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Comprehensive analysis of changes to catchment slope properties in the high-sediment region of the Loess Plateau, 1978-2010

机译:1978 - 2010年黄土高原沉积区流域坡面变化综合分析

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摘要

To control soil erosion and restore the degraded environment in the Loess Plateau, a large number of measures related to soil and water conservation have been employed that have profoundly affected catchment properties. This study constructed three indicators to characterize changes to the catchment slope, proposed both a method for a regression analysis of adjacent images and a sequence model, and applied multisource remotely sensed images and GIS spatial clustering analysis technologies to extract thematic information and comprehensively analyze the catchment change characteristics. The results indicate that the catchment slope properties changed significantly. At catchment scale, the average values of ARC, DVC and ART were 6.43%, 25.57% and 4.30%, respectively. There were six clustering types of catchment slope property changes. The maximum and minimum of the average similarities of the clustering types were 0.992 and 0.935. Each slope control measures had a distinct effect on catchment slope; the dominating factor of each clustering type was identified as: Type 1: D-VC, Type 2: D-VCLU, Type 3: D-LUVC, Type 4: D-TAVC, Type 5: D-TAC and Type 6: D-MFC. Type 5 and Type 1 covered the largest areas, respectively occupying 37.28% and 31.01%. Catchment slope property changes also had distinct types that depended on their geomorphological conditions. These findings provide a useful basis from which to further study catchment slope hydrological and soil erosion processes.
机译:为了控制水土流失并恢复黄土高原退化的环境,已采取了许多与水土保持有关的措施,这些措施对集水性质产生了深远的影响。这项研究构建了三个指标来表征流域坡度的变化,提出了一种相邻图像的回归分析方法和一个序列模型,并应用了多源遥感图像和GIS空间聚类分析技术来提取专题信息并全面分析流域改变特征。结果表明,流域边坡性质发生了明显变化。在集水规模上,ARC,DVC和ART的平均值分别为6.43%,25.57%和4.30%。流域边坡性质变化有六类聚类。聚类类型的平均相似度的最大值和最小值分别为0.992和0.935。每种边坡控制措施对集水区边坡都有明显的影响。每个聚类类型的主导因素被标识为:类型1:D-VC,类型2:D-VCLU,类型3:D-LUVC,类型4:D-TAVC,类型5:D-TAC和类型6:D -MFC。 5型和1型覆盖面积最大,分别占37.28%和31.01%。流域边坡性质的变化也有不同的类型,这取决于它们的地貌条件。这些发现为进一步研究流域边坡的水文和土壤侵蚀过程提供了有用的基础。

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