Modelling reactions between alkaline fluids and fractured rock: The Maqarin natural analogue

[1]  S. Norris,et al.  The Tournemire industrial analogue: reactive-transport modelling of a cement–clay interface , 2013, Clay Minerals.

[2]  G. Kosakowski,et al.  The evolution of clay rock/cement interfaces in a cementitious repository for low- and intermediate level radioactive waste , 2013 .

[3]  O. Kolditz,et al.  Reactive transport modeling of the clogging process at Maqarin natural analogue site , 2013 .

[4]  D. Savage,et al.  A review of analogues of alkaline alteration with regard to long-term barrier performance , 2011, Mineralogical Magazine.

[5]  E. Salameh,et al.  Natural Analogues of Cement: Overview of the Unique Systems in Jordan , 2010 .

[6]  Urs Mäder,et al.  Alteration of compacted bentonite by diffusion of highly alkaline solutions , 2009 .

[7]  Karen Scrivener,et al.  A thermodynamic and experimental study of the conditions of thaumasite formation , 2008 .

[8]  Barbara Lothenbach,et al.  Thermodynamic properties of Portland cement hydrates in the system CaO–Al2O3–SiO2–CaSO4–CaCO3–H2O , 2007 .

[9]  D. Bartier,et al.  Mineralogical characterization of the Tournemire argillite after in situ interaction with concretes. , 2006, Waste management.

[10]  B. Wehrli,et al.  DISSOLUTION-PRECIPITATION BEHAVIOUR OF ETTRINGITE, MONOSULFATE, AND CALCIUM SILICATE HYDRATE , 2004 .

[11]  D. Pellegrini,et al.  Coupled modeling of cement/claystone interactions and radionuclide migration. , 2004, Journal of contaminant hydrology.

[12]  O. Pokrovsky,et al.  Kinetics and Mechanism of Dolomite Dissolution in Neutral to Alkaline Solutions Revisited , 2001 .

[13]  P. Bons,et al.  Development of crystal morphology during unitaxial growth in a progressively widening vein : II. Numerical simulations of the evolution of antitaxial fibrous veins , 2001 .

[14]  H. Waber,et al.  Hydrogeochemistry of the Maqarin Area , 1998 .

[15]  A. Bauer,et al.  Kaolinite and smectite dissolution rate in high molar KOH solutions at 35° and 80°C , 1998 .

[16]  Carl I. Steefel,et al.  Multicomponent reactive transport in discrete fractures: II: Infiltration of hyperalkaline groundwater at Maqarin, Jordan, a natural analogue site , 1998 .

[17]  A. Lasaga.  Kinetic theory in the earth sciences , 1998 .

[18]  S. Plettinck.  Kinetics and mechanisms of dissolution of silica at room temperature and pressure , 1994 .

[19]  J. Pearce,et al.  Recarbonation of metamorphosed marls, Jordan , 1993 .

[20]  M. Cave,et al.  The reaction kinetics of laumontite under hydrothermal conditions , 1993 .

[21]  C. Appelo,et al.  Geochemistry, groundwater and pollution , 1993 .

[22]  C. Linklater,et al.  A natural analogue of high pH cement pore waters from the Maqarin area of northern Jordan. II: results of predictive geochemical calculations , 1992 .

[23]  C. Rochelle,et al.  Rate and mechanism of the reaction of silicates with cement pore fluids , 1992 .

[24]  R. Garrels,et al.  Comparative study of the kinetics and mechanisms of dissolution of carbonate minerals , 1989 .

[25]  K. Knauss,et al.  Dependence of albite dissolution kinetics on ph and time at 25°c and 70°c , 1986 .