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194                                                   6 Soil Pollution

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            contamination of soils worldwide. Contamination in excess of 1,000 mg As kg    has
            been recorded at many sites throughout Australia. Similar contaminated sites also
            exist in the USA, Africa, and other parts of the world (Smith et al.  1998a ,  b ). The
            main sources of As in soils is the parent materials from which the soil is derived
            (Yan-Chu  1994 ). The distribution of As in soils may vary with soil type, depending
            on the nature of the parent material. Background concentrations do not generally
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            exceed 15 mg As kg    (NRCC  1978 ), although concentrations ranging from 0.2 to
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            40 mg As kg    soil have been reported (Walsh et al.  1977 ). Dudas and Pawluk ( 1980 )
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            reported background As concentrations that averaged 5 mg As kg    in 78 soil samples
            in Alberta. Much higher As concentrations have been reported in acid sulfate soils
            developed on pyritic parent material. For instance, Dudas ( 1987 ) attributed elevated
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            As concentrations that ranged from 8 to 40 mg As kg    in Canadian acid sulfate soils
            to the weathering of pyrites in the parent material. Many different As compounds

            have been identified in the soil environment, and they may be classified into two

            major groups: inorganic As compounds and organic As compounds. As (V) and
            As  (III) are the most important inorganic As species in the soil, because their
            compounds are highly soluble in water (Masscheleyn et al.  1991 ).

                  Arsenic Contamination to Groundwater and Arsenicosis in Asia
                Arsenic contamination in groundwater has invaded in several regions of the
              Southeast Asian countries like Bangladesh, China, India, and Nepal. Water
              drawn from shallow aquifers through shallow tube wells exceeds the national
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              standards (0.050 mg L   ) and USEPA and WHO standards (0.01 mg L   ) of As
              level for drinking water. The cause of this contamination to groundwater is geo-
              chemical; the sedimentary rocks there contain high As. People use shallow tube
              well water for domestic uses including drinking. Large-scale occurrences of
              arsenicosis have been reported  from the contaminated areas. Health problems
              associated with elevated levels of arsenic include thickening and discoloration of
              the skin, stomach pain, nausea, vomiting, diarrhea, numbness in hands and feet,
              partial paralysis, and blindness. Arsenic has been linked to cancer of the blad-
              der, lungs, skin, kidney, nasal passages, liver, and prostate. Thirty million peo-
              ple in Bangladesh use arsenic contaminated water for drinking.  About
              10,000–30,000 people have been diagnosed with arsenicosis (Alam et al.  2002 ).
              In China, endemic arsenicosis was found successively in many areas in the
              mainland during 1980s, and more than 10,000 arsenicosis patients were diag-
              nosed by 2001.  The main  As-contaminated provinces are Xinjiang, Inner
              Mongolia, Shanxi, Ningxia, Jilin, and Qinghai. In India, arsenic- contaminated
              groundwater occurs mainly in the states of West Bengal, Bihar, Uttar Pradesh,
              Assam, Jharkhand, Chhattisgarh, and Madhya Pradesh. According to UNICEF,
              over 13.8 million people are at risk of arsenicosis in West Bengal (Chakraborti
              et al.  2002 ). The problems are mainly related with As-contaminated drinking
              water, but there is also the risk of contaminating the food chain. Shallow aquifer
              water is the major source of irrigation in rice growing areas of Asia.
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