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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 wikiPageRevisionID "442006328".
- Moisture_equivalent hasPhotoCollection Moisture_equivalent.
- Moisture_equivalent subject Category:Soil_physics.
- 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=442006328.
- Moisture_equivalent isPrimaryTopicOf Moisture_equivalent.