Evidence map›Paper›PMID 39539464›Full record

ArticleACS ES&T air2024

Formation of Sodium Chloride on the Surface of Sulfate-Rich Gobi Desert Salt in Response to Water Adsorption.

Nicolas Fauré, Jie Chen, Luca Artiglia, Markus Ammann, Thorsten Bartels-Rausch, Zamin A Kanji, Sen Wang, Jan B C Pettersson, Erik S Thomson, Ivan Gladich and 1 more

Abstract read
In one paragraph

Article in ACS ES&T air, 2024. 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
–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

1 citing paper in PubMed.

  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

11 authors.

Nicolas FauréDepartment of Chemistry and Molecular Biology, Atmospheric Science, University of Gothenburg, SE-41390 Gothenburg, Sweden.ORCID https://orcid.org/0000-0003-3200-2337
Jie ChenDepartment of Environmental Systems Science, ETH Zürich, Zürich, 8092, Switzerland.ORCID https://orcid.org/0000-0001-5353-1110
Luca ArtigliaLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, CH-5232 Villigen PSI, Switzerland.ORCID https://orcid.org/0000-0003-4683-6447
Markus AmmannLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, CH-5232 Villigen PSI, Switzerland.ORCID https://orcid.org/0000-0001-5922-9000
Thorsten Bartels-RauschLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, CH-5232 Villigen PSI, Switzerland.ORCID https://orcid.org/0000-0002-7548-2572
Zamin A KanjiDepartment of Environmental Systems Science, ETH Zürich, Zürich, 8092, Switzerland.ORCID https://orcid.org/0000-0001-8610-3921
Sen WangShaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, Northwest University, Xi'an 710127, China.
Jan B C PetterssonDepartment of Chemistry and Molecular Biology, Atmospheric Science, University of Gothenburg, SE-41390 Gothenburg, Sweden.ORCID https://orcid.org/0000-0001-8420-6126
Erik S ThomsonDepartment of Chemistry and Molecular Biology, Atmospheric Science, University of Gothenburg, SE-41390 Gothenburg, Sweden.ORCID https://orcid.org/0000-0003-2428-7539
Ivan GladichEuropean Centre for Living Technology (ECLT), Dorsoduro, Calle Crosera, 30124 Venice, Italy.ORCID https://orcid.org/0000-0003-0929-3439
Xiangrui KongDepartment of Chemistry and Molecular Biology, Atmospheric Science, University of Gothenburg, SE-41390 Gothenburg, Sweden.ORCID https://orcid.org/0000-0002-7205-0723

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Dust storms in arid regions transport desert salts and dust, affecting geochemical processes, atmospheric chemistry, climate, and human health. This study examines how the gas-salt interface composition of desert salt changes with varying relative humidity (RH), using ambient pressure X-ray photoelectron spectroscopy (APXPS), near-edge X-ray absorption fine structure (NEXAFS) spectroscopy, and molecular dynamics (MD) simulations. Ion chromatography analysis of desert salt indicates it is predominantly composed of sulfate, sodium, and magnesium ions, with traces of calcium, chloride, nitrate, and potassium ions. APXPS and NEXAFS surface analyses show that, at 0% RH, the gas-salt interface primarily features Na

Identifiers

PMID39539464
PMCPMC11555638

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.