United States
                 Environmental Protection
                 Agency
   Engineering  Issue
           Biotransformation of Dimethylarsinic Acid
             Table Contents

1.0 PURPOSE                         1

2.0 INTRODUCTION                     1

3.0 BACKGROUND                     2

   3.1 Chemical Properties               2

   3.2 Toxicity                        3

4.0 BIOTRANSFORMATION OF DMA(V)       4

   4.1 Microbial Arsenic Tolerance          6

   4.2 Biotransformation of DMA(V) and Related
     Arsenic-Containing Compounds       6

       4.2.1 Studies in Aerobic
           Biotransformation           7

       4.2.2 Studies in Anaerobic
           Biotransformation           7

5.0 FATE AND TRANSPORT IN
   THE ENVIRONMENT                 10

6.0 SUMMARY                       10

7.0 ACKNOWLEDGEMENTS              10

9.0 REFERENCES                     11

ACRONYMS AND ABBREVIATIONS          13
Disclaimer: The U.S. Environmental Protection Agency, through its Office
of Research and Development, funded and managed the literature review
on the state of the science described herein. It has been subjected to the
Agency's peer and administrative review. Any opinions expressed in this
report are those of the author(s) and do not necessarily reflect the views of the
Agency, therefore, no official endorsement should be inferred. Any mention
of trade names or commercial products does not constitute endorsement or
recommendation for use.
1.0 PURPOSE
The U.S. Environmental Protection Agency (EPA) Engineering Issue
Papers (EIPs) are a series of documents that summarize the available
information on specific  contaminants, selected  treatment and  site
remediation technologies, and related issues. This EIP is intended to
provide remedial  project  managers (RPMs),  on-scene coordinators
(OSCs), contractors, and other state or private remediation managers
with an overview regarding the biotransformation of dimethylarsinic
acid (DMA[V]).  The (V) suffix in DMA(V) denotes the +5 oxidation
state of arsenic.

This  EIP   summarizes the  state  of  the  science regarding  the
biotransformation of DMA(V) and was developed from peer-reviewed
literature, scientific documents, EPA reports, internet sources, input
from  experts in  the field, and other pertinent  sources.  This EIP
includes a review of the current understanding of biologically-mediated
transformation of DMA(V) and its metabolites. Given the challenges
remaining in transitioning from laboratory studies to field applications,
this  EIP provides  summary guidance for implementing currently
recommended remediation strategies for DMA(V) at  contaminated
sites.

The table of contents shows the type of information covered in this EIP.
Important information has been summarized, while references and web
site links are provided for readers interested in additional information.
The web site links, verified as accurate at the time of publication, are
subject to change.

2.0 INTRODUCTION
Historically, DMA(V) and  its  salts have been  used  as herbicides
and defoliants and became one of the most popular herbicides used
worldwide in terms  of volume [1-3]. It is estimated that during the
1970s and 1980s,  10 to 12 million acres were treated annually with 2.1
million kilograms (kg) of monomethylarsonic acid (MMA[V]) and
DMA(V) in the U.S. [4]. At present, large amounts of organic arsenical
herbicides are used  for agricultural and aesthetic reasons (e.g., golf
course maintenance) [5, 6].  DMA is also one of the primary sources
of arsenic in orchards, and is likely a source of arsenic  in apples and
juice that the public became keenly aware of in 2011. In 2011, it was
estimated that 100,000 pounds of DMA(V) were commercially used
in the U.S. in over 150 products [5].  However, EPA banned the use of
organic arsenicals (including DMA[V]) after December 31, 2013.

-------
A mixture of DMA(V) and sodium cacodylate was applied
to crops during the Vietnam  conflict.  This  herbicidal
mixture was named 'Agent Blue . Between 1962 and 1971,
an estimated 1.2 million gallons of varying concentrations
of Agent Blue were released under the herbicide program
known  as "Operation  Trail Dust"  [3].   Information
available regarding this program indicates that Agent Blue
was applied to crops  using low-flying aircraft equipped
with sprayers.  The intention of this herbicide application
program was to reduce crop growth through desiccation.

In addition to anthropogenic sources  of DMA(V),  it
is likely that  biotransformation  processes within  the
environmental  arsenic cycle  are  significant sources of
organic arsenicals [5]. For example, phytoplankton  have
been observed to methylate arsenate  to MMA(V)  and
DMA(V) within marine  environments [7]. Within the
arsenic biogeochemical cycle, it is important to note  that
pentavalent organoarsenicals are less toxic than inorganic
arsenates, whereas  trivalent  inorganic  arsenic species
are generally both more toxic and more mobile in the
environment than pentavalent inorganic arsenic species.
Thus,  understanding the  potential biotransformation
pathways of organoarsenicals within the environment as
well as  the fate, transport,  and risk associated with the
various arsenic species  will help to guide remediation
strategies for DMA(V).  This EIP discusses the following
in sections below:

    1. Chemical properties and toxicity;
   2. Biological transformation processes, and;
   3. Fate of these compounds in the environment.
3.0 BACKGROUND
3.1 Chemical Properties
DMA(V) is comprised of a single arsenic atom connected
by three single covalent bonds (two methyl groups and
one hydroxyl group) and a double bond to oxygen (see
Figure 1). This results in a +5 oxidation state for arsenic.

