2020
DOI: 10.1016/j.apgeochem.2020.104795
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Thermochemical stability of delafossite and other relevant ternary phases in the Cu–Fe–S–O–H system

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Cited by 2 publications
(1 citation statement)
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“…The amount of Cu 2+ measured in the leachate solutions ranged from 0.23 to 0.65% for the materials of the Cu:GP pH series and increased slightly with increasing initial Cu:GP pH ratio (Figure 5c), which suggests that a partial dissolution of CuO and Cu(OH) 2 phases accounted for the Cu 2+ release. This assertion is supported by the lower stability of these minerals under acidic conditions and their higher solubility in pure water (K tenorite = 10 −8.6 ; K spertiniite = 10 −11.3 ; 25 • C) compared to gerhardtite [58,[62][63][64]. No visible microstructural modifications were recognized for the leached Cu-GPs of the Cu:GP pH series (Figure 5d).…”
Section: Implications For Water Treatment and Environmental Remediationmentioning
confidence: 80%
“…The amount of Cu 2+ measured in the leachate solutions ranged from 0.23 to 0.65% for the materials of the Cu:GP pH series and increased slightly with increasing initial Cu:GP pH ratio (Figure 5c), which suggests that a partial dissolution of CuO and Cu(OH) 2 phases accounted for the Cu 2+ release. This assertion is supported by the lower stability of these minerals under acidic conditions and their higher solubility in pure water (K tenorite = 10 −8.6 ; K spertiniite = 10 −11.3 ; 25 • C) compared to gerhardtite [58,[62][63][64]. No visible microstructural modifications were recognized for the leached Cu-GPs of the Cu:GP pH series (Figure 5d).…”
Section: Implications For Water Treatment and Environmental Remediationmentioning
confidence: 80%