Phenol compounds in the borehole 5G, Vostok station, after the unlocking of the subglacial lake

The main results after the first unlocking into the subglacial Lake Vostok were as follows: the Lake had been opened and not polluted; the water pressure within the lake was not balanced by a column of the drilling liquid that resulted in unplanned rise of water in the borehole up to 340 m. The main...

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Published in:Ice and Snow
Main Authors: I. Alekhina A., A. Moskvin L., A. Ekaykin A., V. Lipenkov Ya., И. Алехина А., А. Москвин Л., А. Екайкин А., В. Липенков Я.
Format: Article in Journal/Newspaper
Language:Russian
Published: IGRAS 2017
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/407
https://doi.org/10.15356/2076-6734-2017-3-417-426
id ftjias:oai:oai.ice.elpub.ru:article/407
record_format openpolar
institution Open Polar
collection Ice and Snow (E-Journal)
op_collection_id ftjias
language Russian
topic Antarctica
drilling fluid
freezing
hydrocarbons
SALE
secondary ice core
Антарктида
вторичный лёд
заливочная жидкость
ледяные керны
углеводороды
spellingShingle Antarctica
drilling fluid
freezing
hydrocarbons
SALE
secondary ice core
Антарктида
вторичный лёд
заливочная жидкость
ледяные керны
углеводороды
I. Alekhina A.
A. Moskvin L.
A. Ekaykin A.
V. Lipenkov Ya.
И. Алехина А.
А. Москвин Л.
А. Екайкин А.
В. Липенков Я.
Phenol compounds in the borehole 5G, Vostok station, after the unlocking of the subglacial lake
topic_facet Antarctica
drilling fluid
freezing
hydrocarbons
SALE
secondary ice core
Антарктида
вторичный лёд
заливочная жидкость
ледяные керны
углеводороды
description The main results after the first unlocking into the subglacial Lake Vostok were as follows: the Lake had been opened and not polluted; the water pressure within the lake was not balanced by a column of the drilling liquid that resulted in unplanned rise of water in the borehole up to 340 m. The main problem during the drilling in the lake ice was to prevent a pollution of water by the drilling fluid, which filled the borehole, and thus, to avoid a compression of the fluid which could be the main source of chemical and biological pollution of not only the Lake itself, but also the Lake water samples and ice cores. The article presents results of analysis of causes for the occurrence of phenolic compounds in the central channel in the core of secondary ice, being formed by the lake water that rose into the well after the first penetration (the range of depths was 3426–3450 m). It was found that the process, running within the borehole during the drilling, can be described as the fractionation of phenolic compounds, being contained in the filling liquid, to the water phase with its subsequent freezing. We have developed methods for the determination of concentrations of phenolic compounds in the original aviation kerosene and Freon HCFC-141b: 6. mg·l−1 and 0.032 mg·l−1, respectively. To analyze the composition of phenolic compounds in the extract of real filling liquid, located at the bottom of the borehole, the method of gas chromatography-mass spectrometry (GC-MS) was used. The corresponding peaks were quite well resolved and identified as phenol and its derivatives. The main components of the extract were phenol (20%), 2.5-dimethyl phenol (23,8%), 2,4,6-trimethylphenol, and other congeners of phenol. In our case, the Lake Vostok was not polluted during both, the first and second penetrations, however, the problem of human impact on these pristine and unique subglacial reservoirs remains extremely relevant. This impact includes not only direct water pollution of the lake by the drilling fluid, but also possible ...
format Article in Journal/Newspaper
author I. Alekhina A.
A. Moskvin L.
A. Ekaykin A.
V. Lipenkov Ya.
И. Алехина А.
А. Москвин Л.
А. Екайкин А.
В. Липенков Я.
author_facet I. Alekhina A.
A. Moskvin L.
A. Ekaykin A.
V. Lipenkov Ya.
И. Алехина А.
А. Москвин Л.
А. Екайкин А.