DMA(V)  is  an  amphoteric  compound  (exhibiting
properties  of both an acid and  base)  with  an acid
dissociation constant (pKa) value of 6.4. DMA(V) exists
in a white crystalline solid form with a melting point of
195°C.  Its water solubility is 2,000 g/L at 25°C [8]. The
soil organic carbon-water partitioning  coefficient (Koc)
for DMA(V) is reported to be 43.89 L/kg [9].
                    H3C
                  H3C	As =
                      /
                    HO
Figure 1. Chemical structure of DMA(V)
There are a relatively small number of related organic and
inorganic arsenic compounds which have been identified
as the main chemical species involved in the transformation
of DMA(V) (see Table 1).  The compounds in Table 1
contain arsenic in either the +3 or +5 valence state.  These
compounds include inorganic forms (As[III] and As[V])
as well as mono-  and di-methyl  species (MMA[III],
MMA[V], DMA[III] and  DMA[V]), and  one  relatively
non-toxic and volatile trimethyl species (TMAO).  These
compounds have been chosen for further discussion as
they represent the  main products of transformations of
DMA(V) in the natural environment.  They have been
detected and  quantified in laboratory studies relating to
the amount and rate of biotransformation of DMA(V).
                                             Engineering Issue: Biotransformation of Dimethylarsinic Acid

-------
Table 1. Chemical Properties of Select Inorganic and Organic Arsenic Compounds
Compound
Arsenite (As[lll])

Arsenate (As[V])

Monomethylarsonous acid (MMA[III])

Monomethylarsonic acid (MMA[V])

Dimethylarsinous acid (DMA[III])

Dimethylarsinic acid (DMA[V])



Molecular Formula
As033

As043

As(CH3)(OH)2

AstCH^OHJjO

As(CH3)2(OH)

As(CHJ2(OH)0

hc./ru \ n
AS(OH3)3U
Arsenic
Oxidation State
3+

5+

3+

5+

3+

5+

5+

Chemical Structure
(fully protonated forms)
\
OAc

\
/
\
1 \C\ A r
HO
\
HO
\
Hf~ A r
/
Ho
\
/
HO
\
H3C
3.2 Toxicity
Overall, DMA(V) and other pentavalent organoarsenicals
are less toxic than inorganic arsenic. All trivalent forms of
arsenic species (both inorganic and organic) are generally
both more mobile and more toxic to humans than the
pentavalent forms of arsenic compounds (organic and
inorganic). This is apparent in both the minimum risk level
(MRL) values derived by the Agency for Toxic Substances
and Disease Registry [8] and from EPA regional screening
levels (RSLs) for soil and tap water. The MRL is an estimate
of the daily human exposure to a hazardous substance that
is likely to be without appreciable risk of adverse, non-
cancer health effects over a specified duration of exposure.
Table 2 summarizes available MRLs and RSLs for inorganic
arsenic and organic arsenic (V) species discussed in this
paper.
Biotransformation of Dimethylarsinic Acid:  Engineering Issue

-------
Table 2.  Summary of MRL and RSL Values for Inorganic Arsenic and Organoarsenicals

MRL, acute duration (14 days or less) oral
exposure [8]
MRL, intermediate duration (15 to 364
days) oral exposure [8]
MRL, chronic duration (365 days or more)
oral exposure [8]
Residential Soil RSL [9]
Tapwater RSL [9]
Inorganic Arsenic
0.005 mg As/kg/day
NE
0.0003 mg As/kg/day
0.39 mg/kg
0.045 |jg/L
MMA(V)
NE
0.1 mg MMA/kg/day
0.1 mg MMA/kg/day
610 mg/kg
160|jg/L
DMA(V)
NE
NE
0.2 mg DMA/kg/day
1,200 mg/kg
3,100 |jg/L
NE - Not established

4.0  BIOTRANSFORMATION OF DMA(V)
The  term  "biotransformation"  refers  to  biologically-
mediated reactions which change the composition and/
or distribution of contaminants  in the environment.
"Bioremediation"  is  a  process  where  microorganisms
biotransform hazardous contaminants to other comp ounds
that are intended to  be  less hazardous than the parent
material. Therefore, the term "biotransformation" should
not be interpreted as a synonym for "bioremediation".
Understanding biotransformation processes for DMA(V)
will help to inform the optimum operating conditions for
potential application in remediation efforts.

As  presented  in  Table 3  and  Figure  2,  the  four
biotransformation reactions associated with arsenic are:

