Spatio-temporal variability of soil water at three seasonal floodplain sites: A case study in Tarim Basin, Northwest China

被引:6
作者
Grashey-Jansen, Sven [1 ]
Kuba, Martin [2 ]
Cyffka, Bernd [2 ]
Halik, Umut [2 ,3 ]
Aishan, Tayierjiang [2 ,3 ]
机构
[1] Univ Augsburg, Inst Geog, D-86135 Augsburg, Germany
[2] Catholic Univ Eichstaett Ingolstadt, D-85072 Eichstatt, Germany
[3] Xinjiang Univ, Coll Resources & Environm Sci, Key Lab Oasis Ecol, Urumqi 830046, Peoples R China
基金
中国国家自然科学基金;
关键词
soil moisture; soil texture; soil water tensions; Tarim River; water retention; LOWER REACHES; CLIMATE-CHANGE; RIVER; XINJIANG; DYNAMICS; DESERT; MOISTURE; FOREST; LAND; MANAGEMENT;
D O I
10.1007/s11769-014-0717-y
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
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.
引用
收藏
页码:647 / 657
页数:11
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