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Arsenic
Risk to Residents – An Understanding for Spring Valley,
DC
Steven
H. Lamm, MD Consultants
in Epidemiology and Occupational Health, Inc., Washington,
DC, Tel: 202-333-2364
Background:
Spring Valley in Washington, DC was the site for
ordinance development and testing for the US Army before
and during World War I.
Subsequently, both American University and a
high-end residential area have developed there.
Both arsenic has now been found at levels of 20-400
ppm, and community members are anxious.
Methods
and Materials: A
review of the world’s literature on arsenic and adverse
human health effects has been undertaken.
The results have been separated out by disease of
concern – organ pathology, cancers, and reproductive
risk. Information
has been presented with respect to arsenic exposure levels
for which adverse effects are known.
These dosages have been compared with estimated
exposure levels from the local contamination using
standard toxicological data and local data.
Results:
Information to the community has been developed
that places potential risk into context. Variation in risk estimates relate to underlying assumptions
rather than to fundamental data.
The major sources of risk presentation to the
community came from risk assessments that defaulted to
linearity without examining the underlying data and from
failure to consider bio-availability as a modifying factor
for exposure.
Conclusion:
Community risk analyses are of greater help when
they flag the policy assumptions that fail to take
knowledge into consideration.
Fuller knowledge provided the community the
opportunity to focus remediation and prioritize.
Arsenic: A Potential Toxic Metal In Urban Soils Under High
Traffic Pressure
Gebhard
B. Luilo, University of Dar es Salaam, C/o
Department of Chemistry, PO Box 35061, Dar es Salaam,
Tanzania, Tel: +255-744-587546, Fax: +255-22-2410038
Othman C. Othman and Faustin N. Ngassapa, University of
Dar es Salaam, Department of Chemistry, PO Box 35061, Dar
es Salaam, Tanzania, Tel: +255-22-2410038, Fax:
+255-22-2410038
Urban
soils are vulnerable to traffic-induced toxic metal
pollution particularly lead. However, little attention has
been given to arsenic. Reports from ATSDR, 1989 and
US-EPA, 2000 pointed out arsenic is present in fossil
fuels in trace amounts. Increasing motor traffic in urban
areas may be a source of arsenic in cities and along
highways. This study, therefore, aimed at determining the
levels of arsenic in roadside soils in the Dar es Salaam
City. Soil samples were collected at a depth of 0 – 5 cm
from the roadside soils at distances of 1, 5, 15, 35, 50,
and 150 m from the road edges and control samples were
obtained at 1000 m off the highway. Thirty composite soil
samples were analyzed for arsenic by AAS (model AAnalyst
300). The results showed that soils were contaminated with
arsenic and its levels ranged from 0.03 - 0.65 ppm. The
amount of arsenic in the soil decreased exponentially with
increasing distance up to 35 m distance from the road
edge. Arsenic levels in the soils varied significantly
among the study sites (F = 4.140, p = 0.0096). Pearson
rank correlation indicated that arsenic in the roadside
soils is related to traffic density (r2 =
0.4729) and the low correlation value is attributed to of
sandy texture of the soils for which arsenic may not be
found in large amounts at the surface soils... In
conclusion this study is that arsenic, to some extent,
owes its source from the passing motor vehicles and
therefore we call upon detailed investigation of arsenic
pollution of urban environment in high traffic towns and
cities.
Arsenic
in Soil and CCA Treated Wood by Field Portable X-ray
Fluorescence
David
Mercuro, Debbie Schatzlein, and Volker
Thomsen, NITON
LLC, 900 Middlesex Turnpike, Bldg. 8, Billerica, MA 01821,
Tel: 800-875-1578, Fax: 978-670-7422
In
recent years, issues surrounding the use of chromated
copper arsenate (CCA) preservative chemical have
increased. There are concerns of possible As leaching into
soil both during the lumber’s in-use life and when the
wood is eventually disposed of in un-lined landfills.
This leaching could cause an increase of arsenic in
topsoil, which would be a major concern to the health of
children and adults.
This potential hazard has led treatment
manufacturers to voluntarily stop producing CCA as of the
end of 2003, and to begin using alternative wood
preservatives.
X-ray
Fluorescence (XRF) has been a widely accepted means of
analyzing the preservative content of wood by treatment
plants for many years.
CCA is the most widely used wood preservative for
decks, playgrounds and exterior housing structures and its
analysis in wood is straightforward by XRF.
However, data generated has also shown that XRF,
and more specifically field-portable XRF (FPXRF), has the
ability to analyze low levels (ppm) of arsenic in soil as
well. Therefore
FPXRF is the complete package for CCA measurement. It can
be used to monitor proper treatment of wood, sort treated
and untreated wood at a construction and demolition
landfill, and screen for arsenic leaching in soil.
Removal
of Arsenic from Contaminated Water Using Alkali Fly Ash
Permeable Reactive Barrier (AFA-PRB) Material
Hossein
Rostami, Philadelphia University, Henry Ave. and School
House Lane, Philadelphia, PA
19144, Tel: 215-951-2877, Fax: 215-951-6812, Email:
rostamih@philau.edu
William Brendley, Philadelphia University, Email:
brendleyw@philau.edu
Over
the past 15 years, about one half million sites with
potential contamination have been reported to federal or
state authorities. Of
these, about 217,000 sites still need remediation
and new contaminated sites continue to appear each
year. The
most common type of contaminants are metals, solvents and
petroleum products. Heavy
metals are present in two thirds of Department of Defense
(DOD) and superfund sites and about 50% of Department of
Energy (DOE) and Resource Conservation and Recovery Act (RCRA)
sites.