   1.  Methylation.  The process in which  a  compound
      gains a methyl group. For example, methylation
      of the organic compound MMA(V) to the organic
      compound DMA(V).
   2.  Demethylation. The process in which a compound
      loses a methyl group.  For example, demethylation
      of the organic compound MMA(V) to the inorganic
      compound As(V).
   3.  Oxidation. The process in which the valence state of
      the compound is increased. For example, oxidation
      of the organic compound MMA(III) to the organic
      compound MMA(V) increases the valence state of
      arsenic from +3 to  +5.
   4.  Reduction. The process in which the valence state of
      the compound is decreased. For example, reduction
      of the inorganic compound As(V) to the inorganic
      compound As(III)  decreases the valence state from
      +5 to +3.
Organic and inorganic arsenic compounds can undergo
any  of  these  four  reactions based  on environmental
conditions. In general, methylation and demethylation of
arsenic are facilitated by microorganisms via enzymatic
processes  [7,  10].  As illustrated in Figure 2, DMA(V)
can be demethylated to MMA(V), which can be further
demethylated to inorganic As(V) biotically  Conversely,
inorganic  As(V) has  been  shown to  be  biotically
methylated to MMA(V) and DMA(V).   While arsines
can be formed from As(V) compounds, the contribution
of this mechanism to the fate of DMA(V) is minimal and
therefore will not be described in detail in this paper [10].
Oxidation and reduction reactions may occur abiotically
when  environmental  conditions  change,   such  as
photochemical oxidation of reduced arsenic compounds.
However, oxidation and reduction processes can be a result
of biotic processes. As shown in Figure 2, microorganisms
have been observed to reduce As(V) to As(III) as well as
oxidize As(III) to As(V) [7]. As shown in Table 2, As(V)
species (organic and inorganic) are less toxic than As(III)
species  (organic and inorganic).  The  general toxicity
trend by species increases  in the TMAO(V) < DMA(V)
< MMA (V)<  [As(V),  As(III)]  < MMA(III) [10].  Given
the wide  variety of potential reactions in the arsenic
biogeochemical cycle, the following sections focus on the
role  that microorganisms play with respect to DMA(V)
biotransformation processes.
                                            Engineering Issue: Biotransformation of Dimethylarsinic Acid

-------
               Table 3. Summary of the Potential Biotransformation Reactions for DMA(V) and Related Compounds
               with Respect to Relative Toxicity
Reactant
DMA(V)
DMA(V)
DMA(V)
MMA(V)
MMA(V)
MMA(V)
MMA(V)
MMA(V)
Inorganic As(V)
Inorganic As(V)
Inorganic As (V)
Inorganic As (V)
Inorganic As (III)
Inorganic As (III)
MMA(III)
MMA(III)
MMA(III)
TMAO(V)
Transformation Reaction
Demethylation
Demethylation
Reduction
Demethylation
Methylation
Methylation
Reduction
Reduction
Methylation
Methylation
Reduction
Reduction
Methylation
Oxidation
Demethylation
Oxidation
Oxidization
Reduction
Product
MMA(V)
Inorganic As (V)
Arsines
Inorganic As (V)
TMAO(V)
DMA(V)
Arsines
MMA(III)
MMA(V)
DMA(V)
Arsines
Inorganic As (III)
MMA(III)
Inorganic As (V)
Inorganic As (III)
MMA(V)
TMAO(V)
MMA(III)
Relative Toxicity
More Toxic
More Toxic
More Toxic
More Toxic
Less Toxic
Less Toxic
More Toxic
More Toxic
Less Toxic
Less Toxic
More Toxic
More Toxic
More Toxic
Less Toxic
Less Toxic
Less Toxic
Less Toxic
More Toxic
Biotransformation of Dimethylarsinic Acid: Engineering Issue

-------
            Demethylated
             As(V)
                -»-MMA(V)-«—    —*- |>\1A(V)
                                                                       Methylated
                                                                                   I M V I, •. .
                                                                     0ne-WtyAr$#iig (As) Ttanslocmation

                                                                     Two-Wajf As TransJocmaflion
.vim i.
Higher Toxicity
                                                       ne. (111)
Figure 2. Overview of Biological Transformation Processes of Organic and Inorganic Arsenic Compounds
4.1 Microbial Arsenic Tolerance
Biotransformation processes can  only  occur if active
biological species capable of transforming DMA(V) and
related compounds thrive within the environment.  For
example, microbial arsenic-tolerant species have  been
isolated from gold and antimony mines  [11, 12], highly-
contaminated soils and sediments [13-16], and golf course
greens [6, 17].   In general,  it is unusual for organisms
to be arsenic-tolerant as arsenic is generally used as an
antimicrobial agent.  These  microorganisms  are either
tolerant of arsenic uptake or have developed the ability to
detoxify arsenic.  One detoxification mechanism uses an
arsenic-resistance operon (denoted 'ars') that facilitates
biological transformation [18, 19].  Tolerance to arsenic-
containing compounds is highly species-, environment-,
and compound-specific [20,  21]. For example, reported
arsenic  tolerance for  Stenotrophomonas  maltophilia
ranged over two orders of magnitude [11].  Additionally,
phytoplankton  are thought to accumulate inorganic
                                          arsenic species and generate organoarsenic compounds
                                          as a detoxification mechanism [22, 23]. Regardless of the
                                          detoxification mechanism, microbial action contributes
                                          to  the  arsenic biogeochemical cycle  and can  include
                                          methylated, demethylated, oxidized or reduced forms of
                                          arsenic.

                                          4.2 Biotransformation of DMA(V) and Related
                                          Arsenic-Containing Compounds
                                          Tables 4 and 5 present key aspects of research conducted
                                          over the past 40 years under controlled conditions to study
                                          methylation, demethylation, oxidation and reduction. The
                                          tables include, to a lesser extent, oxidation and reduction
                                          of organoarsenic compounds related to  DMA(V).  The
                                          studies reviewed here have  been separated  into those
                                          conducted under aerobic (or oxic) conditions (Table 4) and
                                          those conducted under anaerobic (or anoxic) conditions
                                          (Table 5).   The following discussion will provide  insight
                                             Engineering Issue:  Biotransformation of Dimethylarsinic Acid

-------
into the research work conducted in understanding the
complexity of biotransformation of DMA(V) and related
organoarsenicals.

