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印度泰米尔纳德邦坎奇普兰区曼巴卡姆小流域的水文地球化学与地质调查。

A hydrochemical and geological investigation on the Mambakkam mini watershed, Kancheepuram District, Tamil Nadu.

机构信息

Centre for Water Resources, Anna University, Chennai, India.

出版信息

Environ Monit Assess. 2012 May;184(5):3293-306. doi: 10.1007/s10661-011-2189-1. Epub 2011 Jun 29.

Abstract

The hydrochemical characterization of groundwater is important to bring out its nature and usefulness. The main objective of this paper was to discuss the major ion chemistry of groundwater in the Mambakkam mini watershed. Besides its semi-arid nature, rapid socioeconomic development encourages a greater demand for water, which leads to uncontrolled groundwater development. The groundwater of the study area is characterized by the dominance of alkaline earth (Ca(2+), Mg(2+)) and strong acids (Cl(-), SO(4)(-)) over alkalies (Na(+), K(+)) and weak acids (HCO(3)(-), CO(3)(-)) during both post-monsoon and pre-monsoon seasons of the year 2010, based on the hydrochemical facies. These have been probably derived from natural chemical weathering of rock minerals, ion exchange and anthropogenic activities of the fertilizer source. The classification based on the total hardness reveals that a majority of groundwater samples fall in the hard to very hard category during the pre-monsoon season. Based on the values of EC, SAR and RSC and the diagrams of USSL and Wilcox, most of the groundwater samples range from excellent to permissible for irrigation purposes, with a low alkalinity and high salinity hazard, except for a few samples in the study area.

摘要

地下水的水化学特征对于揭示其性质和用途非常重要。本文的主要目的是讨论 Mambakkam 小流域地下水的主要离子化学。除了半干旱的性质外,快速的社会经济发展鼓励了对水的更大需求,这导致了对地下水的不受控制的开发。根据水化学相,研究区地下水的特征是在 2010 年的后季风和前季风季节中,碱性土(Ca(2+)、Mg(2+))和强酸(Cl(-)、SO(4)(-))对碱性土(Na(+)、K(+))和弱酸(HCO(3)(-)、CO(3)(-))的支配。这些可能是源于岩石矿物的天然化学风化、离子交换和肥料源的人为活动。基于总硬度的分类表明,在前季风季节,大多数地下水样本属于硬水到极硬水类别。根据 EC、SAR 和 RSC 的值以及 USSL 和 Wilcox 图,除了研究区的少数样本外,大多数地下水样本的灌溉用途范围从优秀到可接受,具有低碱度和高盐度危害。

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