Earth`s Cryosphere, 2017, Vol. XXI, No. 3, p. 30-37
FORMATION OF CLATHRATE HYDRATES OF HYDROCHLOROFLUOROCARBON 141B IN THE DEEP BOREHOLE AT VOSTOK STATION (ANTARCTICA) IN THE COURSE OF THE UNSEALING OF SUBGLACIAL LAKE VOSTOK
A.Yu. Manakov1, A.V. Ildyakov1, V.Ya. Lipenkov2,4, A.A. Ekaykin2, T.V. Khodzher3
1 Nikolaev Institute of Inorganic Chemistry, SB RAS,
3, Acad. Lavrentiev ave., Novosibirsk, 630090, Russia; manakov@niic.nsc.ru
2 Arctic and Antarctic Research Institute, 38, Beringa str., St. Petersburg, 199387, Russia; lipenkov@aari.ru
3 Limnological Institute, SB RAS, 3, Ulan-Batorskaya str., Irkutsk, 664033, Russia; khodzher@lin.irk.ru
4Institute of Earth Science, St. Petersburg State University,
33-35, 10th Line of Vasilievsky Ostrov, St. Petersburg, 199178, Russia
We have presented the results of a study of core samples which were recovered from a deep borehole after the second unsealing of subglacial Lake Vostok in 2015 (borehole 5G-3, in which a mixture of kerosene and HCFC-141b densifier was used as the drilling fluid). The intensive mixing of the subglacial water and the drilling fluid resulted in the formation of a solid plug that filled the volume of the borehole and blocked the access to the lake. We have demonstrated that this solid plug consists of kerosene, ice and clathrate hydrate of HCFC-141b. The obtained data suggest that the drilling fluid presently used at Vostok should be replaced, at least in the bottom section of the hole, by another fluid which does not react with subglacial water.
Lake Vostok, drilling, gas hydrate, Freon HCFC-141b