4.2.7 Studies in Aerobic Biotransformation

Research  conducted   in  aerobic  environments  has
studied the ability of indigenous  microorganisms from
contaminated soils, sediments and aqueous environments
to  transform  organoarsenicals.    Overall,  DMA(V)
biotransforms to MMA(V), inorganic As(V), and arsines
over time in  the environment with  inorganic As(V) as
the predominant end product. The  reverse pathways of
methlyation of inorganic As(V) to MMA(V) and DMA(V)
are also possible; however, anaerobic methlyation of As(V)
appears more prevalent in the environment  [10].

In an early study by Von Endt et al. [24], demethylation rates
were observed to be much higher in pure cultures than in
soils as would be expected. In later studies, three similar
soil types were used to evaluate  DMA(V) degradation
and three metabolites were identified: As(V), MMA(V),
and arsines [25, 26]. Although the organisms responsible
for  DMA(V)  transformation  were  not specifically
identified, a large  consortium of microorganisms was
assumed responsible for the biotransformation. Specific
organisms responsible for the biotransformation of these
compounds were  not identified  until recently when
advanced microbiological techniques  were employed [10].
Additionally, impacts  of amendments such as manure,
hay or sewage sludge were  investigated  on  DMA(V)
biotransformation  [26].   Although no   difference in
transformation rate was observed between  amendments,
DMA(V) was degraded more rapidly  in unamended soils.
This difference is assumed to  be due to reduced DMA(V)
bioavailability through adsorption to amended organic
matter.   More  recent studies used  low concentrations
of DMA(V) as  the reactant  organic  arsenic compound.
Huang et al. [27] studied the demethylation and reduction
of 755 to 1,035 parts per billion concentrations of DMA(V)
in soils collected from Germany.   In  contrast to Gao
and Burau shown in Table 4  [28],  Huang et al. observed
the sequential formation of MMA(V)  before complete
demethylation to inorganic forms of arsenic.

With respect to other organoarsenicals, MMA(V) was the
subject of two studies in both soil and pure culture [29,30].
In soil, parts per million concentrations of MMA(V) were
demethylated to As(V). Separate pure cultures of bacteria
(Mycobacterium neoaurum and Scopulariopsis koningii)
as well as three fungi (Fomitopsis pinicola, Puccinia gladioli
and  Scopulariopsis brevicaulis)  methylated  MMA(V)
finally to TMAO.  These organisms were also found to
oxidize and methylate MMA(III) to TMAO.  Therefore,
the dynamic nature of the arsenic biogeochemical cycle
should be recognized when investigating a contaminated
site such that analyzing  for specific arsenic compounds
and oxidation states is recommended.

4.2.2 Studies in Anaerobic Biotransformation

As with aerobic studies, research conducted in anaerobic
environments   evaluated  the  ability  of  indigenous
microorganisms to transform organoarsenicals. Overall,
the entire range of potential biotransformation pathways
(see Figure 2) can be observed under anaerobic conditions.
Demethylation of DMA(V) as well as methylation of As(V)
can  occur under the appropriate  conditions.   Anoxic
contaminated sites with arsenic contamination should be
monitored for all As(III) and As(V) species to understand
the distribution of arsenic compounds.

Demethylation of DMA(V) can produce in MMA(V) and
inorganic As(V).   Woolson and Kearney [25]  repeated
their  earlier aerobic experiments  on three soils under
anoxic conditions.   As  with the  aerobic conditions,
DMA(V) was  converted  to inorganic  As(V) as well as
arsines,  however DMA(V) transformations were not as
efficient under anaerobic conditions.  Furthermore, As(V)
reduction to As(III) has been observed by iron-reducing,
sulfate-reducing, and fermenting  populations  as  well
as methanogens [10]. This indicates that reduction to
the more toxic  trivalent  forms is a possibility.  Another
potential pathway for As(III) formation  includes the
reduction of MMA(V) to MMA(III) as an intermediate
compound before producing inorganic As(III).

Studies  have  also been completed to determine the
anaerobic transformation of MMA(V)  [2,  5, 15, 29] and
inorganic forms of arsenic [31,32]. In the case of MMA(V),
transformation products include either inorganic arsenic
or volatile arsines.  Yoshinaga et  al. [5] identified two
specific  bacteria that were necessary and  sufficient for
transformation  of  MMA(V) to As(III).  Reduction of
MMA(V) to  MMA(III)  by Burkholderia species was
first required  before demethylation of  MMA(III) to
As(III) by Streptomyces  species. This indicates that full
transformation  of some  organoarsenic compounds may
not be accomplished by the same organism, but rather
as sequential steps of methylation/demethylation and
oxidation/reduction.
 Biotransformation of Dimethylarsinic Acid:  Engineering Issue

