     M  = local gas average molecular weight,  g/mole
     T^ = local gas static temperature, °K
for P£, we obtain
                                                V2Ap R T
                                                -^
              UG "n = UG COS 9 =
                                                 p  M
                                                 roo
Substituting into equations (A-2) and (A-3),  we obtain
     Single point:
                                           R T
                                              00
                     A  \rk cos  e
                                                                    (A-9)
                                   22

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     Traverse:
                                 n=l    n         I   °°n  n
     The conservation of mass equation is  now presented  in  terms  of normal
engineering parameters.   Of the terms in equations  (A-ll) and (A-12),  the
following are usually measured directly with sample train components and
support equipment:  mA> V ,  Ap, T^.   The area A is either measured or
determined from blueprints.  The static pressure p^ is  often determined
by adding (or subtracting,  as required) the differential pressure between
the stream pressure and ambient pressure to barometric   pressure, which is
usually available.   The average molecular weight, fT, is  either measured or
estimated from plant operating conditions.  The pitot probe calibration
constant should be determined by pre- and post-test calibration.   The slip
velocity factor «  is usually ignored (therefore considered to be unity).
Flow  angularity is also typically ignored, meaning cos  8=1, but it is
possible to use a velocity probe which automatically compensates  for
angularities up to 30°,  as is discussed in Appendix B.   Equations (A-ll)
and (A-12), which appear as equations (3) and (4) in Section 4, serve as
the basis for the error analysis in Section 5.
                                    23

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                  APPENDIX  B.   ERROR  SOURCE  EVALUATION

      The  purpose  of this  appendix  is  to  provide  background  to support the
 summaries of evaluations  presented in Section  6.   Emphasis  here will be
 placed  on understanding the physics of some  of the  key parameters, and on
 presentation of empirical data,  in particular  for  stratification.  Emphasis
 is  placed on three  areas:   velocity measurement, collected  particulate
 mass, and stratification.
 1.    Particle Slip  Velocity Factor
      Of the  "generally small, well understood  error sources", only
 the slip  velocity factor a  warrants additional treatment here.
 Particle  velocities will differ  from the gas velocity due to gravity
 forces  and inertial forces,  the  latter arising when there is a change
 in flow direction.  The magnitude  of the particle/gas velocity differen-
 tial  is most  easily illustrated  for the case of a flow going directly
 up a  vertical  stack.  In this situation, gravity produces a downward
 force which makes the particle velocity less than the gas velocity.
 The result is a local Stokes flow  condition in which the differential
 velocity  is identified as the settling velocity of the particles.
 Settling  velocity is plotted in  Figure B-l  as a function of particle
 size  (spherical particles)  for two different values of particle density
and gas viscosity.  The slip velocity factor would then be calculated
 from the  particle settling  (terminal)  velocity and the gas velocity.
As Figure B-l shows, the settling  velocity will be at most a few
centimeters/second for particles smaller than 10 microns.  A vertical
flow represents the worst case in  terms of gravitational  effects.
 Inertial  effects can usually be  ignored due to the velocities involved.
 It typically takes a special effort, as in the case of cyclones  and
impactors, to produce the high velocities and sharp turning angles
required  to make inertial  effects  important.
                                    24

-------
              60  r-
ro
tn
               50
               40
               30
a.
oo
cu
              10
                              IN A STACK,  WE HAVE
                      CURVE
 1

8.0
                                         -4
                       j  , poise    1.7x10
                                             10          20          40        70
                                                    PARTICLE DIAMETER, MICRONS
                                                                           100
                                                                                                MOST  PROCESS  STREAM
                                                                                                CONDITIONS FALL
                                                                                                IN THIS REGION
                                                           200
                             Figure  B-l.   Settling speed of spherical  particles in a combustion
                                          stream as a  function of particle size

