State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation , Chinese Academy of Sciences and Ministry of Water Resources, Xinong Rd. 26, Yangling, 712100, Shaanxi, China.
University of Chinese Academy of Sciences, Beijing, 100049, China.
Sci Rep. 2021 Aug 2;11(1):15595. doi: 10.1038/s41598-021-95111-6.
The Loess Plateau in China has suffered severe soil erosion. To control soil erosion, extensive conservation measures aimed at redistributing rainfall, hindering flow velocity and intercepting sediment were implemented on the Loess Plateau. To accurately evaluate the combined effect of conservation measures in the Chabagou watershed, this study classified intra-event-based floods into four regimes via cluster and discriminant analyses. Regime A was characterized by short flood duration and low erosive energy, regime B was characterized by short flood duration and high erosive energy, regime C was characterized by long flood duration and low erosive energy, and regime D was characterized by long flood duration and high erosive energy. The results indicated that peak discharge (q), runoff depth (H), mean discharge (q), and runoff erosion power (E) decreased by 75.2%, 56.0%, 68.0% and 89.2%, respectively, in response to conservation measures. Moreover, area-specific sediment yield (SSY), average suspended sediment concentration (SCE), and maximum suspended sediment concentration (MSCE) decreased by 69.2%, 33.3% and 11.9%, respectively, due to conservation measures. The nonlinear regression analysis revealed a power function relationship between SSY and E in both the baseline (1961-1969) and measurement period (1971-1990) in all regimes. Conservation measures reduced sediment yield by not only reducing the runoff amount and soil erosion energy but also transforming the flood regime, for example, transforming a high-sediment-yield regime into a low-sediment-yield regime. Moreover, conservation measures altered the SSY-E relationship in regime A, whereas no obvious difference in regime B or C/D was observed between the measurement period and the baseline period. This study provides a better understanding of the mechanism of runoff regulation and the sediment yield reduction under comprehensive conservation measures in a small watershed on the Chinese Loess Plateau.
中国黄土高原遭受了严重的土壤侵蚀。为了控制土壤侵蚀,在黄土高原实施了广泛的保护措施,旨在重新分配降雨、阻碍流速和拦截泥沙。为了准确评估察八沟流域保护措施的综合效果,本研究通过聚类和判别分析将基于事件的洪水分为四个区。区 A 的特点是洪水持续时间短,侵蚀能低;区 B 的特点是洪水持续时间短,侵蚀能高;区 C 的特点是洪水持续时间长,侵蚀能低;区 D 的特点是洪水持续时间长,侵蚀能高。结果表明,响应保护措施,峰值流量(q)、径流深(H)、平均流量(q)和径流侵蚀力(E)分别减少了 75.2%、56.0%、68.0%和 89.2%。此外,由于保护措施,流域特定产沙量(SSY)、平均悬移质浓度(SCE)和最大悬移质浓度(MSCE)分别减少了 69.2%、33.3%和 11.9%。非线性回归分析表明,在基线期(1961-1969 年)和测量期(1971-1990 年)的所有区,SSY 与 E 之间均存在幂函数关系。保护措施不仅减少了径流量和土壤侵蚀能,而且改变了洪水区,例如将高泥沙产生产生区转变为低泥沙产生产生区,从而减少了泥沙产沙量。此外,保护措施改变了区 A 的 SSY-E 关系,而在区 B 或 C/D 中,测量期与基线期之间没有明显差异。本研究提供了对中国黄土高原小流域综合保护措施下径流调节和泥沙产沙减少机制的更好理解。