2012
DOI: 10.1063/1.4766816
|View full text |Cite
|
Sign up to set email alerts
|

Experimental evidence of superionic conduction in H2O ice

Abstract: Ionic conductivity and molar volume measurements were performed on H(2)O ice at high pressure (P) and temperature (T) in a resistive-heated diamond anvil cell. The conductivity data obtained at P = 20-62 GPa, T = 304-930 K are well fitted with a single Arrhenius equation. Isothermal volume measurements at T = 873 K, P = 30-101 GPa indicate that H(2)O ice undergoes phase transitions at P = 50 GPa and 53 GPa due to hydrogen-bond symmetrization. Combining these results, we suggest that the conduction mechanism do… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

2
37
0

Year Published

2013
2013
2024
2024

Publication Types

Select...
7
1
1

Relationship

0
9

Authors

Journals

citations
Cited by 62 publications
(39 citation statements)
references
References 28 publications
2
37
0
Order By: Relevance
“…The prediction that ice enters a superionic state 162 has been validated experimentally. 69,[163][164][165] Similar predictions have been made for ammonia. 162 Moreover, full ionization of ammonia to contains H À (blue) and H 2 (white), 83 ) (i.e.…”
Section: Predictions For Experimentssupporting
confidence: 74%
“…The prediction that ice enters a superionic state 162 has been validated experimentally. 69,[163][164][165] Similar predictions have been made for ammonia. 162 Moreover, full ionization of ammonia to contains H À (blue) and H 2 (white), 83 ) (i.e.…”
Section: Predictions For Experimentssupporting
confidence: 74%
“…This ice phase is thought to be the dominant phase of the interior of giant icy planets and may be responsible for the observed anomalous magnetic moment of Uranus and Neptune. Recent studies showed experimental evidence for superionic conduction at significantly low temperature compared with earlier theoretical estimates (17,18,50). The presence of salt impurities in natural ice, incorporated via ocean-ice interaction, rock-ice interaction at depth, or processes that occurred during accretion (1,2,(23)(24)(25), could strongly modify the thermodynamic conditions and the mechanism for the appearance of change in such an extreme state of matter, and eventually promote novel exotic properties, thus challenging our present description of the physics of these bodies, essentially based on the assumption of the properties of pure ice under high pressure.…”
Section: Resultsmentioning
confidence: 99%
“…8 Whether H 2 O is in the superionic or liquid state in the planetary interior is of great importance to understanding the source of the planetary magnetic field. 9,10 Although some experimental studies reported the existence of the superionic phase, 11,12 recent measurements of the melting temperature of H 2 O above the superionic phase show low melting temperatures and a quite gentle melting curve compared with those of the QMD prediction, 13 which implies that H 2 O should remain in the liquid state even at deep interior conditions. This discrepancy between experimental and theoretical studies suggests that the QMD based EOS model is disputable for modeling the planetary interior.…”
Section: Introductionmentioning
confidence: 95%