Solubility Equilibria in the System Mg(OH)2–MgCl2–H2O from 298 to 393 K
The solubility equilibria of the ternary system Mg(OH)2–MgCl2–H2O were determined at temperatures from 298 to 393 K applying equilibration periods of up to 3.5 years. As a result, four thermodynamically stable magnesium chloride hydroxide hydrates (Sorel phases) exist in the ternary system within t...
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Veröffentlicht in: | Journal of chemical and engineering data 2017-04, Vol.62 (4), p.1384-1396 |
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description | The solubility equilibria of the ternary system Mg(OH)2–MgCl2–H2O were determined at temperatures from 298 to 393 K applying equilibration periods of up to 3.5 years. As a result, four thermodynamically stable magnesium chloride hydroxide hydrates (Sorel phases) exist in the ternary system within the investigated temperature range. These are the 3-1-8 phase [3Mg(OH)2·MgCl2·8H2O], the 9-1-4 phase [9Mg(OH)2·MgCl2·4H2O], the 2-1-4 phase [2Mg(OH)2·MgCl2·4H2O], and the 2-1-2 phase [2Mg(OH)2·MgCl2·2H2O]. The also known 5-1-8 phase [5Mg(OH)2·MgCl2·8H2O] was found to be metastable in the solid–liquid system. With this work, a reliable solubility data set is now available, for example, to prove the long-term stability of magnesia building materials in the presence of salt-bearing media, a challenging demand on the material in a special application as a barrier construction material in salt formation. |
doi_str_mv | 10.1021/acs.jced.6b00928 |
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As a result, four thermodynamically stable magnesium chloride hydroxide hydrates (Sorel phases) exist in the ternary system within the investigated temperature range. These are the 3-1-8 phase [3Mg(OH)2·MgCl2·8H2O], the 9-1-4 phase [9Mg(OH)2·MgCl2·4H2O], the 2-1-4 phase [2Mg(OH)2·MgCl2·4H2O], and the 2-1-2 phase [2Mg(OH)2·MgCl2·2H2O]. The also known 5-1-8 phase [5Mg(OH)2·MgCl2·8H2O] was found to be metastable in the solid–liquid system. With this work, a reliable solubility data set is now available, for example, to prove the long-term stability of magnesia building materials in the presence of salt-bearing media, a challenging demand on the material in a special application as a barrier construction material in salt formation.</description><identifier>ISSN: 0021-9568</identifier><identifier>EISSN: 1520-5134</identifier><identifier>DOI: 10.1021/acs.jced.6b00928</identifier><language>eng</language><publisher>American Chemical Society</publisher><ispartof>Journal of chemical and engineering data, 2017-04, Vol.62 (4), p.1384-1396</ispartof><rights>Copyright © 2017 American Chemical Society</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><orcidid>0000-0001-5522-2848</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://pubs.acs.org/doi/pdf/10.1021/acs.jced.6b00928$$EPDF$$P50$$Gacs$$H</linktopdf><linktohtml>$$Uhttps://pubs.acs.org/doi/10.1021/acs.jced.6b00928$$EHTML$$P50$$Gacs$$H</linktohtml><link.rule.ids>314,776,780,27055,27903,27904,56716,56766</link.rule.ids></links><search><creatorcontrib>Pannach, Melanie</creatorcontrib><creatorcontrib>Bette, Sebastian</creatorcontrib><creatorcontrib>Freyer, Daniela</creatorcontrib><title>Solubility Equilibria in the System Mg(OH)2–MgCl2–H2O from 298 to 393 K</title><title>Journal of chemical and engineering data</title><addtitle>J. Chem. Eng. Data</addtitle><description>The solubility equilibria of the ternary system Mg(OH)2–MgCl2–H2O were determined at temperatures from 298 to 393 K applying equilibration periods of up to 3.5 years. As a result, four thermodynamically stable magnesium chloride hydroxide hydrates (Sorel phases) exist in the ternary system