查里雅尔河库鲁曼普扎小流域地理空间分析——基于遥感和GIS的地貌评价方法

Adarsha Gopalakrishna Bhat, Vinayak Paradkar, None Aishwarya M. S., Pragya Balley, None Rema K. P.
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 Study Design: Morphometric analysis of Kurumanpuzha sub-watershed was carried out using remote sensing and Geographic Information System (GIS) which is pivotal for sustainable resource management.
 Place and Duration of Study: This study was conducted at Kelappaji College of Agricultural Engineering and Technology, Tavanur, Malappuram, Kerala during 2020-2021.
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摘要

目的:研究库鲁曼普扎小流域的地貌特征,了解库鲁曼普扎小流域的水文行为、侵蚀敏感性和地质特征。研究设计:利用遥感和资源可持续管理关键的地理信息系统(GIS)对库鲁曼普扎小流域进行形态计量学分析。 研究地点和时间:本研究于2020-2021年在喀拉拉邦马拉普兰邦塔瓦努尔的克拉帕吉农业工程技术学院进行。 方法:利用地理信息系统(GIS)对库鲁曼普扎流域的地貌特征进行分析,为库鲁曼普扎流域的水资源规划、水土流失治理、基础设施建设和生态保护提供精确的地形信息。基于线性、面积和地形特征评估形态计量参数。利用USGS地球探测平台从多个来源下载卫星图像,包括ISRO资源卫星、陆地卫星、哨兵、雷达等。然后,这些图像被用于开发土地利用和土地覆盖(LULC)地图以及研究区域的其他地图。结果:小流域为树枝状水系,平均分岔比为2.05,低峰水流持续时间较长,有利于洪水管理。分析显示,细细的水系,表明易受侵蚀的软岩普遍存在。该流域地势高,坡度陡,以丘陵、断裂带和低山为特征。坡度曲线表明地貌演化处于平衡阶段。在小流域水平上,形态计量参数被分成3个簇,显示出空间变异性。森林/茂密植被是主要的土地利用方式,其次是橡胶种植园和灌木林地。结论:研究结果有助于认识库鲁曼普扎流域的水文行为、侵蚀敏感性和地质特征。这对有效的流域管理、侵蚀控制和土地利用规划和工程项目的明智决策是有用的。
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Geospatial Analysis of Kurumanpuzha Sub Watershed in the Chaliyar River Basin: A Remote Sensing and GIS Approach for Geomorphological Assessment
Aims: This study aimed to determine geomorphological characteristics of Kurumanpuzha sub-watershed for understanding its hydrological behaviour, erosion susceptibility and geological characteristics. Study Design: Morphometric analysis of Kurumanpuzha sub-watershed was carried out using remote sensing and Geographic Information System (GIS) which is pivotal for sustainable resource management. Place and Duration of Study: This study was conducted at Kelappaji College of Agricultural Engineering and Technology, Tavanur, Malappuram, Kerala during 2020-2021. Methodology: The geomorphological characteristics of Kurumanpuzha sub-watershed were determined using GIS offering precise terrain insights to guide water resource planning, erosion control, infrastructure development and ecological conservation. Morphometric parameters were assessed based on linear, areal, and relief characteristics. USGS Earth Explorer platform was employed to download satellite images from multiple sources, including ISRO Resourcesat, Landsat, Sentinel, RADAR, and others. These images were then used to develop a Land Use Land Cover (LULC) map as well as other maps of the study area. Results: The sub-watershed had a dendritic drainage pattern with a mean bifurcation ratio of 2.05, indicating easier flood management due to longer durations of low peak flows. The analysis revealed fine drainage, indicating a prevalence of soft rocks prone to erosion. The watershed had high relief and steep slopes, characterized by hills, breaks, and low mountains. The hypsometric curve indicated an equilibrium stage of geomorphic evolution. Morphometric parameters were grouped into three clusters at the sub-watershed level, demonstrating spatial variability. Forest/dense vegetation were the dominant land use, followed by rubber plantations and scrubland. Conclusion: The findings of this study contribute to understanding of the hydrological behaviour, erosion susceptibility and geological characteristics of Kurumanpuzha sub-watershed. It is useful for effective watershed management, erosion control and informed decision-making in land use planning and engineering projects.
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