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Artificial culture of biological soil crusts and its effects on overland flow and infiltration under simulated rainfall

文献类型: 外文期刊

作者: Xiao, Bo 1 ; Wang, Qing-hai 1 ; Zhao, Yun-ge 2 ; Shao, Ming-an 2 ;

作者机构: 1.Beijing Acad Agr & Forestry Sci, Res & Dev Ctr Grasses & Environm, Beijing 100097, Peoples R China

2.Chinese Acad Sci, State Key Lab Soil Eros & Dryland Farming Loess P, Inst Soil & Water Conservat, Yangling 712100, Shaanxi, Peoples R China

3.Minist Water Resources, Yangling 712100, Shaanxi, Peoples R China

关键词: Loess Plateau;Soil and water loss;Moss crusts;Soil hydrology;Desertification control;Arid and semiarid regions

期刊名称:APPLIED SOIL ECOLOGY ( 影响因子:4.046; 五年影响因子:4.884 )

ISSN: 0929-1393

年卷期: 2011 年 48 卷 1 期

页码:

收录情况: SCI

摘要: Biological soil crusts are receiving increasing attention due to their potentially positive effects on desert ecosystems. Artificial propagation of crusts is one way to restore degraded desert soils. However, little is known about their effectiveness on overland flow or water infiltration. Consequently, a study was done on soils of the Loess Plateau of China that had crusts propagated on different slopes. The results show that: (1) it is feasible to artificially grow moss-dominated biological soil crusts (moss crusts) in laboratory; when inoculated by sprinkling crushed fragments of stems and leaves of natural moss crusts they will cover the soil surface almost completely after about 10 months; (2) the artificially propagated moss crusts significantly increase infiltration consequently decreasing overland flow and this increase in infiltration is positively correlated to the soil coverage extent; (3) overland flow results increased by slope in moss-protected and bare soils, consequently the action of moss crusts is particularly important for protecting steep slopes; (4) the start time of runoff process is delayed by moss crusts, and the soil water redistribution process is also greatly affected. These results may be useful for helping to control desertification on the Loess Plateau of China or similar regions. (C) 2011 Elsevier B.V. All rights reserved.

  • 相关文献

[1]Artificial culture of biological soil crusts and their effects on runoff and infiltration under simulated rainfall on the Loess Plateau of China. Xiao Bo,Zhao Yun-ge. 2011

[2]Effects of Artificial Biological Soil Crusts on Runoff and Infiltration under Simulated Rainfall. Xiao Bo,Zhao Yun-ge,Wang Qing-hai. 2010

[3]Application of the SCS-CN Model to Runoff Estimation in a Small Watershed with High Spatial Heterogeneity. Xiao Bo,Wang Qing-Hai,Xiao Bo,Fan Jun,Han Feng-Peng,Dai Quan-Hou. 2011

[4]Natural recovery of moss-dominated biological soil crusts after surface soil removal and their long-term effects on soil water conditions in a semi-arid environment. Xiao, Bo,Wu, Juying,Xiao, Bo,Zhao, Yunge,Wang, Huifang. 2014

[5]Biological soil crusts decrease soil temperature in summer and increase soil temperature in winter in semiarid environment. Xiao, Bo,Xiao, Bo,Wang, Huifang,Fan, Jun,Fischer, Thomas,Veste, Maik.

[6]Influence of Forest Coverage on Basin Runoff in China's Loess Plateau. Wang, Xiaoyan,Bi, Huaxing,Song, Qingfeng,Lu, Shaowei. 2015

[7]Characteristics and numeric simulation of soil evaporation in biological soil crusts. Xiao, B.,Zhao, Y. -G.,Shao, M. -A.,Xiao, B.,Zhao, Y. -G.,Shao, M. -A.,Xiao, B.,Zhao, Y. -G.,Shao, M. -A.,Xiao, B..

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