Evidence map›Paper›PMID 36037025›Full record

ReviewChemistry (Weinheim an der Bergstrasse, Germany)2022

Calcium Carbonate Dissolution from the Laboratory to the Ocean: Kinetics and Mechanism.

Christopher Batchelor-McAuley, Minjun Yang, Rosalind E M Rickaby, Richard G Compton

Abstract readReview
PubMed Full text at PMC Publisher
In one paragraph

Review in Chemistry (Weinheim an der Bergstrasse, Germany), 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 4 papers.

0numbers the graph read from it
0cells of the map it votes in
4citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

4 citing papers in PubMed.

  1. Article
  2. Article
  3. Article
  4. Review
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

4 authors.

Christopher Batchelor-McAuleySchool of Chemistry, Trinity College Dublin, Dublin 2, Ireland.ORCID http://orcid.org/0000-0001-7276-9319
Minjun YangPhysical and Theoretical Chemistry Laboratory Department of Chemistry, University of Oxford South Parks Road, Oxford, OX1 3QZ, UK.ORCID http://orcid.org/0000-0001-8829-5883
Rosalind E M RickabyDepartment of Earth Sciences, University of Oxford, South Parks Road, Oxford, OX1 3AN, UK.ORCID http://orcid.org/0000-0002-6095-8419
Richard G ComptonPhysical and Theoretical Chemistry Laboratory Department of Chemistry, University of Oxford South Parks Road, Oxford, OX1 3QZ, UK.ORCID http://orcid.org/0000-0001-9841-5041

Funding

Oxford Martin School, University of Oxford
6 · The paper itself

Abstract

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.

Indexed as

Calcium CarbonateCalcium Carbonatecalcite compensationcarbonate chemistryheterogeneous reactionmass-transportpH buffer

Identifiers

PMID36037025
PMCPMC10092336

What OpenQuestion holds

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Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.