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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/m²∙s in <i>Stage II</i>, remained constant during <i>Stage III</i>, and decreased to 11 mg/m²∙s in <i>Stage IV</i>. In contrast, the lean clay showed a longer <i>Stage II</i> (34 to 14 mg/m²∙s), a near constant <i>Stage III</i>, albeit a similar <i>Stage IV</i> (13 to 3 mg/m²∙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 <i>Stage II</i>–<i>Stage III</i> boundary. Furthermore, the shrinkage curve was J-shaped for silty sand with the only void ratio decrease in <i>Stage II</i>, whereas that for the lean clay showed a significant void ratio decrease in <i>Stage II</i>, marginal decrease in <i>Stage III</i>, and no decrease in <i>Stage IV</i>. Under high demand, the silty sand exhibited <i>Stage III</i> and <i>Stage IV</i> evaporation, whereas the lean clay also showed significant flux during <i>Stage II</i>. For the investigated range of water content, the total water loss under high demand was found to be 7 times that under low demand.