Microorganisms
Associated with Private Wells with High Levels of Arsenic
Located in
Northport
,
Maine
Student Presenter
Jennifer M Weldon,
University
of
Maine
Dr. Jean D. MacRae,
University
of
Maine
Background
versus Risk-Based Cleanup Goals - An Examination of
Arsenic Background Concentrations in Seven States
Kelly A.S. Vosnakis, M.S., ENSR,
Westford
,
MA
Karen Madsen, M.A., M.S., ENSR,
Westford
,
MA
Lisa J.N. Bradley, Ph.D., DABT, ENSR,
Westford
,
MA
Arsenic
in Historic Fill Soils, Consideration of the Occurrence
and Impact of the Natural and Anthropogenic Components.
William R. Swanson, CDM Inc.,
Cambridge
,
MA
Variation
of Total Arsenic in Playground Soil as a Function of
Distance from CCA-Treated Wooden Structures
Cielito DeRamos King,
PhD
Bridgewater
State
College,
Bridgewater
,
MA
Microorganisms
Associated with Private Wells with High Levels of Arsenic
Located in
Northport
,
Maine
Student Presenter
Jennifer
M Weldon, University of Maine, 5711 Boardman Hall
Room 101, Orono, ME 04469-5711, USA, Tel:
207-581-3401, Fax:
207-581-3888, Email:
Jennifer.Stowe@umit.maine.edu
Dr. Jean
D. MacRae, University of Maine, 5711 Boardman Hall
Room 101, Orono, ME 04469-5711, USA, Tel:
207-581-2137, Fax:
207-581-3888, Email:
Jean.MacRae@umit.maine.edu
Consumption of arsenic laden drinking water can cause a
variety of health effects. In
Maine
, approximately 40% of residents obtain their drinking
water from private wells, many of which contain arsenic in
excess of the 10ppb EPA limit. As a result thousands of
residents may unknowingly consume arsenic laden water.
For arsenic to occur in groundwater it must be present in
aquifer materials and conditions must be favorable for its
release. Many microorganisms accelerate natural weathering
processes or alter arsenic speciation. Some microorganisms
can reduce arsenate, As (V), to the more toxic and mobile
form arsenite, As (III).
Others can alter the iron oxyhydroxides that bind
arsenic to surfaces, causing the arsenic to be released.
As the redox potential of the groundwater decreases,
microbial activities that can increase total arsenic and
arsenite concentrations are favored.
The microbial populations in groundwater samples from four
wells of varying arsenic concentrations from a single
aquifer in
Northport
,
ME
were identified using molecular biology techniques.
Based on Ribosomal Intergenetic Spacer Analysis (RISA)
it appears that the microbial populations in the recharge
region of the aquifer are similar to one another and
different from the discharge wells.
Also, populations from the two wells in the
discharge region of the aquifer appear to be quite
different from each other.
Organisms from the samples were identified using cloning
and it appears that wells in the recharge region contain a
greater proportion of bacteria from Gamma Proteobacteria
and Eubacteria divisions.
Only the discharge region wells contained organisms
from the Delta Proteobacteria division.
The populations from the wells in the discharge
region differed in that one contained a greater proportion
of organisms from the Beta Proteobacteria division and the
other from the Alpha Proteobacteria division.
Additional studies are being conducted to analyze
for temporal variations in the microbial communities.
Background
versus Risk-Based Cleanup Goals - An Examination of
Arsenic Background Concentrations in Seven States
Kelly A.S. Vosnakis, M.S., ENSR, 11 Phelp's Way, P.O.
BOX 506
,
Willington
,
CT
,
06279-0506
,
USA
, Tel: 860-429-5323 x 226, Fax: 860-429-5378, Email:
kvosnakis@ensr.aecom.com
Elizabeth Perry, M.S., PG, ENSR,
2 Technology Park Drive,
Westford
,
MA
01886
,
USA
, Tel: 978-589-3167, Fax: 978-589-3100, Email: eperry@ensr.aecom.com
Karen Madsen, M.A., M.S., ENSR,
2 Technology Park Drive,
Westford
,
MA
01886
,
USA
, Tel: 978-589-3427, Fax: 978-589-3100, Email:
kmadsen@ensr.aecom.com
Lisa J.N. Bradley, Ph.D., DABT, ENSR,
2 Technology Park Drive,
Westford
,
MA
01886
,
USA
, Tel: 978-589-3059, Fax: 978-589-3100, Email: lbradley@ensr.aecom.com
Arsenic is often present in
soils naturally or from historical anthropogenic
activities. Arsenic
is commonly a constituent of potential concern at
environmental remediation sites, even where there is no
reason to suspect a release. Site risks are frequently
driven by arsenic, and risk-based cleanup goals below
background are not uncommon.
However, determining whether arsenic concentrations
are consistent with background requires an extensive
background data set. Consequently,
many sites undergo characterization and potentially
remediation for arsenic concentrations in soil that may in
reality be representative of background (natural or
anthropogenic). This
study examines a large soil arsenic background data set to
provide insight on typical concentrations of arsenic that
are naturally occurring or represent anthropogenic
background.
