Effects of rock fragment cover on hydrological response and soil loss from Regosols in a semi-humid environment in South-West China

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• 作者：Xiaoyan Wang^a ; Zhaoxia Li^a ; Chongfa Cai^a ; ^{cfcaiwh@gmail.com} ; ^{cfcai@mail.hzau.edu.cn} ; Zhihua Shi^a ; Qinxue Xu^a ; ^b ; Zhiyong Fu^a ; Zhonglu Guo^a
• 关键词：Surface runoff ; Subsurface runoff ; Rainwater distribution ; Sediment concentration ; Soil loss ratio ; Three Gorge Reservoir Area
• 刊名：Geomorphology
• 出版年：2012
• 期刊代码：31_0169555x
• 类别：soc
• 出版时间：15 May, 2012
• 卷：151-152
• 期：Complete
• 页码：234-242
• 文件大小：1880 K

摘要

Controlling soil hydrological processes and combating soil erosion on agricultural fields are high priorities for crop production and ecological environments. In this research, the effect of land application of rock fragments on surface runoff, subsurface runoff, infiltration and soil loss on Regosols had been investigated under field conditions using a portable rainfall simulator. Experimental twin-plot (two subplot with 1-m wide by 2-m long, 32%slope) with different rock fragment covers ranging from 0-40%were exposed to three rainfall intensities, low (57 卤 2 mm h^-1), medium (91 卤 3 mm h^-1), and high (122 卤 5 mm h^-1). Fifteen treatments were conducted in the experiments in duplicates. Surface runoff, subsurface runoff, soil moisture and sediment were measured. Results show that surface rock fragment cover retarded surface runoff, increased infiltration and subsurface runoff, and diminished sediment concentration and soil loss. The final infiltration rates, which increased with increasing rock fragment covers, were 16.5-42.7 mm h^-1 at low intensity, 19.7-50.8 mm h^-1 at medium intensity and 23.8-56.4 mm h^-1 at high intensity. Compared with bare soils, surface runoff rates were reduced to 24%, 51%and 64%in soils with 40%rock fragment cover at low, medium and high intensity rainfall, respectively. Subsurface runoff volume was significantly higher and time to start subsurface runoff was shorter as surface rock fragment cover increased. Compared with bare soils, subsurface runoff coefficients increased to 3.5, 3.3 and 2.9 times in soils with 40%rock fragment cover at low, medium and high intensity, respectively. Sediment concentrations increased from 9.8 g L^-1 for 40%rock fragment cover under high intensity rainfall to 51.5 g L^-1 for bare soils with rain falling at high intensity. The erosion rate was < 12 g m^-2 min^-1 for soils with 40%rock fragment cover, even when rainfall intensity was high, while it was > 15 g m^-2 min^-1 for bare soils under low intensity. The relationship between rock fragment cover and soil loss ratio can be expressed by an exponential function with a high degree of reliability, regardless of rainfall intensities. Overall, results indicate the surface rock fragments can be influential in shaping hydrological processes and soil loss from sloping farmland.