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On the moisture relationships in an ideal soil

Published online by Cambridge University Press:  27 March 2009

Bernard A. Keen
Affiliation:
Rothamsted Experimental Station, Harpenden.

Extract

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.

Type
Research Article
Copyright
Copyright © Cambridge University Press 1924

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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