Concentrations of inorganic arsenic in groundwater, agricultural soils and subsurface sediments from the middle Gangetic plain of Bihar, India

• Published in: The Science of the total environment Vol. 573; pp. 1103 - 1114
• Main Authors: Kumar, Manoj, Ramanathan, AL, Rahman, Mohammad Mahmudur, Naidu, Ravi
• Format: Journal Article
• Language: English
• Published: Netherlands Elsevier B.V 15.12.2016
• Subjects: Agricultural soil; Arsenic - analysis; Environmental Monitoring - methods; Extractable arsenic; Geologic Sediments - chemistry; Groundwater - chemistry; India; Inorganic arsenic; Middle Gangetic plain; Soil - chemistry; Soil Pollutants - analysis; Subsurface sediments; Water Pollutants, Chemical - analysis; India, Bihar; India; Extractable arsenic; Agricultural soil; Middle Gangetic plain; Subsurface sediments; Inorganic arsenic
• ISSN: 0048-9697; 1879-1026
• DOI: 10.1016/j.scitotenv.2016.08.109

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. [Display omitted] •As(III) observed as major species in groundwater while As(V) in soils and sediments.•Higher As concentrations in fine and dark grey clay in subsurface sediments.•Alteration of oxyhydroxide and transformation in goethite in aquifers.•Presence of As(III) and As(V) associated with siderite in aquifer sediment.