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Arsenic and Manganese Contamination of Drinking Water Resources in Cambodia: Coincidence of Risk Areas with Low Relief Topography

机译:柬埔寨饮用水中砷和锰的污染:地形低洼的危险区的重合

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Arsenic contamination of groundwater has been identified in Cambodia, where some 100,000 family-based wells are used for drinking water needs. We conducted a comprehensive groundwater survey in the Mekong River floodplain, comprising an area of 3700 km~2 (131 samples, 30 parameters). Seasonal fluctuations were also studied. Arsenic ranged from 1 to 1340 μg L~(-1) (average 163 μg L~(-1)), with 48% exceeding 10 μg L~(-1). Elevated manganese levels (57% > 0.4 mg L~(-1)) are posing an additional health threat to the 1.2 million people living in this area. With 350 people km~(-2) potentially exposed to chronic arsenic poisoning, the magnitude is similar to that of Bangladesh (200 km~(-2)). Elevated arsenic levels are sharply restricted to the Bassac and Mekong River banks and the alluvium braided by these rivers (Kandal Province). Arsenic in this province averaged 233 μg L~(-1) (median 100 μg L~(-1)), while concentrations to the west and east of the rivers were < 10 μg L~(-1). Arsenic release from Holocene sediments between the rivers is most likely caused by reductive dissolution of metal oxides. Regions exhibiting low and elevated arsenic levels are co-incident with the present low relief topography featuring gently increasing elevation to the west and east of a shallow valley—understood as a relict of pre-Holocene topography. The full georeferenced database of groundwater analysis is provided as Supporting Information.
机译:柬埔寨已发现地下水被砷污染,那里约有100,000口家庭用水井用于饮用水需求。我们在湄公河漫滩进行了一次全面的地下水调查,面积为3700 km〜2(131个样本,30个参数)。还研究了季节性波动。砷的范围为1至1340μgL〜(-1)(平均163μgL〜(-1)),其中48%的砷超过10μgL〜(-1)。锰水平升高(57%> 0.4 mg L〜(-1))对居住在该地区的120万人构成了另外的健康威胁。可能有350人km〜(-2)可能遭受慢性砷中毒,其规模类似于孟加拉国(200 km〜(-2))。升高的砷含量被严格限制在Bassac和湄公河两岸以及由这些河流编织的冲积层(Kandal Province)。该省的砷平均含量为233μgL〜(-1)(中位数为100μgL〜(-1)),而河流西部和东部的砷浓度均小于10μgL〜(-1)。从河流之间的全新世沉积物中释放出的砷很可能是由于金属氧化物的还原性溶解引起的。砷含量低和升高的地区与目前的低起伏地貌同时发生,其特征是浅谷西部和东部的海拔逐渐升高,这被认为是全新世前地形的遗迹。完整的地下水分析地理参考数据库作为支持信息提供。

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