Reactive CaCO 3 Formation from CO 2 and Methanolic Ca(OH) 2 Dispersions: Transient Methoxide Salts, Carbonate Esters and Sol-Gels
A combination of and characterization techniques was used to determine the mechanism of calcium carbonate (CaCO ) formation from calcium hydroxide (Ca(OH) ) dispersions in methanol/water (CH OH/H O) systems. Mid-infrared (mid-IR) analysis shows that in the absence of carbon dioxide (CO ) Ca(OH) esta...
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creator | Kathyola, Thokozile A Willneff, Elizabeth A Willis, Colin J Dowding, Peter J Schroeder, Sven L M |
description | A combination of
and
characterization techniques was used to determine the mechanism of calcium carbonate (CaCO
) formation from calcium hydroxide (Ca(OH)
) dispersions in methanol/water (CH
OH/H
O) systems. Mid-infrared (mid-IR) analysis shows that in the absence of carbon dioxide (CO
) Ca(OH)
establishes a reaction equilibrium with CH
OH, forming calcium hydroxide methoxide (Ca(OH)(OCH
)) and calcium methoxide (Ca(OCH
)
). Combined
mid-IR, thermogravimetric analysis (TGA), X-ray diffraction (XRD), X-ray absorption spectroscopy and scanning electron microscopy examination of the reaction product formed in the presence of CO
reveals the formation of calcium dimethylcarbonate (Ca(OCOOCH
)
). This strongly suggests that carbonation takes place by reaction with the Ca(OCH
)
formed from a Ca(OH)
and CH
OH reaction. Time-resolved XRD indicates that in the presence of H
O the Ca(OCOOCH
)
ester releases CH
OH and CO
, forming ACC, which subsequently transforms into vaterite and then calcite. TGA reveals that thermal decomposition of Ca(OCOOCH
)
in the absence of H
O mainly leads to the reformation of Ca(OCH
)
, but this is accompanied by a significant parallel reaction that releases dimethylether (CH
OCH
) and CO
. CaCO
is the final product in both decomposition pathways. For CH
OH/H
O mixtures containing more than 50 mol % H
O, direct formation of calcite from Ca(OH)
becomes the dominant pathway, although the formation of some Ca(OCOOCH
)
was still evident in the
mid-IR spectra of 20 and 40 mol % CH
OH systems. In the presence of ≤20 mol % H
O, hydrolysis of the ester led to the formation of an ACC sol-gel. In both the 90 and 100 mol % CH
OH systems, diffusion-limited ACC → vaterite → calcite transformations were observed. Traces of aragonite were also detected. We believe that this is the first time that these reaction pathways during the carbonation of Ca(OH)
in a methanolic phase have been systematically and experimentally characterized. |
doi_str_mv | 10.1021/acsphyschemau.4c00041 |
format | Article |
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and
characterization techniques was used to determine the mechanism of calcium carbonate (CaCO
) formation from calcium hydroxide (Ca(OH)
) dispersions in methanol/water (CH
OH/H
O) systems. Mid-infrared (mid-IR) analysis shows that in the absence of carbon dioxide (CO
) Ca(OH)
establishes a reaction equilibrium with CH
OH, forming calcium hydroxide methoxide (Ca(OH)(OCH
)) and calcium methoxide (Ca(OCH
)
). Combined
mid-IR, thermogravimetric analysis (TGA), X-ray diffraction (XRD), X-ray absorption spectroscopy and scanning electron microscopy examination of the reaction product formed in the presence of CO
reveals the formation of calcium dimethylcarbonate (Ca(OCOOCH
)
). This strongly suggests that carbonation takes place by reaction with the Ca(OCH
)
formed from a Ca(OH)
and CH
OH reaction. Time-resolved XRD indicates that in the presence of H
O the Ca(OCOOCH
)
ester releases CH
OH and CO
, forming ACC, which subsequently transforms into vaterite and then calcite. TGA reveals that thermal decomposition of Ca(OCOOCH
)
in the absence of H
O mainly leads to the reformation of Ca(OCH
)
, but this is accompanied by a significant parallel reaction that releases dimethylether (CH
OCH
) and CO
. CaCO
is the final product in both decomposition pathways. For CH
OH/H
O mixtures containing more than 50 mol % H
O, direct formation of calcite from Ca(OH)
becomes the dominant pathway, although the formation of some Ca(OCOOCH
)
was still evident in the
mid-IR spectra of 20 and 40 mol % CH
OH systems. In the presence of ≤20 mol % H