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2.   Gas Velocity Measurement
     Present concern is limited to measurement techniques involving a
pitot probe and differential pressure measurement device.  The most
common types of pitot probes are the S-type probe typically used in
field testing, and the pi tot-static probe, which has tended to acquire
a reputation of being acceptable for use only in the laboratory.  The
2a calibration factor accuracies of +_ .5% and + 1% for the pitot-static
probe and S probe,  respectively, shown in Table 2 in the main text were
obtained from References B-l and B-2.  Angularity sensitivity data in
Table 2 were obtained from the same sources.  The data are shown in
Table B-l below.
                Table B-l.   Errors due to Flow Angularity for
                            S-Type and Pi tot-Static Probes

Flow Angularity
yaw, degrees
± 5
±10
±20
±30
pitch, degrees
+ 5
+10
+20
+30
- 5
-10
-20
-30
2a Velocity Error, 2 (tan e) a0xlOO%
t)
"S" Pitot Probe

+1.6
+3.5
+4.5
+7.5

+1.5
+2.0
+3.5
+4.5
-1.5
-2.5
-5.0
-8.0
Pitot Static Probe

+0.3
+1.0
+1.3
+0.2

+0.3
+ 1.0
+1.3
+0.2
+0.3
+1.0
+1.3
+0.2
                                    26

-------
     For the "near flow  disturbance"  case  in  Table  2,  a  flow  angu-
larity range of ±30° was assumed,  while  the range  was  selected to  be
±5° for the "far from flow disturbance"  case.   As  the  data  show, the
pitot static probe has the more desirable characteristics.
     Accuracy of differential  pressure measurement devices  is  presented
in Figure B-2.  The zig-zag in the SASS  train  curve  corresponds to a
switch from the low range to the high  range Magnehelic gage.   Summary
data in Table 2 were taken from this plot.
3.   Collected Particulate Mass
     The Level 1 particulate collection  procedure  has  been  questioned
(Reference B-3) for single point sampling and  for  not  sampling in  a
strictly isokinetic manner.  The isokinetic problem  is addressed here,
while single point sampling (mapping)  errors are discussed  in  the  fol-
lowing section.
      The  term  am   gives  the accuracy with which the sampling  probe
obtains an  aerosol  sample  representative of the point at which the
probe  is  placed.   The major contributions to error come from anisoki-
netic  sampling and  from  sample  loss or gain within the probe.   Loss
of  sample could occur due  to  poor system design or procedural  errors,
while  sample  gain  is due  to vapor condensation, which would also  be
hardware  and/or procedure  related.  Sample alteration should not  be a
major  problem in a  properly designed and operated system.
      Isokinetic sampling  errors will occur in even the most careful
work  due  to equipment random  errors and stream conditions.  Some
general comments about  the concept  of isokinetic  sampling are in
order  here.   Textbook explanations  of isokinetic  sampling show
smooth  streamlines  in the  flow  around the sample  probe inlet,  with
streamline  deviations illustrating  anisokinetic conditions.   In
reality,  such  a situation  exists only in steady laminar flows, as
can be  produced in  a  good  wind  tunnel.  Laminar flows will not^ be
encountered in the field.   In  steady, laminar  flows,  streamlines  are
                                     27

-------
       1.5
   100
APPROXIMATE VELOCITY, M/S
5                    15
                       r~
                                                   45
                                    U-TUBE
                                   MANOMETER
    10
o
cc.
oo
3
GO
CO
    .1
           SASS
           TRAIN
                ARATRON 145
             (MKS INSTRUMENTS)
   .01
                     1
      .01
        Figure B-2.
      .1                     1
    DIFFERENTIAL PRESSURE, TORR

