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Spatio-temporal Variability of Soil Water at Three Seasonal Floodplain Sites: A Case Study in Tarim Basin,Northwest China

查看全文 作  者:Sven GRASHEY-[1]JANSEN;Martin [2]KUBA;Bernd [2]CYFFKA;müt [2,3]HALIK;Tayierjiang [2,3]AISHAN 高影响力作者 机构地区:[1]Institute of Geography,University of Augsburg Augsburg 86135,Germany;[2]Applied Physical Geography,Catholic University of Eichstaett-Ingolstadt Eichstaett 85072,Germany;[3]Key Laboratory of Oasis Ecology,College of Resources and Environmental Science,Xinjiang University高影响力机构 出  处:《Chinese Geographical Science》索引2014年第24卷第6期,共11页高影响力期刊 基  金:Under the auspices of Federal Ministry of Education and Research of Germany Project-Sustainable Management of River Oases along the Tarim River(No.01LL0918D);National Natural Science Foundation of China(No.31270742,31360200) 摘  要:The floodplain vegetation of the Tarim River in Northwest China is strongly influenced by irrigated agriculture. The abstraction of river water disturbs the natural dynamics of the floodplain ecosystem. The human impact on the hydrological system by bank dams and the irrigation of cotton plantings have caused adverse changes of the Tarim River and its floodplains, so the current stocks of the typical Tugai vegetation show significant signs of degradation. Field studies of soils and statistical analysis of soil moisture data have shown that the vitality of the Tugai vegetation is primarily determined by its position to the riverbank and the groundwater. There exist complex interactions between soil hydrological conditions and the vitality of the vegetation. But the availability of water is not only influenced by the groundwater level and seasonal flood events. The spatial distribution of stocks at different states of vitality seems also to be decisively influenced by physical soil properties. Our results show that the water supply of plant communities is strongly influenced by the soil texture. Spatial differences of soil moisture and corresponding soil water tensions may be the decisive factors for the zonation of vegetation. Physical soil properties control the water retention and rising of capillary water from deeper soil layers and the phreatic zone and may supply the root systems of the phreatophytic vegetation with water. 关 键 词:土壤水分 中国西北 河漫滩 季节性 塔里木盆地 时空变异 塔里木河流域 植被退化
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