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                       /A newsletter about soil, sediment, and ground-water characterization and remediation technologies
                        Issue 34

This issue o/Technology News and Trends highlights strategies for remediating sites with
inorganic contaminants and radionuclides. Enhanced research has led to increased use of
bioremediation as a viable technology for removing or transforming inorganic contami-
nants. Due to the length of time needed to address radionuclide contamination, research also
focuses on the potential for monitored natural attenuation (MNA) to complement aggressive
cleanup technologies.

          Hanford Demonstrates Bioimmobilization of Hexavalent
                         Chromium in Ground Water
                                                                                                     January 2008
The U.S. Department of Energy (DOE) is
evaluating long-term efficacy of lactate-
stimulated bioreduction to treat ground water
contaminated with hexavalent chromium
[Cr(VI)] atHanford's "Site 100H" along the
Columbia River in Washington. The study
includes identification of critical microbial
community-structure changes and stressors
helping   to   control  and  predict
biogeochemical processes causing Cr(VI)
bioimmobilization. Polylactate in the form of
Hydrogen Release Compound® (HRC) was
injected into the ground water in 2004.
Cr(VI) concentrations now are below the
drinking water standard of 10 ppb due to
transformation of Cr(VI) into insoluble Cr
(III) complexes, which is largely affected
by bioimmobilization stressors. Common
stressors identified during the study include
oxygen, nitrate, salt, and sulfate.

Chromium contamination at Site 1OOH likely
resulted from a release of sodium dichromate
once used to control corrosion at Hanford's
former plutonium reactor systems, and to
decontaminate   shut-down  reactor
complexes. Ground-water analysis in 2004
at Site 100H showed a Cr(VI) concentration
of approximately  100 mg/L, a level
unchanged over the previous 20 years. Sand
and gravel extend approximately 50  feet
below ground surface (bgs) at the site.  The
sand and gravel are underlain by clay and
silt layers that in turn overlay basalt.  The
water table is at 42 feet bgs.

Bench-scale studies on Site 100H ground-
water and sediment samples showed  that
                                          introduction of various forms of lactate
                                          stimulated an increase in bacterial population
                                          exceeding 108 cells/g. This increase generated
                                          reducing conditions  leading to  nearly
                                          complete Cr(VI) removal from the pore
                                          solution after only three weeks of incubation.
                                          The most viable remediation alternative
                                          involved use of a diothionite reducing
                                          permeable reactive barrier (PRB), but onsite
                                          studies suggested difficulty in long-term PRB
                                          maintenance sufficient to prevent Cr(VI)
                                          breakthrough.

                                          Field testing in 2004 involved a single injection
                                          of 40  pounds of HRC labeled with stable
                                          isotope carbon (13C) in a well extending 50
                                          feet bgs.  A multi-screened extraction well
                                          approximately 15 feet from the injection
                                          location was pumped for 27 days to obtain
                                          water samples from the sand/gravel, clay,
                                          and silt layers.

                                          Post-injection analysis of ground water
                                          indicated an increase in the 813C (ratio of
                                          13C to other carbon isotopes) of dissolved
                                          inorganic carbon from 15%o (parts  per
                                          thousand) to over 50%o,  exceeding  the
                                          HRC's proportion and indicating that CO2
                                          was created  as a byproduct of  lactate
                                          metabolism. Depletion of competing terminal
                                          electron acceptors (oxygen,  nitrate,  and
                                          sulfate) occurred sequentially. Evidence of
                                          subsurface lactic  acid buildup further
                                          indicated that the injection stimulated
                                          bioreduction of Cr(VI) to Cr(III) through
                                          precipitation. Naturally occurring microbial
                                          reducers of the sulfate and iron (Fe)
                                                           [continued on page 2]
                                                                                             Contents
 Hanford Demonstrates
 Bioimmobilization of
 Hexavalent Chromium
 in Ground Water       page 1

 SRNL Evaluates
 Sustainable
 Remediation Strategies
 for Metals and
 Radionuclides         page 2

 Bioremediation
 Evaluated for Long-Term
 Immobilization of
 Uranium               page 3

 Research Shows
 Growing Potential of
 Bioremediation for
 Arsenic and Selenium  page 5

 EPA Releases
 Technical Resource for
 MNA of Inorganics      page 6
      CLU-IN Resources
CLU-IN's Contaminant Focus
area provides background
information on a range of issues
concerning soil or ground water
with arsenic or chromium (VI)
contamination. Topics include
contaminant chemistry and
behavior, toxicology, and
regulatory guidance. Visit these
topics at http://cluin.org/
contaminantfocus/.
              Recycled/Recyclable
              Printed with Soy/Canola Ink on paper that
              contains at least 50% recycted fiber

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[continued from page 1]
apparently maintain the presence of
hydrogen sulfide and ferrous iron [Fe(II)],
subsequently maintaining Cr(VI) below 5
ppb in the injection well.

