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IVES 9 IVES Conference Series 9 Reconocimiento geoedafológico para la zonificación vitivinícola de la D.O. Montilla-Moriles

Reconocimiento geoedafológico para la zonificación vitivinícola de la D.O. Montilla-Moriles


En la región vitivinícola con D.O. Montilla-Moriles (Córdoba) la variabilidad geologico-petrográfica de los terrenos es grande (ROLDÁN GARCÍA y DIVAR RODRÍGUEZ, 1988 a; roldán garcía et al., 1988 b; DIVAR RODRÍGUEZ et al. 1988; DÍAZ DE NEIRA et al., 1992). Por otro lado, distintos modelos fisiográficos —dependientes de procesos estructurales, erosivos y/o sedimentarios- (RUIZ LÓPEZ, 1988 a, b, c), contribuyen también en el desarrollo de diferentes Grupos de Suelos (Leptosols, Regosols, Cambisols, Luvisols, Vertisols) (Paneque et al., 1998; Paneque et al., 1999 a; Fernández Mancilla et al., 1999) con distintas aptitudes vitícolas (Paneque et al., 1999 b). La influencia antrópica, ejercida desde muy antiguo, ha modificado la cubierta de suelos haciéndola depender estrechamente del substrato geológico y de su disposición en el marco ambiental (PÉREZ CAMACHO et al., 1998). Por esta razón, los autores estudian las características de interés vitícola de los terrenos de la D.O. Montilla-Moriles ocupados por el viñedo en orden a la zonificación de la misma.


Publication date: February 24, 2022

Issue: Terroir 2000

Type: Article



Departamento de Cristalografía, Mineralogía y Química Agrícola
Facultad de Química. Universidad de Sevilla
Campus de Reina Mercedes s/n. 41071 Sevilla


IVES Conference Series | Terroir 2000


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