Abstract
Quantifying soil evaporation is required on studies of soil water balance and applications aiming to improve water use efficiency by crops. The performance of a microlysimeter (ML) to measure soil evaporation under irrigation and non-irrigation was evaluated. The MLs were constructed using PVC tubes, with dimensions of 100 mm inner diameter, 150 mm depth and 2.5 mm wall thickness. Four MLs were uniformly distributed on the soil surface of two weighing lysimeters conducted under bare soil, previously installed at Iapar, in Londrina, PR, Brazil. The lysimeters had 1.4 m width, 1.9 m length and 1.3 m depth and were conducted with and without irrigation. Evaporation measurements by MLs (E ML) were compared with measurements by lysimeters (E L) during four different periods in the year. Differences between E ML and E L were small either for low or high atmospheric demand and also for either irrigated or non-irrigated conditions, which indicates that the ML tested here is suitable for measurement of soil evaporation.
Subject
Agricultural and Biological Sciences (miscellaneous)
Reference22 articles.
1. REF-ET: Reference evapotranspiration calculation software. Version 2.0;ALLEN R.G.,2000
2. Crop evapotranspiration: Guidelines for computing crop water requirements;ALLEN R.G.,1998
3. Measurement and estimation of evaporation from soil under sparse barley crops in northern Syria;ALLEN S.J.;Agricultural and Forest Meteorology,1990
4. The ASCE standardized reference evapotranspiration equation: technical committee report to the Environmental and Water Resources Institute of the American Society of Civil Engineers from the Task Committee on Standardization of Reference Evapotranspiration,2005
5. A "micro-lysimeter" method for determining evaporation from bare soil: description and laboratory evaluation;BOAST C.W.;Soil Science Society of America Journal,1982
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