DOE's "16s rDNA microarray" method
was used to detect the composition and
diversity of microbes  in ground-water
samples (Figure 1).  The method is
capable of identify ing the 9,900 microbial
species of 16S rDNA from up to 550,000
probes in a 1.28 cm2 array.

Evidence of bioreduction was supported
by a  decrease in reduction/oxidation
from  240 to -130 mV and a decrease in
oxygen content from 9 mg/L to nearly
zero. Cr(VI)  concentrations in the
monitoring well decreased to less than
5 ppb as a result of the polylactate
injection, and have remained lower than
upgradient (background) concentrations.
Study  findings  suggest  that  the
prevailing  mechanisms for Cr(VI)
reduction  are  direct enzymatic
chromate  reduction and/or abiotic
geochemical processes involving
formation of insoluble complexes of
Cr(III) with Fe(II) or sulfide (S2').
   •3- 3000
              Desulfovibrio hatophilus
              Geobacter metellineducens
              Dechloromonas agitatus
              Pseudomonas put/da
                            11      17
                       Days Since HRC Injection
Overall  study  results demonstrate
significant potential for using naturally
occurring microorganisms  to enhance
in-situ Cr(VI) immobilization.

Ongoing monitoring indicates minimal
chemical rebound. DOE will further
examine the lateral extent and potential for
rebound as well as the impact of Site 100H
Cr treatment on regional ground water.
Future onsite investigations also will
determine the optimal number of injection
wells needed for Crbioimmobilization and
the appropriate frequency of lactate
reinjection. Based on the favorable Site 100
results, DOE anticipates using this remedy
to control Cr(VI) concentrations  in
ground water at other sites such as the
Idaho National Laboratory, Savannah
River Site, and Pantex Plant. Updated
project details are available from DOE's
Office of Environmental Management at
http://esd.lbl.gov/ERT/hanfordlOOh/.

Contributed by  Terry Hazen, DOE
ftchazen&lbl.gov  or 510-486-6223)
           SRNL Evaluates Sustainable Remediation Strategies for Metals and Radionuclides
DOE's  Savannah  River National
Laboratory (SRNL)  recently  initiated
studies under the Department's Office
of Environmental Management (EM) to
identify  methods  for  increasing
sustainability of remediation addressing
metal- and radionuclide-contaminated
ground water. Sustainable strategies will
help meet site-specific cleanup objectives,
including long-term risk reduction, while
minimizing maintenance, cost,  and
collateral environmental  damage
associated with remediation. Current
SRNL work focuses  on estimating the
duration  of aggressive  remediation
strategies before natural processes can
be relied upon to return the site to pre-
contamination conditions. Opportunities
for using follow-on  natural processes
are critical to  sites with contaminants
known to exist in the environment for
a long time.
One SRNL study area at the Savannah
River Site (SRS), SC, is a 1-km2 metals/
radionuclides waste site known as the "F-
Area Seepage Basins," where a modified
funnel-and-gate barrier system  has
operated since 2005 to treat ground water
containing strontium (Sr)-90, uranium
(U) isotopes, iodine-129, technetium-99,
and tritium. The ground water is acidic
(pH 3.2-4.0), aprimary factor facilitating
mobility of certain contaminants  and
associated risk drivers. In the current
treatment  strategy, alkaline  solutions of
pH 10 are injected periodically into the
gates to neutralize ground water  and
reduce mobility of some contaminants.
Injection  frequency  is determined by
monitoring pH in wells  downgradient
from the injection wells; when a trigger
of pH 5.5 is reached, alkaline solution is
reinjected. In the three years of operation,
injections  were required approximately
each  12  months at one gate and 18
months at the second gate.

