Evidence map›Paper›PMID 39893673›Full record

ArticleEnvironmental science & technology2025

Ice Nucleation Abilities and Chemical Characteristics of Laboratory-Generated and Aged Biomass Burning Aerosols.

Jie Chen, Fähndrich Martin Othmar Jakob, Aristeidis Voliotis, Huihui Wu, Sara Aisyah Syafira, Osayomwanbor Oghama, Nadia Shardt, Nicolas Fauré, Xiangrui Kong, Gordon Mcfiggans and 1 more

Abstract read
In one paragraph

Article in Environmental science & technology, 2025. 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.

Jie ChenInstitute for Atmospheric and Climate Science, ETH Zürich, Zurich 8092, Switzerland.ORCID 0000-0001-5353-1110
Fähndrich Martin Othmar JakobInstitute for Atmospheric and Climate Science, ETH Zürich, Zurich 8092, Switzerland.
Aristeidis VoliotisCentre for Atmospheric Science, Department of Earth and Environmental Sciences, School of Natural Sciences, University of Manchester, Manchester M13 9PL, U.K.ORCID 0000-0001-9710-9851
Huihui WuCentre for Atmospheric Science, Department of Earth and Environmental Sciences, School of Natural Sciences, University of Manchester, Manchester M13 9PL, U.K.
Sara Aisyah SyafiraCentre for Atmospheric Science, Department of Earth and Environmental Sciences, School of Natural Sciences, University of Manchester, Manchester M13 9PL, U.K.
Osayomwanbor OghamaCentre for Atmospheric Science, Department of Earth and Environmental Sciences, School of Natural Sciences, University of Manchester, Manchester M13 9PL, U.K.
Nadia ShardtInstitute for Atmospheric and Climate Science, ETH Zürich, Zurich 8092, Switzerland.
Nicolas FauréDepartment of Chemistry and Molecular Biology, University of Gothenburg, SE-413 90 Gothenburg, Sweden.ORCID 0000-0003-3200-2337
Xiangrui KongDepartment of Chemistry and Molecular Biology, University of Gothenburg, SE-413 90 Gothenburg, Sweden.ORCID 0000-0002-7205-0723
Gordon McfiggansCentre for Atmospheric Science, Department of Earth and Environmental Sciences, School of Natural Sciences, University of Manchester, Manchester M13 9PL, U.K.ORCID 0000-0002-3423-7896
Zamin A KanjiInstitute for Atmospheric and Climate Science, ETH Zürich, Zurich 8092, Switzerland.ORCID 0000-0001-8610-3921

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Biomass burning aerosol (BBA) contributes significantly to the global aerosol burden, yet its chemical nature and ice nucleation activities (INAs) are unconstrained due to the heterogeneity in biomass sources and complex evolution of atmospheric aging processes. This study comprehensively investigates the chemical composition and INA of BBA generated through laboratory-controlled burns with different biomasses and burning conditions. Both freshly emitted and photochemically aged BBA produced from different processes exhibit distinct and reproducible chemical compositions. However, the INA of BBA shows substantial variability at mixed-phase cloud temperatures and cannot be predicted by the chemical variability of the enriched carbonaceous materials. This indicates the negligible role of carbonaceous materials in determining the INA of BBA. Using laboratory data, we further evaluate the impact of BBA on atmospheric ice nucleation using particulate matter mass concentration and particle equivalent spherical radius. The estimated ice nucleating particle (INP) concentrations contributed by laboratory-produced BBA are lower than those observed during BBA pollution in field studies. This discrepancy is likely attributed to co-lofted mineral particles during real-world biomass burning, such as ash or soil particles, rather than carbonaceous-rich particles from combustion. We encourage further research to quantify the contribution of mineral particles to the INP concentrations of BBA.

Indexed as

BiomassIceAerosolsLaboratoriesParticulate MatterAerosolsIceParticulate Matterbiomass burning aerosolice nucleationphotochemical aging

Identifiers

PMID39893673
PMCPMC11823448

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Registered trials

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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.