GSPAC water movement by greenhouse method in the extremely dry area
GSPAC water movement by greenhouse method in the extremely dry area
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发表时间:
2010
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影响因子:
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通讯作者:
Li Hongshou;Wang Wanfu;Zhang Guobin;Zhang Zhengmo;Wang Xiaowei
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作者:
Li Hongshou;Wang Wanfu;Zhang Guobin;Zhang Zhengmo;Wang Xiaowei
In typically and extremely dry climate condition,a PVC greenhouse-canopy was built on Mogao Grottoes' roof on a gobi.After 235 days' continuously extracting out of condensation water from the film of the greenhouse,and through monitoring soil water content,it was found that there were 2.1 g·m-2·d-1 groundwater being moved up and exported from the greenhouse soil in the extreme dry area where groundwater was more than 200 m deep.After long-term exporting water,the soil water content was not getting lower,instead,it was obviously higher than that before it being controlled and coved.From monitoring these elements,such as soil air RH,absolute humidity and temperature inside and outside the canopy,it was discovered that the condition and mechanism of groundwater continuing moving up was existed,and the possibilities of water inside the greenhouse coming from outside soil and atmosphere could be debarred.By these judgment,in the extremely dry areas where the phreatic water was buried deeply,its evaporation is existed.The phreatic water is soil moisture's important source.Through soil's "respiration",the moisture exchanging between soil and atmosphere is kept.Soil salinity has important effects on soil moisture movement and spatio-temporal distribution of its heterogeneity.The extremely dry climate,terrestrial heat and upper soil's temperature change are an ultimate reason why GSPAC's moisture transportation and phreatic water's evaporation are taken place.