Soil moisture is highly dependent on evapotranspiration (ET) the rate of which, in the abscence of plants, is largely governed by ambient air conditions above the soil surface which, one would expect to be roughly some proportional constant given the soil

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Ник: Soil moisture is highly dependent on evapotranspiration (ET) the rate of which, in the abscence of plants, is largely governed by ambient air conditions above the soil surface which, one would expect to be roughly some proportional constant given the soil

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