В. Липенков Я.
author_sort I. Alekhina A.
title Phenol compounds in the borehole 5G, Vostok station, after the unlocking of the subglacial lake
title_short Phenol compounds in the borehole 5G, Vostok station, after the unlocking of the subglacial lake
title_full Phenol compounds in the borehole 5G, Vostok station, after the unlocking of the subglacial lake
title_fullStr Phenol compounds in the borehole 5G, Vostok station, after the unlocking of the subglacial lake
title_full_unstemmed Phenol compounds in the borehole 5G, Vostok station, after the unlocking of the subglacial lake
title_sort phenol compounds in the borehole 5g, vostok station, after the unlocking of the subglacial lake
publisher IGRAS
publishDate 2017
url https://ice-snow.igras.ru/jour/article/view/407
https://doi.org/10.15356/2076-6734-2017-3-417-426
long_lat ENVELOPE(106.000,106.000,-77.500,-77.500)
ENVELOPE(106.837,106.837,-78.464,-78.464)
geographic Lake Vostok
Vostok Station
geographic_facet Lake Vostok
Vostok Station
genre Annals of Glaciology
Antarc*
Antarctic Science
Antarctica
ice core
Memoirs of National Institute of Polar Research
Polar Research
Антарктида
genre_facet Annals of Glaciology
Antarc*
Antarctic Science
Antarctica
ice core
Memoirs of National Institute of Polar Research
Polar Research
Антарктида
op_source Ice and Snow; Том 57, № 3 (2017); 417-426
Лёд и Снег; Том 57, № 3 (2017); 417-426
2412-3765
2076-6734
10.15356/2076-6734-2017-3
op_relation https://ice-snow.igras.ru/jour/article/view/407/234
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Christner B.C., Priscu J.C., Achberger A.M., Barbante C., Carter S.P., Christianson K., Michaud A.B., Mikucki J.A., Mitchell A.C., Skidmore M.L., Vick-Majors T.J., the WISSARD Science Team . A microbial ecosystem beneath the West Antarctic Ice Sheet // Nature . 2014 . V . 512 . P . 310–313 .
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Alekhina I.A., Marie D., Petit J.R., Lukin V.V., Zubkov V.M., Bulat S.A. Molecular analysis of bacterial diversity in kerosene-based drilling fluid from the deep ice borehole at Vostok, East Antarctica // FEMS Microbiology Ecology . 2007 . V . 59 . P . 289–299 .
Code of conduct for the exploration and research of subglacial aquatic environments . 2011 . ATCMIP 33 .34 . Antarctic Treaty Consultative Meeting; Buenos Aires, 20 June – 1 July 2011 .
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Алехина И.А., Васильев Н.И., Екайкин А.А., Липенков В.Я. Предварительные результаты исследований химического состава воды, замерзшей в буровой скважине после вскрытия озера Восток // Проблемы Арктики и Антарктики . 2014 . Вып . 2 (100) . С . 5–14 .
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Манаков А.Ю., Илдяков А.В., Липенков В.Я., Екайкин А.А., Ходжер Т.В. Образование клатратных гидратов гидрохлорофлуорокарбона 141b в глубокой скважине на ст . Восток (Антарктида) в процессе вскрытия подледникового озера Восток // Криосфера Земли . 2017 . Т . 21 . № 3 . С . 32–40 .
Murshed M.M., Faria S.H., Kuhs W.F., Kipfstuhl S., Wilhelms F. The role of hydrochlorofluorocarbon densifiers in the formation of clathrate hydrates in deep boreholes and subglacial environments // Annals of Glaciology . 2007 . V . 47 . P . 109–114 .
Лейченков Г.Л., Липенков В.Я., Антонов А.В., Булат С.А., Charlot F., Алехина И.А., Екайкин А.А., Беляцкий Б.В. Природа микрочастиц, обнаруженных в скважине после вскрытия озера Восток // Проблемы Арктики и Антарктики . 2014 . Вып . 1 (99) . С . 114–122 .
Liska I., Slobodnik J. GC/MS screening of organic pollutants / Еds . P . Literáthy, V . Koller-Kreimel, I . Liska // Joint Danube Survey, Technical Report, ICPDR . 2002 . Vienna, 2002 . http://www.icpdr.org/main/activities-projects/joint-danube-survey-1 .
Licha T. Short chained alkyl phenols (SCAP) in groundwater – chemical analysis, adsorption mechanism and field cases . Ph .D . Thesis . 2003 . Friedrich-Schiller-University of Jena, Germany .
Bernabei M., Bocchinfuso G., Carrozzo P., De Angelis C. Determination of phenolic antioxidants in aviation jet fuel // Journ . of Chromatography A . 2000. V . 871 . P . 235–241 .
https://ice-snow.igras.ru/jour/article/view/407
doi:10.15356/2076-6734-2017-3-417-426
op_rights Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access).
