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      Moisture movement in porous materials under temperature gradients

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          Studies in the physical properties of soil. V. The hysteresis effect in capillary properties, and the modes of moisture distribution associated therewith

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            Gas and vapour movements in the soil: I. The diffusion of vapours through porous solids

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              A NUMERICAL METHOD FOR SOLVING THE FLOW EQUATION FOR WATER IN UNSATURATED MATERIALS

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                Author and article information

                Journal
                TAGUAT
                Transactions, American Geophysical Union
                Trans. AGU
                American Geophysical Union (AGU)
                0002-8606
                1957
                1957
                : 38
                : 2
                : 222
                Article
                10.1029/TR038i002p00222
                0edc6a6b-0930-4412-9bae-474a0a2e7a32
                © 1957

                http://doi.wiley.com/10.1002/tdm_license_1.1

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