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| | Geochemistry Department |
 | | He also studied the dehydration kinetics of laumontite, a common Ca-zeolite in nature, to investigate the rates and mechanisms of mineral devolatilization that could largely influence upper crustal processes such as earthquake failure and therefore hazardous seismicity. |
 | | An experimental study of the reactive surface area of the Fontainebleau sandstone as a function of porosity, permeability, and fluid flow rate, Geochimica Cosmochimica Acta Vol. |
 | | Jové, C.F., Liou, J. G., Potter, J., and Bird, D. Experimental investigation of the effects of fluid flow rate on fluid-mineral interaction: implications for reactive surface area and reactive-transport in porous media (to be submitted). |
| www.sandia.gov /eesector/gs/gc/cfjcvita.htm (484 words) |
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