The  treatment  strategy  is  more
sustainable than the previous, inefficient,
pump-and-treat (P&T) system. P&T
operations  cost  approximately $1
million per month and  produced  a
significant quantity of solid radioactive
waste requiring disposal. The alkaline-
enhanced funnel-and-gate system,
however, treats all contaminants by
mixing the stratified plume at the
barrier wall as well as pH-sensitive
contaminants such as 90Sr and uranium
isotopes  at the gates. Early  analytical
data from downgradient wells indicate
the  system  effectively   reduces
concentrations  of 90Sr,  uranium
isotopes, and tritium to below drinking
water standards.
               [continued on page 3]

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[continued from page 2]
Chemical effects of the alkaline injection
were demonstrated in a small-scale field
test conducted over five months in 2002-
2003, prior to installing the full-scale
injection system. Alkaline solutions were
injected below the water table at closely
spaced points upgradient of the extraction
well. The extraction well was pumped
continually to draw injectate toward the
well. Breakthrough of the injectate at the
extraction well was indicated by decrease
in specific conductance. The pH did not
increase  until   four  weeks   after
breakthrough due to the need for the
injectate to first neutralize acidified
surfaces of the aquifer minerals (Figure 2).
Adjustments to the injection system in
late December 2002 caused temporary
decreases  in   pH  and  specific
conductance four to five weeks later.

This series of chemical changes controls
the time needed to return ground water
to a near-natural pH of 6. When acid flux
from  the vadose  zone  becomes
insignificant, uncontaminated ground
water with pH near 6 migrates into the
plume zone. The resulting pH front will
migrate more slowly than ground water
as a result of the buffering effect of
acidified mineral  surfaces.  Duration of
the injection system will depend on the
migration rate of the trailing pH gradient
through the treatment zone, the point
at  which  contaminants  will  not
remobilize. By avoiding remobilization
of sequestered metals and radionculides
and reducing treatment duration,
sustainability of this  remediation
strategy is improved.

Findings from this  and other waste sites
suggest the rate of biogeochemical gradient
migration through a treatment zone  is
controlled by hydrogeology and mineralogy
as well as  relative  biogeochemical
conditions of the treatment zone, plume
zone, and uncontaminated zone. At sites
employing treatment technologies that
establish reducing zones, for example,
mineralogy   affects   remediation
sustainability. The reduced  iron  and
                           manganese minerals formed during
                           treatment will act as redox buffers and
                           decrease migration rates of  dissolved
                           oxygen  gradients,   consequently
                           remobilizing contaminants.

                           Understanding factors that control the rate
                           at which F-Area Seepage Basins ground
                           water returns to near natural conditions
                           is a primary goal of this study, driven by
                           SRS long-term remediation. EM's broader
                           goal is to address these issues for other
                           wastes and at other sites using different
                           remediation strategies.

                           Contributed by Miles Denham, SRNL
                           (miles.denham(q)srnl.doe.gov or
                           803-725-5521)
   7001

 I 600-1
 CO

 ^500-
   400-
 O 300-
 8 200-
 M
   100
Injection Begins
Probable Breakthrough
                   -•-Specific Conductance
                   —pH
Figure 2.  Weekly
measurements of
extraction well
ground-water
parameters at the
SRS F-Area
Seepage Basins
indicate a delay in
pH response after
breakthrough of
the alkaline
injectate.

                   Bioremediation Evaluated for long-Term Immobilization of Uranium
 Oak Ridge  National  Laboratory
 (ORNL) and Stanford University
 researchers are developing a strategy
 for bioimmobilizing uranium in the
 highly contaminated subsurface of the
 former "S3 Ponds" site at DOE's Oak
 Ridge Field Research Center in Oak
 Ridge, TN. The approach  employs a
 treatment  train involving  flow-field
 hydraulic  control,   subsurface
 preconditioning, and  delivery of
 ethanol as an electron donor for in-
 situ U(VI) reduction/immobilization.
 Results of pilot-scale field tests will
 be integrated into DOE  decision-
 making in 2015 regarding  S3 Ponds
 cleanup. Additional EM  assistance in
 evaluating site-specific environmental
engineering, hydrogeology, microbiology,
geo-chemistry, and physics is provided by
the University of Oklahoma, Argonne
National Laboratory, Michigan State
University, Montana State University, and
Georgia Institute of Technology.

Storage of atomic  weapons production
wastes in the unlined S3 Ponds from 1951
until 1984  caused extensive subsurface
contaminant plumes migrating in three
separate pathways, including one that
discharges to a nearby creek. Remediation
planning required  detailed analysis of
geophysical and geochemical conditions.
The plume  depths range from 30 to 100
ft bgs within subsurface media containing
fracture densities  as high  as 100-200
                           fractures per meter.  The fractures
                           account for less than 5-10% of matrix
                           porosity but carry more than 95% of
                           ground-water flow.  The surrounding
                           highly porous soil and sediment have a
                           low permeability and serve as a sink (and
                           continuing source) of contamination.

