File:Soil physics laboratory manual (1912) (20778976976).jpg

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Title: Soil physics laboratory manual
Identifier: CUbiodiversity108419 (find matches)
Year: 1912 (1910s)
Authors: Mosier, Jeremiah George, 1862-1922; Gustafson, Axel Ferdinand, 1880- joint author
Subjects: Agricultural physics; Soils
Publisher: Boston, New York (etc. ) Ginn and company
Contributing Library: Cornell University Library
Digitizing Sponsor: Mann Library, Cornell

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PRACTICE XI (Continued) The apparent specific gravity of soils varies with the degree of compaction. Ar freshly plowed field is much lighter per cubic foot than one compacted by rains, tramping, or by means of the roller.
Text Appearing After Image:
Fig. 3. Soil Compactor A, movable interior to be lifted, which, by dropping, compacts the soil; B, soil tube in place on base of ^; C, rubber stopper closing tube; D, felt or rubber cushion Why is the apparent specific gravity of a sandy soil higher than that of a silt loam ? Why is the apparent specific gravity of peat so low ? 24

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Mosier, Jeremiah George, 1862-1922;

Gustafson, Axel Ferdinand, 1880- joint author
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23 August 2015



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current10:12, 23 August 2015Thumbnail for version as of 10:12, 23 August 20151,346 × 2,870 (931 KB) (talk | contribs)== {{int:filedesc}} == {{information |description={{en|1=<br> '''Title''': Soil physics laboratory manual<br> '''Identifier''': CUbiodiversity108419 ([https://commons.wikimedia.org/w/index.php?title=Special%3ASearch&profile=default&fulltext=Search&sear...

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