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    WANG Xiao-yong, YIN Li-he, DAI Ze-bing, et al. A Study of Evapotranspiration in Hailiutu River Basin, Ordos[J]. Northwestern Geology, 2014, 47(1): 244-248.
    Citation: WANG Xiao-yong, YIN Li-he, DAI Ze-bing, et al. A Study of Evapotranspiration in Hailiutu River Basin, Ordos[J]. Northwestern Geology, 2014, 47(1): 244-248.
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    A Study of Evapotranspiration in Hailiutu River Basin, Ordos

    • 1. China University of Geosciences, Beijing 100083, China;

    • 2. Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China;

    • 3. General Corporation of Geological Engineering Investigation of Yunnan, Kunming 650011, China;

    • 4. Institute of Geological Engineering Investigation of Tianjin, Tianjin 300191, China;

    • 5. Fourth Branch of Gansu Provincial Geology and Mineral Exploration Bureau, Jiuquan 735000, China

    More Information
    • Received Date: January 03, 2014
    • Revised Date: February 27, 2014
    • Available Online: July 28, 2022
    • Published Date: March 04, 2014
      Graphical Abstract
      • Abstract
    • Based on SEBS (Surface Energy Balance System), an inversion of evapotranspiration of dry season and rainy season in 2012 in Hailiutu river basin was carried out. The authors analyzed the spatial distribution of evapotranspiration, and discussed the effects caused by depth of groundwater level. The results show that, in dry season, the major factor of influence is the extent of moisture content of surface soil. In rainy season, the major factor of influence is the covered condition of vegetation and the extent of moisture content of surface soil. According to the result, the total evapotranspiration in Hailiutu river basin in 2012 is about 8.76bou8m3.
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      • References (30)
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