                           Sample analyses indicated the highest
                           contaminant concentrations existed in
                           ground water at a depth of 30-50 feet
                           bgs. To date, maximum concentrations
                           measured for metals are 40  mg/L of
                           depleted uranium, 540 mg/L aluminum
                           (Al), 930 mg/L calcium (Ca), and 11-
                           14 mg/L nickel. Perchloroethene and
                           c/5-dichloroethene in concentrations of
                                          [continued on page 4]

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[continued from page 3]
2-3 mg/L and 1 mg/L, respectively, are
co-contaminants.  Concentrations of
8,000  g/L nitrate and 1 g/L  sulfate
resulted from disposal of nitric and
sulfuric acids that lowered the pH of the
ground water to 3.4-3.6, hampering in-
situ uranium bioremediation.

Solid-phase uranium in hot spots with
concentrations of 200-700 mg/kg serve
as  a long-term  source  of  U(VI)
contamination, and aqueous-phase
uranium concentrations  currently
exceed the federal drinking water
standard by over 1,000-fold. Most of
the uranium is associated with the solid
phase.  Laboratory and field tests
showed that uranium sorption points
(0.1 g soil per  15 mL solution) and
desorption points  (13.5  g/15 mL
solution) are strongly pH dependent;
high uranium adsorption was observed
at pH around 6.0.

Bioremediation at the S3 Ponds relies
on  converting soluble U(VI) into
sparingly soluble U(IV), which is more
resistant to dissolution and  desorption
and posing less potential for ground-
water  migration.   A   range   of
microorganisms,  including  certain
sulfate-reducing (SRB) and iron(III)-
reducing bacteria (FeRB), can mediate
this conversion. Reduced compounds
such as  sulfide  and green rusts
generated by microorganisms also can
convert U(VI) to U(IV) under certain
reduced conditions.

Prior to startup of the pilot-scale
bioimmobilization system, a nested
circulation well system containing an
inner  loop and an outer  loop was
installed to improve hydraulic control in
the treatment area.  Injection of clean
water into the outer loop protected the
inner   loop   from   invasion  of
contaminated ground water. Extracted
ground water was then treated through
an  aboveground system employing
vacuum stripping to remove volatile
organic   compounds    (VOCs),
precipitation of Al and Ca sludge in a
settling tank, and nitrate removal through
a biological granular-activated-carbon
fluidized bed reactor. Treated water was
injected back into the outer loop.

In November 2002, a bromide tracer study
was conducted to characterize the test area's
hydrology. The treatment-area subsurface
was flushed with clean water (tap water
and nitrate-free water from an aboveground
treatment facility) during the following fall
to achieve a pH of 4.0-4.5 and remove
clogging agents and inhibitors such as Al,
Ca, nitrate, and VOCs. A second clean-
water flushing was performed in November
2003 to increase pH to 6.0-6.3, facilitating
maximum uranium sorption capability and
enhancing conditions for bioremediation.
Residual nitrate in ground water was
removed further by in-situ denitrification.

After an additional year of ethanol injections,
uranium concentrations decreased below
the maximum contaminant level (0.03 mg/
L) within fast-flowing zones of the
subsurface   (3-8  m/day  hydraulic
conductivity) demonstrating that they were
hydrologically connected to the injection
well.  Intermittent ethanol injections
sequentially stimulated in-situ denitrification
followed by  sulfate and Fe(III) reduction
and U(VI) reduction. Treatment-area
sediment samples changed color from
yellow-brown to dark green or black,
providing further evidence of reduction
and  expansion within the zone of
reduction. Reduction of U(VI) to U(IV)
was confirmed by X-ray absorption near-
edge  structure  spectroscopy.  Before
biostimulation, no U(IV) was observed in
sediment samples. After biostimulation, up
to 80% of the uranium sorbed to soil was
reduced to U(IV).

Microbial community  analysis indicated
that SRB and  FeRB populations are
stimulated by delivery of electron donor.
Prior to biostimulation, only denitrifiers
were  found in ground water, at an
extremely low level (3 cells/mL). The
amount of bacterial DNA also was too
low to extract from sediment samples.
Most probable estimates  for denitrifiers,
SRB, and FeRB in sediments (cells/g dry
weight) after biostimulation increased to
107-108. Post-treatment tests indicate that
microorganisms  capable of reducing
U(VI)  to  U(IV)  (including  SRB
Desulfovibrio, Desulfoporosinus, and
Desulfotomaculum  spp.  and FeRB
Geobacter wAAnaeromyxobacter spp.)
were present in both ground water and
sediment. These results confirm that
biostimulation promoted biotic and
secondary abiotic reductions of U(VI) in
ground water.

