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GIS-based geomorphometric analysis for potential applications in reversing land and biosystem degradation

机译:基于GIS的潜在应用在逆转土地和生物系统降解中的潜在应用

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Watershed morphometric assessment is about measurements and calculations of land surface forms for the purpose of understanding hydro-geomorphological character and patterns. Important natural environment geo-information and summary of the spatial characteristics of Tana River Basin (TRB) in Kenya have been obtained through hydro-geomorphometric analysis. Advanced Spaceborne Thermal Emission and Reflection Radiometer Digital Elevation Model (ASTERDEM) data and ArcGIS (ESRI Inc., version 10.4.1) together with published mathematical equations were applied to extract morphometric parameters of the drainage basin, which covers a total area of 94,930 km(2)and a span of 527.75 km. The quantitative morphometric analysis considered a total of 28 relief, areal, and linear hydro-morphometric characteristics of the TRB. Relief parameters of the basin suggest moderate-to-low overall watershed steepness, upland with rolling land surface patterns, rugged landforms susceptible to erosion and sediment transportation, and a landscape in evolution process tending towards maturity. This means stability of the land surface can be attained with intensive land degradation reversing strategies like erosion control measures. Areal characteristics further support the basin's susceptibility to erosion as shown by stream length, stream drainage density, and circulatory ratio values. Also, the areal aspects portray peak runoffs with short duration flashes. Linear parameter value results such as bifurcation ratio imply that infiltration capacity varies with stream orders across the watershed. This hydro-geomorphometric analysis would be useful to land and water managers, researchers and practitioners of TRB, and other similar systems in designing and planning soil and water conservation and management practices such as soil erosion control, groundwater recharge activities, catchment modelling, runoff and flood studies, prospecting groundwater mapping, and biological applications.
机译:流域的形态学评估是关于陆地表面形式的测量和计算,以了解水力 - 地貌特征和模式。通过水性地板形状分析获得了肯尼亚塔纳河流域(TRB)空间特征的重要自然环境信息和概要。高级星载热发射和反射辐射计数字高度型号(Asterdem)数据和ArcGIS(ESRI Inc.,ESRI Inc.)以及公布的数学方程式的数据,以提取排水盆地的形态学参数,占地面积为94,930公里(2)和527.75公里的跨度。定量的形态学分析认为TRB的总共28个浮雕,区域和线性水电相影特征。盆地的浮雕参数表明了中度到低的整体流域陡坡,高地与滚动陆地图案,崎岖地貌易受侵蚀和沉积物运输,以及进化过程中的景观趋向于成熟。这意味着土地表面的稳定性可以通过密集的土地退化逆转策略,如侵蚀控制措施。由于流长度,流引流密度和循环比值,因此特征进一步支持盆地对腐蚀的敏感性。此外,由于持续时间闪烁的峰值径流,因此区域的方面描绘了峰值径流。线性参数值诸如分岔比的结果意味着渗透容量随着流域的流订单而变化。这种水力地形分析对于土地和水管理人员,研究人员和从业者,以及在设计和规划水土保持和管理实践中的其他类似系统,如土壤侵蚀控制,地下水充电活动,集水区建模,径流和洪水研究,勘探地下水测绘和生物应用。

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