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- W2368122548 abstract "It is important to conduct research on precipitation,soil water and soil water carrying capacity of vegetation for forest management.In this paper,the authors investigated the canopy interception,surface runoff,plant growth,and soil water dynamics since2002in Shanghuang E-co-experimental Station in semi-arid regions of Loess Plateau.The results show that the water in-tercepted by the Caragana canopies is0.2～6.47mm with an interception rate of3.1%～53.3%.The total canopy interception is16.9%of precipitation.The runoff is0.24～1.5mm,1.5%～6.6%of rainfall.Precipitation is the only source of soil water supply.The vertical change of soil water can be divided into three layers:fast change layer,active layer and hypoactive layer according to precipitation impact on soil water and the character of the dynamic curve of soil water.The seri-ous stress of soil water on plant growth can change the color of leave,reduce plant's mean water content,lead to leaf drop,even to the dropping of most of the leaves,but does not lead to the death of Caragana shrub immediately in a short term less than a year.Soil water carrying capac-ity of vegetation is the ability of soil water to carry vegetation.The limit is the largest density of the vegetation community when soil water consumption is equal to or lower than soil water sup-ply in the root zone of soil layers from which plant roots can take and utilize water on an annual basis under modern management conditions." @default.
- W2368122548 created "2016-06-24" @default.
- W2368122548 creator A5057730188 @default.
- W2368122548 date "2003-01-01" @default.
- W2368122548 modified "2023-09-25" @default.
- W2368122548 title "Precipitation,soil water and soil water carrying capacity of vegetation" @default.
- W2368122548 hasPublicationYear "2003" @default.
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