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Conferència: Time and Length Scales of Crystal Dissolution Kinetics

Notícia | 06-06-2007

Andreas Lüttge, Dept. de Geologia, Rice University, Houston, Texas, EE.UU.
Organitzat conjuntament CSIC-UB
Sala de conferències de l'Institut J. Almera (CSIC), 12h

Various experimental techniques (e.g., Vertical Scanning Interferometry, Electron and Atomic Force Microscopy) and modelling techniques (Monte Carlo and ab initio methods) open up a new field of study on the surface dynamics on minerals, glasses and metals and their role in water/rock interactions. The possibility of direct measurements of dissolution/ precipitation rates at specific locations on the mineral surface provides a better understanding of reactive surface area. The determination of reactive surface area is known to be a central problem in fluid/solid interactions. Quantitative kinetic rate data are urgently needed for modeling water/rock systems that provide a better understanding of the dynamics governing many geologic processes.


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