Introduction Arsenic is a metalloid that can be found in the environment in rocks, soil, and water. It occurs naturally as the minerals arsenopyrite (FeAsS),

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Introduction Arsenic is a metalloid that can be found in the environment in rocks, soil, and water. It occurs naturally as the minerals arsenopyrite (FeAsS), realgar (AsS), and orpiment, (As2S3). Levels of arsenic in the soil can be found to be from 0.1 to 40 ppm. Arsenic can enter groundwater by erosion, dissolution, and weathering. Other sources include geothermal springs and volcanic activity. It can also be released by brines that are used to produce natural oil and gas, as a by-product of gold and lead mining and the combustion of coal. Industrial contaminations occurs through production of lead-acid batteries, paper production, glass and cement manufacturing. Arsenic occurs in drinking-water as As(III) or As (V). ). Organic arsenic species are concentrated in seafood but are much less harmful to health than inorganic arsenic compounds as they are readily eliminated by the body. The European Union and the World Health Organisation recommend arsenic limits in drinking water of 0.01 ppm. Arsenic poisoning or arsenicosis results in many ailments such as skin cancer, cancers of the bladder, kidney and lung, gangrene, diabetes, high blood pressure and reproductive disorders. It is obviously important to be able to detect low levels of arsenic in aqueous sample. Method In this project the arsenic species were separated by ion exchange chromatography and measured by ICPMS. A Dionex ion-exchange column was used with gradient elution with 2 mM tetramethylammonium hydroxide and 10 mM ammonium carbonate binary mobile phase. Six arsenic species were separated over a period of 20 min in the order AsB, DMA V, MMA V, As III and As V. A Shimadzu inductively coupled plasma mass spectrometer with a miniaturized torch was used for the detection. The eluent from the ion exchange column was introduced into the plasma by a nebulizer. Standards of each of the arsenic compounds were prepared in water over the range0-50 ppm. Six- point calibration curves for the arsenic species were obtained by plotting the peak areas against the concentration of arsenic for each species Table 1 Common arsenic species in groundwater nameabbreviationformula ArseniteAs(III)As(OH) 3 ArsenateAs(V)AsO(OH) 3 Monomethylarsonic acid MMA(V)CH 3 AsO(OH) 2 Dimethylarsinic acid DMA(V)(CH 3 ) 2 AsOH ArsenobetaineAsB(CH 3 ) 3 As + Ch 2 CH 2 COO – Results The calibration curves gave corellation coefficients in excess of The detection limits ranged from to 0.40 ppm. The concentration of each of the arsenic species in the groundwater sample are given in table 2. Table 2 Results Arsenic species Concentration/ppm As(II)5 As(V)11 MMA(V)0 DMA(V)0 AsB0 Conclusions As effective method for determination of arsenic in grou8nwdayer was developed,. The levels of organoarsenic compounds was below the recommended limit. However, there was significant inorganic arsenic present. References B.K. Mandal, O. Yasumitsu and K.T. Suzuki, Identification of Dimethylarsinous and monomethylarsonous acids in human urine of the arsenic-affected areas in West Bengal, India, Chem. Res. Toxicol., 2001, 14, Z. Gong, X. Lu, M. Ma, C. Watt and X. Le, Arsenic speciation analysis, Talanta, 2002, 58, 1, T. Nakazato, T. Taniguchi, H. Tao, M. Tominaga and A. Miyazaki, Ion-exclusion chromatography combined with ICP-MS and hydride generation-ICP-MS for the determination of arsenic species in biological matrices, J. Anal. At. Spectrom., 2000, 15,