Francisco Patiño, Mizraim U Flores, Iván A Reyes, Martín Reyes, Juan Hernández, Isauro Rivera, Julio C Juárez
{"title":"Alkaline decomposition of synthetic jarosite with arsenic","authors":"Francisco Patiño, Mizraim U Flores, Iván A Reyes, Martín Reyes, Juan Hernández, Isauro Rivera, Julio C Juárez","doi":"10.1186/1467-4866-14-2","DOIUrl":null,"url":null,"abstract":"<p>The widespread use of jarosite-type compounds to eliminate impurities in the hydrometallurgical industry is due to their capability to incorporate several elements into their structures. Some of these elements are of environmental importance (Pb<sup>2+</sup>, Cr<sup>6+</sup>, As<sup>5+</sup>, Cd<sup>2+</sup>, Hg<sup>2+</sup>). For the present paper, AsO<sub>4</sub><sup>3-</sup> was incorporated into the lattice of synthetic jarosite in order to carry out a reactivity study. Alkaline decomposition is characterized by removal of sulfate and potassium ions from the lattice and formation of a gel consisting of iron hydroxides with absorbed arsenate. Decomposition curves show an induction period followed by a conversion period. The induction period is independent of particle size and exponentially decreases with temperature. The conversion period is characterized by formation of a hydroxide halo that surrounds an unreacted jarosite core. During the conversion period in NaOH media for [OH<sup>-</sup>]?>?8?×?10<sup>-3</sup>?mol?L<sup>-1</sup>, the process showed a reaction order of 1.86, and an apparent activation energy of 60.3?kJ?mol<sup>-1</sup> was obtained. On the other hand, during the conversion period in Ca(OH)<sub>2</sub> media for [OH<sup>-</sup>]?>?1.90?×?10<sup>-2</sup>?mol?L<sup>-1</sup>, the reaction order was 1.15, and an apparent activation energy of 74.4?kJ?mol<sup>-1</sup> was obtained. The results are consistent with the spherical particle model with decreasing core and chemical control.</p>","PeriodicalId":12694,"journal":{"name":"Geochemical Transactions","volume":"14 1","pages":""},"PeriodicalIF":0.9000,"publicationDate":"2013-04-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1186/1467-4866-14-2","citationCount":"19","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochemical Transactions","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1186/1467-4866-14-2","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 19
Abstract
The widespread use of jarosite-type compounds to eliminate impurities in the hydrometallurgical industry is due to their capability to incorporate several elements into their structures. Some of these elements are of environmental importance (Pb2+, Cr6+, As5+, Cd2+, Hg2+). For the present paper, AsO43- was incorporated into the lattice of synthetic jarosite in order to carry out a reactivity study. Alkaline decomposition is characterized by removal of sulfate and potassium ions from the lattice and formation of a gel consisting of iron hydroxides with absorbed arsenate. Decomposition curves show an induction period followed by a conversion period. The induction period is independent of particle size and exponentially decreases with temperature. The conversion period is characterized by formation of a hydroxide halo that surrounds an unreacted jarosite core. During the conversion period in NaOH media for [OH-]?>?8?×?10-3?mol?L-1, the process showed a reaction order of 1.86, and an apparent activation energy of 60.3?kJ?mol-1 was obtained. On the other hand, during the conversion period in Ca(OH)2 media for [OH-]?>?1.90?×?10-2?mol?L-1, the reaction order was 1.15, and an apparent activation energy of 74.4?kJ?mol-1 was obtained. The results are consistent with the spherical particle model with decreasing core and chemical control.
期刊介绍:
Geochemical Transactions publishes high-quality research in all areas of chemistry as it relates to materials and processes occurring in terrestrial and extraterrestrial systems.