Evidence map›Paper›PMID 36449568›Full record

ArticleEnvironmental science & technology2022

Sulfidation and Reoxidation of U(VI)-Incorporated Goethite: Implications for U Retention during Sub-Surface Redox Cycling.

Olwen Stagg, Katherine Morris, Luke Thomas Townsend, Kristina O Kvashnina, Michael L Baker, Ryan L Dempsey, Liam Abrahamsen-Mills, Samuel Shaw

Open access · hybridAbstract read
In one paragraph

Article in Environmental science & technology, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 3 papers.

0numbers the graph read from it
0cells of the map it votes in
3citing papers in PubMed
0.8field-weighted citation impact, top 31% of its field
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

3 citing papers in PubMed, 13 citations in OpenAlex.

  1. Article
  2. Article
  3. Determination of Uranium Central-Field Covalency with 3Journal of the American Chemical Society · 2024
    Article
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

8 authors at 4 institutions in 3 countries.

Olwen StaggResearch Centre for Radwaste Disposal and Williamson Research Centre for Molecular Environmental Science, Department of Earth and Environmental Sciences, The University of Manchester, ManchesterM13 9PL, U.K.ORCID 0000-0002-3365-4110
Katherine MorrisResearch Centre for Radwaste Disposal and Williamson Research Centre for Molecular Environmental Science, Department of Earth and Environmental Sciences, The University of Manchester, ManchesterM13 9PL, U.K.ORCID 0000-0002-0716-7589
Luke Thomas TownsendResearch Centre for Radwaste Disposal and Williamson Research Centre for Molecular Environmental Science, Department of Earth and Environmental Sciences, The University of Manchester, ManchesterM13 9PL, U.K.ORCID 0000-0002-7991-9444
Kristina O KvashninaThe Rossendorf Beamline at ESRF─The European Synchrotron, CS40220, Grenoble Cedex 938043France.ORCID 0000-0003-4447-4542
Michael L BakerDepartment of Chemistry, The University of Manchester, ManchesterM13 9PL, U.K.ORCID 0000-0002-8246-3177
Ryan L DempseyDepartment of Chemistry, The University of Manchester, ManchesterM13 9PL, U.K.
Liam Abrahamsen-MillsNational Nuclear Laboratory, WarringtonWA3 6AE, Cheshire, U.K.
Samuel ShawResearch Centre for Radwaste Disposal and Williamson Research Centre for Molecular Environmental Science, Department of Earth and Environmental Sciences, The University of Manchester, ManchesterM13 9PL, U.K.ORCID 0000-0002-6353-5454
University of Manchester · GBDiamond Light Source · GBHelmholtz-Zentrum Dresden-Rossendorf · DENational Nuclear Laboratory · GB

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Over 60 years of nuclear activity have resulted in a global legacy of contaminated land and radioactive waste. Uranium (U) is a significant component of this legacy and is present in radioactive wastes and at many contaminated sites. U-incorporated iron (oxyhydr)oxides may provide a long-term barrier to U migration in the environment. However, reductive dissolution of iron (oxyhydr)oxides can occur on reaction with aqueous sulfide (sulfidation), a common environmental species, due to the microbial reduction of sulfate. In this work, U(VI)-goethite was initially reacted with aqueous sulfide, followed by a reoxidation reaction, to further understand the long-term fate of U species under fluctuating environmental conditions. Over the first day of sulfidation, a transient release of aqueous U was observed, likely due to intermediate uranyl(VI)-persulfide species. Despite this, overall U was retained in the solid phase, with the formation of nanocrystalline U(IV)O

Indexed as

IronUraniumIron CompoundsMineralsOxidation-ReductionOxidesSulfidesgoethiteIronIron CompoundsMineralsOxidesSulfidesUraniumiron (oxyhydr)oxidespersulfidesulfidationuraniumXAS

Identifiers

PMID36449568
PMCPMC9775214
OpenAlexW4310433493

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

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.