Evidence of Freezing Pressure in Sea Ice Discrete Brine Inclusions and Its Impact on Aqueous‐Gaseous Equilibrium-Reference-Cited by-同舟云学术

Evidence of Freezing Pressure in Sea Ice Discrete Brine Inclusions and Its Impact on Aqueous‐Gaseous Equilibrium

Published:2019-03 Issue:3 Volume:124 Page:1660-1678
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:J. Geophys. Res. Oceans

Author:

Crabeck O.¹²^ORCID,Galley R. J.¹,Mercury L.³,Delille B.⁴,Tison J.‐L.⁵^ORCID,Rysgaard S.¹⁶⁷

Affiliation:

1. The Centre for Earth Observation Science, Department of Geological ScienceUniversity of Manitoba Winnipeg Manitoba Canada

2. Centre for Ocean and Atmospheric Sciences, School of Environmental SciencesUniversity of East Anglia Norwich UK

3. Institut des sciences de la Terre d'OrléansUniversité d'Orléans, CNRS, BRGM Orleans France

4. Unité d'Océanographie ChimiqueUniversité de Liège Liege Belgium

5. Laboratoire de Glaciologie, DGESUniversité Libre de Bruxelles Brussels Belgium

6. Greenland Climate Research CentreGreenland Institute of Natural Resources Nuuk Greenland

7. Arctic Research CentreAarhus University Aarhus Denmark

Funder

European Union Agency for Network and Information Security

Natural Sciences and Engineering Research Council of Canada

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JC014597

Reference45 articles.

1. Assur A.(1960).Composition of sea ice and its tensile strength. SIPRE research report 44 U.S. Army snow ice and permafrost research establishment Corps of Engineers Wilmette Illinois December 1960.

2. Some Crystal Growth Features of Sea Ice

3. Equations for Determining the Gas and Brine Volumes in Sea-Ice Samples

4. First “in situ” determination of gas transport coefficients ( DO2, DAr, and DN2) from bulk gas concentration measurements (O2, N2, Ar) in natural sea ice

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