Chronic Arsenic Poisoning:
History, Study and
Remediation
by S. Sambu and R. Wilson
"It is an uncanny thought that
this lurking poison (arsenic) is everywhere about us,
ready to gain unsuspected entrance to our bodies from the food
we eat,
the water we drink and the air we breathe" Karl
Vogel, 1928.
Acute
Effects
.
Arsenic has been used since 3000 BC. In the United Kingdom, for
example, it was used to extract iron from iron ore. It has long
been known that arsenic is acutely toxic. Anyone who drinks
arsenic in water at 60 parts per million (ppm) will soon die.
There are several toxicological summary references for acute
effects available on the web such as
SCORECARD,
ASTDR,
USEPA
and
LSUMC.
Beneficial
Effects
.
Arsenic has been used for many years
for medicinal purposes. It used to be used as a cure for
diseases such as syphilis and has been shown to assist in curing
some leukemias. It was taken as a medicine in Fowler's Solution
for well over a century. That arsenic at low levels is safe seemed
to be reinforced by animal studies that seemed to show that
arsenic is beneficial (to animals) at low doses. Indeed, the fact
that laboratory animals could not be persuaded to develop cancer
misled toxicologists throughout the world and greatly contributed
to the present catastrophe. Others have written about other
possible
beneficial
effects at very low levels. It is important to note that the
beneficial effects are for different medical outcomes (end points)
than either the acute or chronic adverse effects and that both
beneficial and adverse effects can be observed simultaneously (as
is well known for alcohol ingestion). Another detailed
article about beneficial uses of arsenic can be found
here.
Mineral hot springs in the USA still advertise arsenic pools and
their users, including this webmaster, are convinced that the
effects are beneficial! (But arsenic penetrates the skin only
slowly)
Chronic Adverse Effects
.
Chronic effects of prolonged low level exposure have
recently showed up. Among various summaries we link to an
information site run by
ASTDR. Skin pigmentation,
keratoses
and skin cancers were found by Tseng in Taiwan in 1966
among people who drank from arsenic contaminated wells (but no
effect was seen below about 150 parts per billion (ppb), which
might therefore be a biological threshold) and a very high
incidence of lung, bladder and other cancers was found in Taiwan
by Dr Chien-Jen Chen in 1986 and by
Dr Allan
Smith and collaborators in Chile in 1993. These
convinced WHO to recommend lowering the regulatory level
from 50 ppb to 10 ppb for arsenic in water. It appears that
there are no data on humans to contest the idea that prolonged
exposure to low doses is dangerous. Although arsenic was used
medicinally in "Fowler's Solution" (1% arsenite),
prolonged use had led to these chronic skin effects. This was
observed as early as 1888 by Hutchinson. A follow up of a number
of English patients treated with Fowler's Solution has
been reported by Dr Susan Evans in published literature, in a
report at the February 1998 conference in Dhaka and in a
presidential address by Susan Evans to the Liverpool
Medical Institute, which is available for download in PDF
format. This shows that the use of "Fowler's solution" (which is
primarily medicinal arsenic) in the UK is probably responsible
for 5 bladder cancer cases among the patients among whom
only 1.6 were expected from natural causes. The arsenic
dose was equivalent to an average lifetime dose that would come
from drinking water with about 25 ppb of arsenic therein.
After
several years of low level arsenic exposure, various skin
lesions appear. These are manifested by hyperpigmentation
(dark spots), hypopigmentation (white spots) and keratoses of
the hands and feet. After a dozen or so years skin cancers are
expected. Twenty or thirty years after exposure to 500
ppb of arsenic, internal cancers (lung, kidney, liver and
bladder) appear among 10% of all exposed. Moreover, the
dose-response relationship for these internal cancers is
consistent with being linear with no threshold. Photographs of
a number of victims of this
poisoning are available both from Bangladesh
and from Inner
Mongolia.