O, hydrolysis of the ester led to the formation of an ACC sol-gel. In both the 90 and 100 mol % CH
OH systems, diffusion-limited ACC → vaterite → calcite transformations were observed. Traces of aragonite were also detected. We believe that this is the first time that these reaction pathways during the carbonation of Ca(OH)
in a methanolic phase have been systematically and experimentally characterized.</description><identifier>ISSN: 2694-2445</identifier><identifier>EISSN: 2694-2445</identifier><identifier>DOI: 10.1021/acsphyschemau.4c00041</identifier><identifier>PMID: 39364354</identifier><language>eng</language><publisher>United States</publisher><ispartof>ACS Physical Chemistry Au, 2024-09, Vol.4 (5), p.555-567</ispartof><rights>2024 The Authors. Published by American Chemical Society.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c694-e0dc027239e9266e8e499929179fd548bd6ebe79c7b8dd322b514f22cb54ca5e3</cites><orcidid>0000-0002-4232-5378 ; 0000-0003-1752-7469 ; 0000-0002-5351-0210</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,860,27903,27904</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/39364354$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Kathyola, Thokozile A</creatorcontrib><creatorcontrib>Willneff, Elizabeth A</creatorcontrib><creatorcontrib>Willis, Colin J</creatorcontrib><creatorcontrib>Dowding, Peter J</creatorcontrib><creatorcontrib>Schroeder, Sven L M</creatorcontrib><title>Reactive CaCO 3 Formation from CO 2 and Methanolic Ca(OH) 2 Dispersions: Transient Methoxide Salts, Carbonate Esters and Sol-Gels</title><title>ACS Physical Chemistry Au</title><addtitle>ACS Phys Chem Au</addtitle><description>A combination of
and
characterization techniques was used to determine the mechanism of calcium carbonate (CaCO
) formation from calcium hydroxide (Ca(OH)
) dispersions in methanol/water (CH
OH/H
O) systems. Mid-infrared (mid-IR) analysis shows that in the absence of carbon dioxide (CO
) Ca(OH)
establishes a reaction equilibrium with CH
OH, forming calcium hydroxide methoxide (Ca(OH)(OCH
)) and calcium methoxide (Ca(OCH
)
). Combined
mid-IR, thermogravimetric analysis (TGA), X-ray diffraction (XRD), X-ray absorption spectroscopy and scanning electron microscopy examination of the reaction product formed in the presence of CO
reveals the formation of calcium dimethylcarbonate (Ca(OCOOCH
)
). This strongly suggests that carbonation takes place by reaction with the Ca(OCH
)
formed from a Ca(OH)
and CH
OH reaction. Time-resolved XRD indicates that in the presence of H
O the Ca(OCOOCH
)
ester releases CH
OH and CO
, forming ACC, which subsequently transforms into vaterite and then calcite. TGA reveals that thermal decomposition of Ca(OCOOCH
)
in the absence of H
O mainly leads to the reformation of Ca(OCH
)
, but this is accompanied by a significant parallel reaction that releases dimethylether (CH
OCH
) and CO
. CaCO
is the final product in both decomposition pathways. For CH
OH/H
O mixtures containing more than 50 mol % H
O, direct formation of calcite from Ca(OH)
becomes the dominant pathway, although the formation of some Ca(OCOOCH
)
was still evident in the
mid-IR spectra of 20 and 40 mol % CH
OH systems. In the presence of ≤20 mol % H
O, hydrolysis of the ester led to the formation of an ACC sol-gel. In both the 90 and 100 mol % CH
OH systems, diffusion-limited ACC → vaterite → calcite transformations were observed. Traces of aragonite were also detected. We believe that this is the first time that these reaction pathways during the carbonation of Ca(OH)
in a methanolic phase have been systematically and experimentally characterized.</description><issn>2694-2445</issn><issn>2694-2445</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNpVkF1LwzAUhoMobsz9BCWXCnam-WgX76TuQ5gM3O5LmpyyStuUpBN36T-3-1D06hwOz_PCeRG6DskoJDR8UNo3m53XG6jUdsQ1IYSHZ6hPI8kDyrk4_7P30ND79w6hImQ0EpeoxySLOBO8j77eQOm2-ACcqGSJGZ5aV6m2sDXOna1wd6NY1Qa_QrtRtS0L3ZG3y_ldd38ufAPOd7B_xGunal9A3R5Q-1kYwCtVtv6-E1xma9UCnvi2Ew6BK1sGMyj9FbrIVelheJoDtJ5O1sk8WCxnL8nTItD7R4AYTWhMmQRJowjGwKWUVIaxzI3g48xEkEEsdZyNjWGUZiLkOaU6E1wrAWyAxDFWO-u9gzxtXFEpt0tDku5LTf-Vmp5K7bybo9dsswrMr_VTIfsGaYF2OQ</recordid><startdate>20240925</startdate><enddate>20240925</enddate><creator>Kathyola, Thokozile A</creator><creator>Willneff, Elizabeth A</creator><creator>Willis, Colin