基于地理信息系统的流域计量分析

R. Kadlag, P. P. Pawase, N. Gatkal, J. Khurdal, S. Nalawade
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引用次数: 0

摘要

流域区划(面积-高程分析)通常用于揭示地貌发育阶段(稳定、成熟和年轻)。本研究以位于马哈拉施特拉邦纳西克区的卡诺里河流域为研究区。利用Arc/Info GIS生成的数字等高线图,将流域划分为7个子流域,并对每个子流域进行拟合分析。在分析中,通过绘制相对高度(h/ h)和相对面积(a/ a)得出曲线;得到的曲线称为半对称曲线。假设曲线下的面积是假设积分(HI)。卡诺里河各子流域的拟合积分值在0.45 ~ 0.88之间。从HI观测,WS2、WS4、WS6子流域处于成熟阶段,并向恶化阶段迈进。小流域WS3具有较高的半对称积分值,说明其处于后期年轻化阶段,需要采取相应的水土保持措施。此外,WS1、WS5和WS7子流域的亚拟积分值非常高,这使它们处于年轻阶段,即非常容易受到侵蚀。因此,这些子流域更容易发生后续侵蚀活动,需要立即采取适当的水土保持措施
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hypsometric Analysis of Watershed using Geographical Information System
Hypsometry of drainage basins (area-elevation analysis) has generally been used to reveal the stages of geomorphic development (stabilized, mature and young). In the present study, Kanoli river watershed located in Nashik district of Maharashtra was considered as the study area. The watershed was delineated into seven sub-watersheds and hypsometric analysis was carried out for all of them using the digital contour map, which was generated using Arc/Info GIS. In analysis, a curve is derived by plotting the relative heights (h/H) and relative areas (a/A); the obtained curve is called as hypsometric curve. The area under the Hypsometric curve is the Hypsometric Integral (HI). The hypsometric integral values for all of the sub-watersheds of Kanoli river ranges between 0.45 and 0.88. It was observed from HI that the sub-watersheds WS2, WS4, WS6 are in the mature stage and moving toward the deteriorating stage. The sub-watershed WS3 yielded higher hypsometric integral value, explaining its late youthful stage which calls for suitable measures of soil and water conservation. Further, sub-watersheds WS1, WS5 and WS7 have got very high value of hypsometric integral which takes them to young stage i.e. very susceptible to erosion. Therefore, these sub-watersheds are more prone to subsequent erosion activities and needs immediately appropriate soil and water conservation measures
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