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流域地貌对纳迪亚地区砷分布的影响。

Influence of basin-wide geomorphology on arsenic distribution in Nadia district.

机构信息

Department of Chemistry, University of Kalyani, Kalyani, West Bengal, India.

Department of Chemistry, University of Kalyani, Kalyani, West Bengal, India; Department of Geology & Geophysics, Texas A&M University, College Station, TX, 77843-3115, USA.

出版信息

Environ Res. 2021 Jan;192:110314. doi: 10.1016/j.envres.2020.110314. Epub 2020 Oct 8.

Abstract

The present study depicts the geospatial relation between basinal geomorphology and heterogeneous arsenic (As) distribution in the Bengal Delta Plain (BDP). The distribution pattern largely varies throughout the study area (higher: Karimpur-II As average 214.73 μgL; lower: Tehatta As average 27.84 μgL). Both safe (low As) and unsafe (high As) areas are identified within the single shallow aquifer (<50 m), where they are in close vicinity. Statistical analysis shows that Padma river basin is the most contaminated (As avg. 214.7 ± 160 μgL) and Churni-Ichhamati river basin (As avg. 108.54 ± 89.43 μgL) is the least contaminated with groundwater As. Moreover, the role of geomorphological features influencing the geospatial distribution of As has been studied and meandering features are found to correlate with high As wells (r = 0.52), whereas, natural levees are correlated with safer wells (r = 0.57). In the meandering features, the deposition of sedimentary organic matter (SOM) facilitates the reduction of As bearing Fe(III) oxy-hydroxides and subsequent higher As mobilization. In natural levees, surface derived labile organic matter (DOC and FOM, Fresh Organic Matter) from different land-use patterns (Habitation, degraded waterbodies, cattle dwelling, sanitation, etc.) is transported to shallow aquifers (notably protein rich leakage sewage). The fresh organic carbon transported to the shallow aquifers, thereby triggering As release by microbe-mediated reductive dissolution of hydrated Fe(III)-oxides (HFO). Iron reduction (mostly amorphous) is playing an important role in the release of As depending on basin-wise sedimentation pattern, local recharge, accumulation of silt/clay/micas at the top with corresponding reactive oxidation of organic carbon. These are important components and often helping the cyclic water-rock interaction of As causing such heterogeneous geospatial distribution. The delineation of aquifer with regard to safer and unsafe areas would immensely help to supply safe drinking water to the rural community.

摘要

本研究描绘了孟加拉三角洲平原(BDP)盆地地貌与砷(As)非均一分布的地理空间关系。研究区的分布模式差异较大(较高:Karimpur-II 的平均砷含量为 214.73 μgL;较低:Tehatta 的平均砷含量为 27.84 μgL)。在单一浅层含水层(<50 m)内,既有安全(低砷)区域,也有不安全(高砷)区域,且二者位置相近。统计分析表明,帕德玛河流域的污染最严重(平均砷含量 214.7 ± 160 μgL),而 Churni-Ichhamati 河流域的污染程度最低(平均砷含量 108.54 ± 89.43 μgL)。此外,本研究还研究了地貌特征对砷地理空间分布的影响,发现曲流特征与高砷水井相关(r = 0.52),而自然堤岸则与安全水井相关(r = 0.57)。在曲流特征中,沉积有机质(SOM)的沉淀促进了含砷的三价铁(Fe(III))水合氢氧化物的还原和随后的更高砷迁移。在自然堤岸,来自不同土地利用模式(居住、退化水体、牛舍、卫生等)的地表衍生的可利用有机物质(DOC 和 FOM,新鲜有机物质)被输送到浅层含水层(特别是富含蛋白质的渗漏污水)。输送到浅层含水层的新鲜有机碳,从而通过微生物介导的含水 Fe(III)-氧化物(HFO)的还原溶解触发砷释放。铁还原(主要是非晶态)在砷释放中起着重要作用,这取决于流域范围内的沉降模式、局部补给、顶部的淤泥/粘土/云母的积累以及相应的有机碳的氧化反应。这些都是重要的组成部分,通常有助于砷的水岩循环相互作用,导致这种非均一的地理空间分布。对安全和不安全区域的含水层进行划分,将极大地有助于为农村社区提供安全饮用水。

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