Geochemistry of groundwater, Markandeya River Basin, Belgaum district, Karnataka State, India  

作　　者：Ravikumar P. Somashekar R.K. 

机构地区：[1]Department of Environmental Science, Bangalore University, Bangalore-560 056,India

出　　处：《Chinese Journal Of Geochemistry》2011年第1期51-74,共24页中国地球化学学报

摘　　要：The Markandeya River Basin stretches geographically from 15o56′ to 16o08′ N latitude and 74o37′ to 74o58′ E longitude, positioned in the midst of Belgaum district, in the northern part of Karnataka. The groundwater quality of 54 pre-monsoon samples in the Markandeya River Basin was evaluated for its suitability for drinking and irrigation purposes by estimating pH, EC, TDS, hardness and alkalinity besides major cations (Na+, K+, Ca2+, Mg2+) and anions (HCO3–, Cl–, SO42–, PO43-, F-, NO3–), boron, SAR, % Na, RSC, RSBC, chlorinity index, SSP, non-carbonate hardness, Potential Salinity, Permeability Index, Kelley’s ratio, Magnesium hazard and Index of Base Exchange. Negative Index of Base Exchange indicates the chloro-alkaline disequilibrium in the study area and the majority of water samples fall in the rock dominance field based on Gibbs’ ratio. Permeability indices of classes I and II suggest suitability of groundwater for irrigation. Based on Cl, SO4, HCO3 concentrations, water samples can be classified as normal chloride (96.3%) and normal sulfate (94.4%) and normal bicarbonate (44.4%) water types.The Markandeya River Basin stretches geographically from 15°56＇ to 16°08＇ N latitude and 74°37＇ to 74°58＇ E longitude, positioned in the midst of Belgaum district, in the northern part of Karnataka. The groundwater quality of 54 pre-monsoon samples in the Markandeya River Basin was evaluated for its suitability for drinking and irrigation purposes by estimating pH, EC, TDS, hardness and alkalinity besides major cations （Na＋, K＋, Ca2＋, Mg2＋） and anions （HCO3- , Cl-, SO42- , PO43- , F-, NO3-）, boron, SAR, % Na, RSC, RSBC, chlorinity index, SSP, non-carbonate hardness, Potential Salinity, Permeability Index, Kelley＇s ratio, Magnesium hazard and Index of Base Exchange. Negative Index of Base Exchange indicates the chloro-alkaline disequilibrium in the study area and the majority of water samples fall in the rock dominance field based on Gibbs＇ ratio. Permeability indices of classes I and II suggest suitability of groundwater for irrigation. Based on Cl, SO4, HCO3 concentrations, water samples can be classified as normal chloride （96.3%） and normal sulfate （94.4%） and normal bicarbonate （44.4%） water types.

关 键 词：水地球化学 流域 贝尔 纳塔 地下水水质 碳酸盐硬度 印度 碳酸氢钠 

分 类 号：P641.3[天文地球—地质矿产勘探]