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• W2394451640 abstract "A located observation and study of water transport at so il-atmosphere interface was conducted. The results show that there are differe nc es in soil evaporation among different agricultural cultivations while no differ ence in the dynamic variation of water vapor transfer flux.The daily variation c urve of soil evaporation is a typical single peak curve.Many factors may affect the surface water transport.When surface vegetational types are stable and the e ffects of crop are not remarkable,the water transfer at soil-atmosphere interfa ce is affected not only by climatic condition but also apparently by soil water contents (0～20cm).The water vapor transfer through interface is significantly p ositively correlated with the net radiation and is correlated with the environme ntal temperature.It is also affected by water potential and has a highly signifi cant negative correlation with the air humidity. Therefore, the water vapor tran sfer at interface is mainly controlled by soil surface(0～20cm)water contents. T heir relationship has a linear correlativity. The amount of soil evaporation is 1/3 of the total field evapotranspiration. There are potentials for controll ing the consumption to these none productive water moisture. Measures such as so il-manuring, irrigation-controlling, physical obstacle of preventing soil evap oration are presented." @default.
• W2394451640 created "2016-06-24" @default.
• W2394451640 creator A5072898727 @default.
• W2394451640 date "2003-01-01" @default.
• W2394451640 modified "2023-09-22" @default.
• W2394451640 title "Study on surface water transport in agricultural landsca pe on the slop lands of red soil (dry season)II.Water transport at leaf-atmosphere interface" @default.
• W2394451640 hasPublicationYear "2003" @default.
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