Evidence map›Paper›PMID 33479173›Full record

ArticleProceedings of the National Academy of Sciences of the United States of America2021

Diagenetic formation of uranium-silica polymers in lake sediments over 3,300 years.

Pierre Lefebvre, Alkiviadis Gourgiotis, Arnaud Mangeret, Pierre Sabatier, Pierre Le Pape, Olivier Diez, Pascale Louvat, Nicolas Menguy, Pauline Merrot, Camille Baya and 9 more

Open access · bronzeAbstract read
In one paragraph

Article in Proceedings of the National Academy of Sciences of the United States of America, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing papers in PubMed
0.9field-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

1 citing paper in PubMed, 15 citations in OpenAlex.

  1. 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

19 authors at 3 institutions in 2 countries.

Pierre LefebvreInstitut de Minéralogie, de Physique des Matériaux et de Cosmochimie, UMR 7590 Sorbonne Université-CNRS-MNHN-IRD (Museum National d'Histoire Naturelle-Institut de Recherche pour le Développement), 75005 Paris, France; pierre.lefebvre@sorbonne-universite.fr.ORCID https://orcid.org/0000-0003-2298-4234
Alkiviadis GourgiotisInstitut de Radioprotection et de Sûreté Nucléaire, PSE-ENV SEDRE, 92260 Fontenay-aux-Roses, France.
Arnaud MangeretInstitut de Radioprotection et de Sûreté Nucléaire, PSE-ENV SEDRE, 92260 Fontenay-aux-Roses, France.ORCID https://orcid.org/0000-0002-2629-0400
Pierre SabatierUMR 5204, Université Grenoble Alpes-Université Savoie Mont Blanc-CNRS-EDYTEM (Environnements DYnamiques et TErritoires de la Montagne), 73370 Le Bourget-Du-Lac, France.ORCID https://orcid.org/0000-0002-9620-1514
Pierre Le PapeInstitut de Minéralogie, de Physique des Matériaux et de Cosmochimie, UMR 7590 Sorbonne Université-CNRS-MNHN-IRD (Museum National d'Histoire Naturelle-Institut de Recherche pour le Développement), 75005 Paris, France.ORCID https://orcid.org/0000-0002-8100-936X
Olivier DiezInstitut de Radioprotection et de Sûreté Nucléaire, PSE-ENV SEDRE, 92260 Fontenay-aux-Roses, France.
Pascale LouvatUMR 7154, Université de Paris-Institut de Physique du Globe de Paris-CNRS, 75005 Paris, France.
Nicolas MenguyInstitut de Minéralogie, de Physique des Matériaux et de Cosmochimie, UMR 7590 Sorbonne Université-CNRS-MNHN-IRD (Museum National d'Histoire Naturelle-Institut de Recherche pour le Développement), 75005 Paris, France.
Pauline MerrotInstitut de Minéralogie, de Physique des Matériaux et de Cosmochimie, UMR 7590 Sorbonne Université-CNRS-MNHN-IRD (Museum National d'Histoire Naturelle-Institut de Recherche pour le Développement), 75005 Paris, France.
Camille BayaInstitut de Minéralogie, de Physique des Matériaux et de Cosmochimie, UMR 7590 Sorbonne Université-CNRS-MNHN-IRD (Museum National d'Histoire Naturelle-Institut de Recherche pour le Développement), 75005 Paris, France.
Mathilde ZebrackiInstitut de Radioprotection et de Sûreté Nucléaire, PSE-ENV SEDRE, 92260 Fontenay-aux-Roses, France.
Pascale BlanchartInstitut de Radioprotection et de Sûreté Nucléaire, PSE-ENV SEDRE, 92260 Fontenay-aux-Roses, France.
Emmanuel MaletUMR 5204, Université Grenoble Alpes-Université Savoie Mont Blanc-CNRS-EDYTEM (Environnements DYnamiques et TErritoires de la Montagne), 73370 Le Bourget-Du-Lac, France.
Didier JézéquelUMR 7154, Université de Paris-Institut de Physique du Globe de Paris-CNRS, 75005 Paris, France.ORCID https://orcid.org/0000-0002-1983-9899
Jean-Louis ReyssUMR 5204, Université Grenoble Alpes-Université Savoie Mont Blanc-CNRS-EDYTEM (Environnements DYnamiques et TErritoires de la Montagne), 73370 Le Bourget-Du-Lac, France.
John R BargarStanford Synchrotron Radiation Lightsource, SLAC National Accelerator Laboratory, Menlo Park, CA 94025.ORCID https://orcid.org/0000-0001-9303-4901
Jérôme GaillardetUMR 7154, Université de Paris-Institut de Physique du Globe de Paris-CNRS, 75005 Paris, France.
Charlotte CazalaInstitut de Radioprotection et de Sûreté Nucléaire, PSE-ENV SEDRE, 92260 Fontenay-aux-Roses, France.
Guillaume MorinInstitut de Minéralogie, de Physique des Matériaux et de Cosmochimie, UMR 7590 Sorbonne Université-CNRS-MNHN-IRD (Museum National d'Histoire Naturelle-Institut de Recherche pour le Développement), 75005 Paris, France.ORCID https://orcid.org/0000-0001-9304-4202
Centre National de la Recherche Scientifique · FRInstitut de Radioprotection et de Sûreté Nucléaire · FRSLAC National Accelerator Laboratory · US

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The long-term fate of uranium-contaminated sediments, especially downstream former mining areas, is a widespread environmental challenge. Essential for their management is the proper understanding of uranium (U) immobilization mechanisms in reducing environments. In particular, the long-term behavior of noncrystalline U(IV) species and their possible evolution to more stable phases in subsurface conditions is poorly documented, which limits our ability to predict U long-term geochemical reactivity. Here, we report direct evidence for the evolution of U speciation over 3,300 y in naturally highly U-enriched sediments (350-760 µg ⋅ g

Indexed as

diagenetic aginglake sedimentsnoncrystalline speciesuraniumuranium isotopes

Identifiers

PMID33479173
PMCPMC7848604
OpenAlexW3125001277

What OpenQuestion holds

Textmetadata
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.