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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />( CONSTITUENTS OF" CONCERN :) <br /> <br />M~enlc <br /> <br />Descri ption <br /> <br />Arsenic (As) is a metalloid, with properties <br />intermediate between those of a metal and a <br />nonmetal. In its pure state, it generally takes <br />the fon:n of a dense, gray metal, although a <br />much lighter, yellowish powder may be <br />formed through sublimation of the vapor. In <br />nature, arsenic exists in four oxidation states <br />(As-3, Aso, As+3 [referred to as MAs (ill)"], and <br />As+s ["As (V)"]), and it may be in either <br />organic or inorganic forms. Its common ores <br />include the minerals arsenopyrite (FeAsS) and <br />realgar (As2S2). Arsenopyrite is a white to <br />gray orthorhombic mineral resembling pyrite, <br />commonly found in lead and silver veins. <br />~ealgar ~orms red to reddish-orange nodules <br />more vems and similarly colored coatings <br />around some hot springs. <br /> <br />Occurrence <br /> <br />Arsenic is ubiquitous-present in air, water, <br />soil, plants, and other living organisms. In <br />water, common forms of arsenic are As (III), <br />As (V), methane arsonic acid, and dimethyl- <br />arsinic acid (EP A 1985). Inorganic As (V) is <br />the most common species in water. As (III) in <br />water converts readily to As (V) under aerobic <br />conditions (Clement and Faust 1973), but <br />some As (III) may persist depending on <br />microorganisms, temperature, and other <br />factors. <br /> <br />Background Concentrations.-The arsenic <br />concentration in soil normally ranges from <br />1 to 50 mg/kg, though it does not generally <br />exceed 10 mg/kg (Brown et al. 1983), and in <br />water it is normally <10 pg/L (Eisler 1988). <br />Terrestrial flora and fauna, birds, and <br />freshwater biota usually contain <1 mg As/kg <br /> <br />by wet weight (ww). Arsenic at 0.27 mg/kg <br />ww (=: 1 mg/kg dry weight [dw]) is reported <br />to be the 85th percentile concentration for <br />freshwater fish (Schmitt and Brumbaugh <br />1990), and background concentrations in <br />terrestrial plants range from 0.01 to 1.7 mg/kg <br />dw (Bodek et al. 1988). Concentrations of <br />arsenic in livers of adult amphibians collected <br />in an apparently uncontaminated area <br />averaged 0.164 mg/kg ww (Byrne et al. 1975). <br />These levels are sometimes much higher in <br />biota collected near areas with high geo- <br />thermal activity and near manufacturers of <br />arsenical defoliants and pesticides (Eisler <br />1988). <br /> <br />Each year, as a result of agricultural and <br />industrial activities, large quantities of <br />arsenicals that may be hazardous to fish and <br />wildlife are released into the environment <br />(Eisler 1988). Agricultural applications <br />provide the largest artificial source of arsenic <br />in the environment (Eisler 1988). It is <br />contained in wastes from the production of <br />certain herbicides, fungicides, insecticides, <br />algicides, and wood preservatives (Brown et <br />al. 1983); in particular, sodium arsenite was <br />commonly used as an aquatic herbicide <br />between 1940 and the 1970's, especially in the <br />United States (Tanner and Clayton 1990). <br />Arsenic is also present in large amounts in <br />water contaminated by mine tailings, smelter <br />wastes, and natural mineralization (Eisler <br />1988). EP A also states that sources of arsenic <br />in drinking water include glass, electronic <br />wastes, and orchards (EPA 1994). <br /> <br />Summary of Effects <br /> <br />Arsenic is not normally considered an <br />essential element to most species, and it has <br />been shown to be both teratogenic and <br /> <br />8 <br />