Авторы, публикующие статьи в данном журнале, соглашаются на следующее:Авторы сохраняют за собой авторские права и предоставляют журналу право первой публикации работы, которая по истечении 6 месяцев после публикации автоматически лицензируется на условиях Creative Commons Attribution License , что позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Редакция журнала будет размещать принятую для публикации статью на сайте журнала до выхода её в свет (после утверждения к печати редколлегией журнала). Авторы также имеют право размещать их работу в сети Интернет (например в институтском хранилище или персональном сайте) до и во время процесса рассмотрения ее данным журналом, так как это может привести к продуктивному обсуждению и большему количеству ссылок на данную работу (См. The Effect of Open Access).
op_rightsnorm CC-BY
op_doi https://doi.org/10.15356/2076-6734-2017-3-417-426
https://doi.org/10.15356/2076-6734-2017-3
https://doi.org/10.1098/rsta.2014.0466
https://doi.org/10.1098/rsta.2014.0290
https://doi.org/10.1098/rsta.2014.0303
container_title Ice and Snow
container_volume 57
container_issue 3
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spelling ftjias:oai:oai.ice.elpub.ru:article/407 2023-05-15T13:29:50+02:00 Phenol compounds in the borehole 5G, Vostok station, after the unlocking of the subglacial lake Фенольные соединения в скважине 5Г на станции Восток после вскрытия подледникового озера I. Alekhina A. A. Moskvin L. A. Ekaykin A. V. Lipenkov Ya. И. Алехина А. А. Москвин Л. А. Екайкин А. В. Липенков Я. 2017-10-12 application/pdf https://ice-snow.igras.ru/jour/article/view/407 https://doi.org/10.15356/2076-6734-2017-3-417-426 rus rus IGRAS https://ice-snow.igras.ru/jour/article/view/407/234 Kennicutt M.C., Chown S.L., Cassano J.J., Liggett D., Peck L.S., Massom R., Rintoul S.R., Storey J., Vaughan D.G., Wilson T.J., Allison I., Ayton J., Badhe R., Baeseman J., Barrett P.J., Bell R.E., Bertler N., Bo S., Brandt A., Bromwich D., Cary S.C., Clark M.S., Convey P., Costa E.S., Cowan D., Deconto R., Dunbar R., Elfring C., Escutia C., Francis J., Fricker H.A., Fukuchi M., Gilbert N., Gutt J., Havermans C., Hik D., Hosie G., Jones C., Kim Y.D., Le Maho Y., Lee S.H., Leppe M., Leitchenkov G., Li X., Lipenkov V., Lochte K., López-Martínez J., Lüdecke C., Lyons W., Marenssi S., Miller H., Morozova P., Naish T., Nayak S., Ravindra R., Retamales J., Ricci C.A., Rogan-Finnemore M., Ropert-Coudert Y., Samah A.A., Sanson L., Scambos T., Schloss I.R., Shiraishi K., Siegert M.J., Simões J.C., Storey B., Sparrow M.D., Wall D.H., Walsh J.C., Wilson G., Winther J.G., Xavier J.C., Yang H., Sutherland W.J. A road- map for Antarctic and Southern Ocean science for the next two decades and beyond // Antarctic Science . 2015 . V . 27 . P . 1–17 . Siegert M.J., Priscu J., Alekhina I., Wadham J., Lyons B. Antarctic subglacial lake exploration: first results and future plans // Philosophical Transactions of the Royal Society A . 2016 . V . 374 . 20140466 . doi:10.1098/rsta.2014.0466 . Mikucki J.A., Lee P.A., Ghosh D., Purcell A.M., Mitchell A.C., Mankoff K.D., Fisher A.T., Tulaszuk S., Carter S., Siegfried M.R., Fricker H.A., Hodson T., Coenen J., Powell R., Scherer R., Vick-Majors T., Achberger A.A., Christner B.C., Tranter M., WISSARD Science Team . Subglacial Lake Whillans microbial biogeo chemistry: a synthesis of current knowledge // Philosophical Transactions of the Royal Society A . 2016 . V . 374 . 20140290 . doi:10.1098/rsta.2014.0290 . Christner B.C., Priscu J.C., Achberger A.M., Barbante C., Carter S.P., Christianson K., Michaud A.B., Mikucki J.A., Mitchell A.C., Skidmore M.L., Vick-Majors T.J., the WISSARD Science Team . A microbial ecosystem beneath the West Antarctic Ice Sheet // Nature . 2014 . V . 512 . P . 310–313 . Попов С.В., Масолов В.Н., Лукин В.