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Shallow alluvial aquifers for drinking and agricultural purposes: a case study from Jia Bharali River Basin, North Brahmaputra Plain, India

机译:用于饮用和农业用途的浅层冲积含水层:以印度北布拉马普特拉平原的贾巴拉河河流域为例

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A preliminary assessment of groundwater quality for drinking and irrigational purposes in the lower Jia Bharali river catchment and adjoining areas of North Brahmaputra Plain, India, was carried out with respect to major cations, anions, and trace elements. Water samples from 50 shallow alluvial dug wells were collected in wet and dry seasons for a period of 3 hydrological years (2008-2011). Seasonal analysis showed major cation and anion contents in a definite trend across the basin as Ca: 4.2-68.9 mg/L>Na 1.9-62.5 mg/L>Mg:1.0-29.2 mg/L>K (1.3-26.1 mg/L) and HCO_3 (16-118 mg/L)>Cl (2.8-138.3 mg/L)>SO_4 (1.2-99.5 mg/L)>PO_4 (BDL-1.50 mg/L)>NO_3 (BDL-1.20 mg/L) within WHO acceptable limit for drinking water in all the seasons. Low SAR (< 10) and RSC (< 1.25 meq/L) values of shallow wells showed their suitability as potential source for agricultural purposes, while a few wells were found unsuitable with respect to Na% > 60% and Kelly's Index > 1. However, majority of the wells were found not suitable for drinking as well as irrigational purposes due to the presence of trace elements Cd (BDL-0.070 mg/L), Cr (BDL-0.24 mg/L), Fe (0.10-11.76 mg/L), Mn (BDL-1.37 mg/L), Ni (BDL-0.18 mg/L), and Pb (BDL-0.22 mg/L) beyond their respective standard limits. Piper trilinear diagram identified the major hydrochemical facies of the groundwater as alkaline earths (Ca, Mg) and weak acids (HCO_3) over alkalis (Na, K) and strong acids (SO_4, Cl).
机译:初步评估了印度北部贾布拉普特拉特拉平原及其毗邻地区饮用水和灌溉目的地下水水质中的主要阳离子,阴离子和微量元素。在3个水文年(2008-2011年)的干燥和潮湿季节,从50个浅冲积挖掘井中收集水样。季节性分析显示,整个盆地内主要阳离子和阴离子含量呈一定趋势,Ca:4.2-68.9 mg / L> Na 1.9-62.5 mg / L> Mg:1.0-29.2 mg / L> K(1.3-26.1 mg / L )和HCO_3(16-118 mg / L)> Cl(2.8-138.3 mg / L)> SO_4(1.2-99.5 mg / L)> PO_4(BDL-1.50 mg / L)> NO_3(BDL-1.20 mg / L) )在所有季节都在WHO可接受的饮用水限制内。浅井的低SAR(<10)和RSC(<1.25 meq / L)值表明它们适合作为农业用途的潜在来源,而发现有几口井的Na%> 60%和Kelly's Index> 1。但是,由于存在微量元素Cd(BDL-0.070 mg / L),Cr(BDL-0.24 mg / L),Fe(0.10-11.76 mg),发现大多数井都不适合饮用和灌溉。 / L),Mn(BDL-1.37 mg / L),Ni(BDL-0.18 mg / L)和Pb(BDL-0.22 mg / L)超出各自的标准限值。 Piper三线性图确定了地下水的主要水化学相为碱土(Na,K)和强酸(SO_4,Cl)上的碱土(Ca,Mg)和弱酸(HCO_3)。

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