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Abstract Soil evaporation (Es) is quite challenging to measure directly, and researchers most commonly resort to using mini-lysimeter’s to measure Es from both bare soil and from soil beneath the… Click to show full abstract
Abstract Soil evaporation (Es) is quite challenging to measure directly, and researchers most commonly resort to using mini-lysimeter’s to measure Es from both bare soil and from soil beneath the crop canopy. However, this technique is unable to measure Es during and shortly after periods of irrigation or rain, and an approach to fill data gaps during these periods would be valuable. One possible approach is the use of the relationship between Es, pan evaporation (Ep) and gravimetric soil water content (θg). To this end, a mini-lysimeter field study was carried out during periods of low evaporative demand (Ep ≤ 3 mm) and high evaporative demand (Ep > 3 mm) to determine the relationship between Es, Ep and θg. There was a highly significant multi-linear relationship between Es, Ep, θg and time after wetting (R2 = 0.78; p
Journal Title: Agricultural Water Management
Year Published: 2019
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