The pilot system continues to operate to
evaluate  stability of reduced uranium.
Bioreduced U(IV) was stable following
suspension of ethanol delivery for a 50-
day period when anaerobic conditions
were maintained. Two-year microcosm
tests also confirmed long-term stability of
the reduced uranium. Other field tests
involving injections of dissolved oxygen
(DO) or nitrate  to the reduced-zone
subsurface demonstrated reoxidizationof
U(IV) and remobilization of U(VI).
Subsurface delivery of ethanol  as  an
electron  donor, however,  effectively
restored reducing  conditions and
decreased uranium concentrations to the
previously low  levels. Ongoing research
involves  additional characterization of
U(VI) reduction by  delivery of multiple
or slowly-degrading electron donor
sources and maintenance of long-term
stability of immobilized uranium.

Monitoring results to date indicate that
very low aqueous-phase concentrations
of uranium can be achieved despite high
solid-phase concentrations due to the
low solubility of U(IV) and low rates of
desorption/dissolution relative to the rate
of reduction. Findings suggest that long-
term bioremediation  at S3 Ponds will
need strategies  for DO and nitrate
control  or methods  to increase
resistance of the immobilized uranium
to remobilization by reoxidation.

Contributed by Craig Criddle, Ph.D
fcriddle&stanford.edu or
650-723-9032) and Wei-Min Wu,  Ph.D
(wei-min.wu(q)stanford.edu  or
650-724-5310), Stanford University,
and Philip Jardine,  Ph.D
(jardinepm&ornl.gov or
865-574-8058) and David Watson
(watsondb (q).ornl. gov or
865-241-4749), ORNL

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            Research Shows Growing Potential of Bioremediation for Arsenic and Selenium
Collaborative research among Duquesne
University, the University of Pittsburgh,
and the U.S. Geological Survey (USGS)
is underway to identify bacteria and plant
species with  potential  to  improve
bioremediation efficacy for arsenic (As)
and selenium (Se). Bioremediation of
these contaminants is an alternative to
abiotic  methods based on activated
alumina, coagulation/filtration, lime
softening, and reverse osmosis. Abiotic
methods generally  cost more, remove
As(III)  less  effectively,   require
manipulation of pH, and produce more
waste.  Integrated laboratory  and
greenhouse test results show significant
potential for arsenite-oxidizing, arsenate-
reducing, or sulfidogenic bacteria as
well  as hyperaccumulating yeast
(Saccharomyces) and brake fern (Pteris).

Many Pteris species such as P. vittata
(ladder  brake) and P.  cretica (Cretan
brake) have proven to hyperaccumulate
As  in the stems and  leaves. Arsenic
typically enters the plant as As(V) through
phosphate channels in the roots, where
it is reduced to As(III) and stored in other
plant tissues. When accumulation of
As(III)  is complete, harvested plant
tissues are disposed as hazardous waste.

In Duquesne/University of Pittsburgh
greenhouse studies, P. cretica exposed
to water containing 300 [ig/L As(III)
resulted in 100% oxidization to As(V)
and subsequent plant uptake of As(V)
within 100 hours (Figure 3). Rates of
As uptake showed similar trends across
Pteris spp.  Arsenic uptake in control
experiments with non As-accumulating
Boston fern (Nephorlepsis exaltata) also
showed rapid As(III) oxidation, but no
uptake of As.

Researchers also are evaluating various
changes in the rhizosphere of P. cretica.
Addition of an antibiotic mixture to the
water was found to  significantly reduce
microbial populations, reducing the
As(III) oxidation rate by approximately
50% within 48 hours and consequently
delaying As uptake.  These results
suggested that the rhizosphere microbiota
is one of the controlling factors in As
uptake. Testing now focuses on the use
of specific nutrient amendments to
enhance rhizosphere bacterial activity.

Selenium (Se) commonly accumulates as
a result  of erosion  and industrial or
agricultural runoff folio wed by evaporation
in areas with extensive hydrocarbon
content. It is  frequently present in
wastewater discharged by petroleum-
processing  facilities. Phytoremediation
employing   plant    species   that
hyperaccumulate (selenium weed Neptunia
amplexicaulis,  and Astragalus spp. such
as loco weed and milk vetch) or volatilize
(Indian mustard Brassica juncea) has
shown limited success with Se.

