Discovery and characterization of submarine groundwater discharge in the Siberian Arctic seas

A case study in the Buor-Khaya Gulf, Laptev Sea

Alexander N. Charkin, Michiel Rutgers Van Der Loeff, Natalia E. Shakhova, Örjan Gustafsson, Oleg V. Dudarev, Maxim S. Cherepnev, Anatoly N. Salyuk, Andrey V. Koshurnikov, Eduard A. Spivak, Alexey Y. Gunar, Alexey S. Ruban, Igor P. Semiletov

Research output: Contribution to journalArticle

4 Citations (Scopus)

Abstract

It has been suggested that increasing terrestrial water discharge to the Arctic Ocean may partly occur as submarine groundwater discharge (SGD), yet there are no direct observations of this phenomenon in the Arctic shelf seas. This study tests the hypothesis that SGD does exist in the Siberian Arctic Shelf seas, but its dynamics may be largely controlled by complicated geocryological conditions such as permafrost. The field-observational approach in the southeastern Laptev Sea used a combination of hydrological (temperature, salinity), geological (bottom sediment drilling, geoelectric surveys), and geochemical (224Ra, 223Ra, 228Ra, and 226Ra) techniques. Active SGD was documented in the vicinity of the Lena River delta with two different operational modes. In the first system, groundwater discharges through tectonogenic permafrost talik zones was registered in both winter and summer. The second SGD mechanism was cryogenic squeezing out of brine and water-soluble salts detected on the periphery of ice hummocks in the winter. The proposed mechanisms of groundwater transport and discharge in the Arctic land-shelf system is elaborated. Through salinity vs. 224Ra and 224Ra / 223Ra diagrams, the three main SGD-influenced water masses were identified and their end-member composition was constrained. Based on simple mass-balance box models, discharge rates at sites in the submarine permafrost talik zone were 1. 7 × 106ĝ€m3ĝ€†dĝ'1 or 19.9ĝ€m3ĝ€†sĝ'1, which is much higher than the April discharge of the Yana River. Further studies should apply these techniques on a broader scale with the objective of elucidating the relative importance of the SGD transport vector relative to surface freshwater discharge for both water balance and aquatic components such as dissolved organic carbon, carbon dioxide, methane, and nutrients.

Original languageEnglish
Pages (from-to)2305-2327
Number of pages23
JournalCryosphere
Volume11
Issue number5
DOIs
Publication statusPublished - 5 Oct 2017

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groundwater
talik
permafrost
shelf sea
sea
gulf
salinity
winter
salt water
river
water mass
dissolved organic carbon
brine
water budget
mass balance
carbon dioxide
methane
diagram
drilling
ice

ASJC Scopus subject areas

  • Water Science and Technology
  • Earth-Surface Processes

Cite this

Discovery and characterization of submarine groundwater discharge in the Siberian Arctic seas : A case study in the Buor-Khaya Gulf, Laptev Sea. / Charkin, Alexander N.; Van Der Loeff, Michiel Rutgers; Shakhova, Natalia E.; Gustafsson, Örjan; Dudarev, Oleg V.; Cherepnev, Maxim S.; Salyuk, Anatoly N.; Koshurnikov, Andrey V.; Spivak, Eduard A.; Gunar, Alexey Y.; Ruban, Alexey S.; Semiletov, Igor P.

In: Cryosphere, Vol. 11, No. 5, 05.10.2017, p. 2305-2327.

Research output: Contribution to journalArticle

Charkin, AN, Van Der Loeff, MR, Shakhova, NE, Gustafsson, Ö, Dudarev, OV, Cherepnev, MS, Salyuk, AN, Koshurnikov, AV, Spivak, EA, Gunar, AY, Ruban, AS & Semiletov, IP 2017, 'Discovery and characterization of submarine groundwater discharge in the Siberian Arctic seas: A case study in the Buor-Khaya Gulf, Laptev Sea', Cryosphere, vol. 11, no. 5, pp. 2305-2327. https://doi.org/10.5194/tc-11-2305-2017
Charkin, Alexander N. ; Van Der Loeff, Michiel Rutgers ; Shakhova, Natalia E. ; Gustafsson, Örjan ; Dudarev, Oleg V. ; Cherepnev, Maxim S. ; Salyuk, Anatoly N. ; Koshurnikov, Andrey V. ; Spivak, Eduard A. ; Gunar, Alexey Y. ; Ruban, Alexey S. ; Semiletov, Igor P. / Discovery and characterization of submarine groundwater discharge in the Siberian Arctic seas : A case study in the Buor-Khaya Gulf, Laptev Sea. In: Cryosphere. 2017 ; Vol. 11, No. 5. pp. 2305-2327.
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