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- 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. (en)
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- 47584 (xsd:nonNegativeInteger)
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- Trace Elements (en)
- Boron and Soil Fertility (en)
- Copper and Soil Fertility (en)
- Growth of Plants (en)
- Iron and Soil Fertility (en)
- Living Organisms in the Soil (en)
- Manganese and Soil Fertility (en)
- Nitrogen and Soil Fertility (en)
- Organic Matter (en)
- Physical Properties (en)
- Plant Nutrition and Soil Fertility (en)
- Soil Management and Insect Control (en)
- Soil Moisture (en)
- Soil Phosphorus and Fertility (en)
- Soil Potassium and Fertility (en)
- Sulfur and Soil Fertility (en)
- The Chemistry of Soil pH (en)
- We Seek; We Learn (en)
- What Soils Are (en)
- Zinc and Soil Fertility (en)
- pH, Soil Acidity, and Plant Growth (en)
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| dbp:first
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- W.H. (en)
- Charles E. (en)
- R.S. (en)
- Walter (en)
- F.E. (en)
- C.H. (en)
- L.A. (en)
- N.T. (en)
- M.B. (en)
- Walter E. (en)
- P.R. (en)
- R.F. (en)
- Francis E. (en)
- Darrell A. (en)
- Franklin E. (en)
- G. Donald (en)
- Howard V. (en)
- Lloyd F. (en)
- Roy W. (en)
- Sterling R. (en)
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- Jordan (en)
- Allison (en)
- Brown (en)
- Dean (en)
- Holmes (en)
- Johnson (en)
- Olsen (en)
- Clark (en)
- Russell (en)
- Coleman (en)
- Stout (en)
- Richards (en)
- Russel (en)
- Flemming (en)
- Sherman (en)
- Kellogg (en)
- Broadbent (en)
- Fried (en)
- Wadleigh (en)
- Simonson (en)
- Mehlich (en)
- Reisenauer (en)
- Reuther (en)
- Allaway (en)
- Jurinak (en)
- Reitemeier (en)
- Seatz (en)
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- //archive.org/stream/yoa1957#page/n100/mode/1up (en)
- //archive.org/stream/yoa1957#page/n105/mode/1up (en)
- //archive.org/stream/yoa1957#page/n115/mode/1up (en)
- //archive.org/stream/yoa1957#page/n123/mode/1up (en)
- //archive.org/stream/yoa1957#page/n129/mode/1up (en)
- //archive.org/stream/yoa1957#page/n133/mode/1up (en)
- //archive.org/stream/yoa1957#page/n138/mode/1up (en)
- //archive.org/stream/yoa1957#page/n145/mode/1up (en)
- //archive.org/stream/yoa1957#page/n154/mode/1up (en)
- //archive.org/stream/yoa1957#page/n162/mode/1up (en)
- //archive.org/stream/yoa1957#page/n167/mode/1up (en)
- //archive.org/stream/yoa1957#page/n17/mode/1up (en)
- //archive.org/stream/yoa1957#page/n179/mode/1up (en)
- //archive.org/stream/yoa1957#page/n185/mode/1up (en)
- //archive.org/stream/yoa1957#page/n34/mode/1up (en)
- //archive.org/stream/yoa1957#page/n367/mode/1up (en)
- //archive.org/stream/yoa1957#page/n49/mode/1up (en)
- //archive.org/stream/yoa1957#page/n57/mode/1up (en)
- //archive.org/stream/yoa1957#page/n68/mode/1up (en)
- //archive.org/stream/yoa1957#page/n87/mode/1up (en)
- //archive.org/stream/yoa1957#page/n92/mode/1up (en)
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- 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. (en)
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