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Statements

Subject Item
dbr:Soil_matrix
rdfs:label
Soil matrix
rdfs:comment
The soil matrix is the solid phase of soils, and comprise the solid particles that make up soils. Soil particles can be classified by their chemical composition (mineralogy) as well as their size. The particle size distribution of a soil, its texture, determines many of the properties of that soil, in particular hydraulic conductivity and water potential, but the mineralogy of those particles can strongly modify those properties. The mineralogy of the finest soil particles, clay, is especially important.
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dbc:Soil
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dbp:chapter
Soil Moisture Manganese and Soil Fertility The Chemistry of Soil pH Soil Potassium and Fertility Living Organisms in the Soil We Seek; We Learn Iron and Soil Fertility Plant Nutrition and Soil Fertility Nitrogen and Soil Fertility Zinc and Soil Fertility Growth of Plants Soil Management and Insect Control Physical Properties Organic Matter Sulfur and Soil Fertility Trace Elements Soil Phosphorus and Fertility What Soils Are pH, Soil Acidity, and Plant Growth Boron and Soil Fertility Copper and Soil Fertility
dbp:first
P.R. R.S. C.H. Roy W. W.H. L.A. Lloyd F. Sterling R. N.T. G. Donald Charles E. Howard V. Franklin E. F.E. Walter E. Darrell A. Francis E. Walter R.F. M.B.
dbp:last
Coleman Holmes Olsen Broadbent Richards Russell Allaway Reuther Allison Reitemeier Jurinak Johnson Jordan Brown Seatz Reisenauer Simonson Fried Dean Kellogg Clark Mehlich Sherman Flemming Wadleigh Russel Stout
dbp:oclc
704186906
dbp:url
//archive.org/stream/yoa1957#page/n129/mode/1up //archive.org/stream/yoa1957#page/n167/mode/1up //archive.org/stream/yoa1957#page/n100/mode/1up //archive.org/stream/yoa1957#page/n367/mode/1up //archive.org/stream/yoa1957#page/n138/mode/1up //archive.org/stream/yoa1957#page/n17/mode/1up //archive.org/stream/yoa1957#page/n115/mode/1up //archive.org/stream/yoa1957#page/n92/mode/1up //archive.org/stream/yoa1957#page/n57/mode/1up //archive.org/stream/yoa1957#page/n185/mode/1up //archive.org/stream/yoa1957#page/n145/mode/1up //archive.org/stream/yoa1957#page/n49/mode/1up //archive.org/stream/yoa1957#page/n123/mode/1up //archive.org/stream/yoa1957#page/n179/mode/1up //archive.org/stream/yoa1957#page/n162/mode/1up //archive.org/stream/yoa1957#page/n68/mode/1up //archive.org/stream/yoa1957#page/n133/mode/1up //archive.org/stream/yoa1957#page/n34/mode/1up //archive.org/stream/yoa1957#page/n105/mode/1up //archive.org/stream/yoa1957#page/n87/mode/1up //archive.org/stream/yoa1957#page/n154/mode/1up
dbp:year
1957
dbp:in
Stefferud
dbo:abstract
The soil matrix is the solid phase of soils, and comprise the solid particles that make up soils. Soil particles can be classified by their chemical composition (mineralogy) as well as their size. The particle size distribution of a soil, its texture, determines many of the properties of that soil, in particular hydraulic conductivity and water potential, but the mineralogy of those particles can strongly modify those properties. The mineralogy of the finest soil particles, clay, is especially important.
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dbr:Soil_moisture
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dbr:Ectomycorrhizal_extramatrical_mycelium
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dbr:Soil_matrix
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dbr:Physical_properties_of_soil
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