Journal
AGRICULTURAL WATER MANAGEMENT
Volume 67, Issue 2, Pages 133-143Publisher
ELSEVIER
DOI: 10.1016/j.agwat.2004.02.004
Keywords
Bowen ratio energy balance method; capillary rise; Hargreaves equation; Penman-Monteith equation; time-domain reflectometry
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This study was performed to examine seasonal changes in evapotranspiration (ET), soil water content, and crop coefficients (K-c) for sugarcane, cassava, and maize fields in Northeast Thailand. ET rates during the rainy season varied between 2 and 6 mm per day but remained around I mm per day in the dry season. The normal dry season ET was much greater than the water loss from the top 0.5 m of soil, suggesting that capillary rise from deeper soil layers provides significant amounts of water to the upper soil layer. The K-c for sugarcane and cassava reached growing season peaks of approximately 1.10 and 1.20, respectively, in June. The maximum K-c for the maize field was approximately 1.20. Although the ET estimated by the Hargreaves equation exceeded the FAO reference ET value for this region, the values had a high correlation when the Hargreaves ET was calculated using solar radiation measurements. (C) 2004 Elsevier B.V. All rights reserved.
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