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Congelation ice : ウィキペディア英語版 | Congelation ice
Congelation ice is ice that forms on the bottom of an established ice cover. == Seawater ==
On seawater, congelation ice is ice that forms on the bottom of an established sea ice cover, usually in the form of platelets which coalesce to form solid ice.〔(Sea Ice Types, Sea Ice Geophysics, University of Alaska )〕〔(National Snow and Ice Data Center: All About Sea Ice: Ice Formation )〕 Only the water freezes to ice, the salt from the seawater is concentrated into brine, some of which is contained in pockets in the new ice. Due to the brine pockets, congelation ice on seawater is neither as hard nor as transparent as fresh water ice.〔(National Snow and Ice Data Center: All About Sea Ice: Salinity and Brine )〕
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