Artículo

Reply to Vogt's comments on the paper "Fibrous-clay mineral formation and soil evolution in Aridisols of northeastern Patagonia, Argentina" by P.J. Bouza, M. Simón, J. Aguilar, H. del Valle and M. Rostagno

Bouza, Pablo JoseIcon
Fecha de publicación: 04/2009
Editorial: Elsevier Science
Revista: Geoderma
ISSN: 0016-7061
Idioma: Inglés
Tipo de recurso: Artículo publicado
Clasificación temática:

Resumen

Vogt's comments emphasize the potential influence that the cryogenic processes could have had on the genesis of the soils analyzed in this study. We really appreciate her comments. Indeed, we took into consideration and cited one of her studies dealing with cryogenic processes and sepiolite formation. However, our results led us to conclusions different to the ones held by Vogt.
Palabras clave: SEPIOLITE , PALYGORSKITE , PEDOGENIC ORIGIN , CALCRETES
 
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info:eu-repo/semantics/openAccess Excepto donde se diga explícitamente, este item se publica bajo la siguiente descripción: Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Unported (CC BY-NC-SA 2.5)
Identificadores
URI: http://hdl.handle.net/11336/95837
DOI: http://dx.doi.org/10.1016/j.geoderma.2009.01.018
URL: https://www.sciencedirect.com/science/article/pii/S0016706109000378
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Articulos(CCT-CENPAT)
Articulos de CTRO.CIENTIFICO TECNOL.CONICET - CENPAT
Citación
Bouza, Pablo Jose; Reply to Vogt's comments on the paper "Fibrous-clay mineral formation and soil evolution in Aridisols of northeastern Patagonia, Argentina" by P.J. Bouza, M. Simón, J. Aguilar, H. del Valle and M. Rostagno; Elsevier Science; Geoderma; 150; 1-2; 4-2009; 228-229
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