31:. 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
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the percentage of water which a soil can retain in opposition to a centrifugal force 1000 times that of gravity
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Note: volume of water stored in root zone is equal to the depth of water in root zone (Vw=Dw)
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105:; J. W. McLane (1910). "Moisture equivalent determinations and their application".
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The wilting coefficient for different plants and its indirect determination
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for fine-textured soil materials. Moisture equivalent is defined as
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Moisture
Equivalent = 0.02 sand + 0.22 silt + 1.05 clay
133:. USDA Bureau of Plant Industry. Bulletin 230.
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113:. American Society of Agronomy: 138–147.
119:10.2134/agronj1910.00021962000200010024x
107:American Society of Agronomy Proceedings
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97:. USDA Bureau of Soils. Bulletin 45.
23:and McLane (1910) as a measure of
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95:The moisture equivalents of soils
35:, replaced by field capacity.
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58:Available water capacity
129:; H. L. Shantz (1912).
93:; J. W. McLane (1907).
78:Permanent wilting point
68:Nonlimiting water range
73:Pedotransfer function
127:Lyman, James Briggs
103:Lyman, James Briggs
91:Lyman, James Briggs
42:(1912) found that:
17:Moisture equivalent
40:Homer LeRoy Shantz
38:Lyman Briggs and
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153:Equivalent units
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19:is proposed by
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63:Field capacity
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25:field capacity
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148:Soil physics
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33:soil physics
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21:Lyman Briggs
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142:Categories
84:References
52:See also
115:doi
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111:2
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