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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Arsenic and other drinking water quality issues, Muzaffargarh District, Pakistan
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Arsenic and other drinking water quality issues, Muzaffargarh District, Pakistan

机译:巴基斯坦穆扎法尔加尔区砷和其他饮用水水质问题

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In 49 samples of groundwater, sampled in Muzaffargarh District of south-western Punjab, central Pakistan. concentrations of As exceeded the World Health Organisation provisional guideline value. and United States, Environmental Protection Agency (USEPA) Maximum Contaminant Level (MCL), of 10 mug L-1 in 58% of samples and reached up to 906 mug L-1. In this semi-arid region canal irrigation has lead to widespread water-logging. and evaporative concentration of salts has the potential to raise As concentrations in shallow groundwater well above 10 mug L-1. In fact, in rural areas, concentrations stay below 25 mug L-1 because As in the oxic shallow groundwater. and in recharging water. is sorbed to aquifer sediments. In some urban areas, however, shallow groundwater is found to contain elevated levels of As. The spatial distribution of As-rich shallow groundwater indicates either direct contamination with industrial or agricultural chemicals, or some other anthropogenic influence. Geochemical evidence suggests that pollutant organics from unconfined sewage and other sources drives reduction of hydrous ferric oxide (HFO) releasing sorbed As to shallow groundwater. The situation is slightly less clear for seven wells sampled which tap deeper groundwater. all of which were found with >50 pg L-1 As. Here As concentrations seem to increase with depth and differing geochemical signatures are seen, suggesting that As concentrations in older groundwater may be governed by different processes. Other data on parameters of potential concern in drinking water are discussed briefly at the end of the paper. (C) 2004 Elsevier Ltd. All rights reserved.
机译:在巴基斯坦中部西南旁遮普邦的穆扎法加尔区(Muzaffargarh)抽取的49个地下水样本中。砷的浓度超过了世界卫生组织的暂行准则值。美国和美国环境保护署(USEPA)的最大污染物水平(MCL)为58%样品中的10杯L-1,最高达到906杯L-1。在这个半干旱地区,渠道灌溉导致普遍的涝灾。盐的蒸发浓度有可能使砷在浅层地下水中的浓度升高到远高于10杯L-1。实际上,在农村地区,其浓度保持在25马克L-1以下,这是因为在有氧浅层地下水中的砷含量较高。并补充水。被吸收到含水层沉积物中。但是,在某些城市地区,发现浅层地下水中砷含量较高。富含砷的浅层地下水的空间分布表明工业或农业化学物质受到直接污染,或其他一些人为影响。地球化学证据表明,来自无限制污水和其他来源的污染物有机物推动了含水三氧化二铁(HFO)的减少,从而将吸附的砷释放到浅层地下水中。对于抽取了较深层地下水的7口采样井而言,情况还不太清楚。所有这些都被发现> 50 pg L-1 As。在这里,砷的浓度似乎随着深度的增加而增加,并且观察到不同的地球化学特征,这表明较老的地下水中的砷浓度可能受不同过程的控制。本文末尾简要讨论了饮用水中潜在关注参数的其他数据。 (C)2004 Elsevier Ltd.保留所有权利。

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