Nair Hema C, Padmalal D, Joseph Ammini
School of Environmental Studies, CUSAT, Kochi, 682022, Kerala, India,
Environ Monit Assess. 2015 Feb;187(2):48. doi: 10.1007/s10661-014-4164-0. Epub 2015 Feb 1.
The paper deals with the hydrochemical characterization and water quality assessment of springs emerging from the Archaean crystalline basements at the foothills of Western Ghat mountains in the highlands and Neogene sedimentary formations in the coastal lowlands of Kerala in south west India. A total of 19 springs from two important river basins of southern Kerala such as Ithikkara and Kallada river basins were studied for 18 physico-chemical (temperature, pH, electrical conductivity (EC), total dissolved solids (TDS), dissolved oxygen (DO), total hardness (TH), Na(+), K(+), Ca(2+), Mg(2+), CO3 (2-), HCO3 (-), Cl(-), SO4 (2-) , NO3 (-), SiO2, Fe(2+), and F(-) ) as well as bacteriological parameters. The discharge computations show that free-falling type of springs in the area discharge about 256.23 million liters of water a year. A comparative study between the spring water samples of highland and lowland regions reveal that the quality of spring water, except pH and bacteriological contents, satisfies the standards set by the Bureau of Indian Standards and World Health Organization for drinking water. Spring water samples collected from the lowlands register high value of Na(+) and Cl(-) compared with the highlands. Bicarbonate, Ca(2+), Mg(2+), and K(+) values are high in highland than lowland springs. The present study reveals that the spring water sources in the region can be developed as an alternate source for drinking water, provided pH correction and proper disinfection are done prior to its end use.
本文研究了印度西南部喀拉拉邦高地西高止山脉山麓太古宙结晶基底涌出的泉水以及沿海低地新近纪沉积地层的水化学特征和水质评估。对喀拉拉邦南部两个重要流域(如伊蒂卡拉河和卡拉达河流域)的19处泉水进行了18项物理化学参数(温度、pH值、电导率(EC)、总溶解固体(TDS)、溶解氧(DO)、总硬度(TH)、Na⁺、K⁺、Ca²⁺、Mg²⁺、CO₃²⁻、HCO₃⁻、Cl⁻、SO₄²⁻、NO₃⁻、SiO₂、Fe²⁺和F⁻)以及细菌学参数的研究。流量计算表明,该地区自由落体式泉水每年的出水量约为2.5623亿升。高地和低地地区泉水样本的对比研究表明,除pH值和细菌学含量外,泉水水质符合印度标准局和世界卫生组织制定的饮用水标准。与高地相比,从低地采集的泉水样本中Na⁺和Cl⁻含量较高。高地泉水的碳酸氢根、Ca²⁺、Mg²⁺和K⁺值高于低地泉水。本研究表明,该地区的泉水水源可开发为替代饮用水源,但在最终使用前需进行pH值校正和适当消毒。