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Soil water response to precipitation in different microtopographies on the semi-arid Loess Plateau,China

Soil water response to precipitation in different microtopographies on the semi-arid Loess Plateau,China

作     者:Huan Ma Qingke Zhu Weijun Zhao Huan Ma;Qingke Zhu;Weijun Zhao

作者机构:Forestry Ecological Engineering Research CenterSchool of Soil and Water ConservationBeijing Forestry UniversityBeijing 100083People’s Republic of China Key Laboratory of Tourism and Resources Environment in Colleges and Universities of Shandong ProvinceTaishan UniversityTaianShandong 271000People’s Republic of China 

出 版 物:《Journal of Forestry Research》 (林业研究(英文版))

年 卷 期:2020年第31卷第1期

页      面:245-256页

核心收录:

学科分类:09[农学] 0903[农学-农业资源与环境] 090301[农学-土壤学] 

基  金:financially supported by Forestry Industry Research Special Funds for Public Welfare Projects(201104002-2) China National Scientific and Technical Innovation Research Project for 12th Five Year Plan(2015BAD07B0201) 

主  题:Semi-arid Loess Plateau Micro-topography Afforestation Time series analysis Soil water 

摘      要:Soil water is an important factor restricting afforestation on the semi-arid Loess *** microtopography of the loess slope has changed the distribution pattern of soil water on the *** improve water utilization efficiency and optimize afforestation configuration patterns,the relationship between soil water and precipitation at micro-topographic scale must be *** used time series analysis to study the temporal variation of soil water and its response to precipitation in four kinds of micro-topographies and undisturbed slope on loess ***-topographies significantly influenced soil water distribution and dynamics on the *** water stored in the platform,sinkhole,and ephemeral gully influenced subsequent soil water for 4 weeks,whereas soil water stored in the scarp and undisturbed slope could influence soil water for 2 *** took 12 weeks,10 weeks,18 weeks,6 weeks,and 12 weeks for precipitation to reach the deeper soil layer in the platform,sinkhole,scarp,ephemeral gully,and undisturbed slope,*** soil water characteristics in different micro-topographies are vital factors that should be taken into consideration when undertaking afforestation on the Loess Plateau.

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