Models of transport and reaction describing weathering of fractured rock with mobile and immobile water
We propose models for calculating the rate of chemical weathering of minerals as a function of depth in the weathering zone. A macropore network is assumed to be responsible for the transport of mobile water, which removes soluble weathering products at the interface of that network and the matrix....
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Veröffentlicht in: | Journal of geophysical research. Earth surface 2017-03, Vol.122 (3), p.735-757 |
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Sprache: | eng |
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