Global Centre for Environmental Remediation (GCER), Faculty of Science and Information Technology, University of Newcastle, University Drive, Callaghan, NSW 2308, Australia; Cooperative Research Centre for Contamination Assessment and Remediation of the Environment (CRC-CARE), University of Newcastle, ATC Building, University Drive, Callaghan, NSW 2308, Australia; School of Environmental Sciences, Jawaharlal Nehru University, New Delhi 110067, India.
School of Environmental Sciences, Jawaharlal Nehru University, New Delhi 110067, India.
Sci Total Environ. 2016 Dec 15;573:1103-1114. doi: 10.1016/j.scitotenv.2016.08.109. Epub 2016 Sep 16.
Concentrations of inorganic forms [arsenite, As(III) and arsenate, As(V) of arsenic (As) present in groundwater, agricultural soils and subsurface sediments located in the middle Gangetic plain of Bihar, India were determined. Approximately 73% of the groundwater samples (n=19) show As(III) as the dominant species while 27% reveals As(V) was the dominant species. The concentration of As(III) in agricultural soil samples varies from not detectable to 40μg/kg and As(V) was observed as the major species (ranging from 1050 to 6835μg/kg) while the total As concentration varied from 3528 to 14,690μg/kg. Total extracted concentration of As was higher in the subsurface sediments (range 9119-20,056μg/kg in Methrapur and 4788-19,681μg/kg in Harail Chapar) than the agricultural soil, indicating the subsurface sediment as a source of As. Results of X-ray diffraction (XRD) and environmental scanning electron microscope (ESEM) revealed the presence of hematite and goethite throughout the vertical section below while magnetite was observed only in the upper oxidized layer at Methrapur and Harail Chapar. Alteration of Fe-oxides and presence of fibrous goethite indicating presence of diagenetic sediment. Siderite plays a crucial role as sinks to the As in subsurface sediments. The study also concluded that decomposition of organic matter present in dark and grey sections promote the redox conditions and trigger mobilization of As into groundwater.
对印度比哈尔邦中部恒河平原地下水中、农业土壤中和地下沉积物中存在的无机砷[亚砷酸盐、As(III)和砷酸盐、As(V)]浓度进行了测定。大约 73%的地下水样本(n=19)显示 As(III)为主要形态,而 27%的样本显示 As(V)为主要形态。农业土壤样本中 As(III)的浓度从无法检测到 40μg/kg 不等,而 As(V)则是主要形态(范围为 1050 至 6835μg/kg),而总砷浓度则从 3528 至 14690μg/kg 不等。Methrapur 的地下沉积物中总提取砷浓度较高(范围为 9119-20056μg/kg),而 Harail Chapar 的地下沉积物中总提取砷浓度较高(范围为 4788-19681μg/kg),高于农业土壤,表明地下沉积物是砷的来源。X 射线衍射(XRD)和环境扫描电子显微镜(ESEM)的结果表明,在整个垂直剖面中都存在赤铁矿和针铁矿,而在 Methrapur 和 Harail Chapar 中仅在上层氧化层中观察到磁铁矿。Fe-氧化物的变化和纤维状针铁矿的存在表明存在成岩沉积物。菱铁矿在地下沉积物中作为砷的汇起着至关重要的作用。研究还得出结论,存在于暗带和灰带中的有机物的分解促进了氧化还原条件,并触发了砷向地下水的迁移。