印度南部卡纳塔克邦乌杜皮地区沿海含水层地下水和盐水入侵的水文地球化学评估

IF 1.827 Q2 Earth and Planetary Sciences Arabian Journal of Geosciences Pub Date : 2024-09-19 DOI:10.1007/s12517-024-12082-4
Ayushi Agarwal, Ratnakar Dhakate
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引用次数: 0

摘要

在全球范围内,地下水被广泛用于饮用、灌溉和工业活动。然而,地下水的质量正在严重恶化,尤其是在盐水渗透成为主要问题的沿海地区。本研究对印度卡纳塔克邦乌杜皮地区的沿海含水层(面积约 80 平方公里)进行了调查,对季风前后 57 个空间分布位置的地下水样本进行了水文地球化学分析。分析的主要阴阳离子参数包括 Cl-、HCO₃-、SO42-、NO₃-、Na+、Ca2+、K+ 和 Mg2+。分析结果显示,pH 值范围在 2.9 至 8.3 之间,呈酸性至微碱性,总溶解固体 (TDS) 浓度范围在 110 至 6683 毫克/升之间,主要显示出海岸线的盐碱化特征。水文地质化学评估(包括查达地形图)在大多数样本中发现了 Na-Cl 型水,表明受到盐度的影响。根据渗透指数值,季风前和季风后分别约有 21% 和 67% 的样本不适合灌溉,其中 2% 至 3% 的样本具有高盐度危害。季风前和季风后时期相关系数的变化表明,盐水入侵、淡水补给和地球化学相互作用影响着沿岸地下水系统。Na⁺ 与 Cl- 的摩尔比表明存在反向阳离子交换过程,突出了盐水与淡水之间复杂的相互作用。总体而言,季风前和季风后分别有 79% 和 80% 的样本被认为适合灌溉,而 21% 和 20% 的样本被归类为完全不适合灌溉。
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Hydrogeochemical assessment of groundwater and saline water intrusion along the coastal aquifer in Udupi region of Karnataka (southern India)

Groundwater is extensively utilized for drinking, irrigation, and industrial activities globally. However, its quality is deteriorating significantly, particularly in coastal regions where saline water infiltration is a major issue. This study investigates the coastal aquifer of Udupi district in Karnataka, India, covering approximately 80 km2, through hydro-geochemical analysis of groundwater samples from 57 spatially distributed locations, pre- and post-monsoon. The major anion and cation parameters analyzed include Cl, HCO₃, SO42−, NO₃, Na+, Ca2+, K+, and Mg2+. The analysis revealed a pH range of 2.9 to 8.3, indicating acidic to slightly alkaline conditions, and total dissolved solids (TDS) concentrations ranging from 110 to 6683 mg/L, predominantly showing saline characteristics toward the coastline. Hydrogeochemical assessment, including Chadha’s plot, identified Na-Cl type water in most samples, indicating the influence of salinity. Approximately 21% of pre-monsoon and 67% of post-monsoon samples were deemed unsuitable for irrigation based on permeability index values, with 2 to 3% exhibiting high salinity hazards. The variation in correlation coefficients between pre-monsoon and post-monsoon periods suggests that saline water intrusion, freshwater recharge, and geochemical interactions influence the coastal groundwater system. The molar ratio of Na⁺ to Cl suggested a reverse cation exchange process, highlighting the complex interactions between saline and freshwater. Overall, 79% of pre-monsoon and 80% of post-monsoon samples were deemed suitable for irrigation, while 21% and 20% were classified as completely unsuitable, respectively.

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来源期刊
Arabian Journal of Geosciences
Arabian Journal of Geosciences GEOSCIENCES, MULTIDISCIPLINARY-
自引率
0.00%
发文量
1587
审稿时长
6.7 months
期刊介绍: The Arabian Journal of Geosciences is the official journal of the Saudi Society for Geosciences and publishes peer-reviewed original and review articles on the entire range of Earth Science themes, focused on, but not limited to, those that have regional significance to the Middle East and the Euro-Mediterranean Zone. Key topics therefore include; geology, hydrogeology, earth system science, petroleum sciences, geophysics, seismology and crustal structures, tectonics, sedimentology, palaeontology, metamorphic and igneous petrology, natural hazards, environmental sciences and sustainable development, geoarchaeology, geomorphology, paleo-environment studies, oceanography, atmospheric sciences, GIS and remote sensing, geodesy, mineralogy, volcanology, geochemistry and metallogenesis.
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