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Page 59
THE EFFECT OF THE REPLACEMENT OF OTHER CATIONS BY SODIUM ON THE DISPERSION OF SOILS THE effect on physical properties of soils by ... The moisture equivalent of the soil usually is taken as a measure of its water - holding capacity .
THE EFFECT OF THE REPLACEMENT OF OTHER CATIONS BY SODIUM ON THE DISPERSION OF SOILS THE effect on physical properties of soils by ... The moisture equivalent of the soil usually is taken as a measure of its water - holding capacity .
Page 60
soils , not given in the table , which become so dense during the centrifuging process that water will not pass through them . In some cases this condition has resulted when the centrifuge is brought up to speed too quickly , the soil ...
soils , not given in the table , which become so dense during the centrifuging process that water will not pass through them . In some cases this condition has resulted when the centrifuge is brought up to speed too quickly , the soil ...
Page 149
activity of various important groups of soil microbes as well as a microbial climax in the soil flora was suggested . Work on nitrification reported from the Intermountain Forest and Range Experiment Station showed that the numbers of ...
activity of various important groups of soil microbes as well as a microbial climax in the soil flora was suggested . Work on nitrification reported from the Intermountain Forest and Range Experiment Station showed that the numbers of ...
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Contents
VOL LXXXVI | 1 |
Electrolytes Theory of D A MACINNES 23 | 7 |
KNIGHT H G Biological Specimens 333 | 12 |
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Bibliographic information
| Title | Science |
| Editor | John Michels (Journalist) |
| Contributor | American Association for the Advancement of Science |
| Published | 1937 |
| Original from | University of Minnesota |
| Digitized | 17 Dec 2019 |
| Export Citation | BiBTeX EndNote RefMan |