An assessment of evaporation losses from soils is critical for sustainable agriculture in semi-arid regions. The purpose of this research was to determine the effect of desaturation and shrinkage on evaporative flux from representative soils. Results indicated that the surface area did not change for silty sand (6% volume reduction) and substantially increased for lean clay (17% volume reduction). The evaporative flux for silty sand decreased from 31 to 25 mg/m
2∙s in
Stage II, remained constant during
Stage III, and decreased to 11 mg/m
2∙s in
Stage IV. In contrast, the lean clay showed a longer
Stage II (34 to 14 mg/m
2∙s), a near constant
Stage III, albeit a similar
Stage IV (13 to 3 mg/m
2∙s). The air entry and residual suction values were 1 kPa and 100 kPa for silty sand and 5 kPa and 1400 kPa for lean clay. In both soils, the total suction merged with the matric suction at
Stage II–
Stage III boundary. Furthermore, the shrinkage curve was J-shaped for silty sand with the only void ratio decrease in
Stage II, whereas that for the lean clay showed a significant void ratio decrease in
Stage II, marginal decrease in
Stage III, and no decrease in
Stage IV. Under high demand, the silty sand exhibited
Stage III and
Stage IV evaporation, whereas the lean clay also showed significant flux during
Stage II. For the investigated range of water content, the total water loss under high demand was found to be 7 times that under low demand.
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