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通过升华和冷凝进行冰烧结

Ice Sintering by Sublimation and Condensation.

作者信息

Demmenie Menno, Woutersen Sander, Bonn Daniel

机构信息

Institute of Physics, University of Amsterdam, Science Park 904, 1098 XH Amsterdam, The Netherlands.

Van 't Hoff Institute for Molecular Sciences, University of Amsterdam, Science Park 904, 1098 XH Amsterdam, The Netherlands.

出版信息

J Phys Chem Lett. 2025 Feb 27;16(8):2104-2109. doi: 10.1021/acs.jpclett.5c00050. Epub 2025 Feb 20.

DOI:10.1021/acs.jpclett.5c00050
PMID:39976459
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11874037/
Abstract

The sintering behavior of ice has been the subject of controversy for more than 160 years. Various factors have led to confusion about the mechanisms behind mass transport during sintering; erroneously derived growth rate exponents, experimental challenges in achieving equilibrium conditions, and incorrect comparisons between ice sintering and snow densification have all played a role. Here we demonstrate that sintering of ice under equilibrium conditions proceeds primarily through sublimation and condensation. Mass transfer occurs through the vapor phase, driven by increased volatility at the formed neck due to its high curvature. Our findings on the sintering of ice spheres are consistent with the healing of micrometer-sized scratches in ice under similar conditions.

摘要

在超过160年的时间里,冰的烧结行为一直是一个有争议的话题。各种因素导致了对烧结过程中质量传输背后机制的混淆;错误推导的生长速率指数、实现平衡条件的实验挑战以及冰烧结与雪致密化之间的错误比较都起到了一定作用。在这里,我们证明了在平衡条件下冰的烧结主要通过升华和凝结进行。质量传输通过气相发生,这是由形成的颈部由于其高曲率而增加的挥发性驱动的。我们关于冰球烧结的发现与在类似条件下冰中微米级划痕的愈合情况一致。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f06/11874037/d96223a42f6d/jz5c00050_0005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f06/11874037/7f654a62553b/jz5c00050_0001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f06/11874037/e737f9660c8c/jz5c00050_0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f06/11874037/53ff8120f42a/jz5c00050_0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f06/11874037/99158db01515/jz5c00050_0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f06/11874037/d96223a42f6d/jz5c00050_0005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f06/11874037/7f654a62553b/jz5c00050_0001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f06/11874037/e737f9660c8c/jz5c00050_0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f06/11874037/53ff8120f42a/jz5c00050_0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f06/11874037/99158db01515/jz5c00050_0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f06/11874037/d96223a42f6d/jz5c00050_0005.jpg

相似文献

1
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本文引用的文献

1
Damage due to ice crystallization.冰晶造成的损害。
Sci Rep. 2025 Jan 16;15(1):2179. doi: 10.1038/s41598-025-86117-5.
2
Scratch-Healing Behavior of Ice by Local Sublimation and Condensation.冰通过局部升华和凝结的划痕愈合行为。
J Phys Chem C Nanomater Interfaces. 2022 Feb 3;126(4):2179-2183. doi: 10.1021/acs.jpcc.1c09590. Epub 2022 Jan 19.
3
The microstructural evolution of water ice in the solar system through sintering.太阳系中通过烧结作用实现的水冰微观结构演化。
J Geophys Res Planets. 2019 Feb;124(2):243-277. doi: 10.1029/2018je005773. Epub 2018 Dec 26.
4
The Surface of Ice under Equilibrium and Nonequilibrium Conditions.平衡和非平衡条件下的冰表面
Acc Chem Res. 2019 Apr 16;52(4):1006-1015. doi: 10.1021/acs.accounts.8b00615. Epub 2019 Mar 29.
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Why Is It So Difficult to Identify the Onset of Ice Premelting?为何识别冰预融的起始如此困难?
J Phys Chem Lett. 2018 Sep 6;9(17):5179-5182. doi: 10.1021/acs.jpclett.8b02244. Epub 2018 Aug 28.
6
Molecular Insight into the Slipperiness of Ice.冰的滑性的分子见解。
J Phys Chem Lett. 2018 Jun 7;9(11):2838-2842. doi: 10.1021/acs.jpclett.8b01188. Epub 2018 May 16.
7
Grand Canonical Investigation of the Quasi Liquid Layer of Ice: Is It Liquid?大正则研究冰的类液相层:它是液相吗?
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Proc Natl Acad Sci U S A. 2017 Jan 10;114(2):227-232. doi: 10.1073/pnas.1612893114. Epub 2016 Dec 12.