Mass spectrometric study of the dissolution behaviour of sanidine

Abstract

Secondary ion mass spectrometry has been used to measure the silicon isotope ratio as a function of depth in feldspars after their interaction with dilute acid solutions. The reaction of feldspars with aqueous solutions implies the formation of relatively thick K, Na and Al depleted surface layers, especially when the dissolution experiments are conducted in the presence of silica powder. The latter is used to lower the silicon concentration gradient at the solid-solution interface. This generates an uncertainty in the interpretation of the results: the depleted surface layer may have been formed by leaching of the above-mentioned elements from the solid, or by precipitation of silica from the solution. Measurements using isotopically enriched silica powder (³⁰SiO₂) were therefore performed in the hope that they would solve the uncertainty. The measured silicon isotope ratio at the surface of the mineral appears to be different from its normal terrestrial value and from the enriched powder value, having a value somewhere in between which decreases towards its normal value as a function of depth. In addition the silicon isotope ratio of the solution, which was measured using thermal ionization mass spectrometry, shows an altered value compared with the enriched silica powder. The results of both analyses therefore indicate an exchange in silicon between solid and solution and suggest the combination of two or more mechanisms during dissolution.