Differential pressure measurement
accuracy of various devices

              28
                                           10

-------
steady state entities,  which makes flow visualization techniques such
as smoke filaments in air flow or dye filaments in liquid flow viable.
In a turbulent stream,  streamlines exist instantaneously only-- the
streamline pattern varies greatly from millisecond to millisecond.
These changes are typically not small.  In a fully developed turbulent
pipe flow, the turbulence is structured such that turbulent eddies
tend to move downstream as units (Reference B-4).  Experimental studies
have shown that the size of these turbulent eddies is about 7% of the
pipe diameter (Reference B-5).  In a fully developed turbulent pipe
flow, the velocity component parallel to the sample probe axis can  be
expected to fluctuate over about a ±10% (of axial flow velocity) range,
with similar fluctuations in the angle of the velocity vector at the
probe tip (Reference B-6).  For operation near an elbow or other large
disturbance, these fluctuations will be even worse due to the larger
local scale of turbulence caused by flow detachment.
     What this all means is that in real life, isokinetic sampling is
a type of averaging process.  In all cases, we can expect that the
stream turbulence scale will be large with respect to the sampling
orifice, so there is no easy way to get around the turbulence problem.
The primary reason for the above commentary is to illustrate that
while isokinetic sampling*can be performed in a good laminar flow wind
tunnel, it can only be approximated in actual process streams.
     Watson's expression for isokinetic sampling errors  (Refereces
B-7 and B-8), the experimental verification for which was obtained in
a low turbulence wind tunnel, is as follows:
            ' C
                 UG
               A
(B-l)
                                    29

-------
where
      C   =  aerosol  concentration  inside probe  entry, g/cm3
      C.  =  true  aerosol  concentration  in  the stream ahead of the
           probe, g/cm3
      Ug  =  true  gas  velocity ahead of  the probe, cm/s
      U   =  mean  velocity at probe inlet, cm/s

         -  DP PP UG
         "
              Ds
      f = empirical functional relationship
     D  = particle diameter, cm

     p  = particle density, g/cm3
      u = gas viscosity, poise
     DS = sample probe orifice diameter, cm

Equation (B-l) is plotted in Figure B-3 for different values of the
various parameters.  In practice, the plot says that anisokinetic
sampling does not lead to concentration errors as the particles become
very small, while in the limit of large, dense particles, the concen-
tration error is inversely proportional to the velocity error, i.e.

         C    U6
         ~— -v TT-   for large,  dense particles.
         LA   um
In normal  practice, the stream velocity is measured with a pitot
probe and  the sampling velocity Um is set equal to the measured
velocity.   For this mode of operation, the measured aerosol  mass
flux at the sampling point becomes (ignoring <* for the moment)
              = CmUm
                                   30

-------
        4  i-
co = UI
"$»r
a - K •
) UG
  o
o
  o
C£
                                                  _ •>
f(B)  DIAMETER, MI^ONS

 0         >50
                                                                                                      40
                                                                                                      30
                                                                                                      22
                                                                                                      13
   CP =
   V
    s
                                                                                                     FOR

                                                                                                  1  g/cm3

                                                                                                  10 m/s

                                                                                                  1.27  cm
                                                                                                          -4
                                                                                                = 2.3 x 10   poise
                                        UG   TRUE GAS SPEED
                                        Um ' SAMPLING SPEED

               Figure B-3.  Particulate measured concentration error as a function of sampling
                            velocity  (Anisokinetic) error for various aerosol  conditions
                            (from Watson,  Reference B-7)

-------
while the true mass flux is
               =  CAUG
                               (B-3)
applying the small and large particle limits of equation (B-l), we
obtain
        0 <
                   meas
true
                               (B-4)
where zero error occurs for the case of large particles, while non-zero
error occurs for very small particles and is in fact solely a velocity
measurement error unrelated to the sampling process.  In other words,
as long as sampling velocity and measured velocity are kept identical,
anisokinetic sampling of large particles compensates for velocity
measurement errors, while anisokinetic sampling of small particles
does not lead to a concentration measurement error.   For total particu-
late measurement errors, then, we may make the following statement:
     Particle mass emission errors at a point will not be larger
     than errors in the measured stream velocity as  long as the
     sample velocity is maintained equal to the measured velocity
     and the sampling probe is properly aligned with the stream.
It must be noted that the above statement applies only to particle
mass emission and only at individual  points.   The relationship between
point measurements and the total  emission is  related to stratification,
which is treated below.  The important point  is that isokinetic errors
and velocity measurement errors are compensating rather than additive.
     Concentration measurement errors due to  anisokinetic sampling
depend,  of course, on all  the factors shown in equation B-l.   Reference
B-7 recommends the values shown in Table B-2  "for the size distribution
of dusts encountered in practice".   The following general rule is also
                                   32

