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Arsenic and Salinity Affected Groundwater in South-Western Bangladesh: An Assessment of Managed Aquifer Recharge and Sub-Surface Arsenic Removal as Mitigation Techniques

机译:孟加拉国西南部受砷和盐度影响的地下水:作为缓解技术的含水层补给和地下砷去除的评估

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摘要

Naturally occurring groundwater arsenic contamination is a major problem in Narail, Bangladesh. Analyses of 32 groundwater samples showed arsenic concentrations ranged 20.33–158.90 µg/L. Relatively deeper aquifer (>45 m depth) in addition to arsenic, is contaminated with substantial amount of salinity. Electrical conductivity (EC) ranged 1.01–7.90 mS/cm indicating the enormity of salinity. The groundwater is mainly Na–Cl to Na–HCO3 type, and is SO4 limited. This research demonstrates the effectiveness of two mitigation techniques (i) managed aquifer recharge (MAR) and (ii) sub-surface arsenic removal (SAR) for in-situ salinity and arsenic treatment of contaminated groundwater. A two-year long experiment revealed that the MAR system was effective in reducing both salinity and arsenic. Groundwater EC reduced 72–81 from an initial value of 3.4 mS/cm to less than 1 mS/cm. Arsenic concentration dropped below 50 µg/L from an initial concentration of 100 µg/L. The SAR system reduced arsenic concentration below 50 µg/L from an initial concentration of 100 µg/L. The system was capable of yielding 1500 liters of arsenic safe water when injected volume of oxygen saturated water was 2000 liters indicating 70–80 recovery. Both systems can provide 1000 liters of safe drinking water at a cost of $2.00.
机译:天然发生的地下水砷污染是孟加拉国纳雷尔的一个主要问题。对32个地下水样本的分析显示,砷浓度在20.33-158.90微克/升之间,除砷外,相对较深的含水层(>45米深)也受到大量盐度的污染。电导率 (EC) 范围为 1.01–7.90 mS/cm,表明盐度巨大。地下水主要为Na-Cl至Na-HCO3型,SO4含量有限。这项研究证明了两种缓解技术(i)管理含水层补给(MAR)和(ii)地下除砷(SAR)对受污染地下水的原位盐度和砷处理的有效性。一项为期两年的实验表明,MAR系统可有效降低盐度和砷。地下水EC从初始值3.4 mS/cm降低到1 mS/cm以下,降低了72-81%。砷浓度从初始浓度100 μg/L降至50 μg/L以下。SAR系统将砷浓度从初始浓度100 μg/L降低到50 μg/L以下。当注入的氧饱和水量为 2000 升时,该系统能够产生 1500 升砷安全水,表明回收率为 70-80%。这两个系统都可以提供 1000 升安全饮用水,成本为 2.00 美元。

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