Weathering of Viamão granodiorite, south Brazil: Part 2 – Initial porosity of un-weathered rock controls porosity development in the critical zone
Schematic representation of the development of the pore network during weathering. Macrocracks are shown in red, microcracks in blue, and the microporosity of the minerals is shown in grey (Dµ = density of microcracks; DM = density of macrocracks; ΦMp = microporosity; ΦM = porosity of macrocracks; Φ...
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Veröffentlicht in: | Geoderma 2023-01, Vol.429, p.116247, Article 116247 |
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