Evidence map›Paper›PMID 29184152›Full record

ArticleScientific reports2017

Pressure driven spin transition in siderite and magnesiosiderite single crystals.

Christopher Weis, Christian Sternemann, Valerio Cerantola, Christoph J Sahle, Georg Spiekermann, Manuel Harder, Yury Forov, Alexander Kononov, Robin Sakrowski, Hasan Yavaş and 2 more

Open access · goldAbstract read
In one paragraph

Article in Scientific reports, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 2 papers.

0numbers the graph read from it
0cells of the map it votes in
2citing papers in PubMed
3.2field-weighted citation impact, top 9% 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

2 citing papers in PubMed, 32 citations in OpenAlex.

  1. FeCOACS omega · 2023
    Article
  2. 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

12 authors at 4 institutions in 2 countries.

Christopher WeisFakultät Physik/DELTA, Technische Universität Dortmund, Dortmund, 44227, Germany. christopher.weis@tu-dortmund.de.
Christian SternemannFakultät Physik/DELTA, Technische Universität Dortmund, Dortmund, 44227, Germany.ORCID 0000-0001-9415-1106
Valerio CerantolaEuropean Synchrotron Radiation Facility, 71 Avenue des Martyrs, Grenoble, 38000, France.
Christoph J SahleEuropean Synchrotron Radiation Facility, 71 Avenue des Martyrs, Grenoble, 38000, France.ORCID 0000-0001-8645-3163
Georg SpiekermannInstitute of Earth and Environmental Science, Universität Potsdam, Potsdam, 14476, Germany.
Manuel HarderDeutsches Elektronen-Synchrotron DESY, Hamburg, 22607, Germany.
Yury ForovFakultät Physik/DELTA, Technische Universität Dortmund, Dortmund, 44227, Germany.
Alexander KononovFakultät Physik/DELTA, Technische Universität Dortmund, Dortmund, 44227, Germany.
Robin SakrowskiFakultät Physik/DELTA, Technische Universität Dortmund, Dortmund, 44227, Germany.
Hasan YavaşDeutsches Elektronen-Synchrotron DESY, Hamburg, 22607, Germany.
Metin TolanFakultät Physik/DELTA, Technische Universität Dortmund, Dortmund, 44227, Germany.
Max WilkeInstitute of Earth and Environmental Science, Universität Potsdam, Potsdam, 14476, Germany.
TU Dortmund University · DEDeutsches Elektronen-Synchrotron DESY · DEEuropean Synchrotron Radiation Facility · FRUniversity of Potsdam · DE

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Iron-bearing carbonates are candidate phases for carbon storage in the deep Earth and may play an important role for the Earth's carbon cycle. To elucidate the properties of carbonates at conditions of the deep Earth, we investigated the pressure driven magnetic high spin to low spin transition of synthetic siderite FeCO

Identifiers

PMID29184152
PMCPMC5705641
OpenAlexW2768743350

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.