-------
00  Table 4. Summary of Selected Biotransformation Studies of DMA(V) and Related Compounds in Aerobic Environments
Initial Arsenic
Species
DMA(V)
MMA(V)
MMA(III)
Biotransformation
Demethylation
Demethylation/
Arsine
Demethylation/
Reduction
Demethylation
Methylation
Methylation
Transformation
Pathway
(see Figure 2)
DMA(V)^As(V)
DMA(V)^As(V),Ars
DMA(V) -> MMA(V) ->
iAs
MMA(V)^As(V)
MMA(V) -> TMAO
MMA(III) -> TMAO
Microorganism
Fungus, Actinomycete,
Bacterium
Consortium
Consortium
Consortium
Consortium
Consortium
Consortium
Consortium
Mycobacterium neoaurum,
Scopulariopsis koningii, F.
pinicola, P. gladioli,
S. brevicaulis
Mycobacterium neoaurum,
Scopulariopsis koningii, F.
pinicola, P. gladioli,
S. brevicaulis
Initial
Concentration
10 ppm
10 ppm, 100 ppm
10ppb
184 ppm
1 ppm, 10 ppm,
100 ppm
1545 ppm
755 ppb, 1035 ppb
3.7 ppm, 9.2 ppm
920 ppb
930 ppb
Temperature
30 °C
28-30 °C
20 °C
5°C,25°C
25 °C
25 °C
5°C
15°C,30°C
21 °C
21 °C
Percent
transformed/
3-20%/11 d
1.7-10%/60d
37%/24h
5-90%/70 d
76%/168d
25%/91d
80%/100d
72%/120d
3-1 7% / 28 d
8-38% / 28 d
Media
Pure Culture
Soil
Mixed
Culture
Soil
Soil
Mixed
Culture
Soil
Soil
Pure Culture
Pure Culture
Reference
[24]
[24]
[33]
[28]
[25]
[34]
[27]
[29]
[30]
[30]
    DMAr(lll) = dimethylarsine
    Ars = volatile arsine compounds (arsine, methylarsine, dimethylarsine, trimethylarsine)
    iAs = inorganic arsenic
    100% removal indicates final concentration was nondetect for the method employed

-------
Table 5. Summary of Selected Biotransformation Studies of DMA(V) and Related Compounds in Anaerobic Environments
Initial Arsenic
Species
DMA(V)
MMA(V)
As(V)
As(V)
Biotransformation
Demethylation/
Reduction
Demethylation
Demethylation/
Methylation
Demethylation/
Reduction
Demethylation/
Reduction
Demethylation/ Meth-
ylation
Reduction
Reduction/ Methyla-
tion/Oxidation
Methylation
Transformation
Pathway
(see Figure 2)
DMA(V) -> iAs
DMA(V) -> MMA(V) ->
iAs
DMA(V) -> MMA(V) ->
iAs
DMA(V) -> MMA(V)
DMA(V) -> iAs and Ars
DMA(V) -+ MMA(V),
As(V) and Ars
DMA(V)^Ars
MMA(V) -+ MMA(III) -+
As(lll)
MMA(V) -+ MMA(III) -+
As(lll)
MMA(V) -+ iAs
MMA(V)^As(V)and
Ars
MMA(V) -+ MMA(III)
As(V)^As(lll)^
MMA(V) -+ DMA(V) -+
Ars
As(V)^Ars
Microorganism
Phytoplankton
Consortium
Consortium
Consortium
Consortium
Consortium
Consortium
Streptomyces sp.,
Burkholderia sp.
Pseudomonas putida
strain KT2240, Burkhold-
eria sp. MR1
9 separate isolates of
As-resistant bacteria
Consortium
Consortium
Methanobacterium strain
M.o.H
Desulfovibrio vulgaris
strain 8303
Initial
Concentration
138 ppb
1545 ppm
755 ppb, 1035 ppb
138 ppm
21 .4 ppm
10 ppm
1 ppm, 10 ppm, 100
ppm
140 ppb
140 ppb
140 ppb
3.7 ppm, 9.2 ppm
400 ppm, 2000 ppm
75 ppb
75 ppb
Temperature
4-30 °C
25 °C
5°C
30 °C
Ambient
Ambient
25 °C
Ambient
Ambient
20 °C
15°C,30°C
30 °C
Ambient
Ambient
Percent trans-
formed/time
100%/21d
10%/91d
66%/100d
75-95%/217d
85-89%/59 d
60%/60d
61%/168d
100%/7d
100%/7d
5-100%/14d
100%/120d
24-49%/240d
Not quantified
Not quantified
Media
Aqueous
Mixed
Culture
Soil
Sludge
Soil
Soil
Soil
Soil Ex-
tracts
Soil Ex-
tracts
Pure
Culture
Soil
Sludge
Pure
Culture
Pure
Culture
Reference
[14]
[34]
[27]
[2]
[35]
[26]
[25]
[5]
[5]
[15]
[29]
[2]
[31]
[31]
Ars = volatile arsine compounds (arsine, methylarsine, dimethylarsine, trimethylarsine)



iAs = inorganic arsenic



100% removal indicates final concentration was nondetect for the method employed

-------
5.0 FATE AND TRANSPORT IN THE ENVIRONMENT
The fate of DMA(V) in the environment is difficult to assess
in detail because of the number of interrelated abiotic and
biological processes  that occur  simultaneously.  Phase
transfer, advective, and diffusive transport, methylation,
demethylation, oxidation and reduction are examples of
these.

