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with μθ is the mean and is the standard deviation σθ of soil moisture. However, the two values μθ and σθ has only been when I have the sequence of values measured soil moisture was determined directly in addition to the field. To the soil moisture mapping 2D on the whole West African region, necessarily needs to determine the spatial distribution of the values μθ and σθ. To do this, chain of humidity measurement value of land in six groups of measurement stations distributed throughout the area at (Bamba, Zaket, Agoufou Wankama, and Nalohou, Ekia) used for regression analysis and has determined to be a linear relationship between μ-API and μθ, as well as between σθ API and σ (see Figure 1). The two relationships are determined by the following equation:
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