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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Comparison of arsenic concentrations in simultaneously-collected groundwater and aquifer particles from Bangladesh, India, Vietnam, and Nepal
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Comparison of arsenic concentrations in simultaneously-collected groundwater and aquifer particles from Bangladesh, India, Vietnam, and Nepal

机译:来自孟加拉国,印度,越南和尼泊尔的同时采集的地下水和含水层颗粒中的砷浓度比较

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One of the reasons the processes resulting in As release to groundwater in southern Asia remain poorly understood is the high degree of spatial variability of physical and chemical properties in shallow aquifers. In an attempt to overcome this difficulty, a simple device that collects groundwater and sediment as a slurry from precisely the same interval was developed in Bangladesh. Recently published results from Bangladesh and India relying on the needle-sampler are augmented here with new data from 37 intervals of grey aquifer material of likely Holocene age in Vietnam and Nepal. A total of 145 samples of filtered groundwater ranging in depth from 3 to 36 m that were analyzed for As (1-1000 mu g/L), Fe (0.01-40 mg/L), Mn (0.2-4 mg/L) and S (0.04-14 mg/L) are compared. The P-extractable (0.01-36 mg/kg) and HCl-extractable As (0.04-36 mg/kg) content of the particulate phase was determined in the same suite of samples, in addition to Fe(II)/Fe ratios (0.2-1.0) in the acid-leachable fraction of the particulate phase. Needle-sampler data from Bangladesh indicated a relationship between dissolved As in groundwater and P-extractable As in the particulate phase that was interpreted as an indication of adsorptive equilibrium, under sufficiently reducing conditions, across 3 orders of magnitude in concentrations according to a distribution coefficient of 4 mL/g. The more recent observations from India, Vietnam and Nepal show groundwater As concentrations that are often an order of magnitude lower at a given level of P-extractable As compared to Bangladesh, even if only the subset of particularly reducing intervals characterized by leachable Fe(II)/Fe >0.5 and dissolved Fe >0.2 mg/L are considered. Without attempting to explain why As appears to be particularly mobile in reducing aquifers of Bangladesh compared to the other regions, the consequences of increasing the distribution coefficient for As between the particulate and dissolved phase to 40 mL/g for the flushing of shallow aquifers of their initial As content are explored. (C) 2008 Elsevier Ltd. All rights reserved.
机译:导致人们对南亚向地下水释放砷的过程了解甚少的原因之一是浅层含水层中物理和化学性质的高度空间变异性。为了克服这一困难,孟加拉国开发了一种简单的设备,该设备可以从完全相同的时间间隔中收集作为淤浆的地下水和沉积物。孟加拉国和印度最近依靠针头采样器发布的结果在这里得到了新数据的补充,该数据来自越南和尼泊尔可能有全新世年龄的37个灰层含水层材料。总共145个深度为3至36 m的过滤地下水样本,分析了As(1-1000μg / L),Fe(0.01-40 mg / L),Mn(0.2-4 mg / L)比较S和0.04-14 mg / L。除了Fe(II)/ Fe之比,还测定了同一套样品中颗粒相的P可萃取(0.01-36 mg / kg)和HCl可萃取As(0.04-36 mg / kg)含量( 0.2-1.0)在颗粒相的可酸浸部分中。来自孟加拉国的针头采样数据表明,在溶解度充分降低的情况下,根据分配系数,在溶解度达到3个数量级的情况下,地下水中溶解态As与颗粒相中P可萃取As之间的关系被解释为吸附平衡的指示。 4毫升/克。来自印度,越南和尼泊尔的最新观测结果表明,在给定的P可萃取水平下,地下水As的浓度通常比孟加拉国低一个数量级,即使只有以可浸出Fe(II)为特征的特别缩短的时间间隔的子集)/ Fe> 0.5和溶解的Fe> 0.2 mg / L。在不试图解释为什么与其他地区相比,砷在减少孟加拉国含水层中似乎特别可移动的情况下,将颗粒和溶解相之间的砷分配系数提高到40 mL / g的后果,以便冲洗其浅层含水层。探索初始As内容。 (C)2008 Elsevier Ltd.保留所有权利。

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