中国黄土高原植被恢复对径流和泥沙量影响的数值模拟

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
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引用次数: 0

摘要

自 1999 年以来,中国黄土高原地区的大规模植被恢复项目 "绿色谷物"(GFG)已显著减少了径流量和泥沙量。虽然有许多研究定量描述了植被覆盖与地块尺度上径流和泥沙量之间的关系,但很少有此类研究,尤其是有关流域尺度上泥沙量的研究。为了模拟植被恢复的影响,对数字黄河模型(DYRIM)中的土壤入渗能力和土壤侵蚀进行了参数化,该模型是一个分布式流域径流和泥沙动力学模型,包含山坡侵蚀、重力侵蚀和泥沙输移,已广泛应用于黄土高原。在 1986-2015 年期间,植被覆盖率从 15% 增加到 70%,对清涧河上游流域(面积为 913 平方公里)进行了事件和连续模拟验证。模拟结果与观测结果在日流量(标定值 NSE = 0.928,验证值 NSE = 0.602)和日泥沙排放量(标定值 NSE = 0.938,验证值 NSE = 0.520)方面吻合良好。根据我们的模拟,2003 年至 2015 年期间,由于实施了 GFG 项目,该流域的径流量减少了 44%,泥沙量减少了 82%。随着大尺度植被覆盖度的增加,径流量和泥沙量都呈指数级下降,而在极端暴雨事件中,植被覆盖度的影响会减弱。当植被覆盖度的变化与降水量的变化相结合时,模拟的泥沙量峰值出现在年平均降水量约为 450-500 mm⋅yr-1 时。改进后的 DYRIM 模型可以在流域和区域尺度上可靠地捕捉和再现植被变化对径流和泥沙产量的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Numerical modeling of effects of vegetation restoration on runoff and sediment yield on the Loess Plateau, China
The “Grain for Green” (GFG), a large-scale vegetation restoration project, has significantly reduced runoff and sediment yield in the Loess Plateau region of China since 1999. While numerous studies have quantitatively described the relationship between vegetation cover and runoff and sediment yield at the plot scale, there are few such studies, especially those on sediment yield, at the catchment scale. To model the effect of vegetation restoration, soil infiltration capacity and soil erosion were parameterized for the Digital Yellow River Model (DYRIM), which is a distributed watershed runoff and sediment dynamics model that incorporates hillslope erosion, gravitational erosion and sediment transport, and has been widely applied to the Loess Plateau. DYRIM with improved functionality was validated on an event basis and as continuous simulation for the Upper Qingjian River Basin (UQRB, with an area of 913 km2) where the vegetation coverage has increased from 15 % to 70 % during 1986–2015. Simulation agrees well with observation in terms of daily flow (NSE = 0.928 for calibration and NSE = 0.602 for validation) and daily sediment discharge (NSE = 0.938 for calibration and NSE = 0.520 for validation). According to our simulation, the runoff reduced by 44 % and the sediment yield reduced by 82 % for the catchment due to the GFG project from 2003 to 2015. Both runoff and sediment yield decrease exponentially with increasing vegetation cover at large scales, and the effect of vegetation cover diminishes during extreme rainstorm events. When changes in vegetation cover are combined with changes in precipitation, the simulated peak sediment yield occurs with the mean annual precipitation of around 450–500 mm⋅yr−1. The improved DYRIM model can credibly capture and reproduce the effect of the change in vegetation cover on runoff and sediment yield at the catchment and regional scales.
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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