Evidence map›Paper›PMID 33731796›Full record

ArticleScientific reports2021

MgO surface lattice phonons observation during interstellar ice transition.

A Chavarría-Sibaja, S Marín-Sosa, E Bolaños-Jiménez, M Hernández-Calderón, O A Herrera-Sancho

Abstract read
In one paragraph

Article in Scientific reports, 2021. 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

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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

5 authors.

A Chavarría-SibajaEscuela de Física, Universidad de Costa Rica, San Pedro, San José, 2060, Costa Rica.
S Marín-SosaEscuela de Física, Universidad de Costa Rica, San Pedro, San José, 2060, Costa Rica.
E Bolaños-JiménezCentro de Investigación en Ciencia e Ingeniería de Materiales, Universidad de Costa Rica, San Pedro, San José, 2060, Costa Rica.
M Hernández-CalderónEscuela de Ciencia e Ingeniería de Materiales, Instituto Tecnológico de Costa Rica, Cartago, 30101, Costa Rica.
O A Herrera-SanchoEscuela de Física, Universidad de Costa Rica, San Pedro, San José, 2060, Costa Rica. oscar.herrerasancho@ucr.ac.cr.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Relevant information on the origins of the solar system and the early evolution of life itself can be derive from systematic and controlled exploration of water ice here on Earth. Therefore, over the last decades, a huge effort on experimental methodologies has been made to study the multiple crystal ice phases, which are observed outside our home-gravitational-potential. By employing (100)-oriented MgO lattice surface as a microcantilever sensor, we conducted the first ever study on the dynamics of the Structural Phase Transition at 185 K in water ice by means of coherent elastic scattering of electron diffraction. We estimate the amount of phonons caused by this transition applying precise quantum computing key tools, and resulting in a maximum value of 1.23 ± 0.02. Further applications of our microcantilever sensor were assessed using unambiguous mapping of the surface stress induced by the c([Formula: see text]) → p([Formula: see text]) Structural Phase Transition of the interstellar ice formulated on the Williamsom-Hall model. This development paves the way and thus establishes an efficient characterization tool of the surface mechanical strains of materials with potential applications arising from interstellar ice inclusive glaciers to the wide spectrum of solid-state physics.

Identifiers

PMID33731796
PMCPMC7969629

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