Division of Agricultural Engineering, Indian Agricultural Research Institute, New Delhi, India.
Environ Manage. 2010 Mar;45(3):640-50. doi: 10.1007/s00267-010-9436-z. Epub 2010 Feb 4.
The groundwater quantity and quality scenario is of much concern in the National Capital Territory of Delhi, India, which necessitates an investigation to envisage the extent of spatial variability of groundwater depth and pollutant concentration levels in this region. Therefore, in this study, an effort was made to generate the spatial variability map of groundwater depth and quality parameters (viz. chloride, electrical conductivity, fluoride, magnesium, and nitrate). Ordinary kriging was used to analyze the spatial variability of groundwater depth and quality parameters, whereas indicator kriging was used to analyze groundwater quality parameters equal to or greater than the pollution threshold values. It was observed that the semivariogram parameters fitted well in the exponential model for water depth and in the spherical model for water quality parameters. The generated spatial variability maps indicated that in 43% of the study area, groundwater depth was within 20 m. The salinity level was higher than 2.5 dS m(-1) in 69% of the study area and the nitrate concentration exceeded 45 mg l(-1) in 36% of the area. The probability maps showed that about 24% of the area had the highest probability (0.8-1.0) of exceedence of the threshold electrical conductivity value and an area of 2% exhibited the highest probability of exceedence of the threshold value of nitrate concentration in the groundwater. The generated spatial variability and probability maps will assist water resource managers and policymakers in development of guidelines in judicious management of groundwater resources for agricultural and drinking purposes in the study area.
印度首都德里地区非常关注地下水的数量和质量状况,这就需要进行调查,以预测该地区地下水深度和污染物浓度水平的空间变异性程度。因此,在本研究中,努力生成了地下水深度和质量参数(即氯化物、电导率、氟化物、镁和硝酸盐)的空间变异性图。普通克里金用于分析地下水深度和质量参数的空间变异性,而指示克里金则用于分析等于或大于污染阈值的地下水质量参数。观察到,半变异函数参数很好地适合于水深的指数模型和水质参数的球状模型。生成的空间变异性图表明,在研究区域的 43%范围内,地下水深度在 20 米以内。在研究区域的 69%范围内,盐度高于 2.5 dS m(-1),在 36%的区域内,硝酸盐浓度超过 45 mg l(-1)。概率图显示,约 24%的区域具有最高的超标概率(0.8-1.0),即超过阈值电导率值,而 2%的区域则表现出最高的超标概率,即超过地下水硝酸盐浓度的阈值。生成的空间变异性和概率图将有助于水资源管理者和政策制定者制定明智管理地下水资源的指南,以用于农业和饮用水目的。