REACTION KINETICS PARAMETERS DESCRIBING DISPLACEMENT BY ACIDS OF STRUCTURAL METALLIC IONS FROM CLAY MINERALS

Chemical kinetics parameters describing reactions of naturally-occurring clay minerals with acids were determined using batch reaction and analytical techniques. Clay minerals included sodium montmo-rillonite, kaolinite, and illite, reacting with hydrochloric acid, nitric acid, and sulfuric acid. Two acid concentrations were examined at 50 and 70^°C. Displacement by acids of aluminum and magnesium from clays was found to follow pseudo-first order kinetics. Data analysis verified the batch reaction technique for determining kinetics parameters of acid-clay reactions and demonstrated acid neutralization by naturally-occurring clays. For reactions of sodium montmorillonite with hydrochloric acid, nitric acid, and sulfuric acid, reaction rate coefficients for displacement of aluminum ranged from 1·73 × 10^-4 kg/mol-hr at 50^°C to 3·02 × 10^-3 kg/mol-hr at 70^°C. Displacement of magnesium from sodium montmorillonite by these acids occurred at rates ranging from 3·68 × 10^-4 kg/mol-hr at 50^°C to 1·12 × 10^-2 kg/mol-hr at 70^°C. Activation energies for displacement by acids of aluminum from sodium montmorillonite were calculated to range from 31,000J/mol to 112,000J/mol, while activalion energies for displacement of magnesium from sodium montmorillonite ranged from 36.000 J/mol to 103,000 J/mol. For reactions of illite with acids, reaction rate coefficients for displacement of aluminum were determined to be 1·45×10^-4Kg/mol-hr at 50^°C to 1·7×10^-3kg/mol-hr at 70^°C. Displacement of magneisum by acids from illite occurred at rates from 6·06 × 10^-4 kg/mol-hr at 50^°C to 5·97 × 10^-3 kg/mol-hr. Activation energies for reactions of acids with illite ranged from 33,000 J/mol to 62,000 J/mol for displacement of aluminum and from 9,400 J/mol to 29,000 J/mol for displacement of magnesium.