Arsenic in a groundwater environment in Bangladesh: Occurrence and mobilization. (15th May 2020)

• Record Type: Journal Article
• Authors: Huq, Md. Enamul; Fahad, Shah; Shao, Zhenfeng; Sarven, Most Sinthia; Khan, Imtiaz Ali; Alam, Mukhtar; Saeed, Muhammad; Ullah, Hidayat; Adnan, Muahmmad; Saud, Shah; Cheng, Qimin; Ali, Shaukat; Wahid, Fazli; Zamin, Muhammad; Raza, Mian Ahmad; Saeed, Beena; Riaz, Muhammad; Khan, Wasif Ullah
• Is Part Of: Journal of environmental management. Volume 262(2020)
• Publication Date: 2020-05-15
• Subjects: Arsenic -- Geochemical process -- Arsenic sources -- Arsenic mobilization -- Bangladesh; Environmental policy -- Periodicals; Environmental management -- Periodicals; Environment -- Periodicals; Ecology -- Periodicals; 363.705
• DOI: 10.1016/j.jenvman.2020.110318
• Languages: English
• ISSNs: 0301-4797

Abstract

Abstract: Groundwater with an excessive level of Arsenic (As) is a threat to human health. In Bangladesh, out of 64 districts, the groundwater of 50 and 59 districts contains As exceeding the Bangladesh (50 μg/L) and WHO (10 μg/L) standards for potable water. This review focuses on the occurrence, origin, plausible sources, and mobilization mechanisms of As in the groundwater of Bangladesh to better understand its environmental as well as public health consequences. High As concentrations mainly was mainly occur from the natural origin of the Himalayan orogenic tract. Consequently, sedimentary processes transport the As-loaded sediments from the orogenic tract to the marginal foreland of Bangladesh, and under the favorable biogeochemical circumstances, As is discharged from the sediment to the groundwater. Rock weathering, regular floods, volcanic movement, deposition of hydrochemical ore, and leaching of geological formations in the Himalayan range cause As occurrence in the groundwater of Bangladesh. Redox and desorption processes along with microbe-related reduction are the key geochemical processes for As enrichment. Under reducing conditions, both reductive dissolution of Fe-oxides and desorption of As are the root causes of As mobilization. A medium alkaline and reductive environment, resulting from biochemical reactions, is the major factor mobilizing As in groundwater. An elevated pH value along with decoupling of As and HCO3 − plays a vital role in mobilizing As. The As mobilization process is related to the reductive solution of metal oxides as well as hydroxides that exists in sporadic sediments in Bangladesh. Other mechanisms, such as pyrite oxidation, redox cycling, and competitive ion exchange processes, are also postulated as probable mechanisms of As mobilization. The reductive dissolution of MnOOH adds dissolved As and redox-sensitive components such as SO4 2− and oxidized pyrite, which act as the major mechanisms to mobilize As. The reductive suspension of Mn(IV)-oxyhydroxides has also accelerated the As mobilization process in the groundwater of Bangladesh. Infiltration from the irrigation return flow and surface-wash water are also potential factors to remobilize As. Over-exploitation of groundwater and the competitive ion exchange process are also responsible for releasing As into the aquifers of Bangladesh. Highlights: Intensive land use, agrochemicals usage and irrigation are responsible for high As. Elevated As concentrations mainly occurred in shallow Holocene alluvial aquifers. Strong reducing condition and moderate alkalinity facilitated As release process. Evaporation was not an important factor responsible for As enrichment. As is mobilized in biogeochemical and reduction environment with ion exchange process.