Arsenic Pollution of a Loam Soil: Retention Form and Decontamination

S. Wasay, W. Parker, P. Geel, S. Barrington, S. Tokunaga
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引用次数: 39

Abstract

A study was conducted to assess the retention form of arsenic in soil and to evaluate the use of phosphate for releasing it from the soil. In this study, a loam soil was artificially polluted with arsenate at pH 5.5, which is one of the pH values at which maximum arsenic adsorption occurred. The soil was kept for 2.5 months under wet conditions to allow for stabilization. The soil was maintained under aerobic condition and losses of arsenic by volatilization were determined to be minimal. The soil was then sequentially extracted with a series of chemicals to identify the soil fractions in which the arsenic was bound. The percentage of arsenic found in the Fe bound-exchangeable, reducible-residual, Al bound exchangeable, residual, calcium bound exchangeable, and easily exchangeable forms was 31.6, 27.3, 25.2, 5.5, 4.9, and 4.7%, respectively. A batch experiment showed that at 20°C, 80% of the bound arsenic was removed by phosphate in the pH range of 5 to 7. A power function model was found to fit the data with a desorption rate constant of 402 mg/kg As h−1.
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壤土砷污染:保持形式与净化
进行了一项研究,以评估砷在土壤中的保留形式,并评估磷酸盐从土壤中释放砷的使用。在本研究中,用砷酸盐对壤土进行了人工污染,其pH值为5.5,这是砷吸附最大的pH值之一。土壤在潮湿条件下保存了2.5个月,以便稳定。土壤保持在有氧条件下,砷的挥发损失被确定为最小。然后用一系列化学物质对土壤进行连续提取,以确定砷结合的土壤组分。砷在铁结合交换态、可还原残余态、铝结合交换态、残余态、钙结合交换态和易交换态中的含量分别为31.6、27.3、25.2、5.5、4.9和4.7%。批量实验表明,在20℃时,在pH为5 ~ 7的范围内,磷酸盐可脱除80%的结合砷。用幂函数模型拟合数据,解吸速率常数为402 mg/kg As h−1。
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