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Watershed discretization based on multiple factors and its application in the Chinese Loess Plateau

机译:基于多因素的分水岭离散化及其在黄土高原的应用

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摘要

The spatial discretization of watersheds is an indispensable procedure forrepresenting landscape variations in eco-hydrological research, representingthe contrast between reality and data-supported models. When discretizing awatershed, it is important to construct a scheme of a moderate number ofdiscretized factors while adequately considering the actual eco-hydrologicalprocesses, especially in regions with unique eco-hydrological features andintense human activities. Because of their special lithological andpedologic characteristics and widespread man-made vegetation, discretizationof watersheds in the Loess Plateau in Northern China is a challenge. Inorder to simulate the rainfall-runoff process, a watershed in the LoessPlateau, referred as Ansai, was spatially discretized into new units calledland type units. These land type units were delineated under a scheme offactors including land use, vegetation condition, soil type and slope.Instead of using units delineated by overlaying land use and soil maps, theland type units were used in the Soil and Water Assessment Tool (SWAT).Curve numbers were assigned and adjusted to simulate runoff, using the USNatural Resources Conservation Service (NRCS) curve number method. Theresults of the runoff simulation better matched actual observations.Compared to the results that used the original units, the coefficient ofdetermination (R2) and the Nash-Sutcliffe coefficient (ENS) formonthly flow simulation increased from 0.655–0.713 and 0.271–0.550 to0.733–0.745 and 0.649–0.703, respectively. This method of delineating intoland type units is an easy operation and suitable approach foreco-hydrological studies in the Chinese Loess Plateau and other similarregions. It can be further applied in soil erosion simulation and theeco-hydrological assessment of re-vegetation.
机译:流域的空间离散化是表示生态水文学研究中景观变化的必不可少的过程,它代表了现实模型与数据支持模型之间的对比。在离散化流域时,重要的是构建一个适当数量的离散因素的方案,同时充分考虑实际的生态水文过程,尤其是在具有独特生态水文特征和人类活动激烈的地区。由于其特殊的岩性和岩石学特征以及广泛的人造植被,中国北方黄土高原的流域离散化是一个挑战。为了模拟降雨径流过程,在黄土高原的一个分水岭(称为Ansai)在空间上被离散成称为土地类型单位的新单位。这些土地类型单位是根据土地利用,植被状况,土壤类型和坡度等因素进行划分的,而不是使用通过叠加土地用途和土壤图来描述的单位,而是在土壤和水评估工具(SWAT)中使用了土地类型单位使用USNatural Resources Conservation Service(NRCS)曲线编号方法分配和调整曲线编号以模拟径流。径流模拟的结果与实际观测值比较吻合。与使用原始单位的结果相比,测定系数( R 2 )和纳什-苏特克利夫系数( E NS )的月流量模拟分别从0.655-0.713和0.271-0.550分别增加到0.733-0.745和0.649-0.703。这种划定内陆类型单位的方法是一种易于操作的方法,是中国黄土高原和其他类似地区进行生态水文学研究的合适方法。它可以进一步应用于土壤侵蚀模拟和植被的生态水文评估。

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