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Bubbly-ice densification in ice sheets: I. Theory
Salamatin A., Lipenkov V., Duval P.
at the asymptotic phase is mostly determined by the air content in the ice. In the companion paper (Lipenkov
Bubbly-ice densification in ice sheets: II. Applications
Lipenkov V., Salamatin A., Duval P.
in Holocene ice is inferred to be about 0.088 cm3g-1. The corresponding mean air pressure in bubbles
Specifics of geological composition, geochemistry and geochronology of rocks from the Kresty alkaline-ultrabasic massif (Maimecha-Kotui province, Polar Siberia)
Zvyagina, E. A., Gertner, I. F., Krasnova, T. S., Lipenkov, G. P., Sazonov, A. M.
Bubbly-ice densification in ice sheets: I. Theory
Salamatin A., Lipenkov V., Duval P.
at the asymptotic phase is mostly determined by the air content in the ice. In the companion paper (Lipenkov
Air-hydrate crystal growth in polar ice
Salamatin A., Lipenkov V., Hondoh T.
Post-nucleation conversion of an air bubble to clathrate air-hydrate crystal in ice
Salamatin A., Hondoh T., Uchida T., Lipenkov V.
Bubbly-ice densification in ice sheets: II. Applications
Lipenkov V., Salamatin A., Duval P.
in Holocene ice is inferred to be about 0.088 cm3g-1. The corresponding mean air pressure in bubbles
Simple relations for the close-off depth and age in dry-snow densification
Salamatin A., Lipenkov V.
Simple relations for the close-off depth and age in dry-snow densification
Salamatin A., Lipenkov V.
Post-nucleation conversion of an air bubble to clathrate air-hydrate crystal in ice
Salamatin A., Hondoh T., Uchida T., Lipenkov V.

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