Correlación K20-arcilla en las vegas de la provincia de Granada
Abstract
Se estudia la correlación K20-arcilla en suelos de las vegas de Granada, Baza, Guadix y Motril. Se encuentran valores muy diferentes que se interpretan teniendo enCllenta la génesis del suelo y la composición mineralógica de la arcilla y la arena.
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References
MERWIN H. D. and PEECH, M.: Exchangeability of soil potassium in the sand, silt. and clay fractions as influenced by the nature of the complementary exchangeable cation. Soil. Sci. Soc. Amer. Proc. 1950. 15: 125-128.
DELGADO, M. Composición mineralógica de algunas arenas finas, procedentes de suelos de la Vega de Granada. Est. Exp .del Zaidín. (Comunicación privada).
MARTlN VIVALDI, J. L. Mineralogía de los suelos de la Vega de Granada. (En prensa).
HOYOS, A. y colaboradores. Plan de fertilidad de la Vega de Granada. Trabajo presentado a la Diputacíón de Granada.
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