Мобильная версия

Доступно журналов:

3 288

Доступно статей:

3 891 637

 

Скрыть метаданые

Автор Top, Zafer
Автор Martin, Seelye
Автор Becker, Paul
Дата выпуска 1985
dc.description Recently we reported anomalous dissolved neon‐helium ratios in the Arctic Ocean and suggested that the neon supersaturation is caused by the freezing process. We also predicted supersaturation of dissolved gases such as oxygen, which are heavier than neon. To pursue the tracer potential of these gases, we recently collected more seawater samples for the measurements of the noble gases, made dissolved oxygen measurements, and performed a set of laboratory freezing experiments. Here, we report the results of dissolved oxygen measurements made during the laboratory freezing experiments, and during the MIZEX 84 field program. In the laboratory we found that 1cm of ice growth caused approximately 0.5% dissolved oxygen supersaturation in a 90cm deep water column. Conversely, the ice phase was 53±2% undersaturated in dissolved oxygen, a result which is, within experimental uncertainties, identical to that obtained in the field.
Формат application.pdf
Копирайт Copyright 1985 by the American Geophysical Union.
Тема Oceanography: General
Тема Oceanography: General: Arctic and Antarctic oceanography
Тема Oceanography: General: Descriptive and regional oceanography
Тема Oceanography: Physical
Тема Oceanography: Physical: Ice mechanics and air‐sea‐ice exchange processes
Тема Oceanography: Biological and Chemical
Тема Oceanography: Biological and Chemical: Geochemistry
Название On the dissolved surface oxygen supersaturation in the Arctic
Тип article
DOI 10.1029/GL012i012p00821
Electronic ISSN 1944-8007
Print ISSN 0094-8276
Журнал Geophysical Research Letters
Том 12
Первая страница 821
Последняя страница 823
Аффилиация Top, Zafer; University of Miami, RSMAS, 4600 Rickenbacker Cswy., Miami, FL 33149
Аффилиация Martin, Seelye; University of Washington, School of Oceanography, WB10, Seattle, WA 98195
Аффилиация Becker, Paul; University of Washington, School of Oceanography, WB10, Seattle, WA 98195
Выпуск 12
Библиографическая ссылка Carpenter, J. H., The Chesapeake Bay Institute technique for the Winkler dissolved oxygen method, Limnol. Oceanog., 10, 141–143, 1965
Библиографическая ссылка Martin, S.P.Kauffman, The evolution of under‐ice melt ponds, or double diffusion at the freezing point, J. Fluid Mech., 64, 507–527, 1974
Библиографическая ссылка Martin, S. J., Glac, A field study of brine drainage and oil entrainment in first‐year sea ice, 88, 473–502, 1979
Библиографическая ссылка Martin, S., Frazil ice in rivers and oceans, Ann. Rev. Fluid Mech., 13, 379–397, 1981
Библиографическая ссылка Namiot, A.Yu.E. B.Bukhgalter, Clathrates formed by gases in ice, J. Struct. Chem., 6, 873–874, 1965
Библиографическая ссылка Top, Z.W. B.ClarkeR. M.Moore, Anomalous neonhelium ratios in the Arctic Ocean, Geophys. Res. Lett., 10, 1168–1171, 1983
Библиографическая ссылка Weiss, R. F., The solubility of nitrogen, oxygen and argon in water and seawater, Deep Sea Res., 17, 721–735, 1970

Скрыть метаданые