within the investigated temperature range. These are the 3-1-8 phase [3Mg(OH)2·MgCl2·8H2O], the 9-1-4 phase [9Mg(OH)2·MgCl2·4H2O], the 2-1-4 phase [2Mg(OH)2·MgCl2·4H2O], and the 2-1-2 phase [2Mg(OH)2·MgCl2·2H2O]. The also known 5-1-8 phase [5Mg(OH)2·MgCl2·8H2O] was found to be metastable in the solid–liquid system. With this work, a reliable solubility data set is now available, for example, to prove the long-term stability of magnesia building materials in the presence of salt-bearing media, a challenging demand on the material in a special application as a barrier construction material in salt formation.</description><issn>0021-9568</issn><issn>1520-5134</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid/><recordid>eNotkLtOw0AQRVcIJEygp9wSJGxmX_ZuiaxAUBK5CNTWrj0bbDmx8KNIxz_wh3wJDqQ6o9HVHc0h5JZBxICzR1v0UV1gGcUOwHB9RgKmOISKCXlOApgyoVGxviRXfV8DgEw4C8hy0zajq5pqOND55zgNrqssrfZ0-EC6OfQD7uh6e5ct7vnP1_d6mzZHLnhGfdfuKDeaDi0VRtDlNbnwtunx5sQZeX-ev6WLcJW9vKZPq9ByBkNYKGdcLJOEYclFLKWPOcbSatSl1B6NBSdLtAYgQWVQFl46NEo6Bl4pLmbk4b93-jmv27HbT9dyBvlRRP63nETkJxHiFxWGUb0</recordid><startdate>20170413</startdate><enddate>20170413</enddate><creator>Pannach, Melanie</creator><creator>Bette, Sebastian</creator><creator>Freyer, Daniela</creator><general>American Chemical Society</general><scope/><orcidid>https://orcid.org/0000-0001-5522-2848</orcidid></search><sort><creationdate>20170413</creationdate><title>Solubility Equilibria in the System Mg(OH)2–MgCl2–H2O from 298 to 393 K</title><author>Pannach, Melanie ; Bette, Sebastian ; Freyer, Daniela</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a210t-c5b9b64771ed23644f62e64a8e8d48fe9a0b4dea9007e59e4cf4be954b10f5523</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pannach, Melanie</creatorcontrib><creatorcontrib>Bette, Sebastian</creatorcontrib><creatorcontrib>Freyer, Daniela</creatorcontrib><jtitle>Journal of chemical and engineering data</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Pannach, Melanie</au><au>Bette, Sebastian</au><au>Freyer, Daniela</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Solubility Equilibria in the System Mg(OH)2–MgCl2–H2O from 298 to 393 K</atitle><jtitle>Journal of chemical and engineering data</jtitle><addtitle>J. Chem. Eng. Data</addtitle><date>2017-04-13</date><risdate>2017</risdate><volume>62</volume><issue>4</issue><spage>1384</spage><epage>1396</epage><pages>1384-1396</pages><issn>0021-9568</issn><eissn>1520-5134</eissn><abstract>The solubility equilibria of the ternary system Mg(OH)2–MgCl2–H2O were determined at temperatures from 298 to 393 K applying equilibration periods of up to 3.5 years. As a result, four thermodynamically stable magnesium chloride hydroxide hydrates (Sorel phases) exist in the ternary system within the investigated temperature range. These are the 3-1-8 phase [3Mg(OH)2·MgCl2·8H2O], the 9-1-4 phase [9Mg(OH)2·MgCl2·4H2O], the 2-1-4 phase [2Mg(OH)2·MgCl2·4H2O], and the 2-1-2 phase [2Mg(OH)2·MgCl2·2H2O]. The also known 5-1-8 phase [5Mg(OH)2·MgCl2·8H2O] was found to be metastable in the solid–liquid system. With this work, a reliable solubility data set is now available, for example, to prove the long-term stability of magnesia building materials in the presence of salt-bearing media, a challenging demand on the material in a special application as a barrier construction material in salt formation.</abstract><pub>American Chemical Society</pub><doi>10.1021/acs.jced.6b00928</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0001-5522-2848</orcidid></addata></record> |
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title | Solubility Equilibria in the System Mg(OH)2–MgCl2–H2O from 298 to 393 K |
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