2008
DOI: 10.1007/s11663-008-9198-7
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Factors Affecting the Precipitation of Potassium Jarosite in Sulfate and Chloride Media

Abstract: The factors affecting the precipitation of potassium jarosite in both sulfate and chloride media were systematically investigated for the range of conditions likely to be encountered in hydrometallurgical practice. In sulfate solutions at 97°C, the amount of precipitate increases with increasing retention times up to 10 hours, with increasing temperatures to approximately 100°C, and with increasing ferric-ion concentrations. Despite the variations in the amount of precipitate, the composition remains nearly co… Show more

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Cited by 35 publications
(17 citation statements)
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“…Decreasing the K content of the jarosite increases its model age in this scenario. However, as described above, K‐rich jarosite is geochemically likely (Dutrizac, ). For a reasonable lower compositional limit of 1:1 K:Na, the model age of the jarosite alone is 4.25 ± 0.66 Ga.…”
Section: Discussionmentioning
confidence: 90%
“…Decreasing the K content of the jarosite increases its model age in this scenario. However, as described above, K‐rich jarosite is geochemically likely (Dutrizac, ). For a reasonable lower compositional limit of 1:1 K:Na, the model age of the jarosite alone is 4.25 ± 0.66 Ga.…”
Section: Discussionmentioning
confidence: 90%
“…Compared to the bottom samples, the very low K + surface concentrations may be explained by the precipitation of particular sulphate minerals (K-jarosite) (Dutrizac, 2008). Additionally, priority uptake by plants for the synthesis of organic matter could also be involved (Pitter, 2009).…”
Section: Chemical Variablesmentioning
confidence: 99%
“…Many studies have focused on efficiency-enhancing of removal systems and obtaining better working conditions. Among various methods applied in removal efficiency enhancement such optimizing working condition and utilizing more appropriate materials [1][2][3][4]. Jarosite is a promising approach and it is an effective scavenger for metals in iron and sulfate rich acidic solutions.…”
Section: Introductionmentioning
confidence: 99%
“…Diverse jarosite group minerals are formed based on the substitution of A with cations. The A sites can be occupied by monovalent (K, Na, Ag, Tl, H3O), divalent (Ca, Sr, Ba, Pb), trivalent and quadrivalent (Th, U) ions [1][2][3]. Their mineral names, synthetic equivalents, the substitution of A and formulas are listed in Table 1.…”
Section: Introductionmentioning
confidence: 99%
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