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Calcium Carbonate Dissolution from the Laboratory to the Ocean: Kinetics and Mechanism
The ultimate fate, over the course of millennia, of nearly all of the carbon dioxide formed by humankind is for it to react with calcium carbonate in the world's oceans. Although, this reaction is of global relevance, aspects of the calcite dissolution reaction remain poorly described with appa...
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Published in: | Chemistry : a European journal 2022-12, Vol.28 (68), p.e202202290-n/a |
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creator | Batchelor‐McAuley, Christopher Yang, Minjun Rickaby, Rosalind E. M. Compton, Richard G. |
description | The ultimate fate, over the course of millennia, of nearly all of the carbon dioxide formed by humankind is for it to react with calcium carbonate in the world's oceans. Although, this reaction is of global relevance, aspects of the calcite dissolution reaction remain poorly described with apparent contradictions present throughout the expansive literature. In this perspective we aim to evidence how a lack of appreciation of the role of mass‐transport may have hampered developments in this area. These insights have important implications for both idealised experiments performed under laboratory conditions and for the measurement and modelling of oceanic calcite sediment dissolution.
Carbonate chemistry: Although calcite dissolution has been extensively studied there appears to be a problem; apparent contradictions, discrepancies between laboratories and inconsistencies with field measurements seemingly pervade the literature. This review highlights how – in some circumstances – a lack of appreciation of the role of mass‐transport may have hindered development. |
doi_str_mv | 10.1002/chem.202202290 |
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Carbonate chemistry: Although calcite dissolution has been extensively studied there appears to be a problem; apparent contradictions, discrepancies between laboratories and inconsistencies with field measurements seemingly pervade the literature. This review highlights how – in some circumstances – a lack of appreciation of the role of mass‐transport may have hindered development.</description><identifier>ISSN: 0947-6539</identifier><identifier>EISSN: 1521-3765</identifier><identifier>DOI: 10.1002/chem.202202290</identifier><identifier>PMID: 36037025</identifier><language>eng</language><publisher>Germany: Wiley Subscription Services, Inc</publisher><subject>Calcite ; calcite compensation ; Calcium Carbonate ; Carbon dioxide ; carbonate chemistry ; Chemistry ; Dissolution ; heterogeneous reaction ; mass-transport ; Ocean models ; Oceans ; pH buffer ; Review ; Reviews</subject><ispartof>Chemistry : a European journal, 2022-12, Vol.28 (68), p.e202202290-n/a</ispartof><rights>2022 The Authors. Chemistry - A European Journal published by Wiley-VCH GmbH</rights><rights>2022 The Authors. Chemistry - A European Journal published by Wiley-VCH GmbH.</rights><rights>2022. This article is published under http://creativecommons.org/licenses/by-nc/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4690-994d9720d0c00d3f5772e383fa8e385063082ac66ed59736343c4bf01e1331cf3</citedby><cites>FETCH-LOGICAL-c4690-994d9720d0c00d3f5772e383fa8e385063082ac66ed59736343c4bf01e1331cf3</cites><orcidid>0000-0001-7276-9319 ; 0000-0001-8829-5883 ; 0000-0002-6095-8419 ; 0000-0001-9841-5041</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,314,780,784,885,27924,27925</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/36037025$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Batchelor‐McAuley, Christopher</creatorcontrib><creatorcontrib>Yang, Minjun</creatorcontrib><creatorcontrib>Rickaby, Rosalind E. M.</creatorcontrib><creatorcontrib>Compton, Richard G.</creatorcontrib><title>Calcium Carbonate Dissolution from the Laboratory to the Ocean: Kinetics and Mechanism</title><title>Chemistry : a European journal</title><addtitle>Chemistry</addtitle><description>The ultimate fate, over the course of millennia, of nearly all of the carbon dioxide formed by humankind is for it to react with calcium carbonate in the world's oceans. Although, this reaction is of global relevance, aspects of the calcite dissolution reaction remain poorly described with apparent contradictions present throughout the expansive literature. In this perspective we aim to evidence how a lack of appreciation of the role of mass‐transport may have hampered developments in this area. These insights have important implications for both idealised experiments performed under laboratory conditions and for the measurement and modelling of oceanic calcite sediment dissolution.
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Carbonate chemistry: Although calcite dissolution has been extensively studied there appears to be a problem; apparent contradictions, discrepancies between laboratories and inconsistencies with field measurements seemingly pervade the literature. This review highlights how – in some circumstances – a lack of appreciation of the role of mass‐transport may have hindered development.</abstract><cop>Germany</cop><pub>Wiley Subscription Services, Inc</pub><pmid>36037025</pmid><doi>10.1002/chem.202202290</doi><tpages>11</tpages><orcidid>https://orcid.org/0000-0001-7276-9319</orcidid><orcidid>https://orcid.org/0000-0001-8829-5883</orcidid><orcidid>https://orcid.org/0000-0002-6095-8419</orcidid><orcidid>https://orcid.org/0000-0001-9841-5041</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Calcite calcite compensation Calcium Carbonate Carbon dioxide carbonate chemistry Chemistry Dissolution heterogeneous reaction mass-transport Ocean models Oceans pH buffer Review Reviews |
title | Calcium Carbonate Dissolution from the Laboratory to the Ocean: Kinetics and Mechanism |
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