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- W2327939919 abstract "This paper intends, by the theory of three dimentional diffusion, to determine the watercontent capillarily held and its change in the ground, where was fast irrigated through a circular area. The theoretical formulae have been derived, considering the special conditions of soil moisture constants as a change of a capillary conductivity in soil.One of these formulae to show a watercontent at any depth beneath the center of an irrigated circle, is as follows:w=100βQ/2√πkte-z2/4kt⋅(1-e-a2/4kt)where w=watercontent %(wt.), β=apparent specific gravity, Q=applied waterquantity cc/cm2, k=capillary conductivity cm/sec, t=time after irrigation sec., z=depth beneath the soil surface cm. a=radius of irrigation area cm.The discrepancy between the formula and the corresponding experiments has been explained principally by the presence of the field capacity. But a lot of problems, especially on the functional relation of capillary conductivity to soil moisture, remain still unsolved." @default.
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- W2327939919 date "1950-01-01" @default.
- W2327939919 modified "2023-09-24" @default.
- W2327939919 title "Capillary Movement of Soil Water in Circular Irrigation as three Dimentional Diffusion" @default.
- W2327939919 cites W1523050803 @default.
- W2327939919 doi "https://doi.org/10.2480/agrmet.6.1" @default.
- W2327939919 hasPublicationYear "1950" @default.
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