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- W2385685812 abstract "Aims Soil water is one of the most important factors driving succession in the Artemisia ordosica community in the Ordos Plateau, an arid and semi-arid region of northwestern China. Precipitation is the main source of soil water on the sandland. During each rainfall, part of the rain water is intercepted by plants and the surface layer of soil. This usually quickly evaporates and seems to be biologically ineffective for plant life. Therefore, soil water recruitment is affected by both annual precipitation and characteristics of each rainfall event, such as amount and process. Our objective was to describe the dynamics of soil water content and water recruitment during the growing season. Methods We used eddy covariance technology to study the process of hydrological balance at the ecosystem scale and considered rainfall and evaportranspiration characteristics. Important findings In 2006, annual precipitation was about 229.4 mm and rainfall was the main form, mostly occurring from May to October. Rain events differed in rain amount, length of time and intensity. Ecosystem evaportranspiration and rainfall availability were clearly affected by these rain characteristics and other biotic and abiotic factors. Rain events 5.0 mm increased relative humidity and decreased temperature. Rain events 5.0 mm increased soil water in the root layer and were important to community development and stability." @default.
- W2385685812 created "2016-06-24" @default.
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- W2385685812 date "2008-01-01" @default.
- W2385685812 modified "2023-09-24" @default.
- W2385685812 title "EFFECT OF PRECIPITATION PATTERN ON RECRUITMENT OF SOIL WATER IN KUBUQI DESERT,NORTHWESTERN CHINA" @default.
- W2385685812 hasPublicationYear "2008" @default.
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