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Impact of urbanization on groundwater recharge and urban water balance for the city of Hyderabad, India

机译:印度海得拉巴城市化对地下水补给和城市水平衡的影响

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Groundwater recharge processes in an urban area are different than in non-urban areas. There are various new components that must be considered in the case of urban groundwater recharge in addition to the natural recharge from precipitation. These various components are estimated in this study based on the water balance equation for the Hyderabad city of India. Initially, urban recharge components including leakages from water supply network and sewage networks were calculated. To estimate the natural recharge from precipitation, actual evapotranspiration and surface runoff were estimated using remote sensing and GIS techniques. Results indicated that the urban recharge component of groundwater was more than ten times greater than the natural recharge. The net urban recharge component of groundwater was estimated to be approximately 568 mm yr-1 and the natural recharge component was observed to be 53 mm yr-1. Water inflow and outflow components were also estimated to provide the complete scenario of the total urban water balance of Hyderabad. This analysis has provided the information regarding the extent and intensity of percolation of urban contaminants into the aquifer.
机译:城市地区的地下水补给过程与非城市地区的地下水补给过程不同。在城市地下水补给中,除了来自降水的自然补给外,还必须考虑各种新的成分。在这项研究中,根据印度海得拉巴市的水平衡方程估算了这些各个组成部分。最初,计算了城市补给成分,包括供水管网和污水管网的渗漏。为了估算降水的自然补给量,使用遥感和GIS技术估算了实际的蒸散量和地表径流。结果表明,城市地下水补给量是自然补给量的十倍以上。估计城市地下水的净补给成分约为568 mm yr -1 ,而自然补给成分则为53 mm yr -1 。还估计了水的流入和流出部分,可以提供海得拉巴城市总水量平衡的完整情况。该分析提供了有关城市污染物渗入含水层的程度和强度的信息。

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