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Arsenic in groundwater in the Bengal Delta Plain: slow poisoning in Bangladesh

机译:孟加拉三角洲平原的地下水中的砷:孟加拉国缓慢中毒

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The purpose of this paper is to provide an overview of the problems concerning the widespread occurrences of arsenic in groundwater in Bangladesh, a land with enormous resources of precipitation, surface water, and groundwater. Because of the potential risk of microbiological contamination in the surface water, groundwater was relied on as an alternate source of drinking water. Exploitation of groundwater has increased dramatically in Bangladesh since the 1960s to provide safe water for drinking and to sustain wetland agriculture. The presence of arsenic in the groundwater at elevated concentrations has raised a serious threat to public health in the region. Nearly 60-75 million people inhabiting a large geographical area are at potential risk ofarsenic exposure, and several thousands have already been affected by chronic arsenicosis. The source of arsenic in groundwater is geogenic and restricted within the Holocene sedimentary aquifers. Mobilization of arsenic from the alluvial aquifers is primarily effected through a mechanism of reductive dissolution of the iron oxyhydroxides within the sediments, rather than by the oxidation of pyrite, as has been hypothesized by other workers. The problem is further accentuated by the fact that arsenic isalso found at elevated concentrations in vegetables and rice grown in the areas where high-arsenic groundwater is used for irrigation. Dietary habits among the population are also an important pathway for arsenic ingestion. Studies are in progress at national as well as international levels to alleviate the arsenic crisis in Bangladesh. Besides the identification of arsenic-free tubewells in the affected areas for drinking purposes, purification of groundwater at household level by low-cost arsenic removal techniques is suggested. Rehabilitation of the patients with chronic arsenicosis and arsenic education programs for rural communities must be addressed urgently by the government of Bangladesh.
机译:本文的目的是概述与孟加拉国有关的地下水中广泛存在砷的问题,孟加拉国是一个拥有大量降水,地表水和地下水资源的土地。由于地表水中存在微生物污染的潜在风险,因此只能依靠地下水作为饮用水的替代来源。自1960年代以来,孟加拉国的地下水开采量急剧增加,以提供安全的饮用水和维持湿地农业。地下水中砷的浓度升高,对该地区的公共卫生构成了严重威胁。居住在较大地理区域中的近60-75百万人处于砷暴露的潜在风险中,数千人已经受到慢性砷中毒的影响。地下水中的砷源是地质成因的,并被限制在全新世沉积含水层中。从冲积含水层中动员砷主要是通过还原性沉积物中羟基氧化铁的溶解机制来实现的,而不是像其他工人所假设的那样通过黄铁矿的氧化来实现的。由于在高砷地下水用于灌溉的地区种植的蔬菜和大米中也发现了高浓度砷,这一事实使这一问题更加突出。人群中的饮食习惯也是砷摄入的重要途径。减轻孟加拉国砷危机的国家和国际一级研究正在进行中。除了在受灾地区确定无砷的管井以供饮用外,还建议通过低成本除砷技术在家庭一级净化地下水。孟加拉国政府必须紧急处理慢性砷中毒患者的康复和农村社区的砷教育计划。

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