In contrast, more than 20 bacterial species
have demonstrated capability to respire
selenate, converting Se(VI) to Se(IV) and
Se(0). Field tests show effective stimulation
of selenate-respiring bacteria under
anaerobic  conditions, although co-
contaminants such as nitrate commonly
inhibit selenium reduction. Various
methods for avoiding co-contaminant
inhibition have been integrated in pilot-scale
treatment  systems. In the Panoche
Drainage District of northern California,
for example, subsurface drainage is dosed
with algae and injected into settling ponds.
This strategy successfully removes 80%
                  of the Se through microbial precipitation
                  but results in biomass accumulation.

                  The  USGS/Duquesne  study group
                  evaluated a range of bacteria  with
                  potential  for  avoiding  biomass
                  accumulation during Se  removal. Test
                  results indicated that the  soil bacterium
                  Sulfuro spirillum barnesii simultaneously
                  reduces Se(VI) and respires nitrate.
                  Washed suspensions of  nitrate-grown
                  cells removed more than 98% of the 50-
                  |jM Se(VI) as nanospheres of Se(0). The
                  cells exhibited high affinity for both
                  nitrate (0.7 |jM) and selenate (21 \\M)
                  and two separate enzyme pathways.

                  Results from these studies  will be applied
                  in upcoming USGS field applications.
                  Site-specific information about other
                  projects  addressing  As  and Se
                  contamination are  available at http://
                  water.us gs.gov/nrp/proj.bib/
                  oremland.html. http://toxics.usgs.gov/
                  topics/rem_act/saco.html  and http://
                  pubs.usgs.gov/fs/fs-031-03/.

                  Contributed by John Stolz, Ph.D.,
                  Duquesne University fstolz&.duq.edu or
                  412-396-6333), Radisav  Vidic, Ph.D.,
                  University of Pittsburgh
                  (vidic&.engr.pitt.edu or 412-624-1307),
                  and Ronald S.  Oremland, USGS
                  (650-329-4482)
                                    —•-- As (Total)
                                    -•--As (III)
                                    --A-- As(V)
             0
20
 40      60
Time (hours)
80
                                      Figure 3.
                                      Tests using
                                      Pteris cretica
                                      showed that
                                      As(III) must
                                      be oxidized
                                                           before it can
                                                           by the plant.
100

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                                            Solid Waste and
                                            Emergency Response
                                            (5203P)
EPA 542-N-08-001
January 2008
Issue No. 34
United States
Environmental Protection Agency
National Service Center for Environmental Publications
P.O. Box 42419
Cincinnati, OH 45242
Presorted Standard
Postage and Fees Paid
EPA "
Permit No. G-35
Official Business
Penalty for Private Use $300
       EPA Releases Technical Resource for MNA of Inorganics
  The U.S. EPA Office of Research and Development, in cooperation with the
  Office of Superfund Remediation and Technology Innovation and Office of
  Radiation and Indoor Air, recently published a two-volume technical resource
  for selection of MNA as a site-specific remedy  component for inorganic
  contaminants in ground water. Volume  1, Technical Basis for Assessment,
  provides an overview of the technical basis for MNA of inorganic contaminants
  (EPA/600/R-07/139). Volume 2, Assessment for Non-Radionuclides, addresses
  technical aspects of attenuation mechanisms and data collection for arsenic,
  cadmium, chromium, copper, lead, nickel, nitrate,  perchlorate, and selenium
  (EPA/600/R-07/140).

  Together, the documents describe a tiered analysis applicable to MNA site
  screening through an iterative collection of site-specific data that progressively
  reduces MNA uncertainty. This analysis helps cleanup managers develop detailed
  information about site hydrogeology, mechanisms and rates of contaminant
  attenuation, aquifer capacity to sustain attenuation of contaminant mass, and
  long-term stability of immobilized contaminants.  The documents also describe
  methods for  determining attenuation mechanisms by measuring key ground-
  water chemical and physical parameters  (including reduction/oxidation
  characteristics), identifying chemical speciation  of  contaminants and key
  reactants in ground water, and evaluating reactions  between contaminants and
  solid components within the aquifer.  Both volumes of Monitored Natural
  Attenuation of Inorganic Contaminants in Ground  Water may be downloaded
  on CLU-IN at http://www.cluin.org.
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