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首页> 外文期刊>Asian journal of earth sciences >Integrated Geohydrological Studies in the Sedimentary Part of Gadilam River Basin, Cuddalore District, Tamil Nadu
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Integrated Geohydrological Studies in the Sedimentary Part of Gadilam River Basin, Cuddalore District, Tamil Nadu

机译:泰米尔纳德邦库达洛尔区加迪拉姆河流域沉积部分的综合水文研究

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Water is a precious natural resource, without which there would be no life on Earth. Human beings body weight is also composed of two-third water. Our day to day life depends on the availability of inexpensive clean water and safe ways to dispose it after use. As a source of water, groundwater obtained beneath the earth's surface is often cheaper, more convenient and less vulnerable to pollution than surface water. Gadilam river basin covering sedimentary part lies between Latitudes 11°25'00 to 11°45'00 N and Latitudes of 79°18'00 to 79°47'60 E. Earlier Public Works Department (Government of Tamil Nadu), 1992 has done geohydrological field data collection including geological mapping; meteorological data was collected from Public Work Division (PWD); Remote sensing study was done through Landsat TM satellite imagery. The Landsat TM and SRTM satellite images were geometrically rectified with reference to the Survey of India (SOI) topographical sheets of 1:50,000 scale using ERDAS IMAGINE 8.7 software. From SOI toposheets and later using linearly stretched False Colour Composite (FCC) of Landsat TM satellite data and by using other image processing techniques were used to interpreted to map the geomorphology of this region. Water table fluctuations map was prepared using pre and post monsoon water level data. Water level fluctuation map is prepared by using spatial analyst tool of Arc GIS software. From the fluctuation map, it was found that maximum recharge is found in the central and southern part of the study area as water table is occurring at 43 m below the ground level. North-Eastern and western part of the study area shows minimum rise in water level with less than 7 m.
机译:水是一种宝贵的自然资源,没有水,地球上将没有生命。人类的体重也由三分之二的水组成。我们的日常生活取决于廉价清洁水的可用性以及使用后的安全处置方法。作为一种水源,在地表以下获得的地下水通常比地表水更便宜,更方便并且更不易受到污染。加迪兰姆河流域覆盖的沉积部分位于北纬11°25'00至11°45'00 N和东经79°18'00至79°47'60 E之间。早期的公共工程部(泰米尔纳德邦政府)在1992年拥有完成了地质水文现场数据收集,包括地质测绘;气象数据是从公共工作部门(PWD)收集的;遥感研究是通过Landsat TM卫星图像完成的。使用ERDAS IMAGINE 8.7软件参照1:50,000比例的印度测量(SOI)地形图对Landsat TM和SRTM卫星图像进行几何校正。从SOI拓扑表开始,随后使用Landsat TM卫星数据的线性拉伸假彩色合成(FCC)并通过使用其他图像处理技术来解释该区域的地貌。利用季风前后的水位数据准备了地下水位波动图。使用Arc GIS软件的空间分析工具可以绘制水位波动图。从涨落图可以发现,在地下水位低于地面43 m的地方,研究区域的中部和南部获得了最大补给。研究区域的东北部和西部显示出最低水位上升幅度小于7 m。

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