В. Озеро Восток, Восточная Антарктида: мощность ледника, глубина озера, подледный и коренной рельеф // Лёд и Снег . 2011 . № 1 (113) . С . 25–35 . Siegert M., Popov S., Studinger M. Subglacial Lake Vostok: a review of geophysical data regarding its physiographical setting / Еds . M .J . Siegert, M . Kennicutt, R . Bindschadler // Antarctic Subglacial Aquatic Environments . Geophysical Monograph series. 2011 . V . 192 . AGU Geophysical Monograph: Washington, DC . P . 45–60 . Leitchenkov G.L., Antonov A.V., Luneov P.I., Lipenkov V. Geology and environments of subglacial Lake Vostok // Philosophical Transactions of Royal Society A . 2016 . V . 374 . 20140302 . doi:10.1098/rsta.2014.0303 . Litvinenko V.S., Vasiliev N.I., Lipenkov V.Ya., Dmitriev A.N., Podoliak A.V. Special aspects of ice drilling and results of 5G hole drilling at Vostok station, Antarctica // Annals of Glaciology . 2014 . V . 55 . P . 173– 178 . Verkulich S.R., Kudryashov B.B., Barkov N.I., Vasiliev N.I., Vostretsov R.N., Dmitriev A.N., Zubkov V.M., Krasilev A.V., Talalay P.G., Lipenkov V.Ya., Savatyugin L.M., Kuz’mina I.N. Proposal for penetra tion and exploration of subglacial Lake Vostok, Antarctica // Memoirs of National Institute of Polar Research . 2002 . V . 56 . P . 245–252 . Alekhina I.A., Marie D., Petit J.R., Lukin V.V., Zubkov V.M., Bulat S.A. Molecular analysis of bacterial diversity in kerosene-based drilling fluid from the deep ice borehole at Vostok, East Antarctica // FEMS Microbiology Ecology . 2007 . V . 59 . P . 289–299 . Code of conduct for the exploration and research of subglacial aquatic environments . 2011 . ATCMIP 33 .34 . Antarctic Treaty Consultative Meeting; Buenos Aires, 20 June – 1 July 2011 . Васильев Н.И., Липенков В.Я., Дмитриев А.Н., Подоляк А.В., Зубков В.М. Результаты и особенности бурения скважины 5Г и первого вскрытия озера Восток // Лёд и Снег . 2012 . № 4 (120) . С . 12–20 . Алехина И.А., Васильев Н.И., Екайкин А.А., Липенков В.Я. Предварительные результаты исследований химического состава воды, замерзшей в буровой скважине после вскрытия озера Восток // Проблемы Арктики и Антарктики . 2014 . Вып . 2 (100) . С . 5–14 . Lipenkov V., Istomin V.A. On the stability of air clathrate hydrate crystals in subglacial Lake Vostok, Antarc tica // МГИ . 2001 . № 91 . С . 138–149 . Манаков А.Ю., Илдяков А.В., Липенков В.Я., Екайкин А.А., Ходжер Т.В. Образование клатратных гидратов гидрохлорофлуорокарбона 141b в глубокой скважине на ст . Восток (Антарктида) в процессе вскрытия подледникового озера Восток // Криосфера Земли . 2017 . Т . 21 . № 3 . С . 32–40 . Murshed M.M., Faria S.H., Kuhs W.F., Kipfstuhl S., Wilhelms F. The role of hydrochlorofluorocarbon densifiers in the formation of clathrate hydrates in deep boreholes and subglacial environments // Annals of Glaciology . 2007 . V . 47 . P . 109–114 . Лейченков Г.Л., Липенков В.Я., Антонов А.В., Булат С.А., Charlot F., Алехина И.А., Екайкин А.А., Беляцкий Б.В. Природа микрочастиц, обнаруженных в скважине после вскрытия озера Восток // Проблемы Арктики и Антарктики . 2014 . Вып . 1 (99) . С . 114–122 . Liska I., Slobodnik J. GC/MS screening of organic pollutants / Еds . P . Literáthy, V . Koller-Kreimel, I . Liska // Joint Danube Survey, Technical Report, ICPDR . 2002 . Vienna, 2002 . http://www.icpdr.org/main/activities-projects/joint-danube-survey-1 . Licha T. Short chained alkyl phenols (SCAP) in groundwater – chemical analysis, adsorption mechanism and field cases . Ph .D . Thesis . 2003 . Friedrich-Schiller-University of Jena, Germany . Bernabei M., Bocchinfuso G., Carrozzo P., De Angelis C. Determination of phenolic antioxidants in aviation jet fuel // Journ . of Chromatography A . 2000. V . 871 . P . 