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Last modified
7/14/2009 5:02:29 PM
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5/20/2009 10:14:01 AM
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UCREFRP
UCREFRP Catalog Number
7092
Author
Eisler, R.
Title
Arsenic Hazards to Fish, Wildlife, and Invertebrates
USFW Year
1988.
USFW - Doc Type
A Synoptic Review.
Copyright Material
NO
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arsenic cycle only by causing localized high concentrations (NAS 1977). The <br />speciation of arsenic in the environment is affected partly by indiscriminate <br />biological uptake, which consumes about 20% of the dissolved arsenate pool and <br />results in measurable concentrations of reduced and methylated arsenic <br />species. The overall arsenic cycle is similar to the phosphate cycle; <br />however, regeneration time for arsenic is much slower--on the order of several <br />months (Sanders 1980). The ubiquity of arsenic in the environment is evidence <br />of the redistribution processes that have been operating since early geologic <br />time (Woolson 1975). A prehuman steady state solution to the global arsenic <br />cycle (Austin and Millward 1984) indicates that major reservoirs of arsenic <br />(in kilotons) are magma (50 billion), sediments (25 billion), oceanic deep <br />waters (1.56 million), land (1.4 million), and ocean mixed layers (270,000); <br />minor amounts occur in ocean particulates (100), and in continental (2.5) and <br />marine tropospheres (0.069). Arsenic is significantly mobilized from the land <br />to the troposphere by both natural and anthropogenic processes. Industrial <br />emissions account for about 30% of the present day burden of arsenic in the <br />troposphere (Austin and Millward 1984). Agronomic ecosystems, for example, may <br />receive arsenic from agricultural sources such as organic herbicides, <br />irrigation waters, and fertilizers, and from such nonagricultural sources as <br />fossil fuels and industrial and municipal wastes (Woolson 1975). Arsenic is <br />mobile and nonaccumulative in air, plant, and water phases of agronomic <br />ecosystems; arsenicals sometimes accumulate in soils, but redistribution <br />mechanisms usually preclude hazardous accumulations (Woolson 1975). <br />Arsenic compounds have been used in medicine since the time of <br />Hippocrates, ca. 400 BC (Woolson 1975). Inorganic arsenicals have been used <br />for centuries, and organoarsenicals for at least a century in the treatment of <br />syphylis, yaws, amoebic dysentery, and trypanosomiasis (NAS 1977). During the <br />period 1200 to 1650, however, arsenic was used extensively in homicides (NRCC <br />1978). In 1815, the first accidental death was reported from arsine (AsH ) <br />poisoning, and in 1900-1903 accidental poisonings from consumption <br />arsenic-contaminated beer were widely reported (NRCC 1978). In 1938, it was <br />established that arsenic can counteract selenium toxicity (NRCC 1978). The <br />introduction of arsphenamine, an organoarsenical, to control venereal disease <br />earlier this century gave rise to intensive research by organic chemists, <br />which resulted in the synthesis of at least 32,000 arsenic compounds. But the <br />advent of penicillin and other newer drugs nearly eliminated the use of <br />organic arsenicals as human therapeutic agents (EPA 1980). Arsenical drugs <br />are still used in treating certain tropical diseases, such as African sleeping <br />sickness and amoebic dysentery, and are used in veterinary medicine to treat <br />parasitic diseases, including filariasis in dogs (Canis familiaris) and <br />blackhead in turkeys (Meleagris gallopavo) and chickens, Gallus spp. (NAS <br />1977). Today, abnormal sources of arsenic that can enter the food chain from <br />plants or animals include arsenical pesticides such as lead arsenate; arsenic <br />acid, HAsO ; sodium arsenite, NaAs0; sodium arsenate, Na2As04; and cacodylic <br />acid, (CH3J2As(OH) (NAS 1977). 2 <br />4
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