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- Moisture_equivalent abstract "Moisture equivalent is 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 sample of soil 1 cm thick, and subjecting it to a centrifugal force of 1000 times gravity for 30 min. The gravimetric water content after this treatment is its moisture equivalent.This concept is no longer used in soil physics, replaced by field capacity.Lyman Briggs and Homer LeRoy Shantz (1912) found that:Moisture Equivalent = 0.02 sand + 0.22 silt + 1.05 clay".
- Moisture_equivalent wikiPageID "3422049".
- Moisture_equivalent wikiPageLength "1786".
- Moisture_equivalent wikiPageOutDegree "12".
- Moisture_equivalent wikiPageRevisionID "617437530".
- Moisture_equivalent wikiPageWikiLink Available_water_capacity.
- Moisture_equivalent wikiPageWikiLink Category:Soil_physics.
- Moisture_equivalent wikiPageWikiLink Field_capacity.
- Moisture_equivalent wikiPageWikiLink Homer_L._Shantz.
- Moisture_equivalent wikiPageWikiLink Lyman_Briggs.
- Moisture_equivalent wikiPageWikiLink Lyman_James_Briggs.
- Moisture_equivalent wikiPageWikiLink Nonlimiting_water_range.
- Moisture_equivalent wikiPageWikiLink Pedotransfer_function.
- Moisture_equivalent wikiPageWikiLink Permanent_wilting_point.
- Moisture_equivalent wikiPageWikiLink Soil_physics.
- Moisture_equivalent wikiPageWikiLinkText "Moisture equivalent".
- Moisture_equivalent wikiPageWikiLinkText "moisture equivalent".
- Moisture_equivalent hasPhotoCollection Moisture_equivalent.
- Moisture_equivalent wikiPageUsesTemplate Template:Cite_book.
- Moisture_equivalent wikiPageUsesTemplate Template:Cite_journal.
- Moisture_equivalent subject Category:Soil_physics.
- Moisture_equivalent type Physic.
- Moisture_equivalent comment "Moisture equivalent is 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 sample of soil 1 cm thick, and subjecting it to a centrifugal force of 1000 times gravity for 30 min.".
- Moisture_equivalent label "Moisture equivalent".
- Moisture_equivalent sameAs m.09bnmc.
- Moisture_equivalent sameAs Q6894856.
- Moisture_equivalent sameAs Q6894856.
- Moisture_equivalent wasDerivedFrom Moisture_equivalent?oldid=617437530.
- Moisture_equivalent isPrimaryTopicOf Moisture_equivalent.