Journal
PHYSICAL CHEMISTRY CHEMICAL PHYSICS
Volume 24, Issue 1, Pages 35-41Publisher
ROYAL SOC CHEMISTRY
DOI: 10.1039/d1cp03922a
Keywords
-
Funding
- Austrian Science Fund FWF [I1392]
- Centre for Molecular Water Science (CMWS, DESY Hamburg)
- DOC fellowship of the Austrian Academy of Sciences oAW
- University of Innsbruck
- Austrian Science Fund (FWF) [I1392] Funding Source: Austrian Science Fund (FWF)
Ask authors/readers for more resources
The phase transition of hexagonal ice under pressure occurs at different temperature ranges, with ice IX formation being influenced by impurities. Both HDA and ice IX are considered long-lived metastable phases.
For slowly compressed hexagonal ice pressure-induced amorphisation to high-density amorphous ice (HDA) takes place below and at 130 K, but polymorphic transformation to ice IX takes place at 140-170 K. Stable ice II only forms above 170 K. Ice IX impurities trigger ice IX growth even at 120 K. HDA and ice IX are equally long-lived, where both can be regarded as metastable phases.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available
Share Paper
