tudy on the law and simulation of evapotranspiration of spring wheat in northern Xinjiang
View Fulltext  View/Add Comment  Download reader
  
DOI:10.7606/j.issn.1000-7601.2005.04.11
Key Words: spring wheat  evapotranspiration  leaf area index  crop coefficient  crop water stress index
Author NameAffiliation
MU Cai-yun College of Agronomy,Shihezi University/Key Laboratory of Oasis Ecological Agriculture of Xinjiang Corps,Shihezi,Xinjiang 832003,China 
MA Fu-yu College of Agronomy,Shihezi University/Key Laboratory of Oasis Ecological Agriculture of Xinjiang Corps,Shihezi,Xinjiang 832003,China 
ZHENG Xu-rong College of Water Conservancy and Architectural Engineering,Shihezi University,Shihezi,Xinjiang 832003,China 
CHENG Hai-tao College of Agronomy,Shihezi University/Key Laboratory of Oasis Ecological Agriculture of Xinjiang Corps,Shihezi,Xinjiang 832003,China 
LI Jing-yun 194Regiment,Agri.Division8,Xinjiang Construction Crops,Shihezi 832000,China 
ZHANG Wei-guo Chief Farm of Xinhu,Agri.Division6,Xinjiang Construction Crops,Wujiaqu 831300,China 
XU Gong-she Chief Farm of Xinhu,Agri.Division6,Xinjiang Construction Crops,Wujiaqu 831300,China 
Hits: 446
Download times: 174
Abstract:
      By analyzing the experiment data of spring wheat in 2002 to 2003, it is showed that the evpotranspiration in whole growing period of spring wheat in Xinjiang is ranged form 410 mm to 430 mm, both the amount and intensity of evapotranspiration is the highest during heading to milk ripening stage. About 38.3%42.0% of evapotranspiration is consumed by soil evaporation. There is a close relation between leaf area index and evpotranspiration intensity, which can be expressed by compound curve equation. The daily evapotranspiration of spring wheat field is simulated by using Penman-Monteith formula cooperated with crop coefficient and crop water stress index. The result indicates that this method is ideal in precision.