1934
DOI: 10.1021/ie50296a023
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Potassium Sulfate from Syngenite by High–Temperature Extraction with Water

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Cited by 11 publications
(6 citation statements)
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“…Changes in the crystallization areas of the individual salts are also considerable, especially in the cases of polyhalite, syngenite and magnesium sulphate (in comparison with the isotherms for the system K,SO,-Mg SO,-CaSO,-HH,O a t lower temperatures). Thus the polyhalite crystallization area, small at 308 K [5], and situated within the region of high MgSO, concentrations, at 373K undergoes a remarkable cnlargement [9] at the expense of the syngenite [14]). The solubility of calcium sulphate does not change a t temperatures above 373 K and it does not exceed 0,2y0.…”
Section: Resultsmentioning
confidence: 99%
“…Changes in the crystallization areas of the individual salts are also considerable, especially in the cases of polyhalite, syngenite and magnesium sulphate (in comparison with the isotherms for the system K,SO,-Mg SO,-CaSO,-HH,O a t lower temperatures). Thus the polyhalite crystallization area, small at 308 K [5], and situated within the region of high MgSO, concentrations, at 373K undergoes a remarkable cnlargement [9] at the expense of the syngenite [14]). The solubility of calcium sulphate does not change a t temperatures above 373 K and it does not exceed 0,2y0.…”
Section: Resultsmentioning
confidence: 99%
“…The syngenite decomposed into CaSO 4 , which was slightly soluble in water. When the concentration ratio of Ca 2+ /SO4 2− reached a certain value, K 2 SO 4 and CaSO 4 can form double salts in aqueous solution system [15]. Thus, the K and Ca was precipitated with the formation of K 2 Ca 2 (SO 4 ) 3 by crystallization.…”
Section: Effect Of Cao Addition On Water Leaching Productmentioning
confidence: 99%
“…This indicates that the reaction degree of desulfurization was increased. K 2 Ca 2 (SO 4 ) 3 easily decomposed into K 2 SO 4 and CaSO 4 in aqueous solution [15]. The recovery ratio of K remarkably increased, to 72-82%, due to the high solubility of K 2 SO 4 in water.…”
Section: X-ray Diffraction (Xrd) Analysismentioning
confidence: 99%
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“…The data for 210°, 220°, and 230°C. have been plotted together with the data by Hill (11) for the equilibrium with dense anhydrite at 100°and with those by Clarke and Partridge (4) for the equilibrium at 200°C . ; these present a continuous curve from 100°to 230°C.…”
Section: Mixtures Of Complex Saltsmentioning
confidence: 99%