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Table B-2.   Effect of Departure from Isokinetic Conditions
            on Sample Concentrations (from Reference B-7)
UG
US
0.6
0.8
1.2
1.4
1.6
1.8
C
Co
RANGE
0.75-0.90
0.85-0.95
1.05-1.20
1.10-1.40
1.15-1.16
1.20-1.80
TYPICAL VALUE
0.85
0.90
1.10
1.20
1.30
1.40
                             33

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 recommended in Reference B-7:
      "Isokinetic  sampling is  unnecessary for smoke and  fumes which
      are not admixed with particulate  matter over 5y  in  size."
 It is clear that  for purposes  of error analysis,  the  term  o-  should
                                                           m/\
 be coupled  with the  velocity  error  terms due to  the compensating aspects.
 Aside from  the traditional  isokinetic  sampling aspects,  we must also be
 concerned with misalignment of the  sampling  probe with  respect to the
 local  stream direction.   As explained  above,  the  flow direction goes
 through  instantaneous  changes,  but  these average  out  reasonably over
 the sampling period  in most cases when the volumetric flow rate stays
 constant.   Any misalignment of the  sampling  probe reduces  the number
 of large particles  (>  5y)  collected, while collection of small particles
 is affected little,  if at all.   Failure  of the sampling  team to align
 the sampling probe parallel to  the  duct  or stack  axis within two or
 three degrees  constitutes  a mistake rather than a  random error.   Non-
 alignment of the  flow  itself with the  stack  axis  must generally be
 considered  a random  error  since  the sampling  team will usually not
 have  the instruments to  properly determine flow direction.  The best
 way to avoid flow angularity is  to  use the standard "eight diameters
 downstream  and  two diameters upstream  of a disturbance"  approach when
 possible.   In  stacks, the  flow will tend to  be axially aligned within
 a  few diameters from the  breaching  except in  the  case of swirling
 (cyclonic)  flow, which can persist much longer.  Reference  B-9 makes
 the following  statements about such flows:
      "....severe cyclonic motion has not been observed in  large
      power  plant stacks."
 Unfortunately,  it is also concluded that
      "Little qualitative data is available defining flow angularity
      in  large  (>100 MW)  power plant stacks."
     To  summarize the above commentary and relate it  to actual  hard-
ware, it can be said that the major error sources for collected
                                   34

-------
particulate mass are non-isokinetic sampling,  probe/flow misalignment,
and sample gain or loss within the probe.   For the SASS train,  non-
isokinetic sampling occurs because the sample  flow rate must be held
constant.   Since a sampling crew will  have a limited number of inlet
nozzle sizes, there will  be a differential between the nozzle inlet
velocity and the local stream velocity.  In addition, this configuration
does not allow for adjustments in sampling rate during a run to com-
pensate for any free stream velocity changes.   In an optimum train,
the sampling velocity would be continually adjusted so that it matched
the measured stream velocity.  The discussion  associated with equation
(B-4) says that if this can be accomplished, errors in isokinetic
sampling tend to compensate for velocity measurement errors.  In the
turbulent flows which occur in real life,  it will not be possible to
match the sample flow rate to the measured velocity, since the latter
will fluctuate more rapidly than the sample flow can be adjusted.
     The error estimates in Table 3 of the text for a   are based on
known SASS train characteristics, accuracies (velocity measurement in
particular) of other commercially available hardware, and estimates of
actual flow conditions to be encountered at the three types of designated
sampling locations.  For the SASS train, the greatest source of error
is  the  anisokinetic  error, while misalignment will be the largest
source for the hypothetical  "maximum accuracy train".   The basic
difference between the two trains would be greater velocity measurement
accuracy and continuously variable sampling velocity for the "maximum
accuracy train".   Errors are predicted highest at a control device  inlet
due to the size distribution  (maximum number of large particles) and
anticipated  flow angularities.   (See  Reference B-9 for compilations of
control device inlet  and outlet  size  distributions.)  Errors will  be
at  a minimum in a  stack due  to smaller flow angularities and removal
of  large particles in a control  device.
                                   35

