Evidence map›Paper›PMID 31979295›Full record

ArticleMolecules (Basel, Switzerland)2020

Phase Transition of Ice at High Pressures and Low Temperatures.

Jinjin Xu, Jinfeng Liu, Jinyun Liu, Wenxin Hu, Xiao He, Jinjin Li

Open access · goldAbstract read
In one paragraph

Article in Molecules (Basel, Switzerland), 2020. 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
0.4field-weighted citation impact, top 40% 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, 4 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

6 authors at 3 institutions in 1 country.

Jinjin XuShanghai Engineering Research Center of Molecular Therapeutics and New Drug Development, School of Chemistry and Molecular Engineering, East China Normal University, Shanghai 200062, China.
Jinfeng LiuState Key Laboratory of Natural Medicines, Department of Basic Medicine and Clinical Pharmacy, China Pharmaceutical University, Nanjing 210009, China.
Jinyun LiuKey Laboratory of Functional Molecular Solids of the Ministry of Education, Anhui Laboratory of Molecule-Based Materials, College of Chemistry and Materials Science, Anhui Normal University, Wuhu 241000, China.
Wenxin HuThe Computer Center, School of Computer Science and Software Engineering, East China Normal University, Shanghai 200062, China.
Xiao HeShanghai Engineering Research Center of Molecular Therapeutics and New Drug Development, School of Chemistry and Molecular Engineering, East China Normal University, Shanghai 200062, China.
Jinjin LiNational Key Laboratory of Science and Technology on Micro/Nano Fabrication, Key laboratory for Thin Film and Microfabrication of the Ministry of Education, Department of Micro/Nano-electronics, Shanghai Jiao Tong University, Shanghai 200240, China.
China Pharmaceutical University · CNShanghai Jiao Tong University · CNNew York University Shanghai · CN

Funding

Foundation of Anhui Laboratory of Molecule-Based Materials FZJ19014Intergovernmental International Scientific and Technological Cooperation of Shanghai 17520710200National Key R&D Program of China 2016YFA0501700National Natural Science Foundation of China 51672176, 21922301, 21673074, 21761132022, 21901157, and 21703289Science and Technology Major Project of Anhui Province 18030901093Shanghai Municipal Natural Science Foundation 18ZR1412600
6 · The paper itself

Abstract

The behavior of ice under extreme conditions undergoes the change of intermolecular binding patterns and leads to the structural phase transitions, which are needed for modeling the convection and internal structure of the giant planets and moons of the solar system as well as H2O-rich exoplanets. Such extreme conditions limit the structural explorations in laboratory but open a door for the theoretical study. The ice phases IX and XIII are located in the high pressure and low temperature region of the phase diagram. However, to the best of our knowledge, the phase transition boundary between these two phases is still not clear. In this work, based on the second-order Møller-Plesset perturbation (MP2) theory, we theoretically investigate the ice phases IX and XIII and predict their structures, vibrational spectra and Gibbs free energies at various extreme conditions, and for the first time confirm that the phase transition from ice IX to XIII can occur around 0.30 GPa and 154 K. The proposed work, taking into account the many-body electrostatic effect and the dispersion interactions from the first principles, opens up the possibility of completing the ice phase diagram and provides an efficient method to explore new phases of molecular crystals.

Indexed as

IcePhase TransitionCold TemperatureCrystallizationModels, MolecularPressureQuantum TheorySpectrum Analysis, RamanStatic ElectricityThermodynamicsTransition TemperatureWaterIceWaterice IXice phase transitionice XIIIMP2 theoryRaman spectra

Identifiers

PMID31979295
PMCPMC7037513
OpenAlexW3001565061

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.