While highly soluble in water, both DM A( V) and MM A( V)
have high sorption capacities (MMA > DMA) in soil and
sediment systems.  Organoarsenic as well as inorganic
arsenic sorption is dependent on clay and mineral content
(i.e., ferrihydrite and alumina) of the soil, as well as pH of
the system. For example, DMA(V) [36] and MMA(V) [6]
adsorption increased as iron oxide and alumina content
increased.  Overall, inorganic As(V) species  are found
in oxic conditions and can strongly adsorb to soil and
sediment in acidic and neutral  environments, whereas
inorganic  As(III) species are  weakly  retained  by soil
and  sediment, and are mobile in both oxic and  anoxic
environments.  Thus, the potential for desorption and
remobilization of arsenic into the aqueous environment
by reductive transformations of As(V) to As(III) species
should be included in evaluating impacts to site conditions
when considering remedial technologies.
6.0 SUMMARY
Biotransformation of DMA(V) is a significant part of the
arsenic biogeochemical cycle  and can produce a variety
of end products.  Site specific conditions, in particular
the predominant redox  condition,  will direct the most
prevalent forms of arsenic species present.

Under aerobic conditions, DMA(V) is  predominately
demethlyated to inorganic As(V). While inorganic As(V)
is  more toxic  than the organoarsenicals  (DMA[V] and
MMA[V]), this valence  of inorganic As  strongly sorbs
to  iron,  aluminum,  and manganese  oxyhydroxides,
and clay minerals under acidic and  neutral conditions.
Thus, pentavalent species are generally immobile in the
aerobic environment.  Therefore, maintaining an aerobic
environment may aid in reducing transport of arsenic in
the environment.

Under anaerobic conditions, DMA(V) is also demethylated
to  inorganic  arsenic.   Although  the  transformation
pathways   incorporate   a   variety   of  intermediate
compounds, both inorganic As(V)  and As(III)  can  be
produced.   Trivalent arsenic  [As(III)]  species  (both
          organic and inorganic) are generally both more toxic and
          more mobile than pentavalent arsenic species (organic
          and inorganic).   Therefore,  all potential arsenic species
          produced from  biotransformation processes should be
          considered in the remedy selection process when altering
          a site's oxidation/reduction environment and pH.

          These results  indicate that  transitioning  from  aerobic
          to  anaerobic conditions  may increase the toxicity and
          mobility of arsenic in the environment.  As  such, redox
          conditions  play  an  important role during remedial
          alternative evaluation as the  redox conditions impact the
          mobility and toxicity of the arsenic  species.  Therefore,
          understanding the potential  biotransformation pathways
          of organoarsenicals within the environment as well as the
          fate, transport, and risk associated with the various arsenic
          species are important when assessing remedial alternatives
          for sites contaminated with DMA(V).

          Predominant  remediation strategies for  As currently
          include  removal and immobilization [37].  Removal
          consists of excavating the zone identified as contaminated.
          Once removed, contaminated soil may be treated through
          ex-situ means or sent to a hazardous waste landfill. Ex-
          situ arsenic treatment includes (from low to high cost)
          iron seeding for  co-precipitation with aqueous As, soil
          washing with acid extraction, membrane filtration, media
          adsorption, ion exchange, and pyrometallurgical recovery.

          In-situ remediation approaches rely on immobilization of
          arsenic  to reduce the bioavailability  of the contaminant
          and decrease  the associated risk.   Immobilization can
          include  (from  low  to  high  cost)  phytoremediation
          (if  concentrations  are   low), biological   treatment/
          biotransformation, installation of a  permeable reactive
          barrier, soil flushing, amendments for precipitation or co-
          precipitation, solidification and stabilization, electrokinetic
          treatment, and   vitrification.  In-situ amendments  for
          precipitation or co-precipitation include zero valent iron
          (ZVI), titanium  dioxide (TiO2), and ZVI coupled with
          a sulfate compound.  These immobilization methods are
          undergoing evaluation to  ensure that they can serve as
          long term, stable sinks for arsenic despite fluctuations in
          geochemistry.
          7.0  ACKNOWLEDGEMENTS
          This EIP was prepared by the EPA, Office of Research
          and Development, National Risk Management Research
          Laboratory. Dr.  John McKernan served  as  the EPA
          Technical Project Manager.
10
Engineering Issue: Biotransformation of Dimethylarsinic Acid

-------
The following technical experts contributed their time
and expertise by providing review comments:

John Lenhart, Ph.D., The Ohio State University
Heather Rectanus, Ph.D., P.E., Battelle
Ryan Fimmen, Ph.D., Geosyntec Consultants
Kirk Scheckel, Ph.D., EPA
Brian Yates, Battelle

8.0 REFERENCES
1.    Rensing, C; Rosen, B. P., Heavy metal cycles (arsenic,
     mercury, selenium and others). In Encyclopedia of
    Microbiology,  Schaechter, M., Ed. Elsevier: Oxford,
     UK, 2009; pp 205-219.

