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Moisture equivalent

Moisture equivalent was proposed by Lyman Briggs and McLane (1910) as a measure of field capacity for fine-textured soil materials. Moisture equivalent is defined as the percentage of water which a soil can retain in opposition to a centrifugal force 1000 times that of gravity. It is measured by saturating a sample of soil 1 cm thick, and subjecting it…

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Moisture equivalent

Nodes6
Edges5
Triples19
Avg. degree1.67
Density0.333333
Components1

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Moisture equivalent

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related to References · 19
Moisture equivalent → Agronomy, Agronomy Journal, American Society, Application, Bibcode, Bulletin, James Briggs, Lock-gray-alt-2, Lock-green, Lock-red-alt-2, Lyman, McLane, Moisture Equivalent Determinations, Plant Industry, Shantz, Soils, The, USDA Bureau, Wikisource-logo

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moisture equivalent soil lyman briggs water field capacity mclane centrifugal force 1000 times gravity james 1910 shantz 1912 wilting soils

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SubjectPredicateObjectConfidenceSrc
Moisture equivalentrelated to ReferencesLock-green0.60section
Moisture equivalentrelated to ReferencesLock-gray-alt-20.60section
Moisture equivalentrelated to ReferencesLock-red-alt-20.60section
Moisture equivalentrelated to ReferencesWikisource-logo0.60section
Moisture equivalentrelated to ReferencesLyman0.60section
Moisture equivalentrelated to ReferencesJames Briggs0.60section
Moisture equivalentrelated to ReferencesMcLane0.60section
Moisture equivalentrelated to ReferencesThe0.60section
Moisture equivalentrelated to ReferencesUSDA Bureau0.60section
Moisture equivalentrelated to ReferencesSoils0.60section
Moisture equivalentrelated to ReferencesBulletin0.60section
Moisture equivalentrelated to ReferencesMoisture Equivalent Determinations0.60section

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