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4.   Mapping (Handling of Stratification)
      There are  three  major  difficulties  involved  in  dealing with
 stratification  problems:   (1)  The  stratification  level  itself  is
 often  very large,  which  leads  to large errors,  especially  for  single
 point  sampling.   (2)  More background  data  are needed to assess the
 severity  of the  problem.   (3)  There is a shortage  of methodology for
 sampling  techniques in stratified  streams.  The first point is illustrated
 in  Table  B-3, taken from Reference B-10.   Particulate mass concentra-
 tion maps were  taken  for the four  cases  listed  (the  ESP data is true
 field  data).  Large variations from the mean concentration were ob-
 served in each case.  Of particular interest is the  ESP data, which
 shows  that the device was definitely  a source of  stratification.  The
 variations shown  in Table B-3  clearly indicate  that  single point
 sampling  is  likely to result in large mapping errors.
     There is no  question that much more stratification  data exist
 than were examined for this report.   As much data was examined as
 could  be  obtained  within the scope of work.  Comparison data between
 single point impactor sampling and multiple point Method 5 type
 sampling  is shown  in  Tables B-4 and B-5.   The data were obtained from
 References  B-ll and B-12, respectively, supplied by  Joe McCain of
 Southern  Research  Institute.   The  data in  Table B-4  represent a
 summary of many runs.  The  "minimum"  and "maximum" errors are the
 best and  worst correlations obtained  among the  individual runs, while
 the "nominal" error was the average error  for all runs in the category.
The data  in Table  B-5 are for  individual runs.   A very important item
to  keep in mind when  examining these  data  is that entirely different
types  of  sampling  trains were  used to obtain the single point (im-
pactors were used  here) and multiple  point (Method 5   type train) data.
This makes  it impossible to isolate the mapping error due to single
point  sampling.   Data type and quality are discussed  further in
Appendix  C.  What  is needed is more mapping data obtained with a single
                                    36

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      Table B-3.   Summary of Particulate  Mapping  Data  from
                  Fluidyne "Particulate Sampling  Strategies"
                  Report (Reference B-9)
DESCRIPTION
Downstream of ESP
Upstream of ESP
"Theoretical" distri-
bution downstream of
ESP
Laboratory scale
model flow
CENTER POINT
CONCENTRATION
ERROR, %
-16
+13.5
-62.8
- 2.33
VARIATION IN SAMPLE PLANE
FROM MEAN CONCENTRATION, %
LOW
-74
-35
-63
-19
HIGH
+268
+ 30
+160
+117
      Table  B-4.  Summary of Comparison of Single Point Impactor
                  Data Versus Method 5 Traverse at an  ESP Outlet,
                  from Southern Research  Institute EPRI Report
                  (Reference B-ll)
OPERATING
MODE*
With S03
Without S03
SINGLE POINT ERROR USING METHOD 5 TRAVERSE AS A REFERENCE, %
MINIMUM
- 5
-68
NOMINAL
-33
-75
MAXIMUM
-61
-94
*SOo injection was used as a mechanism to minimize re-entrainment due to
 rapping.  Lower loading and less stratification occurred with SO.,
 injection.
                                  37

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Table B-5.  Grain Loading Errors for Single Point Impactor
            Sampling, Using Conventional (ASME, EPA) Mass
            Train Traverse Measurement As Reference Data
            (Data taken from Reference B-12)
SITE
1






2


3


4



RUN NO.
1
2
3
4
5
6
7
1
2
3
1
2
3
1
2
3
4
SINGLE POINT MASS LOADING ERROR, %
+711
+256
+227
+ 26
+ 6
+ 5
+131
- 34
- 35
- 43
- 38
- 19
- 50
- 6
- 45
- 48
- 50
   Sites:   At all  sites,  location was control  device outlet
           1  - Coal  fired power plant
           2  - Coal  fired power plant
           3  - Electric  arc smelting furnace
           4  - Coal  fired power plant
                          38