2.    Sierra-Alvarez, R.; Yenal, U; Field, J.  A.; Kopplin,
     M.; Gandolfi,  A. J.; Garbarino, J.  R., Anaerobic
    biotransformation  of organo-arsenical  pesticides
     monomethylarsonic acid and dimethylarsinic acid.
    Journal of agricultural and food chemistry 2006, 54,
     (11), 3959-66.

3.    Stellman, J. M.; Stellman, S. D.; Christian, R.; Weber,
     T.; Tomasallo, C., The extent and patterns of usage
     of Agent Orange and other herbicides in  Vietnam.
    Nature 2003, 422, (6933), 681-7.

4.    Abernathy,  J. R., Role  of  arsenical  chemicals in
     agriculture.  In  Arsenic;   Industrial,  Biomedical
     and Environmental Perspectives, Lederer,  W. H.;
     Fensterheim,  R.  J.,  Eds. Van Nostrand Reinhold:
     New York, 1983; pp 57-62.

5.    Yoshinaga, M.; Cai, Y; Rosen, B. P., Demethylation
     of methylarsonic acid by a microbial community.
     Environmental microbiology 2011,13, (5), 1205-15.

6.    Pichler,  T.; Brinkmann, R.; Scarzella, G. I., Arsenic
     abundance and variation in golf course lakes. Science
     of The Total Environment 2008, 394, (2-3),  313-320.

7.    Cullen, W. R.; Reimer, K. J., Arsenic speciation in the
     environment.  Chemical Reviews 1989,  89, (4), 713-
     764.

8.    Agency  for Toxic Substances and Disease Registry,
     Toxicological profile for arsenic. In U.S. Department
     of Health and Human Services, Ed. Public Health
     Service,: Atlanta, GA, 2007; Vol. August.
9.   EPA,  Regional  screening  levels  for
    contaminants at superfund sites. 2012.
                                           chemical
10.  Wang,  S.;  Mulligan, C.  N.,  Natural attenuation
    processes for remediation of arsenic contaminated
    soils and groundwater. Journal of hazardous materials
    2006,138, (3), 459-470.

11.  Botes, E.; Van Heerden, E.;  Litthauer, D., Hyper-
    resistance to arsenic in bacteria isolated from an
    antimony mine  in  South Africa. South  African
    Journal of Science 2007,103, 279-281.

12.  Drewniak,  L., Styczek,  A.  and Sklodowska,  A.,
    Arsenic hyper-tolerant bacteria isolated from gold-
    mine rock biofilms. Advanced Material Research
    2007,20-21,576-580.

13.  Cai, L.; Liu, G.; Rensing, C.; Wang, G., Genes involved
    in arsenic transformation and resistance  associated
    with different levels of arsenic-contaminated soils.
    BMC microbiology 2009, 9,4.

14.  Maki, T; Hirota, W; Ueda, K.; Hasegawa, H.; Azizur
    Rahman, M., Seasonal dynamics of biodegradation
    activities for dimethylarsinic acid (DMA)  in Lake
    Kahokugata. Chemosphere 2009, 77, (1), 36-42.

15.  Maki,T.;Takeda,N.;Hasegawa,H.;Ueda,K.,Isolation
    of monomethylarsonic acid-mineralizing bacteria
    from arsenic contaminated soils of Ohkunoshima
    Island. Applied Organometallic  Chemistry 2006, 20,
    (9), 538-544.

16.  Maki,  T; Watarai,  H.; Kakimoto, T.;  Takahashi,
    M.; Hasegawa, H.; Ueda, K.,  Seasonal dynamics of
    dimethylarsenic acid degrading bacteria dominated
    in Lake Kibagata. Geomicrobiology Journal 2006,23,
    (5), 311-318.

17.  Feng, M.; Schrlau, J. E.; Snyder, R.; Snyder, G. H.;
    Chen, M.; Cisar, J. L.; Cai, Y, Arsenic transport and
    transformation associated with MSMA application
    on a golf course green. Journal of agricultural and
    food chemistry 2005, 53, (9), 3556-62.

18.  Liao, V H.; Chu, Y. J.; Su, Y. C.; Hsiao, S. Y; Wei, C.
    C.; Liu, C. W; Liao, C. M.; Shen, W. C.; Chang, F. J.,
    Arsenite-oxidizing and arsenate-reducing bacteria
 Biotransformation of Dimethylarsinic Acid: Engineering Issue
                                                 11

-------
     associated with arsenic-rich groundwater in Taiwan.
     Journal of contaminant hydrology 2011, 123, (1-2),
     20-9.

19.   Paez-Espino,  D.;  Tamames,  J.;  de  Lorenzo,  V.;
     Canovas, D., Microbial responses to environmental
     arsenic.  Biometals  :  an  international journal  on
     the role  of metal ions  in biology,  biochemistry, and
     medicine 2009,22, (1),  117-30.

20.   Bahar, M. M.; Megharaj,  M.; Naidu, R., Arsenic
     bioremediation potential of a new arsenite-oxidizing
     bacterium Stenotrophomonas  sp.  MM-7 isolated
     from soil. Biodegradation 2012,23, (6), 803-12.

21.   Banerjee, S.; Datta, S.; Chattyopadhyay, D.; Sarkar,
     P., Arsenic accumulating and transforming bacteria
     isolated  from contaminated soil  for  potential use
     in bioremediation. Journal of environmental science
     and health. Part A, Toxic/hazardous  substances &
     environmental engineering 2011,46, (14), 1736-47.