Between 1995 and 2001, over
1600 background soil samples were collected from 189 sites
in Kentucky, Maryland, New York, Ohio, Pennsylvania,
Virginia, and West Virginia.
Samples were collected using strict Quality
Assurance/Quality Control procedures under a USEPA
Superfund Administrative Order on Consent (AOC) and were
analyzed by USEPA-approved laboratories.
All data were verified and 10% underwent detailed
data validation. Arsenic
concentrations ranged from 1.1 mg/kg to 89 mg/kg.
Data are considered by state and geologic province
and are compared to USEPA and state risk-based cleanup
goals. Some standard Background Threshold Values (BTVs)
are derived for each state and distinct geologic province.
The BTVs are greater than risk-based cleanup goals.
This extensive, regional data set should be
considered by all stakeholders involved in relevant
risk-based decisions related to arsenic in soils.
The consideration of this data set and the BTVs may
aid in the appropriate identification of arsenic in soils
above typical background concentrations, and in turn, aid
in identifying where risks are truly elevated relative to
background, and thus where remediation may or may not be
appropriate.
Arsenic
in Historic Fill Soils, Consideration of the Occurrence
and Impact of the Natural and Anthropogenic Components.
William R. Swanson, CDM Inc.,
50 Hampshire Street
,
Cambridge
,
MA
02139
, Tel: 617-452-6274, Email: swansonwr@cdm.com
Arsenic in concentrations normal to urban fill soil or
historic fill may present a potential significant risk to
persons who live proximate to as well as may grow
vegetables for consumption. This is because there is a key
component of arsenic in some natural soils and this may be
further added to by human activity over decades or
centuries. Finally, arsenic, along with lead and
benzo(a)pyrene, dominate the human health risk associated
with urban fill soil generally contributing in excess of
85% of the risk.
The objective of this paper is to critically examine
arsenic data for natural soil and historic fill soils in
Massachusetts
, based largely on major urban construction projects, for
the concentrations of arsenic present. To that end a data
base of over 5,000 Central Artery/Tunnel soil samples was
well as data bases consisting of hundreds of other soil
samples will be considered leading to practical answers as
follows:
Determine if the detected
arsenic of natural origin by understanding the occurrence
of arsenic in natural soils and how to recognize if the
distribution of concentrations is evident of natural
conditions.
Provide statistics for
concentrations of anthropogenic arsenic in historic fill
and detail how to recognize background levels versus
distinct sites of release.
What
is the human health risk significance/ what levels
constitute potential significant risk for a variety of
scenarios.
How significant is the
impact of arsenic in urban fill/ historic fill relative to
the other key constituents, lead and benzo(a)pyrene?
The presentation will provide persons with a succinct, yet
comprehensive overview of the topic as well as a handy
tool box for use on sites in which they may have an
interest.
Variation
of Total Arsenic in Playground Soil as a Function of
Distance from CCA-Treated Wooden Structures
Cielito
DeRamos King,
PhD Analytical Chemistry, Department of Chemistry, 24
Park Ave, Bridgewater State College, Bridgewater, MA
02325, Tel: 508-531-2115, Fax: 508-531-1785, Email:
c2king@bridgew.edu
The Rainbow’s
End playground in
Bridgewater
,
Massachusetts
was built in the early 1990s with wooden play structures
treated with chromated copper arsenate (CCA). The EPA
banned the use of pressure-treated wood containing CCA for
residential applications on December 31, 2003. However,
studies showed that existing CCA structures pose a risk of
arsenic exposure especially to small children from
hand-to-mouth contact with CCA structures and accidental
ingestion of contaminated soil. Our earlier investigation
of the study site showed that 33 % of more than 100
subsurface soil samples collected at random have arsenic
levels above the Massachusetts DEP’s action level of 30
mg/kg. The goal of this study is to extend our earlier
investigation and determine the extent of arsenic
contamination as a function of distance from the base of
CCA-treated wooden structures. A total of 105 test and 13
control soil samples were collected in early fall of 2007.
The test
samples were collected approximately 5, 15 and 30 cm from
the base of a wooden fence and two picnic tables, with
additional samples taken underneath the picnic tables.
After sieving and oven-drying at 40 0C,
the soil samples
were analyzed for total arsenic using a Perkin-Elmer
AAnalyst600 graphite furnace atomic absorption
spectrometer following EPA method 3050B.
For the 24 x 75 ft2 wooden fence, mean
total arsenic in mg/kg dry mass were 99.3 ± 47.0, 52.9 ±
36.0 and 23.3 ± 24.5 within 5, 15 and 30 cm,
respectively, from the base of the fence. For the picnic
tables, all but one sample collected underneath the
structure showed more than twice the action level for
arsenic, while levels drop significantly even within 5 cm
from the base of the structure. In comparison, the mean
arsenic concentration of control samples was 4.61 ± 2.60
mg/kg.
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