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instrument, as was done to obtain  the  data  summarized  in Table B-3.
     The data in Table B-4 are a  good  illustration  of  the need for
better sampling methodology.   The  impactor  sampling point used was
not representative of the distribution in  the  stream,  leading to
errors of as high as a factor of  16.   The  Level  1 approach of using
a point of average velocity as the sampling point is a step  in the
right direction since such a point is  less  likely than most  to result
in misalignment errors, will not  be in a recirculation region, and at
least will be representative of total  mass  transport.   For  stack
sampling,  it may be the case that further refinements  to  this approach
will not be needed.  For sampling at a control device  outlet, however,
Table B-4  points out the need for taking the device's  characteristics
into account in the selection of a sampling point or points.
     Particulate stratification originates where the particles
originate, e.g. in  the furnace of a coal fired power plant.   Strati-
fication can be made worse by in-leakage of air.  Removal  devices can
make stratification either more or less severe, according to their
operating  characterisitics.  Changes in ducting shape and direction
simultaneously promote convective mixing (reduces stratification) and
inertial separation  (increases stratification).  The combination of
desired accuracy and stratification provides the answer to the ques-
tion, "To  single point or not to single point?".  This question has
been studied more  extensively for flow measurement  and gas sampling
than for particulate sampling, but should apply to  that case as well.
Reference  B-13, which  is  basically a summarization  of the velocity
measurement data  in  Reference B-10, and Reference  B-14 conclude that
the 2o mapping error of  a 12-to-16 point traverse  is  about  a factor
of  five  less than  that for a  single point measurement for volumetric
flow  (References  B-12  and B-13) and gas composition (Reference B-13).
As  the mean  particle  size becomes small (<5p),  particulate  stratifica-
tion is  almost  identical  in  mechanism  to gas  stratification because of
                                    39

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the dominance of convective mixing in both cases.  In Reference B-15,
the average 2o single point gas composition mapping error was found to
be ±15%.  There is no reason to believe the single point participate
sampling mapping error would be better than this figure, and indeed
will be much worse in most cases.  The data which have been examined
are not sufficient to establish good bounds for single point particulate
sampling.  Accumulated data for volumetric flow and gas composition
lead to the conclusion that a properly performed traverse using about
16 points will result in o^ not being the major source of system
error.
     The single point mapping error estimates in Table 4 in the text
were derived from Tables B-3 and B-5, taking into account the difference
in trains in the latter.   The traverse error estimates were obtained
by comparing the maps in Reference B-10 with gas composition maps in
Reference B-14.  The mapping error itself is independent of the
sampling equipment used.   The mapping error estimates must at present
be considered the least firm of all the error estimates in the text,
which is unfortunate since the mapping error is by far the largest
error in the system for single point sampling.   The need for more data
to "firm up" the estimates is discussed in Appendix C.
                                   40

