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  1. Added 25 mg/L Silicon (Si) and 5 mg/L Aluminium (Al) to the hydrogeochemical baseline of the Svystunova Gully mine water impoundment, modeling clay mineral phase equilibria using RedModRphree + PHREEQC (Thermoddem database, T = 12°C).

    Key thermodynamic outcome (pe–pH diagrams across pH 2–10):
    The solid-phase stability field is completely dominated by Beidellite(Na) and acidic forms of montmorillonite (Hmontmorillonite).

    #Geochemistry #Hydrogeology #PHREEQC #ThermodynamicModeling #EnvironmentalDataScience #Rstats #Geoscience #ClayMineralogy #SvystunovaGully

  2. Added 25 mg/L Silicon (Si) and 5 mg/L Aluminium (Al) to the hydrogeochemical baseline of the Svystunova Gully mine water impoundment, modeling clay mineral phase equilibria using RedModRphree + PHREEQC (Thermoddem database, T = 12°C).

    Key thermodynamic outcome (pe–pH diagrams across pH 2–10):
    The solid-phase stability field is completely dominated by Beidellite(Na) and acidic forms of montmorillonite (Hmontmorillonite).

    #Geochemistry #Hydrogeology #PHREEQC #ThermodynamicModeling #EnvironmentalDataScience #Rstats #Geoscience #ClayMineralogy #SvystunovaGully