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黄河上游土壤侵蚀与泥沙产沙及其与植被覆盖度的关系。

Soil erosion and sediment yield and their relationships with vegetation cover in upper stream of the Yellow River.

机构信息

School of Environment, State Key Laboratory of Water Environment Simulation, Beijing Normal University, Beijing, 100875, China.

出版信息

Sci Total Environ. 2010 Dec 15;409(2):396-403. doi: 10.1016/j.scitotenv.2010.10.020. Epub 2010 Nov 11.

Abstract

Soil erosion is a significant concern when considering regional environmental protection, especially in the Yellow River Basin in China. This study evaluated the temporal-spatial interaction of land cover status with soil erosion characteristics in the Longliu Catchment of China, using the Soil and Water Assessment Tool (SWAT) model. SWAT is a physical hydrological model which uses the RUSLE equation as a sediment algorithm. Considering the spatial and temporal scale of the relationship between soil erosion and sediment yield, simulations were undertaken at monthly and annual temporal scales and basin and sub-basin spatial scales. The corresponding temporal and spatial Normalized Difference Vegetation Index (NDVI) information was summarized from MODIS data, which can integrate regional land cover and climatic features. The SWAT simulation revealed that the annual soil erosion and sediment yield showed similar spatial distribution patterns, but the monthly variation fluctuated significantly. The monthly basin soil erosion varied from almost no erosion load to 3.92 t/ha and the maximum monthly sediment yield was 47,540 tones. The inter-annual simulation focused on the spatial difference and relationship with the corresponding vegetation NDVI value for every sub-basin. It is concluded that, for this continental monsoon climate basin, the higher NDVI vegetation zones prevented sediment transport, but at the same time they also contributed considerable soil erosion. The monthly basin soil erosion and sediment yield both correlated with NDVI, and the determination coefficients of their exponential correlation model were 0.446 and 0.426, respectively. The relationships between soil erosion and sediment yield with vegetation NDVI indicated that the vegetation status has a significant impact on sediment formation and transport. The findings can be used to develop soil erosion conservation programs for the study area.

摘要

当考虑区域环境保护时,土壤侵蚀是一个重大问题,特别是在中国的黄河流域。本研究利用土壤和水评估工具(SWAT)模型,评估了中国陇流流域土地覆盖状况与土壤侵蚀特征的时空相互作用。SWAT 是一个物理水文模型,它使用 RUSLE 方程作为泥沙算法。考虑到土壤侵蚀和泥沙产之间关系的时空尺度,模拟在月和年时间尺度以及流域和子流域空间尺度上进行。相应的时间和空间归一化植被指数(NDVI)信息是从 MODIS 数据中总结出来的,它可以整合区域土地覆盖和气候特征。SWAT 模拟表明,年土壤侵蚀和泥沙产呈现出相似的空间分布模式,但月变化波动很大。月流域土壤侵蚀从几乎没有侵蚀负荷到 3.92 吨/公顷不等,最大月泥沙产为 47540 吨。年际模拟侧重于每个子流域的空间差异及其与相应植被 NDVI 值的关系。研究得出结论,对于这种大陆季风气候流域,较高的 NDVI 植被区阻止了泥沙输运,但同时也造成了相当大的土壤侵蚀。月流域土壤侵蚀和泥沙产均与 NDVI 相关,其指数相关模型的确定系数分别为 0.446 和 0.426。土壤侵蚀和泥沙产与植被 NDVI 的关系表明,植被状况对泥沙形成和输运有重大影响。研究结果可用于制定研究区的土壤侵蚀保护计划。

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