Meteorización (Parte 4)_Meteorización según el tipo de mineral involucrado

Описание: Cuarta parte del curso: Generalidades de la Meteorización
Referencias usadas durante todo el curso:
Bazilevskaya, E., Lebedeva, M., Pavich, M., Rother, G., Parkinson, D. Y., Cole, D., & Brantley, S. L. (2013). Where fast weathering creates thin regolith and slow weathering creates thick regolith. Earth Surface Processes and Landforms, 38(8), 847-858.
Bluth GS and Kump LR (1994) Lithologic and climatic controls of river chemistry. Geochimica et Cosmochimica Acta 58: 2341–2359.
Brady PV (1991) The effect of silicate weathering on global temperature and atmospheric CO2. Journal of Geophysical Research 96: 18101–18106
Brady PV and Carroll SA (1994) Direct effects of CO2 and temperature on silicate weathering: Possible implications for climate control. Geochimica et Cosmochimica Acta 58: 1853–1856.
Casey WH and Sposito G (1992) On the temperature dependence of mineral dissolution rates. Geochimica et Cosmochimica Acta 56: 3825–3830.
Gislason SR, Oelkers EH, Eiriksdottir ES, et al. (2009) Direct evidence of the feedback between climate and weathering. Earth and Planetary Science Letters 277: 213–222.
Hilley GE, Chamberlain CP, Moon S, Porder S, Willett SD. 2010. Competition between erosion and reaction kinetics in controlling silicate weathering rates. Earth and Planetary Science Letters 293: 191–199.
Parsons, I., & Lee, M. R. (2005). Minerals are not just chemical compounds. The Canadian Mineralogist, 43(6), 1959-1992.
White, A. F., & Buss, H. L. (2014). 7.4-Natural weathering rates of silicate minerals. Treatise on Geochemistry, Second Edition. Elsevier, Oxford, 115-155.
White AF, Blum AE, Bullen TD, Vivit DV, Schulz M, and Fitzpatrick J (1999) The effect of temperature on experimental and natural weathering rates of granitic rocks. Geochimica et Cosmochimica Acta 63: 3277–3291.