Although the most dramatic effect was the
observation of internal cancers in Tawian, the most
extensive epidemiological studies have come from the work in
Chile, in which Dr Allan Smith of UC Berkeley has been heavily
involved. They find the extraordinarily surprizing result that
ingested arsenic in
Chile has produced lung cancer at a rate greater than that of
a heavy cigarette smoker! Recently, the group
identified an effect of arsenic exposure to chldren - who have
developing lungs -. Children exposed to arsenic have ten times the normal lung
cancer incidence.
.
.
The Effect of Diet
An
important issue for coping with arsenic exposure is the effect
of diet. A general issue can be stated: there is
frequently more than one cause of a cancer or a lesion.
For example lung cancer can be caused by cigarette smoking or
asbestos or both together, in a synergistic way such that the
risks multiply (rather than add) when both are present. In the
USA it has been found that people who have a good diet of
fresh fruit and vegetables (5 servings per day) have half the
risk of many cancers, including lung cancers caused by
cigarettes, as those without a good diet. By analogy, one
might expect that the lung cancer risk from arsenic will be
less among those with a good diet. Anecdotal indications from
Bangladesh suggests that a good diet reduces skin lesions, and
the effect is seen in West
Bengal, but the effect is small and the
authors recommend that effort is better spent on obtaining
pure water. Nonetheless epidemiological studies to
confirm this are highly desirable. Khaliquzzaman and Khan have
calculated the "Arsenic Exposure of Bangladesh
Population through Food Chain" using known amounts in
food, in an unpublished World Bank
report. The amount is
less than from drinking water but not much less.
There are several specific chemicals that
have been suggested that would either (i) help to prevent
arsenic lesions by rapid removal of arsenic from the body or
(ii) help to cure arsenic lesions. Encouragement of methylation
of the arsenic probably accelerates methylation, but the
methylation has been suggested as a cause of internal cancers.
The specific chemical that has come to the mind of many health
experts is selenium. It was noted in the 1930s that effects of
excess selenium can be counteracted by adding arsenic to the
diet because As and Se combine. Does the inverse take place? It
is reported that areas with high incidence of arsenical lesions
have low selenium in the water. Some victims have low
selenium levels. Does adding selenium to the diet really help,
either to prevent the lesions from forming (likely), or to treat
them afterwards (less likely)? We have, with help from
others, compiled a list of
references and a
recent
paper on the subject.
Professor
Zuberi of Rajshashi University has suggested methionine to
reduce the arsenic lesions. Dr. OGB
Nambiar
has suggested that ferrous sulphate, after conversion to sulfide
by bacteria in the colon, absorbs arsenic and assists safe
excretion. The evidence for these remains indirect, and there
may be (as suggested above) competing adverse effects. Only good
epidemiology can tell and this is under way in several
places.
Regulatory
Limits for Continuous Exposure
The regulatory
limits on arsenic exposure were set primarily to be sure
that these acute toxic effects were avoided. The first
regulatory limit of which the webmasters are aware was set
as a result of a public inquiry (subsequent to arsenic being found
in beer) of six members chaired by the physicist William Thompson,
first Lord Kelvin, in 1903. They recommended that sake of
liquids with more than 100 grains of arsenious oxide per gallon
(which works out at about 90 ppb of arsenic or 0.09 ug/l)
This was reduced two fold over the next century and until recently
the limit set by Bangladesh, the United Kingdom, and
the United States was 50 parts per billion (ppb). But the
discovery that there are adverse
effects of continuous chronic exposure led WHO to lower their recommendation
to 10 parts per billion (10 ppb). The European Union (EU)
plans to enforce a standard of 10 ppb by 2003.
After a long travail , on October 31st 2001, the
administrator of US EPA confirmed a new standard for drinking
water of 10 ppb to be enforced by 2006. In Australia there
does not seem to be a specific regulatory level but there are work
rules for those working around mine tailings sites.
The US EPA has
recently come out with an extensive
review of mechanisms of action of Dimethyl Arsenic (DMA) and its possible mechanisms of action.
They cannot rule out a linear dose response at the lowest doses.
