Department of Environmental Science, Bangalore University, Bangalore, 560 056, India.
Environ Monit Assess. 2011 Feb;173(1-4):459-87. doi: 10.1007/s10661-010-1399-2. Epub 2010 Mar 17.
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. Since the quantity and quality of water available for irrigation in India is variable from place to place, groundwater quality in the Markandeya River basin was evaluated for its suitability for drinking and irrigation purposes by collecting 47 open and bore-well samples during the post-monsoon period of 2008. The quality assessment was made by estimating pH, electrical conductivity, total dissolved solids, hardness, and alkalinity besides major cations (Na+, K+, Ca2+, and Mg2+) and anions (HCO3-, Cl-, SO4(2-), PO4(3-), F-, and NO3-). Based on these analyses, irrigation quality parameters like, sodium absorption ratio, %Na, residual sodium carbonate, residual sodium bicarbonate, chlorinity index, soluble sodium percentage, non-carbonate hardness, potential salinity, permeability index, Kelley's ratio, magnesium hazard/ratio, index of base exchange, and exchangeable sodium ratio were calculated. According to Gibbs' ratio, majority of water samples fall in the rock dominance field. The groundwater samples were categorized as normal chloride (95.75%), normal sulfate (95.75%), and normal bicarbonate (61.70%) water types based on Cl, SO4, and HCO3 concentrations. Based on the permeability index, majority of the samples belongs to classes 1 and 2, suggesting the suitability of groundwater for irrigation. The negative index of base exchange indicates the existence of chloro-alkaline disequilibrium (indirect base exchange reaction) existing in majority of the samples (68.08%) from the study area.
马坎德雅河流域的地理位置在北纬 15°56' 至 16°08' 和东经 74°37' 至 74°58' 之间,位于卡纳塔克邦北部贝尔高姆区的中心地带。由于印度各地可用于灌溉的水量和水质不同,因此在 2008 年后季风期收集了 47 个露天和钻孔井样本,评估了马坎德雅河流域的地下水质量,以确定其是否适合饮用和灌溉。通过评估 pH 值、电导率、总溶解固体、硬度和碱度以及主要阳离子(Na+、K+、Ca2+ 和 Mg2+)和阴离子(HCO3-、Cl-、SO4(2-)、PO4(3-)、F- 和 NO3-)来进行质量评估。基于这些分析,计算了灌溉质量参数,如钠吸收率、%Na、剩余碳酸钠、剩余碳酸氢钠、氯化物指数、可溶性钠百分比、非碳酸盐硬度、潜在盐度、渗透率指数、凯利比、镁危害/比、碱基交换指数和可交换钠比。根据 Gibbs 比,大多数水样都落入岩石主导领域。根据 Cl、SO4 和 HCO3 浓度,地下水样本被归类为正常氯化物(95.75%)、正常硫酸盐(95.75%)和正常碳酸氢盐(61.70%)水类型。根据渗透率指数,大多数样本属于第 1 类和第 2 类,表明地下水适合灌溉。负碱基交换指数表明研究区多数样本(68.08%)存在氯-堿失衡(间接碱基交换反应)。