AFA-PRB
material was used to remove arsenic from contamination
water. Fly
ash from three different sources were used to produce
reactive barrier of different permeability.
AFA-PRB materials with permeability 10-2
cm/sec to 10-1 cm/sec were created.
For reactive barrier material, permeability must be
rapid in the range of 10-2 to 10-1
cm/sec. AFA -
PRB from three ash sources with permeability of
approximately 10-1 were produced and crushed
into pelletized form.
Effectiveness of the various barriers were
determined by batch and column tests .
Laboratory experiment indicates arsenic ion reduces
from 1000 ppm to less than 2 ppm with 7 liters of solution
and arsenic in valent from 10 ppm to less than 1 ppm.
Analyses were performed by Atomic adsorption
techniques.
Arsenic
Speciation in the Tailings Impoundment of a Gold Recovery
Plant in Siberia
Olga V.
Shuvaeva, Institute of
Inorganic Chemistry, RAS, SB, Ac.Lavrentyev, 3, Novosibirsk
630090, Russia
Elena V. Lazareva United
Institute of Geology, Geophysics and Mineralogy, RAS SB,
Ac.Koptug, 3,Novosibirsk 630090, Russia
It is known that arsenic is one of
the most dangerous elements in terms of its potential
impacts to both to human and ecosystem health. The
recovery of gold from ores containing arsenopyrite
releases significant amounts of arsenic into the
environment. The objectives of the present investigation
were to: (1)
document the distribution of arsenic in the solid
waste-materials of a tailings impoundment; (2) determine
the chemical speciation of arsenic in its sediments and
waters; and (3) examine the nature of arsenic
transformations in the tailings impoundment.
This study focuses on the Komsomolsk tailings
impoundment located in the Kemerovo region of southwestern
Siberia. The primary sulphide minerals involved in the
cyanidation of these particular ores include arsenopyrite,
pyrite, pyrrotite and others. Analytical procedures consisted of field
experiments, total arsenic determination in waters and
sediments and arsenic speciation in surface and pore
waters using the combination of microcolumn HPLC with ETA
AAS detection. Arsenic speciation in sediment cores was
done using the sequential leaching procedure with our own
modifications.
There
is an arsenic enrichment in the pore waters with respect
to the surface waters in the gold recovery tailings dams. During
the storage of the waste materials arsenic is
redistributed between solid and dissolved phases and
arsenic content in pore waters may become very high (about
1700
m
g/L). It has been
established that the primary form of arsenic in the
sediments is the mineral arsenopyrite. Only a very small
amount of arsenic dissolves during ore processing.
The arsenic release from the sediment results from a
reductive dissolution of the arsenopyrite and Fe oxides.
In the surface water, arsenate and arsenite are the main
arsenic species (arsenate is dominant), but in the pore
waters methylation processes play a significant role.
Arsenic transport is accompanied by their transformation
into the less toxic compounds (methylated species)
co-existing with the most toxic species (arsenite). The main secondary forms of arsenic in the sediments of the impoundment
(more than 20% of the total content) are associated with
iron hydroxides.
Background
Study of Elevated Arsenic in Soil at a Rhode Island Site
Stephen Zemba, Edmund Crouch, and Shailesh Sahay, Cambridge
Environmental Inc., 58 Charles Street, Cambridge, MA
02141, Tel: 617-225-0810, Fax: 617-225-0813
Eirlys Vanderhoff and Ambrose Donovan, McPhail Associates,
30 Norfolk Street, Cambridge, MA
02139, Tel:
617-868-1420, Fax: 617-868-1423
Arsenic
concentrations in soils at a residential property in
Newport, Rhode Island, were found to exceed both statewide
background levels and remediation criteria.
Arithmetic mean arsenic concentrations of 12.0
mg/kg and 11.7 mg/kg in site and background soils,
respectively, are both about four times greater than a
background level of 2.7 mg/kg published by the Rhode
Island Department of Environmental Management (DEM).
A risk-based concentration of 0.4 mg/kg of arsenic
in soil is necessary to meet the DEM’s incremental
cancer risk target of 1x10-6.
Given the similarity of arsenic concentrations in
site and background soils and a lack of evidence of any
anthropogenic releases of arsenic to soils, a background
study was undertaken to gauge whether concentrations of
arsenic at the site are likely due to natural background
conditions. The
study implemented the DEM’s “Guidance for Arsenic in
Soil,” and was based on measured arsenic concentrations
in 20 soil samples from the site and 21 soil samples
determined by site investigators to represent background
conditions. The
mean arsenic concentrations in both site and background
soils were found to be statistically similar, but the
distributions of on- and off-site data differed, possibly
due to land development patterns.
Specifically, site soils are expected to have been
mixed to a greater degree than background soils due to
extensive excavation and regrading of the site.
Presentation of the background study will focus on
site history, the implementation and implication of
DEM’s arsenic policy, the statistical analyses used to
compare site and background data, and technical and
regulatory conclusions that have been reached based on the
site investigation.
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