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Geophysical characterisation of aquifer and minimisation of impact of urban environment in Vidyadhar Nagar township of Jaipur, India

机译:印度斋浦尔Vidyadhar Nagar镇的含水层地球物理特征和城市环境影响最小化

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Resistivity surveys in about 3.5 sq km barren land of Vidyadhar Nagar area in Jaipur, Rajasthan (India) in year 1985 produced some interesting results leading to the development of glorious township having high-rise housing complex, multiplex, civil structures, etc. Resistivity survey revealed the presence of potential aquifer saturated with good quality drinking water in the study area. Isopach map of aquifer thickness obtained by resistivity sounding exhibits a nala-type structure along Udak-Raniji Ki Bavri-Ambabari with increasing thickness towards the south. The cross-section of this nodal zone of aquifer shows that its thickness is about 95m in header side in Udak area in the north. Its thickness increases to about 127m and the span is narrowed in its footer side in Ambabari area in the south. Thereafter it appears to be merged with the Amanishah-Ka-Nala. This nala-type feature in aquifer appears to be an ancient branch which has turned its course towards east in Udak area and joins with the Amanishah-Ka-Nala to the north of Vidyadhar RHB colony, as it exists today.Impact of urban environment causes imbalance of groundwater budget due to cementing of ground surface vis-avis decrease in percolation and simultaneous increase in pumping of groundwater due to urbanisation. Check-dam at header position of nodal zone of aquifer at Udak branch of nala for harvesting of rainwater drained from adjacent hill and harvesting of rainwater flowing from roof, road, other cemented grounds, etc. would help in balancing the recharge and discharge of groundwater in the
机译:1985年,在印度拉贾斯坦邦斋浦尔的Vidyadhar Nagar地区约3.5平方公里的贫瘠土地上进行了电阻率调查,得出了一些有趣的结果,导致了光荣乡镇的发展,其中包括高层住宅区,多层建筑,土木结构等。揭示了研究区域中存在浸有优质饮用水的潜在含水层。通过电阻率测深获得的含水层厚度的等值线图显示了沿着Udak-Raniji Ki Bavri-Ambabari的纳拉型结构,向南厚度增加。该含水层节带的横截面表明,它在北部乌达克地区的集管侧厚度约为95m。它的厚度增加到大约127m,并且在南部Ambabari地区的页脚侧跨度变窄。此后,它似乎与Amanishah-Ka-Nala合并了。含水层中的这种纳拉型特征似乎是一个古老的分支,它已在Udak地区向东转向,并与今天存在的Vidyadhar RHB殖民地以北的Amanishah-Ka-Nala相连。由于地表胶结造成的地下水预算失衡,城市化导致渗滤减少,同时地下水泵送增加。纳拉Udak支水层结头位置的止水坝,用于收集相邻山丘排放的雨水,以及收集从屋顶,道路,其他水泥地面等流出的雨水,这将有助于平衡地下水的补给和排放在里面

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