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                         APPENDIX B.   REFERENCES
B-1.   "Continuous Measurement of Total Gas Flowrate from Stationary
       Sources," EPA-650/2-75-020, Brooks,  et al..  February 1975.
B-2.   The Measurement of Air Flow, E. Ower and R.  C. Pankhurst; Pergamon
       Press, 1966.
B-3.   "Recent Environmental Assessment Studies," (Draft Copy), Monsanto
       Research Corporation, November 1976.
B-4.   Boundary Layer Theory, H. Schlichting; McGraw-Hill Book Company, 1968.
B-5.   "Correlation Measurements  in a Turbulent Flow Through a Pipe," G. I.
       Taylor, Proc. Roy. Soc. A  157. 537-546,1936.
B-6.   "The Structure of Turbulence in Fully Developed Pipe Flow," J. Laufer,
       NACA TN 2954, 1953.
B-7.   Air Pollution. Volume  II, A. Stern, ed., Academic Press, 1968.
B-8.   H. H. Watson, Am. Ind. Hyg. Assoc.  Quart. 15, 21, 1954.
B-9.   "Particulate Sampling  Strategies  for  Large Power  Plants  Including
       Non-uniform Flow," EPA-600/2-76-170,  Hanson,  et a!.. June 1976.
B-10.  "Fine Particle Emissions  Information  System:  Summary Report  (Summer
       1976)," EPA-600/2-76-174,  Schrag  and  Rao, June 1976.
B-ll.  "Proceedings on  the  Workshop on Sampling, Analysis, and  Monitoring  of
       Stack Emissions," EPRI SR-41,  Southern  Research  Institute, April  1976.
B-12.  "Particulate Sizing  Techniques  for  Control  Device Evaluation,"
       EPA-650/2-74-102-a,  Smith,  et  al.f  August,  1975.
B-13.  "The  Number of Sampling  Points  Needed for Representative Source
       Sampling,"  K. T.  Knapp,  paper  presented at  Fourth National Conference
       on Energy and Environment,  October  1976.
B-14.  "Flow and Gas Sampling Manual,"  EPA-600/2-76-203, Brooks and Williams,
       July  1976.
B-15.  "Continuous Measurement  of Gas Composition  from  Stationary  Sources,"
       EPA-600/2-75-012, Brooks,  et al.. July  1975.
                                    41

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            APPENDIX C.  COMMENTS ON DATA AND ERROR ANALYSES

     As stated in the text, the error analysis performed was identical  in
form to that in Reference C-l.  The explicit portion of the error analysis
is similar in concept to that in Reference C-2.  A nominal 2o system error
of ±16% was obtained for a total participate mass measurement involving a
traverse.  This estimate is similar to those for traverses in Table 5.
A more encompassing error discussion is given in Reference C-3,  and treats
both explicit and non-explicit error sources.  However, error bounds were
not well established in this analysis.
     The nature of the measurement for total particulate mass dictates  that
two distinct groups of information must be consulted to determine system
accuracy - sampling hardware characteristics and source characteristics.
For parameters such as temperature and static pressure, it is normally  the
case that measurement accuracy can be determined from the hardware alone.
The accuracy of parameters such as velocity and collected particulate mass
usually depend on both hardware and source characteristics.   At  the other
extreme, mapping errors depend only on source characteristics.   The great
variety of source characteristics makes it impossible  to perform a system
error analysis and arrive at a single number for system accuracy,  just  as
it would be impossible to arrive at a single number result for an analysis
of a variety of sampling trains.  The final selected approach of looking
at two types of trains in three generalized sampling situations  was in-
tended to show the relative impact of hardware and source on system
accuracy.
     Most error analysis work deals with identification and  evaluation  of
specific error sources.   The interrelationship of hardware and source
characteristics for particulate sampling necessarily complicates isolation
of errors.   During the present study,  this problem caused the most diffi-
culty in evaluation of the error terms a   and o^.   As was  mentioned in
Appendix B, evaluation of  anisokinetic  sampling errors has traditionally
been performed in laminar flow wind tunnels.   The turbulent, unsteady flows
                                   42

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in process streams make  it difficult to  adapt  laminar  flow  data  to  the  real
life case.  That approach has  been  used  of necessity,  however, since  it has
not been possible to obtain high accuracy reference data  needed  for an
error assessment in the  field.
     The bulk of the mapping data summarized in Appendix  B  has the  problem
that the single point data was obtained  with significantly  different  hard-
ware than the traverse data.  This makes it impossible to separate  the
hardware error from the mapping error.    There is no question that  mapping
data of the type desired (a concentration map obtained with a single  probe)
is difficult, time consuming,  and costly to obtain.  In this instance,  it
is felt that the effort would be justified due to the magnitude  of  mapping
errors,  in addition to supporting error analysis work, the same  data  would
be essential to the development of methods for obtaining  representative
samples through judicious selection of a single sampling  point or a small
number of sampling points.
     The  functional purpose of a system error analysis, in addition to
producing the bottom line number for total system accuracy, is to determine
the  relative importance  of the  individual error sources.   This information
tells the worker which hardware components in a given system should be
upgraded  to achieve a desired accuracy, and which components may be replaced
with less expensive, less accurate  ones without significantly altering  the
system accuracy.   The same  is true  of sampling procedures,  the most obvious
example being selection  of  single or multiple point sampling techniques  to
achieve a given accuracy.   A proper error analysis  is thus the technical
foundation  for  optimum allocation of funds and manpower  to  achieve sampling
data of appropriate quality for the tasks at  hand.
                                    43

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                         APPENDIX C.  REFERENCES
C-l.  "Flow and Gas Sampling Manual," EPA-600/2-76-203, Brooks and Williams,
      July 1976.

