Competition between erosion and reaction kinetics in controlling silicate-weathering rates

Weathering rates of minerals may be limited by the reaction kinetics of the constitutive minerals or the supply of fresh minerals delivered to the near surface by denudation. We use a model of denudation and reaction kinetics to analyze the relative importance of each in moderating silicate-weatheri...

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Veröffentlicht in:	Earth and planetary science letters 2010-04, Vol.293 (1), p.191-199
Hauptverfasser:	Hilley, G.E., Chamberlain, C.P., Moon, S., Porder, S., Willett, S.D.
Format:	Artikel
Sprache:	eng
Schlagworte:	Atmospherics chemical weathering Constants Erosion rate Fluxes geologic carbon cycle landscape evolution Minerals Reaction kinetics silicate mineral weathering Silicates Weathering
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