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The correlation analysis on the landscape pattern index and hydrological processes in the Yanhe watershed, China

机译:延河流域景观格局指数与水文过程的相关分析。

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Yanhe watershed, as a typical and experimental district of Soil and Water Conservation District, has long been plagued by soil erosion due to severe human disturbances. Exploring the relationship between watershed landscape pattern and hydrological processes can find effective ways to solve soil erosion problems. At first, with remote sensing and GIS (Geographic Information System) technology and based on SWAT model, this paper analyzed and simulated ecological hydrological processes in Yanhe watershed. It is on subbasin scale that the runoff and sediment yields were simulated monthly in Yanhe watershed using SWAT model. Secondly, it quantified landscape pattern with landscape indices. The seven landscape indices at the landscape level were selected with principal component factor analysis, including Disjunct Core Area Density (DCAD), Radius of gyration (GYRATE_SD), Patch Cohesion Index (COHESION), Shannon's diversity index (SHEI), Total Core Area (TCA), Perimeter-Area Fractal dimension index (PAFRAC), Interspersion and juxtaposition Index (IJI), etc. Thirdly, a new composite landscape index was constructed on the basis of eco-hydrological processes, which was closely related to soil erosion. The results are as follows: (1) Coupled analysis on the relationship of landscape indices and annual runoff as well as annual sediment yields in each subbasin, the correlation coefficient of seven selected landscape indices and runoff is very small, no passing all significant tests. But the correlation between sediment yields and the indices except for TCA and III is significant, and the absolute value of the correlation coefficient is between 0.3 and 0.5. (2) According to the "source-sink" theory of soil erosion, Slope-HRUs landscape index (SHLI) was built and can reflect the relationship between landscape pattern and soil erosion processes to a certain extent. The coupling relationship between Slope-HRUs landscape index (SHLI) and annual sediment yields in each subbasin is very clear, and correlation coefficient is -0.6, which is significantly negatively correlated. (C) 2015 Elsevier B.V. All rights reserved.
机译:延河流域作为水土保持区的典型实验区,长期以来一直受到严重的人为干扰而遭受水土流失的困扰。探索流域景观格局与水文过程之间的关系可以找到解决土壤侵蚀问题的有效途径。首先,利用遥感和GIS技术,基于SWAT模型,对延河流域的生态水文过程进行了分析和模拟。在亚河流域尺度上,使用SWAT模型每月模拟延河流域的径流和泥沙产量。其次,利用景观指数对景观格局进行量化。通过主成分分析选择了景观水平上的七个景观指数,包括分离核心面积密度(DCAD),回转半径(GYRATE_SD),斑块内聚指数(COHESION),香农多样性指数(SHEI),总核心面积( TCA),周长分形维数指数(PAFRAC),散布和并置指数(IJI)等。第三,在生态水文学过程的基础上,建立了与土壤侵蚀密切相关的新的综合景观指数。研究结果如下:(1)各子流域景观指数与年径流量以及年产沙量的耦合分析,七个选择的景观指数与径流量的相关系数很小,没有通过所有显着检验。但是除TCA和III外,沉积物产量与其他指标之间的相关性很显着,相关系数的绝对值在0.3和0.5之间。 (2)根据土壤侵蚀的“源-库”理论,建立了Slope-HRUs景观指数(SHLI),可以在一定程度上反映景观格局与土壤侵蚀过程的关系。每个子流域的坡度-HRUs景观指数(SHLI)与年产沙量之间的耦合关系非常清楚,相关系数为-0.6,呈显着负相关。 (C)2015 Elsevier B.V.保留所有权利。

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