J</creator><creator>Dowding, Peter J</creator><creator>Schroeder, Sven L M</creator><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><orcidid>https://orcid.org/0000-0002-4232-5378</orcidid><orcidid>https://orcid.org/0000-0003-1752-7469</orcidid><orcidid>https://orcid.org/0000-0002-5351-0210</orcidid></search><sort><creationdate>20240925</creationdate><title>Reactive CaCO 3 Formation from CO 2 and Methanolic Ca(OH) 2 Dispersions: Transient Methoxide Salts, Carbonate Esters and Sol-Gels</title><author>Kathyola, Thokozile A ; Willneff, Elizabeth A ; Willis, Colin J ; Dowding, Peter J ; Schroeder, Sven L M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c694-e0dc027239e9266e8e499929179fd548bd6ebe79c7b8dd322b514f22cb54ca5e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kathyola, Thokozile A</creatorcontrib><creatorcontrib>Willneff, Elizabeth A</creatorcontrib><creatorcontrib>Willis, Colin J</creatorcontrib><creatorcontrib>Dowding, Peter J</creatorcontrib><creatorcontrib>Schroeder, Sven L M</creatorcontrib><collection>PubMed</collection><collection>CrossRef</collection><jtitle>ACS Physical Chemistry Au</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kathyola, Thokozile A</au><au>Willneff, Elizabeth A</au><au>Willis, Colin J</au><au>Dowding, Peter J</au><au>Schroeder, Sven L M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Reactive CaCO 3 Formation from CO 2 and Methanolic Ca(OH) 2 Dispersions: Transient Methoxide Salts, Carbonate Esters and Sol-Gels</atitle><jtitle>ACS Physical Chemistry Au</jtitle><addtitle>ACS Phys Chem Au</addtitle><date>2024-09-25</date><risdate>2024</risdate><volume>4</volume><issue>5</issue><spage>555</spage><epage>567</epage><pages>555-567</pages><issn>2694-2445</issn><eissn>2694-2445</eissn><abstract>A combination of
and
characterization techniques was used to determine the mechanism of calcium carbonate (CaCO
) formation from calcium hydroxide (Ca(OH)
) dispersions in methanol/water (CH
OH/H
O) systems. Mid-infrared (mid-IR) analysis shows that in the absence of carbon dioxide (CO
) Ca(OH)
establishes a reaction equilibrium with CH
OH, forming calcium hydroxide methoxide (Ca(OH)(OCH
)) and calcium methoxide (Ca(OCH
)
). Combined
mid-IR, thermogravimetric analysis (TGA), X-ray diffraction (XRD), X-ray absorption spectroscopy and scanning electron microscopy examination of the reaction product formed in the presence of CO
reveals the formation of calcium dimethylcarbonate (Ca(OCOOCH
)
). This strongly suggests that carbonation takes place by reaction with the Ca(OCH
)
formed from a Ca(OH)
and CH
OH reaction. Time-resolved XRD indicates that in the presence of H
O the Ca(OCOOCH
)
ester releases CH
OH and CO
, forming ACC, which subsequently transforms into vaterite and then calcite. TGA reveals that thermal decomposition of Ca(OCOOCH
)
in the absence of H
O mainly leads to the reformation of Ca(OCH
)
, but this is accompanied by a significant parallel reaction that releases dimethylether (CH
OCH
) and CO
. CaCO
is the final product in both decomposition pathways. For CH
OH/H
O mixtures containing more than 50 mol % H
O, direct formation of calcite from Ca(OH)
becomes the dominant pathway, although the formation of some Ca(OCOOCH
)
was still evident in the
mid-IR spectra of 20 and 40 mol % CH
OH systems. In the presence of ≤20 mol % H
O, hydrolysis of the ester led to the formation of an ACC sol-gel. In both the 90 and 100 mol % CH
OH systems, diffusion-limited ACC → vaterite → calcite transformations were observed. Traces of aragonite were also detected. We believe that this is the first time that these reaction pathways during the carbonation of Ca(OH)
in a methanolic phase have been systematically and experimentally characterized.</abstract><cop>United States</cop><pmid>39364354</pmid><doi>10.1021/acsphyschemau.4c00041</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0002-4232-5378</orcidid><orcidid>https://orcid.org/0000-0003-1752-7469</orcidid><orcidid>https://orcid.org/0000-0002-5351-0210</orcidid></addata></record> |
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title | Reactive CaCO 3 Formation from CO 2 and Methanolic Ca(OH) 2 Dispersions: Transient Methoxide Salts, Carbonate Esters and Sol-Gels |
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