基于地理信息技术的卡纳塔克邦北部马拉普拉巴河Hirehalla子流域形态计量学分析

Q4 Computer Science 测绘地理信息 Pub Date : 2023-04-28 DOI:10.58825/jog.2023.18.1.9
PRADNYA GOVEKAR, J. T. Gudagur, AJAYKUMAR N. ASODE
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引用次数: 0

摘要

利用遥感和地理信息技术对卡纳塔克邦巴加尔科特地区Hirehalla子盆地进行了地貌测量。在GIS环境下进行了子流域各形态参数的圈定和计算。研究分为线性、空中和浮雕三个方面。形态计量学分析结果证实了最高阶的第5级,显示了亚树突到树突的排水模式。形状因子(0.16)、延伸率(0.45)和循环率(0.38)的数值表明子盆地在形状上被拉长。平均分岔比值Rb=3.34,反映了地貌特征对盆地的影响。从流频(1.36)和排水密度(1.27)值可以看出,地下透水,起伏度低。流域纹理值为1.74,表明盆地较为粗糙。此外,崎岖度数值越小,表明子流域对侵蚀的抵抗力越强。
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Morphometric analysis of Hirehalla Sub-basin of Malaprabha River, Northern Karnataka using geoinformatics techniques
In the present study, basin morphometry of Hirehalla Sub-basin of Bagalkote District, Karnataka was carried out using remote sensing and geoinformatics techniques. Delineation and calculation of various morphometric parameters of the sub-basin was done in GIS environment. The study was categorized into– Linear, Aerial and Relief aspects. Result obtained from morphometric analysis confirms the highest order of fifth and showing sub-dendritic to dendritic drainage pattern. Values of shape parameters- form factor (0.16), elongation ratio (0.45) and circulatory ratio (0.38), suggests the sub-basin to be elongated in shape. Average bifurcation ratio value (Rb=3.34), indicates the influence of geomorphic features on the basin. From the values of Stream frequency (1.36) and drainage density (1.27) it indicates, permeable subsurface and low relief. Drainage texture value (1.74) suggests the basin is coarse. In addition, a low value of ruggedness number indicates the resistance of sub-basin to erosion.
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测绘地理信息
测绘地理信息 Earth and Planetary Sciences-Earth-Surface Processes
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