Phosphate minerals in a lateritic crust from Venezuela

Ferruginous crusts and pisolites have chemical and mineralogical properties that differ from the surrounding soil due to Fe and Al enrichments which cause cementations that can harden irreversibly. In addition to, and possibly as a result of the Fe and Al accumulation, other ions, particularly phosp...

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Veröffentlicht in:	Biogeochemistry 1996-07, Vol.34 (1), p.1-17
Hauptverfasser:	Tiessen, H, Monaco, S.L, Ramirez, A, Santos, M.C.D, Shang, C
Format:	Artikel
Sprache:	eng
Schlagworte:	Acid soils Earth sciences Earth, ocean, space Exact sciences and technology fertilizers Goethite Materials Mineralogy Minerals Non silicates Phosphates Quartz Resins Sedimentary soils soil chemistry soil fertility soil physics soil science Soils Sorption Surficial geology Tropical soils
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