ScholarLens Back to search
2014•Northwesten GeologyRequires access

A Study of Evapotranspiration in Hailiutu River Basin,Ordos

Wang Xiao-yon

Open publisher page 0 citations

Abstract

Based on SEBS(Surface Energy Balance System),an inversion of evapotranspiration of dry season and rainy season in 2012in 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 2012is about 8.76bou8 m3.

About this research paper

What this paper is about

Based on SEBS(Surface Energy Balance System),an inversion of evapotranspiration of dry season and rainy season in 2012in 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 2012is about 8.76bou8 m3.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Based on SEBS(Surface Energy Balance System),an inversion of evapotranspiration of dry season and rainy season in 2012in 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 2012is about 8.76bou8 m3.

Key concepts: Evapotranspiration, Wet season, Hydrology (agriculture), Water content, Dry season, Structural basin, Environmental science, Groundwater

Related papers

Related paper 1Related paper 2Related paper 3
Back to paper searchBrowse research topicsOriginal source
A Study of Evapotranspiration in Hailiutu River Basin,Ordos — Research Paper | ScholarLens