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印度泰米尔纳德邦钦奈和蒂鲁瓦卢尔地区沿海含水层海水入侵的同位素特征、水化学和多元统计分析。

Isotopic signatures, hydrochemical and multivariate statistical analysis of seawater intrusion in the coastal aquifers of Chennai and Tiruvallur District, Tamil Nadu, India.

机构信息

Department of Applied Geology, School of Earth and Atmospheric Sciences, University of Madras, Guindy Campus, Chennai, Tamilnadu 600 025, India.

MOE Key Laboratory of Western China's Environmental System, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, PR China.

出版信息

Mar Pollut Bull. 2022 Jan;174:113232. doi: 10.1016/j.marpolbul.2021.113232. Epub 2021 Dec 22.

Abstract

In coastal aquifers, seawater intrusion is a significant groundwater issue. The research paper contributes to the understanding of the consequences of seawater intrusion in the Chennai coastal aquifer from Foreshore Estate to Thirunilai along the coastline. 110 groundwater samples were collected and analyzed for physicochemical parameters such as pH, (EC), (TDS), (TH), major anions (Cl, NO, HCO, and SO), and cations (Ca, Mg, Na, and K) during the pre-monsoon (June 2014) and post-monsoon (January 2015) seasons. Stable isotopic analyses of O were performed on 24 groundwater samples collected from various locations throughout the research region based on EC, TDS, Na, and Cl concentrations for both seasons. The stable isotopic composition of O and Deuterium in groundwater samples was determined for the study region. According to the Correlation matrix and Factor analysis, the main contributors to groundwater salinity as a result of seawater intrusion into the coastal aquifer are EC, TDS, Na, and Cl. GMWL exhibits a similar pattern, and the samples have been classified into various molar ratio diagrams to identify seawater intrusions for better evaluation. The result revealed that seasonal, geogenic, and anthropogenic factors always make a significant contribution to the heterogeneous chemistry of groundwater.

摘要

在沿海含水层中,海水入侵是一个重大的地下水问题。本研究论文有助于了解钦奈沿海含水层中海水入侵的后果,该含水层从 Foreshore Estate 延伸到沿海的 Thirunilai。在 Pre-Monsoon(2014 年 6 月)和 Post-Monsoon(2015 年 1 月)两个季节,收集并分析了 110 个地下水样本的理化参数,如 pH 值、电导率(EC)、总溶解固体(TDS)、总硬度(TH)、主要阴离子(Cl、NO、HCO 和 SO)和阳离子(Ca、Mg、Na 和 K)。根据 EC、TDS、Na 和 Cl 浓度,对研究区域内各个位置采集的 24 个地下水样本进行了 O 的稳定同位素分析。研究区域内地下水样本的 O 和氘的稳定同位素组成。根据相关矩阵和因子分析,导致沿海含水层海水入侵的地下水盐分的主要贡献者是 EC、TDS、Na 和 Cl。GMWL 呈现出相似的模式,并且将样本分类为各种摩尔比图,以识别海水入侵,从而进行更好的评估。结果表明,季节性、地质成因和人为因素总是对地下水的非均相化学性质有重要贡献。

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