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. 2024 Jan 3;10(1):eadg8826. doi: 10.1126/sciadv.adg8826

Table 2. Stability of rhomboclase.

Resulting mineralogy after a 1-month suspension of rhomboclase (rbc) in varying concentrations of sulfuric acid. Acid concentration calculation takes into account H2O released from mineral transformation. Rhomboclase is stable up to concentrations of 74.2 wt % and transforms into acid ferric sulfate (AFS) within hours to days in higher concentrations (Fig. 1). It is observed that copiapite transforms into rhomboclase within 9 days in 51.3 wt % sulfuric acid (fig. S6) and follows the same rhomboclase to AFS transformation in higher concentrations.

T = 298.15, P = 1 bar
Ex.No H2SO4 wt % Solution (g) Solid (g) Resulting mineralogy (XRD
and Raman)
rbc-1 51.3 5.9916 0.5453 rbc
rbc-2 74.2 6.7096 0.4445 rbc
rbc-3 79.1 6.8232 0.3000 AFS
rbc-4 83.5 6.9012 0.2792 AFS
rbc-5 90.1 6.5734 0.0611 AFS
rbc-6 97.4 7.2205 0.2735 AFS