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Assessment Of Morphometric Characteristics Of Karwadi-Nandapur Micro Watershed Using Remote Sensing And Geographical Information System

机译:利用遥感和地理信息系统评估Karwadi-Nandapur小流域的形态特征

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Abstract: The study area is Karwadi-Nandapur watershed is a micro watershed which falls in the Kayadhu river watershed in Marathwada region of Maharashtra. Using the remotely sensed images of the Indian Remote Sensing Satellite P6 (IRS P6), Linear Imaging Self Scanner III(LISS III) images captured in October 2010 and November 2011 having resolution of 23.5m X 23.5m and images from Google Earth Pro of study area were used and cartosat satellites. Map of India with scale 1:15,00,000 and soil maps of India were used for the experimental study. The thematic maps like drainage map, land use and land cover map, soil maps and contour map were prepared adopting the PCI Geomatica10.0 software. The geographical information systems (GIS) analysis was made for the said themes using the Arc GIS 'ArcMap10.0. The Karwadi- Nandapur watershed was found to be the third order basin. The present study aims to assess the morphometric characteristics of the watershed basin and it has been assessed by applying GIS techniques. Strahler's method has been employed to assess the fluvial characteristics of the study watershed. Each morphometric characteristic is considered as a single parameter and knowledge based weight age has been assigned by considering its role in soil erosion. The morphometric properties determined for this watershed as a whole and for each watershed will be useful for the efficient planning of water harvesting and groundwater projects on watershed basis.
机译:摘要:研究区域是Karwadi-Nandapur流域,是一个微流域,它位于马哈拉施特拉邦Marathwada地区的Kayadhu河流域。使用印度遥感卫星P6(IRS P6)的遥感图像,分别于2010年10月和2011年11月拍摄的线性成像自我扫描仪III(LISS III)图像,分辨率为23.5m X 23.5m,以及来自Google Earth Pro研究的图像区域被使用和cartosat卫星。实验比例为1:15,00,000比例的印度地图和印度土壤地图。利用PCI Geomatica10.0软件编写了排水图,土地利用和土地覆盖图,土壤图和等高线图等专题图。使用Arc GIS'ArcMap10.0对上述主题进行了地理信息系统(GIS)分析。卡尔瓦迪—南达普尔流域被发现为三阶盆地。本研究旨在评估流域盆地的形态特征,并已通过应用GIS技术对其进行了评估。 Strahler方法已用于评估研究分水岭的河流特征。每个形态特征都被视为一个参数,并通过考虑其在土壤侵蚀中的作用来分配基于知识的体重年龄。为此分水岭整体和每个分水岭确定的形态计量学特性将有助于在分水岭的基础上有效地计划集水和地下水项目。

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