中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Spatial and temporal dynamics of soil moisture after rainfall events along a slope in Regosols of southwest China

文献类型:期刊论文

作者Liu, Gangcai; Zhang, Jianhui
刊名HYDROLOGICAL PROCESSES
出版日期2007-09-30
卷号21期号:20页码:2778-2784
关键词soil moisture dynamics soil moisture content sloped land
ISSN号0885-6087
通讯作者Gangcai Liu(刘刚才)
合作状况其它
英文摘要High frequency seasonal drought in purple soils (Regosols in FAO taxonomy) of the hilly upland areas of Sichuan basin, China. is one of the key restrictive factors for crop production. In order to manage irrigation and fertilizer application in these soils effectively. the soil water content in a sloped plot with 60 cm soil depth was measured by neutron probe devices to investigate the soil moisture regime during the 1998 rainy season after various amounts of rainfall events. The results showed that variation of soil moisture along the slope positions was highest in the top soil layer during the period of sporadic rainfall that did not induce any runoff. The coefficients of variation of soil moisture at various slope positions (upper, middle, and lower) are 17-36%. 8.95% 10.25%. 8.58% 8.05% and 9.21% at the 10 cm, 20 cm, 30 cm, 40 cm, 50 cm and 60 cm soil depths respectively. When surface runoff occurred, the soil moisture dynamics at various positions on the plot were then very different. Soil water content decreased more rapidly on the upper slope than on the middle and lower slope positions. When both surface runoff and throughflow occurred, the soil moisture dynamics in the various layers showed a stable period (soil water content is near constant as time elapses) that lasted about I week. Also, the pattern of moisture dynamics is 'decreasing-stabilization-decreasing'. Thus, irrigation and fertilization management according to the spatial and temporal features of soil moisture dynamics on sloped land can increase the water and fertilizer utilization efficacy by reducing their losses during the stable period. Copyright (c) 2006 John Wiley & Sons, Ltd.
WOS标题词Science & Technology ; Physical Sciences
类目[WOS]Water Resources
研究领域[WOS]Water Resources
关键词[WOS]WATER ; FIELD ; SIMULATION ; RUNOFF
收录类别SCI
语种英语
WOS记录号WOS:000250215800009
公开日期2010-11-08
源URL[http://ir.imde.ac.cn/handle/131551/2450]  
专题成都山地灾害与环境研究所_成都山地所知识仓储(2009年以前)
成都山地灾害与环境研究所_山地灾害与地表过程重点实验室
成都山地灾害与环境研究所_山地表生过程与生态调控重点实验室
作者单位Chinese Acad Sci, Inst Mt Hazard & Environm, Water Res Minist, Chengdu 610041, Peoples R China
推荐引用方式
GB/T 7714
Liu, Gangcai,Zhang, Jianhui. Spatial and temporal dynamics of soil moisture after rainfall events along a slope in Regosols of southwest China[J]. HYDROLOGICAL PROCESSES,2007,21(20):2778-2784.
APA Liu, Gangcai,&Zhang, Jianhui.(2007).Spatial and temporal dynamics of soil moisture after rainfall events along a slope in Regosols of southwest China.HYDROLOGICAL PROCESSES,21(20),2778-2784.
MLA Liu, Gangcai,et al."Spatial and temporal dynamics of soil moisture after rainfall events along a slope in Regosols of southwest China".HYDROLOGICAL PROCESSES 21.20(2007):2778-2784.

入库方式: OAI收割

来源:成都山地灾害与环境研究所

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