A comparative study of the dissolution mechanisms of amorphous and crystalline feldspars at acidic ph conditions

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SUMMARY

    In a recent study, Pérez et_al1 investigated the dissolution mechanisms of oligoclase glass and its crystalline equivalent over a wide range npj Materials Degradation 34 of pH. Building upon the work of Pérez et_al1, the alteration mechanisms of amorphous and crystalline oligoclase with composition close to the albite end member were here investigated at 90 °C in acidic solutions (pH 1.5 and 3) saturated with respect to amorphous silica enriched in H429SiO4(aq) (see section 5, Methods). Whereas oligoclase dissolution rate is moderately impacted by the surface layers developed at pH . . .

     

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