235–241 . https://ice-snow.igras.ru/jour/article/view/407 doi:10.15356/2076-6734-2017-3-417-426 Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access). Авторы, публикующие статьи в данном журнале, соглашаются на следующее:Авторы сохраняют за собой авторские права и предоставляют журналу право первой публикации работы, которая по истечении 6 месяцев после публикации автоматически лицензируется на условиях Creative Commons Attribution License , что позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Редакция журнала будет размещать принятую для публикации статью на сайте журнала до выхода её в свет (после утверждения к печати редколлегией журнала). Авторы также имеют право размещать их работу в сети Интернет (например в институтском хранилище или персональном сайте) до и во время процесса рассмотрения ее данным журналом, так как это может привести к продуктивному обсуждению и большему количеству ссылок на данную работу (См. The Effect of Open Access). CC-BY Ice and Snow; Том 57, № 3 (2017); 417-426 Лёд и Снег; Том 57, № 3 (2017); 417-426 2412-3765 2076-6734 10.15356/2076-6734-2017-3 Antarctica drilling fluid freezing hydrocarbons SALE secondary ice core Антарктида вторичный лёд заливочная жидкость ледяные керны углеводороды info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2017 ftjias https://doi.org/10.15356/2076-6734-2017-3-417-426 https://doi.org/10.15356/2076-6734-2017-3 https://doi.org/10.1098/rsta.2014.0466 https://doi.org/10.1098/rsta.2014.0290 https://doi.org/10.1098/rsta.2014.0303 2022-12-20T13:29:52Z The main results after the first unlocking into the subglacial Lake Vostok were as follows: the Lake had been opened and not polluted; the water pressure within the lake was not balanced by a column of the drilling liquid that resulted in unplanned rise of water in the borehole up to 340 m. The main problem during the drilling in the lake ice was to prevent a pollution of water by the drilling fluid, which filled the borehole, and thus, to avoid a compression of the fluid which could be the main source of chemical and biological pollution of not only the Lake itself, but also the Lake water samples and ice cores. The article presents results of analysis of causes for the occurrence of phenolic compounds in the central channel in the core of secondary ice, being formed by the lake water that rose into the well after the first penetration (the range of depths was 3426–3450 m). It was found that the process, running within the borehole during the drilling, can be described as the fractionation of phenolic compounds, being contained in the filling liquid, to the water phase with its subsequent freezing. We have developed methods for the determination of concentrations of phenolic compounds in the original aviation kerosene and Freon HCFC-141b: 6. mg·l−1 and 0.032 mg·l−1, respectively. To analyze the composition of phenolic compounds in the extract of real filling liquid, located at the bottom of the borehole, the method of gas chromatography-mass spectrometry (GC-MS) was used. The corresponding peaks were quite well resolved and identified as phenol and its derivatives. The main components of the extract were phenol (20%), 2.5-dimethyl phenol (23,8%), 2,4,6-trimethylphenol, and other congeners of phenol. In our case, the Lake Vostok was not polluted during both, the first and second penetrations, however, the problem of human impact on these pristine and unique subglacial reservoirs remains extremely relevant. This impact includes not only direct water pollution of the lake by the drilling fluid, but also possible ... Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctic Science Antarctica ice core Memoirs of National Institute of Polar Research Polar Research Антарктида Ice and Snow (E-Journal) Lake Vostok ENVELOPE(106.000,106.000,-77.500,-77.500) Vostok Station ENVELOPE(106.837,106.837,-78.464,-78.464) Ice and Snow 57 3 417 426