Estimation of water consumption and crop water productivity of winter wheat in North China Plain using remote sensing technology

被引:132
|
作者
Li, Honjun [1 ]
Zheng, Li [1 ]
Lei, Yuping [1 ]
Li, Chunqianq [2 ]
Liu, Zhijun [3 ]
Zhang, Shengwei [1 ]
机构
[1] Chinese Acad Sci, Inst Genet & Dev Biol, Ctr Agr Resources Res, Shijiazhuang 050021, Hebei Province, Peoples R China
[2] Meteorol Inst Hebei Prov, Shijiazhuang 050021, Hebei Province, Peoples R China
[3] Dynam Solut LLC, Knoxville, TN 37919 USA
关键词
Winter wheat; Crop water productivity; Evapotranspiration; SEBAL; Crop coefficient; North China Plain;
D O I
10.1016/j.agwat.2008.05.003
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
The North China Plain (NCP) is one of the most water stressed areas in the world. The water consumption of winter wheat accounts for more than 50% of the total water consumption in this region. An accurate estimate of the evapotranspiration (ET) and crop water productivity (CWP) at regional scale is therefore key to the practice of water-saving agriculture in NCP. In this research, the ET and CWP of winter wheat in 83 counties during October 2003 to June 2004 in NCP were estimated using the remote sensing data. The daily ET was calculated using SEBAL model with NOAA remote sensing data in 17 non-cloud days whereas the reference daily crop ET was estimated using meteorological data based on Hargreaves approach. The daily ET and the total ET over the entire growing season of winter wheat were obtained using crop coefficient interpolation approach. The calculated average and maximum water consumption of winter wheat in these 83 Counties were 424 and 475 mm, respectively. The calculated daily ET from SEBAL model showed good match with the observed data collected in a Lysimeter. The error of ET estimation over the entire growing stage of winter wheat was approximately 4.3%. The highest CWP across this region was 1.67 kg m (3), and the lowest was less than 0.5 kg m (3). We observed a close linear relationship between CWP and yield. We also observed that the continuing increase of ET leads to a peaking and subsequent decline of CWP, which suggests that the higher water consumption does not necessarily lead to a higher yield. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:1271 / 1278
页数:8
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