It is effectively impossible to reduce the content of arsenic in
drinking water to a risk level of one in a million lifetime risk
calculated with a linear dose-response relationship, a risk level
and a calculational procedure frequently used by the U.S. EPA. The
present 10 ppb standard is perhaps the first in which the U.S EPA
explicitly compared costs and benefits and used a value of $6.1
million per calculated life saved. References to the
extensive US national discussion are available on the "countries" page and in particular the
section on travail.
The Worldwide Scope of the Catastrophe
Arsenic contamination has become a
problem in many parts of the world. At
first as a result of leaching from mine tailings in
Australia, Canada,
Japan, Mexico, Thailand,
United Kingdom, and the United
States, but now also from the
arsenic in natural acquifers now or recently used for water supply
in Argentina, Bangladesh, Cambodia, Chile , China,
Ghana, Hungary, Inner
Mongolia, Mexico, Nepal, New
Zealand, Philippines, Taiwan, the United States and Vietnam. Arsenic was also
widely used as a pesticide. 20,000 tons a year was
imported into the USA, and perhaps double that amount was used, to
spray on crops in the USA alone. No attention was paid to
the ultimate fate of the chemical,and in consequence arsenic
now appears in foodstuffs . (Papers
describing data in some of these countries are listed by
country in the list of useful references. ) It is important to
distinguish the problems in Bangladesh, West Bengal and, to a
lesser extent, Inner Mongolia, Chile, Nepal and Vietnam, from
the problems that have been found so far in the rest of the
world. These situations have in common that they are an alluvial
plain where arsenic has been brought down from the surrounding
hills for millenia. It seems that no one has looked
carefully at similar geological situations such as the Mekong
delta or the Irrawaddy delta. In most of the world
exposures above 50 parts per billion (50 ppb) are rare, and once
observed, can easily be avoided. But the sheer scale of the
problems in Bangladesh dwarfs the imagination. The catastrophe is
much worse than the well known catastrophe of the Chernobyl
nuclear power plant accident, the Bhopal isothiocyanate leak
or the Kuwait oil fires. For 90% of the Bangladeshi
communities, pure water is still a long time away.
The World
Bank made a study for SE Asia in the beginning of the 21st century
which is available on the web:
"Arsenic Contamination of
Groundwater in South and East Asian Countries"
The situation in
Bangladesh has received a lot of attention because it is the most
important. The new Bangladeshi government has made the solution of
the problem a priority as stated clearly by Prime
Minister Begum Khaleda Zia as
she opened the special WHO workshop in Dhaka on January 14th -16th
2002. Feroze
Ahmed, presented an excellent
review of the situation at that time. Particpants made recommendations
to
the government of Bangladesh
(GoB). Another (2002)
review from the NGO forum is copied here from the NAISU website in
pdf. Professor
Chakriborti of
Kolkata (Calcutta), a tireless and enthusiastic
worker in the field regularly issues his reports on the
Bangladesh situation, has a year 2001 report on
Bangladesh which we have also
captured in a local file.
Why Does Arsenic Get into
the Water?
This is the subject of a whole issue
of the journal Applied Geochemistry:
Bhattacharya, P., A. H. Welch, K. M. Ahmed, G. Jacks
and R. Naidu (Eds.)
Arsenic is
plentiful in the ground. Yet it does not awlays appear in the
water supply. Scholars at the Cambridge University Department of
Geography have identified the following mechanisms for arsenic
entering the water which vary between locations.
Alkali-desorption, Geothermal, Reductive dissolution and Sulphide
oxidation. lthough the worst arsenic catastrophe is in Bangladesh,
where 35 million people are exposed to levels above the US EPA
standard, the amount of arsenic in the soil is less than in many
other areas, including areas such as Massachussets, USA, where it
does not, nonetheless, appear in unsafe quantities in ground
water. In most of these areas, such as the delta of the Ganges and
Irrawaddy, and the bend of the Yellow river, arsenic has come down
from the mountains over millenia, attached itself to iron, forming
iron pyrites, and been deposited. Professor McArthur of UC London
argues: "It becomes increasingly clear that severe arsenic
pollution of ground water in most alluvial aquifers
worldwide is driven by the microbially-mediated metabolism of
organic matter, with FeOOH acting as the source of oxygen: the
oxide is reduced during the process and its sorbed arsenic is
released to ground water. Despite the widespread acceptance of
this mechanism, much about it remains obscure." One issue is
whether the reduction takes place at the surface before the water
filters down to the aquifer in the monsoon (as suggested by group
(a) below) or whether it is reduced in the aquifer itself.
