Evidence map›Paper›PMID 35883537›Full record

ArticleBiomolecules2022

How Can Ice Emerge at 0 °C?

Alexei V Finkelstein, Sergiy O Garbuzynskiy, Bogdan S Melnik

Erratum issuedAbstract read
In one paragraph

Article in Biomolecules, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. An erratum has been issued. Cited by 4 papers.

0numbers the graph read from it
0cells of the map it votes in
4citing 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

4 citing papers in PubMed.

  1. Review
  2. Article
  3. Article
  4. Article
4 · The record

Corrections and comments

5 · Who and what money

Authors and funding

3 authors.

Alexei V FinkelsteinInstitute of Protein Research, Russian Academy of Sciences, 142290 Pushchino, Russia.ORCID 0000-0002-2138-4803
Sergiy O GarbuzynskiyInstitute of Protein Research, Russian Academy of Sciences, 142290 Pushchino, Russia.ORCID 0000-0001-6592-4528
Bogdan S MelnikInstitute of Protein Research, Russian Academy of Sciences, 142290 Pushchino, Russia.ORCID 0000-0002-9176-6452

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The classical nucleation theory shows that bulk water freezing does not occur at temperatures above ≈ -30 °C, and that at higher temperatures ice nucleation requires the presence of some ice-binding surfaces. The temperature and rate of ice nucleation depend on the size and level of complementarity between the atomic structure of these surfaces and various H-bond-rich/depleted crystal planes. In our experiments, the ice nucleation temperature was within a range from -8 °C to -15 °C for buffer and water in plastic test tubes. Upon the addition of ice-initiating substances (i.e., conventional AgI or CuO investigated here), ice appeared in a range from -3 °C to -7 °C, and in the presence of the ice-nucleating bacterium

Indexed as

Antifreeze ProteinsIceBacteriaFreezingTemperatureAntifreeze ProteinsIcefreezing point of waterice-binding proteinice nucleationmelting point of icePseudomonas syringaetime of freezing

Identifiers

PMID35883537
PMCPMC9313213

What Socratic holds

Textmetadata
LicenceCC BY
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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 Socratic graph.