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Study on Saline Water intrusion into the Shallow Coastal Aquifers of Periyar River Basin, Kerala using Hydrochemical and Electrical Resistivity Methods

机译:康拉河流域盐水侵入盐水侵入研究,喀拉拉邦采用水化学和电阻率法研究

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Seawater intrusion generally occurs when withdrawal of fresh groundwater from coastal aquifers results in declining groundwater levels, facilitating lateral and/or vertical migration of saline water causing deterioration of groundwater quality. Electrical resistivity sounding techniques and hydrochemical studies are widely used to determine the interaction between groundwater and saline water/seawater in coastal aquifers. Vertical electrical soundings were carried out at 15 locations in the midland and coastal plain reaches of Periyar River basin in central Kerala, India (9° 55'-10° 20' N latitude and 76° 05'-76° 25' E longitude) using CRM 500 model aquameter. In-situ water quality parameters of water samples from 63 shallow well were also measured using handheld multi-parameter instrument. The cation and anion content of selected water samples (32 nos.) were also determined. Electrical resistivity profiles were interpreted qualitatively and quantitatively to obtain nature and thickness of different resistivity layers. The depth to fresh-saline water interface was delineated from resistivity model. The study indicates majority of the curves obtained are Q type with 3 layers. The depth to saline-fresh water interface varied from <1 to 5 m at different locations. The high salinity clay horizons are identified at various depths. Hydrochemical data was analysed using hill-piper diagram and statistical plots to understand groundwater-seawater mixing/interaction in the coastal aquifers. The dominant groundwater type is Na-Cl followed by Mg-Cl at few places. Higher pH, EC and TDS is noted in the western part towards seaward side. Turbidity levels are found increasing towards the southern part. The TA, TH, Ca~(2+),Mg~(2+),K~+ content of the water samples found increasing towards southwest parts. The Na~+, CI" and (SO_4)~2' content is found higher in the northwestern parts.
机译:当从沿海含水层撤离新鲜地下水时,海水入侵通常会导致地下水位下降,促进盐水的横向和/或垂直迁移,导致地下水质量恶化。电阻率探测技术和水化学研究被广泛用于确定地下水和盐水/海水在沿海含水层之间的相互作用。在印度喀拉拉邦市中心河流河流域中德兰和沿海平原地区的15个地点进行了垂直电影探测(9°55'-10°20'N纬度和76°05'-76°25'E经度)使用CRM 500模型水电图。使用手持式多参数仪器,还测量了63个浅孔的原位水质参数。还测定了所选水样(32号)的阳离子和阴离子含量。定性地解释电阻率曲线,并定量解释不同电阻率层的性质和厚度。从电阻率模型中描绘了新鲜盐水界面的深度。该研究表明,所获得的大部分曲线是Q型,具有3层。盐水 - 淡水界面的深度在不同位置的<1至5米之间变化。在各种深度识别高盐度粘土视野。使用Hill-Piper图分析了水化学数据和统计地块,以了解沿海含水层的地下水海水混合/相互作用。主导地下水型是Na-Cl,然后在几个地方接下来是Mg-Cl。在西部向海侧朝向海侧注意到pH值较高,EC和TDS。发现浊度水平朝向南部增加。水样的TA,Th,Ca〜(2 +),Mg〜(2 +),K〜+含量朝向西南部件增加。 Na〜+,CI“和(SO_4)〜2'含量在西北部件较高。

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