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地下水硒的形态:季节性变化和氧化还原转化。

Speciation of selenium in groundwater: seasonal variations and redox transformations.

机构信息

Chemical Laboratory, Central Groundwater Board, South Eastern Coastal Region, E1, Rajaji Bhavan, Besant Nagar, Chennai 600 090, India.

出版信息

J Hazard Mater. 2011 Aug 15;192(1):263-9. doi: 10.1016/j.jhazmat.2011.05.013. Epub 2011 May 12.

Abstract

Speciation of selenium in groundwater is essential from the viewpoint of toxicity to organisms and biogeochemical cycling. Selenium speciation in groundwater is controlled by aquifer redox conditions, microbial transformations, dissolved oxygen (DO) and other redox couples. A suburban area of Chennai city in India, where improper waste disposal measures have been practiced is selected for this study. Se(IV), Se(VI) and other hydrochemical parameters were monitored in shallow ground water during pre- and post-monsoon seasons for a period of three years. The objective of the study was to investigate the effect of groundwater recharge on selenium speciation. The concentration of Se(IV), and Se(VI) ranged between 0.15-0.43 μg L(-1) and 0.16-4.73 μg L(-1), respectively. During post-monsoon period the concentration of Se(IV), and Se(VI) ranged between 0.15-1.25 μg L(-1) and 0.58-10.37 μg L(-1), respectively. Se(VI) was the dominant species of selenium during the pre- and post-monsoon periods. During the post-monsoon periods, leaching of selenium from soil was more effective due to the increased oxidizing nature of the groundwater as indicated by the DO and redox potential (Eh) measurements. This finding has important implications on the behavior of selenium in groundwater, and also on the health of people consuming groundwater from seleniferous areas.

摘要

从对生物体的毒性和生物地球化学循环的角度来看,地下水硒的形态至关重要。地下水硒的形态受含水层氧化还原条件、微生物转化、溶解氧(DO)和其他氧化还原对的控制。印度钦奈市的一个郊区,由于采取了不当的废物处理措施,被选为这项研究的地点。在三年的时间里,监测了浅层地下水中的硒(IV)、硒(VI)和其他水化学参数,在季风前和季风后季节进行监测。研究的目的是调查地下水补给对硒形态的影响。Se(IV) 和 Se(VI) 的浓度分别在 0.15-0.43μg/L 和 0.16-4.73μg/L 之间。在季风后时期,Se(IV) 和 Se(VI) 的浓度分别在 0.15-1.25μg/L 和 0.58-10.37μg/L 之间。在季风前和季风后时期,硒(VI)是硒的主要形态。在季风后时期,由于 DO 和氧化还原电位(Eh)测量表明地下水的氧化性质增加,土壤中硒的淋滤更加有效。这一发现对硒在地下水中的行为以及饮用富硒地区地下水的人们的健康具有重要意义。

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