生物结皮分布格局对坡面流水动力特征的影响

生物结皮的分布格局是影响坡面产流产沙的因素之一,但其格局对侵蚀动力的影响机理尚不明确,妨碍了进一步解析生物结皮影响坡面产流产沙的机制。本研究通过室内模拟降雨试验,采用景观生态学方法,对带状、棋盘和随机3种分布格局下生物结皮坡面景观指数和水力学参数的变化规律与裸土坡面进行对比研究。结果表明: 生物结皮显著影响坡面侵蚀动力,其分布格局是影响坡面侵蚀动力的因素之一。与裸土相比,生物结皮显著降低了坡面流速(54.6%)和弗劳德数(67.0%),显著增加了径流深(86.2%)和阻力系数(10.68倍),但对雷诺数和径流功率的影响较小;除径流深外,3种格局的生物结皮坡面的各水力学参数均存在显著差异,其中,随机格局对坡面侵蚀动力的影响最大。基于因子分析和聚类分析,筛选出斑块占景观面积比例、斑块密度、景观形状指数、斑块连结度和分离度5个指标作为描述生物结皮斑块分布特征的指标。其中,生物结皮斑块间的斑块连结度和分离度是影响坡面侵蚀动力的主要格局因子。随着生物结皮斑块间斑块连结度减小、分离度增大,坡面流速增加,阻力减小,坡面侵蚀加剧。

Effects of the distribution of biological soil crust on the hydrodynamic characteristics of surface runoff

The distribution pattern of biological soil crusts (biocrusts) is one of the main factors affecting runoff and sediment yield. The relationship between runoff and sediment yield and biocrusts’ distribution pattern is not clear, which hinders understanding the mechanism underlying the effects of biocrusts on runoff and sediment from slopes. To fill the knowledge gap, we investigated the relationship between the landscape indices of three biocrusts’ distribution patterns, i.e. zonation, chessboard and random, and the hydraulic parameters, using of simulated rainfall experiments and landscape ecology methods. The results showed that biocrust significantly affected the erosion force of slopes and that its distribution pattern could affect slope erosion dynamics. Compared to bare soil, the presence of biocrusts significantly reduced the runoff velocity (54.6%) and Froude number (67.0%), increased the runoff depth (86.2%) and Darcy-Weisbach resistance coefficient (10.68 times), but did not affect the Reynolds number and runoff power. Expect for the runoff depth, there were significant differences in the hydraulic parameters of the three biocrusts’ distribution patterns, with the random pattern having the strongest impacts on the dynamics of slope erosion. Based on factor analysis and cluster analysis, five indices of percentage of patch to landscape area, patch density, landscape shape index, patch cohesion and splitting could be used as the indicators for the distribution characteristics of biocrust patches. The patch cohesion and splitting of biocrust patches were the main distribution pattern indices of the hydrodynamics of surface runoff. As the patches patch cohesion decreased, the splitting increased, which caused the surface runoff velocity increase, the resistance decrease, and the slope erosion became more severe.