Papers
describing this mechanism include:
(a) Two papers were presented by
Charles Harvey et al.:
"Arsenic. Its Biogeochemistry and Transport in
Groundwater," in "Biogeochemical Cycles of the Elements"
"Subsurface geochemistry and
arsenic mobility in Bangladesh"
"Response to Technical Comment on
“Arsenic Mobility and Groundwater Extraction in Bangladesh"
and a brief report
in
Science. Most recently they
suggest that reduction occurs in arsenic ponds before water enters
the aquifer.
(b) The group at Columbia
University have also presented a papers
on the same topic of which
the most recent is:
"Redox
control of arsenic mobilization in Bangladesh groundwater",
Zheng et al., Applied Geochemistry, 19(2), 163-260, Feb 2004,
201-214.
(c) Professor McArthur and
colleagues at UCL in London have several reports available on their webpage of which
the following may be downloaded:
"Arsenic
in groundwater: testing pollution mechanisms for sedimentary
aquifers in Bangladesh"
Their
most recent paper disagrees
with
the hypothesis of group (a) that the reduction occurs in ponds.
An older idea
was that water was being drained from the aquifer, allowing
oxidation. A recent paper describing arsenic contamination in
Perth, Australia - shows that there is one location, in
Perth where pyrite oxidation clearly WAS the source of the
As (although there is evidence that anerobic release from Fe
oxyhydroxides is also taking place deeper in the aquifer). But the
ideas that pyrite oxidation is the problem in Bangladesh
whether caused by recent rapid
pumping that allowed for
oxidation and release of arsenic, or by the man-made change
in river flow, such as the barrage across the Ganges are now
considered to be untenable.
In the Americas, from Alaska in the north,
through Crater Lake in Oregon, Mono Lake and Searles lake in
California, volcanic lakes in Niceragua and Costa Rica, and on to
the Andes, lie a chain of volanic activity that brings arsenic to
the surface. This mecahnism of sulfate reduction in
the arsenic-rich soda lakes (Mono Lake and Searles lake) of is being
studied in detail by Dr Oremland and his group at the US
Geological Survey in Menlo Park. They attrbute the mechanism
to bacteria, but of course different bacteria from those
responsible for the reduction of iron pyrites in SE Asia and
Bangladesh. Presumably this is the same mechanism as is
responsible for the arsenic pollution in the mountains of
Argentine and Chile where so much
epidemiological studies have been made.
Social Issues
Western
experts from developed countries often regard the arsenic
pollution problem as a technical problem to be solved by
purely technical means. But that is naive. There
are tremendous social issues which control the ability of
anyone to help. One set of papers discussing ws prepared by
the Arsenic Policy Support Unit in Bangladesh, (APSU)
which is now defunct, but these papers are copied
on
this site.
Possible
Solutions to the Problems
The first and
most obvious necessity is to measure the arsenic levels in any ground water
that is intended for human use. The next step is to purify
the water or, better still,
provide an alternate supply of pure water. The way in which
this is done varies from country to country. In SE ASIA, and
Bangladesh in particular, two facets of a solution seem to be
agreed.
(1) There is no one solution
for all places and communities. It is vital to involve the local
community in the decision and even more important in the follow up
and maintenance.
(2) The solution in any
community and location must based upon the best possible
scientific understanding. The webmaster has attempted to summarize
the possibilities in the remediation
page. Please add and correct.
It is very important to share data and experiences as set out in declarations from seven arsenic conferences
in Dhaka held by Dhaka Community Hospital.
Contact Us
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