Estimation of maize evapotranspiration under water deficits in a Semiarid Region

被引:8
|
作者
Kang, SH [1 ]
Cai, HJ
Zhang, JH
机构
[1] NW Agr Univ, Inst Agr Soil & Water Engn, Yangling, Shaanxi, Peoples R China
[2] Chinese Acad Sci, Inst Soil & Water Conservat, Yangling, Shaanxi, Peoples R China
[3] Minist Water Resources, Yangling, Shaanxi, Peoples R China
[4] Hong Kong Baptist Univ, Dept Biol, Kowloon Tong, Peoples R China
关键词
evapotranspiration estimation; water deficits; stomatal conductance; soil water adjustment coefficient; maize (zea mays);
D O I
暂无
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
A field study was conducted to investigate the response of leaf water potentials (psi(1)) and stomatal conductance (C-s) of maize crop to soil water availability, and to test and compare the soil water adjustment coefficient (K-s) functions for estimation of actual evapotranspiration (ET) under water deficits. The results showed that correlation coefficients of K-s to C-s and psi(1) peaked at 09:30 hours, and then decreased, indicating that psi(1) and C-s at 09:30 hours were better predictors of plant water status. The correlations of K-s to relative leaf water potential (psi(1)/psi(1m)) and relative leaf stomatal conductance (C-s/C-sm) were better than that of K-s to psi(1) and C-s directly. K-s was also significantly related to soil water availability (A(w)). Correlation with K-s was reduced in the following order: C-s/C-sm > A(w) > psi(1)/psi(1m). The procedure was used that reference crop evapotranspiration (ET0) was estimated by the modified Penman formula and with a crop coefficient (K-s) and different K-s functions. The results showed that it was the best estimation with K-s function based on the relative stomatal conductance, and at least in the case of maize that the soil water adjustment coefficient K-s based on relative stomatal conductance C-s/C-sm provided a means of predicting required adjustments in ET estimation for different soil water status. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
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页码:1 / 14
页数:14
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