22.   Hasegawa, H.; Sohrin, Y.; Seki, K.; Sato, M.; Norisuye,
     K.; Naito, K.; Matsui,  M.,  Biosynthesis and release
     of methylarsenic compounds during the growth of
     freshwater algae. Chemosphere 2001,43, (3), 265-72.

23.   Li, R. Y.; Ago, Y; Liu, W. J.; Mitani, N.; Feldmann, J.;
     McGrath, S. P.; Ma, J. E; Zhao, E J., The rice aquaporin
     Lsil mediates uptake of methylated arsenic species.
     Plant physiology 2009,150,  (4), 2071-80.

24.   Von Endt, D. W.; Kearney, P. C.; Kaufman, D. D.,
     Degradation of MSMA by soil microorganisms.
     Journal of agricultural  and food chemistry  1968, 16,
     (1), 17-20.

25.   Woolson,  E.  A.;  Kearney,  P.  C.,  Persistence
     and  reactions of  [14C]-cacodylic acid  in soils.
     Environmental Science & Technology 1973, 7, (1), 47-
     50.

26.   Woolson,  E. A.;  Aharonson,  N.;  ladevaia,  R.,
     Application   of   the   high-performance   liquid
     chromatography-flameless    atomic    absorption
     method  to  the  study  of alkyl arsenical  herbicide
     metabolism in soil. Journal of agricultural and food
     chemistry 1982, 30, (3), 580-584.

27.   Huang, J.-LL; Scherr, E; Matzner, E., Demethylation
     of dimethylarsinic acid  and arsenobetaine in different
              organic soils. Water Air Soil Pollut 2007, 182, (1-4),
              31-41.

          28.  Gao, S.; Burau, R. G., Environmental factors affecting
              rates of arsine evolution from and mineralization of
              arsenicals in soil. Journal of Environmental Quality
              1997,26, (3), 753-763.

          29.  Akkari, K.  H.;  Frans, R. E.;  Lavy,  T.  L, Factors
              affecting degradation of MSMA in soil. Weed science.
              1986,34, (5), 781-787.

          30.  Lehr, C. R.; Polishchuk, E.; Delisle, M. C.; Franz,
              C.; Cullen,  W. R., Arsenic  methylation by  micro-
              organisms  isolated   from   sheepskin  bedding
              materials. Human & experimental toxicology 2003,
              22, (6), 325-34.

          31.  McBride,  B.  C.;  Wolfe, R.  S.,  Biosynthesis  of
              dimethylarsine by Methanobacterium. Biochemistry
              1971,10, (23), 4312-7.

          32.  Zouboulis, A. L; Katsoyiannis, I. A., Recent advances
              in  the bioremediation   of arsenic-contaminated
              groundwater. Environment  international 2005, 31,
              (2), 213-9.

          33.  Sanders, J. G., Microbial role in the demethylation
              and oxidation of methylated arsenicals in seawater.
              Chemosphere 1979, 8, (3), 135-137.

          34.  Hanaoka,  K. i.; Hasegawa, S.;  Kawabe, N.; Tagawa,
              S.;  Kaise,  T, Aerobic and anaerobic degradation of
              several arsenicals by sedimentary micro-organisms.
              Applied Organometallic Chemistry 1990, 4, (3), 239-
              243.

          35.  Schuth, C. K.; Isensee, A. R.; Woolson, E. A.; Kearney,
              P. C., Distribution of 14C and  arsenic derived from
              (14C)cacodylic acid in an aquatic ecosystem. Journal
              of agricultural and food chemistry 1974, 22, (6), 999-
              1003.

          36.  Wauchope,  R.  D.; Me Dowell, L.  L., Adsorption
              of    phosphate,   arsenate,    methanearsonate,
              and cacodylate  by  lake and stream  sediments:
              comparisons with soils 1. /. Environ. Qual.  1984, 13,
              (3), 499-504.
12
Engineering Issue:  Biotransformation of Dimethylarsinic Acid

-------
ACRONYMS AND ABBREVIATIONS
As(III)    Inorganic/elemental arsenic (arsenite;
          oxidation state +3)

As (V)    Inorganic/elemental arsenic (arsenate;
          oxidation state +5)

DMA(V)  dimethylarsinic acid (oxidation state +5)

EPA      U.S. Environmental Protection Agency

kg        Kilogram

MMA(III) monomethylarsonous acid
          (oxidation state +3)

MMA(V)  monomethylarsonic acid (oxidation state +5)

MRL      minimum risk level

OSC      on-scene coordinator

ppb       parts per billion

ppm      parts per million

RPM      Remedial Project Manager

RSL       regional screening levels

TMAO    trimethylarsine oxide

U.S.       United States
 Biotransformation of Dimethylarsinic Acid: Engineering Issue
13

-------
United States
Environmental Protection
Agency
Office of Research and Development
National Risk Management
   Research Laboratory
Cincinnati, OH 45268
Official Business
Penalty for Private Use
$300
EPA/600/R-14/219
December 2014
www.epa.gov
PRESORTED STANDARD
 POSTAGE & FEES PAID
        EPA
   PERMIT NO. G-35

-------