C-2.  Industrial Source Sampling. Brenchley, Turley,  and Yarmac,  Ann Arbor
      Science Publishers,  Inc., 1973.

C-3.  "A Manual of Electrostatic Precipitator Technology,  Part I  - Funda-
      mentals," NTIS PB-196 380, Oglesby, etal.,  August 1970
                                   44

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                                TECHNICAL REPORT DATA
                          (Please read Instructions on the reverse before completing)
  REPORT NO.
 EPA-600/7-79-155
                           2.
                                                      3. RECIPIENT'S ACCESSION NO.
 4.TITLE AND SUBTITLE
I Total Particulate Mass Emission Sampling Errors
           5. REPORT DATE
            July 1979
                                                      6. PERFORMING ORGANIZATION CODE
 7. AUTHORIS)

  E.F. Brooks
                                                      8. PERFORMING ORGANIZATION REPORT NO.
 9. PERFORMING ORGANIZATION NAME AND ADDRESS
  TRW Systems and Energy
  One Space Park
  Redondo  Beach, California  90278
                                                       10. PROGRAM ELEMENT NO.
            INE624
           11. CONTRACT/GRANT NO.

            68-02-2165, Task 104
 12. SPONSORING AGENCY NAME AND ADDRESS
  EPA, Office of Research and Development
  Industrial Environmental Research Laboratory
  Research Triangle Park, NC  27711
           13. TYPE OF REPORT AND PERIOD COVERED
           Task Final; 11/76 - 4/77
           14. SPONSORING AGENCY CODE
             EPA/600/13
 is. SUPPLEMENTARY NOTES gPA project officer R. M. Statnick is no longer with
  for details, contact F.E.  Briden, Mail Drop 62, 919/541-2557.
 16. ABSTRACT The repOrt gives a first-cut estimate of sampling errors in the measure-
  ment of total particulate mass emissions from stationary sources. IERL-RTP Pro-
  cedures Manual: Level 1 Environmental Assessment expresses the desire to mea-
  sure at accuracies within a factor of -f or - 2 to 3. Measurement errors are divided
  into two general categories: sampling errors and analysis errors. The  report deals
  with evaluation of  total particulate mass sampling errors , within the framework of
  a system error analysis. A mass transport expression is developed in terms  of
  measured parameters to serve as the basis for the analysis. A standard explicit
  error analysis is performed on the derived expression for mass transport. Since
  there are also important non-explicit error sources, terms are added to the explicit
  equation to handle them. The individual error terms are then evaluated on the basis
  of previous  analyses,  available empirical data and, where no data are available,
  estimates. The evaluation leads to a ranking of individual error sources and esti-
  mates of total system  error. Analysis results show that a Level 1 should have  a sam-
  pling  accuracy of better than a factor of + or -2, with a confidence of 95%, except at
  a control device outlet where the accuracy is more likely to be a factor of + or -3,
  especially if the control device is an electrostatic precipitator.
 17.
                              KEY WORDS AND DOCUMENT ANALYSIS
                  DESCRIPTORS
                                           b.lDENTIFIERS/OPEN ENDED TERMS
  Pollution
  Dust
  Emission
  Sampling
  Analyzing
  Error Analysis
Pollution Control
Stationary Sources
Particulates
Mass Emissions
                         . COSATl Field/Group
13B
11G
14B
                         12A
  8. DISTRIBUTION STATEMENT
  Release to Public
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                                           Unclassified
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                             49
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