Arid Zone Research ›› 2025, Vol. 42 ›› Issue (11): 2044-2057.doi: 10.13866/j.azr.2025.11.08

• Land and Water Resources • Previous Articles     Next Articles

Coupled effects of slope and vegetation cover characteristics on hydrodynamic erosion forces and sediment yield processes in the southern Ningxia mountainous area

CHEN Kai1(), ZHANG Yi2, WANG Xing1(), LIU Xiaojun3, HU Renzheng3, LEI Xueyi3, FAN Qinghua2   

  1. 1. College of Ecology and Environment, Ningxia University, Yinchuan 750021, Ningxia, China
    2. Xi’an University of Science Technology, Xi’an 710048, Shaanxi, China
    3. College of Agriculture, Ningxia University, Yinchuan 750021, Ningxia, China
  • Received:2025-05-20 Revised:2025-07-29 Online:2025-11-15 Published:2025-12-13
  • Contact: WANG Xing E-mail:17395125546@163.com;wx08@nxu.edu.cn

Abstract:

Through controlled field-scouring experiments, we examined the soil erosion dynamics and hydrodynamic mechanisms on slopes hosting different vegetation in the southern Ningxia mountainous area. Specifically, we quantify the synergistic effects of slope gradient (10°, 15°, 20°, 25°), vegetation cover type (barren land, grassland, shrubland), and scouring intensity (4, 8, 16 L·min-1) on the sediment yield. They key findings are as follows: (1) on slopes with the same vegetation type, the effects of slope gradient and scouring intensity on sediment yield intensify with increasing slope steepness, with slope gradient exerting the greatest promotional effect on the erosion process. The sediment yield was maximized (15.64 kg) on barren land with a 25° slope gradient and a scouring intensity of 16 L·min-1 and minimized (0.03 kg) on shrubland with a 10° slope angle and a scouring intensity of 4 L·min-1. (2) The hydrodynamic parameters are significantly correlated with sand production (P<0.05), but the dominant factor depends on the environmental flushing conditions. The water-flow power per unit can contribute up to 44.19% of the sand production on grassland and scrubland at low flushing intensity (4 L·min-1), whereas each energy parameter contributes nearly 20.00% at high flushing intensity (16 L·min-1). The factor interactions evolve nonlinearly: the contributions from direct single-factor effects dominate at low scouring intensity (4 L·min-1) but weaken with increasing scouring intensity (16 L·min-1) as the multifactor interactions gain prominence. This study can theoretically guide the optimization of slope configurations for regional soil and water conservation purposes and practically guide the precise prevention and control of erosion in ecologically fragile areas.

Key words: southern Ningxia mountainous area, soil erosion, hydrodynamic parameters, interaction effects