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In irrigation projects, a soil water retention curve that represents the average condition of the experimental domain is important to ensure the accuracy of the irrigation sheet to be applied in the crop. However, a random sample of undisturbed soil samples can not allow the inference of an average. Two experiments were carried out, evaluating a distribution of variable samples of the soil samples in the mesh samples, in many moments to a long process of drying the soil. In each position the samples were collected to determine the water retention curve in the soil. Temporal stability and geoestatistics analyzes were performed. that the soil moisture obtained in the field and originated from the retention curve presents temporal stability and the study of the moisture obtained in the field can be used to infer the sample position that represents the mean retention curve of a domain.

ESTABILIDADE TEMPORAL DA VARIABILIDADE ESPACIAL DA UMIDADE DO SOLO OBTIDA NO CAMPO E NO LABORATÓRIO