The surface area and reactivity of granitic soils: I. Dissolution rates of primary minerals as a function of depth and age deduced from field observations-Reference-Cited by-同舟云学术

The surface area and reactivity of granitic soils: I. Dissolution rates of primary minerals as a function of depth and age deduced from field observations

Published:2015-01 Issue: Volume:237-238 Page:21-35
ISSN:0016-7061
Container-title:Geoderma
language:en
Short-container-title:Geoderma

Author:

Parry Samuel A.^ORCID,Hodson Mark E.^ORCID,Kemp Simon J.,Oelkers Eric H.

Funder

Natural Environment Research Council

Centre National de la Recherche Scientifique

European Community

Publisher

Elsevier BV

Subject

Soil Science

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