TY - JOUR
T1 - Transpiration coefficient and ratio of transpiration to evapotranspiration of pear tree (Pyrus communis L.) under alternative partial root-zone drying conditions
AU - Kang, Shaozhong
AU - Hu, Xiaotao
AU - Du, Taisheng
AU - Zhang, Jianhua
AU - Jerie, Peter
N1 - Copyright:
Copyright 2008 Elsevier B.V., All rights reserved.
PY - 2003/4/30
Y1 - 2003/4/30
N2 - Transpiration coefficient Kcb, crop coefficient Kc, and the ratio of transpiration to evapotranspiration (T/ET) are important parameters for pear orchard irrigation management and may vary with different methods of irrigation. This study investigated their changes under three irrigation methods: conventional flood irrigation (CFI), fixed partial root-zone drying and irrigation (FPRD) and alternative partial root-zone drying and irrigation (APRD), in a semi-arid region of Victoria, Australia. The average seasonal ET was 865.29, 795.63 and 804.72 mm respectively for CFI, FPRD, and APRD with ET0 of 817.59 mm for the pear fruiting season. The seasonal transpiration accounted for 81.1%, 84.4%, and 84.1% of evapotranspiration for CFI, FPRD, and APRD respectively. For the CFI, FPRD, and APRD treatments, the seasonal average Kc were 1.058, 0.973, and 0.984 (with their maximum values of 1.326, 1.211, and 1.257) respectively similarly, the respective seasonal average Kcb were 0.858, 0.822, and 0.828 (with maximum values of 1.059, 1.024, and 1.054). The relationships between Kcb, Kc, T/ET, and days after the season beginning were fitted to a fifth-order polynomial equation with higher coefficients of determination R2. The maximum Kc and Kcb occured in mid-January. The ratio T/ET varied from 0.736 to 0.909, 0.743 to 0.947, and 0.741 to 0.925 in the pear fruiting season for CFI, FPRD, and APRD treatments respectively. Results suggested that APRD and FPRD can improve the ratio of transpiration to evapotranspiration, and reduce transpiration coefficient and crop coefficient. Such effects should help improve of water-use efficiency in pear orchards.
AB - Transpiration coefficient Kcb, crop coefficient Kc, and the ratio of transpiration to evapotranspiration (T/ET) are important parameters for pear orchard irrigation management and may vary with different methods of irrigation. This study investigated their changes under three irrigation methods: conventional flood irrigation (CFI), fixed partial root-zone drying and irrigation (FPRD) and alternative partial root-zone drying and irrigation (APRD), in a semi-arid region of Victoria, Australia. The average seasonal ET was 865.29, 795.63 and 804.72 mm respectively for CFI, FPRD, and APRD with ET0 of 817.59 mm for the pear fruiting season. The seasonal transpiration accounted for 81.1%, 84.4%, and 84.1% of evapotranspiration for CFI, FPRD, and APRD respectively. For the CFI, FPRD, and APRD treatments, the seasonal average Kc were 1.058, 0.973, and 0.984 (with their maximum values of 1.326, 1.211, and 1.257) respectively similarly, the respective seasonal average Kcb were 0.858, 0.822, and 0.828 (with maximum values of 1.059, 1.024, and 1.054). The relationships between Kcb, Kc, T/ET, and days after the season beginning were fitted to a fifth-order polynomial equation with higher coefficients of determination R2. The maximum Kc and Kcb occured in mid-January. The ratio T/ET varied from 0.736 to 0.909, 0.743 to 0.947, and 0.741 to 0.925 in the pear fruiting season for CFI, FPRD, and APRD treatments respectively. Results suggested that APRD and FPRD can improve the ratio of transpiration to evapotranspiration, and reduce transpiration coefficient and crop coefficient. Such effects should help improve of water-use efficiency in pear orchards.
KW - Crop coefficient
KW - Pear tree (Pyrus communis L.)
KW - Ratio of transpiration to evapotranspiration
KW - Sap flow
KW - Soil water balance
KW - Transpiration coefficient
UR - http://www.scopus.com/inward/record.url?scp=0037967268&partnerID=8YFLogxK
U2 - 10.1002/hyp.1188
DO - 10.1002/hyp.1188
M3 - Journal article
AN - SCOPUS:0037967268
SN - 0885-6087
VL - 17
SP - 1165
EP - 1176
JO - Hydrological Processes
JF - Hydrological Processes
IS - 6
ER -