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Brief communication: The hidden labyrinth: deep groundwater in Wright Valley, Antarctica

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Brief communication: The hidden labyrinth: deep groundwater in Wright Valley, Antarctica. / Dugan, Hilary A.; Doran, Peter T.; Grombacher, Denys et al.
I: Cryosphere, Bind 16, Nr. 12, 12.2022, s. 4977-4983.

Publikation: Bidrag til tidsskrift/Konferencebidrag i tidsskrift /Bidrag til avisTidsskriftartikelForskningpeer review

Harvard

Dugan, HA, Doran, PT, Grombacher, D, Auken, E, Bording, T, Foged, N, Foley, N, Mikucki, J, Virginia, RA & Tulaczyk, S 2022, 'Brief communication: The hidden labyrinth: deep groundwater in Wright Valley, Antarctica', Cryosphere, bind 16, nr. 12, s. 4977-4983. https://doi.org/10.5194/tc-16-4977-2022

APA

Dugan, H. A., Doran, P. T., Grombacher, D., Auken, E., Bording, T., Foged, N., Foley, N., Mikucki, J., Virginia, R. A., & Tulaczyk, S. (2022). Brief communication: The hidden labyrinth: deep groundwater in Wright Valley, Antarctica. Cryosphere, 16(12), 4977-4983. https://doi.org/10.5194/tc-16-4977-2022

CBE

Dugan HA, Doran PT, Grombacher D, Auken E, Bording T, Foged N, Foley N, Mikucki J, Virginia RA, Tulaczyk S. 2022. Brief communication: The hidden labyrinth: deep groundwater in Wright Valley, Antarctica. Cryosphere. 16(12):4977-4983. https://doi.org/10.5194/tc-16-4977-2022

MLA

Vancouver

Dugan HA, Doran PT, Grombacher D, Auken E, Bording T, Foged N et al. Brief communication: The hidden labyrinth: deep groundwater in Wright Valley, Antarctica. Cryosphere. 2022 dec.;16(12):4977-4983. doi: 10.5194/tc-16-4977-2022

Author

Dugan, Hilary A. ; Doran, Peter T. ; Grombacher, Denys et al. / Brief communication : The hidden labyrinth: deep groundwater in Wright Valley, Antarctica. I: Cryosphere. 2022 ; Bind 16, Nr. 12. s. 4977-4983.

Bibtex

@article{c0d2c10968fa47c78661577d0803598e,
title = "Brief communication: The hidden labyrinth: deep groundwater in Wright Valley, Antarctica",
abstract = "Since the 1960s, a deep groundwater system in Wright Valley, Antarctica, has been the hypothesized source of brines to hypersaline Don Juan Pond and Lake Vanda, both of which are rich in calcium and chloride. Modeling studies do not support other possible mechanisms, such as evaporative processes, that could have led to the current suite of ions present in both waterbodies. In 2011 and 2018, an airborne electromagnetic survey was flown over Wright Valley to map subsurface resistivity (down to 600 m) in exploration of liquid water. The surveys revealed widespread unfrozen brine in the subsurface near Lake Vanda, Don Juan Pond, and the North Fork of Wright Valley. While our geophysical survey can neither confirm nor deny deep groundwater connectivity between Lake Vanda and Don Juan Pond, it does point to the potential for deep valley-wide brine, likely within the Ferrar Dolerite formation.",
author = "Dugan, {Hilary A.} and Doran, {Peter T.} and Denys Grombacher and Esben Auken and Thue Bording and Nikolaj Foged and Neil Foley and Jill Mikucki and Virginia, {Ross A.} and Slawek Tulaczyk",
note = "Publisher Copyright: {\textcopyright} 2022 Hilary A. Dugan et al.",
year = "2022",
month = dec,
doi = "10.5194/tc-16-4977-2022",
language = "English",
volume = "16",
pages = "4977--4983",
journal = "Cryosphere",
issn = "1994-0416",
publisher = "Copernicus GmbH",
number = "12",

}

RIS

TY - JOUR

T1 - Brief communication

T2 - The hidden labyrinth: deep groundwater in Wright Valley, Antarctica

AU - Dugan, Hilary A.

AU - Doran, Peter T.

AU - Grombacher, Denys

AU - Auken, Esben

AU - Bording, Thue

AU - Foged, Nikolaj

AU - Foley, Neil

AU - Mikucki, Jill

AU - Virginia, Ross A.

AU - Tulaczyk, Slawek

N1 - Publisher Copyright: © 2022 Hilary A. Dugan et al.

PY - 2022/12

Y1 - 2022/12

N2 - Since the 1960s, a deep groundwater system in Wright Valley, Antarctica, has been the hypothesized source of brines to hypersaline Don Juan Pond and Lake Vanda, both of which are rich in calcium and chloride. Modeling studies do not support other possible mechanisms, such as evaporative processes, that could have led to the current suite of ions present in both waterbodies. In 2011 and 2018, an airborne electromagnetic survey was flown over Wright Valley to map subsurface resistivity (down to 600 m) in exploration of liquid water. The surveys revealed widespread unfrozen brine in the subsurface near Lake Vanda, Don Juan Pond, and the North Fork of Wright Valley. While our geophysical survey can neither confirm nor deny deep groundwater connectivity between Lake Vanda and Don Juan Pond, it does point to the potential for deep valley-wide brine, likely within the Ferrar Dolerite formation.

AB - Since the 1960s, a deep groundwater system in Wright Valley, Antarctica, has been the hypothesized source of brines to hypersaline Don Juan Pond and Lake Vanda, both of which are rich in calcium and chloride. Modeling studies do not support other possible mechanisms, such as evaporative processes, that could have led to the current suite of ions present in both waterbodies. In 2011 and 2018, an airborne electromagnetic survey was flown over Wright Valley to map subsurface resistivity (down to 600 m) in exploration of liquid water. The surveys revealed widespread unfrozen brine in the subsurface near Lake Vanda, Don Juan Pond, and the North Fork of Wright Valley. While our geophysical survey can neither confirm nor deny deep groundwater connectivity between Lake Vanda and Don Juan Pond, it does point to the potential for deep valley-wide brine, likely within the Ferrar Dolerite formation.

U2 - 10.5194/tc-16-4977-2022

DO - 10.5194/tc-16-4977-2022

M3 - Journal article

AN - SCOPUS:85145590123

VL - 16

SP - 4977

EP - 4983

JO - Cryosphere

JF - Cryosphere

SN - 1994-0416

IS - 12

ER -