On the moisture relationships in an ideal soil

Bernard A. Keen

doi:10.1017/S0021859600003373

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The movement of water in soil, and the manner in which water is distributed over the particles and within the interstices, i.e. the dynamical and statical aspects respectively of moisture distribution, are of fundamental importance in soil science. The literature of the subject abounds with experimental determinations, but the difficulties of theoretical treatment are great, and it is only within recent years that any serious attempts have been made in this direction.

References

^{page 170 note 1} 19th Annual Report, U.S. Geol. Survey, 1899, pt. 2.Google Scholar

^{page 170 note 2} U.S. Bureau of Soils, Bull. 10, 1897.Google Scholar

^{page 170 note 3} Ibid. Bull. 38, 1907.

^{page 170 note 4} Soil Sci. 1920, 9, 191Google Scholar; 1920,10, 357; 103.

^{page 170 note 5} Mem. Dept. Agric. India (Chem. Series), 1921, 6, No. 3Google Scholar; Proc. Punjab Engineering Congress, 1923.Google Scholar

^{page 172 note 1} U.S. Bureau of Plant Industry, Bull. 230, 1912.Google Scholar

^{page 174 note 1} Loc. cit.

^{page 176 note 1} Journ. Agric. Sci. 13, 243, 340.Google Scholar

^{page 176 note 2} Loc. cit.

^{page 177 note 1} As developed by Oden, , Int. Mitt. Bodenk. 1915, 5, 257Google Scholar; Proc. Faraday Soc. 1922, 17, 327.Google Scholar

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