This study was devoted to the analysis of the evaporation process unde
r natural conditions on a bare layered soil, The first and third layer
s are similar in all the plots. The intermediate layer differs from on
e plot to another by the rate of the clay amendment, The cumulative ev
aporation was estimated using the water balance method, Experimental r
esults indicate that the amendment of 2% is the most efficient in prev
enting evaporation losses when a long time scale is considered, Whatev
er the non-zero rate of the amendment is, the evaporation curves coale
sce in a single one when expressed in a dimensionless form. Differenti
al calculus yields the optimal rate of the amendment for which cumulat
ive evaporation is minimal at a fixed time.