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Изотопный состав атмосферных осадков и природных вод в районе Баренцбурга (Шпицберген). / Скакун, А.А.; Чихачев, К.Б.; Екайкин, А.А.; Козачек, А.В.; Владимирова, Д.О.; Верес, А.Н.; Веркулич, С.Р.; Сидорова, О.С.; Демидов, Н.Э.

в: Лед и Снег, Том 60, № 3, 2020, стр. 379-394.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Скакун, АА, Чихачев, КБ, Екайкин, АА, Козачек, АВ, Владимирова, ДО, Верес, АН, Веркулич, СР, Сидорова, ОС & Демидов, НЭ 2020, 'Изотопный состав атмосферных осадков и природных вод в районе Баренцбурга (Шпицберген)', Лед и Снег, Том. 60, № 3, стр. 379-394. https://doi.org/10.31857/S2076673420030046

APA

Скакун, А. А., Чихачев, К. Б., Екайкин, А. А., Козачек, А. В., Владимирова, Д. О., Верес, А. Н., Веркулич, С. Р., Сидорова, О. С., & Демидов, Н. Э. (2020). Изотопный состав атмосферных осадков и природных вод в районе Баренцбурга (Шпицберген). Лед и Снег, 60(3), 379-394. https://doi.org/10.31857/S2076673420030046

Vancouver

Скакун АА, Чихачев КБ, Екайкин АА, Козачек АВ, Владимирова ДО, Верес АН и пр. Изотопный состав атмосферных осадков и природных вод в районе Баренцбурга (Шпицберген). Лед и Снег. 2020;60(3):379-394. https://doi.org/10.31857/S2076673420030046

Author

Скакун, А.А. ; Чихачев, К.Б. ; Екайкин, А.А. ; Козачек, А.В. ; Владимирова, Д.О. ; Верес, А.Н. ; Веркулич, С.Р. ; Сидорова, О.С. ; Демидов, Н.Э. / Изотопный состав атмосферных осадков и природных вод в районе Баренцбурга (Шпицберген). в: Лед и Снег. 2020 ; Том 60, № 3. стр. 379-394.

BibTeX

@article{59e96d3ba8274a21a3de0131f05e97f0,
title = "Изотопный состав атмосферных осадков и природных вод в районе Баренцбурга (Шпицберген)",
abstract = "In 2016-2017, during Russian Arctic Expedition on Svalbard (RAE-S) we have collected the samples of atmospheric precipitation, terrestrial waters, snow and ice on Spitsbergen island in the vicinity of Gr{\o}nfjorden. The measurements of stable water isotope content (δ18O and δD) in the atmospheric precipitation has allowed to draw the Local Meteoric Water Line (δD = 6,93δ18O - 0,35) and to analyze the relationship between the isotopic content and condensation temperature. Aside from this, the d-excess values in precipitation (dexc = δD - 8δ18O) was interpreted as a marker of the moisture source. It has been demonstrated that the isotopic content of the surface waters (lakes and rivers) clearly pointsto the dominating type of feeding (atmospheric, ground) of these hydrological objects. We have discovered the interannual variability of the isotopic composition of Lake Kongress water during 2 years and defined the sources of water in its tributes: 13 of them have atmospheric source and 9 - ground source. In general, isotopic content of water in the vicinity of Gr{\o}nfjorden (mean values are: δ18O = -10,3 ‰, δD = -72,5 ‰) is higher than in other regions of Svalbard.",
keywords = "ICE, Svalbard, atmospheric precipitation, isotopic composition, natural waters",
author = "А.А. Скакун and К.Б. Чихачев and А.А. Екайкин and А.В. Козачек and Д.О. Владимирова and А.Н. Верес and С.Р. Веркулич and О.С. Сидорова and Н.Э. Демидов",
year = "2020",
doi = "10.31857/S2076673420030046",
language = "русский",
volume = "60",
pages = "379--394",
journal = "Лед и Снег",
issn = "2076-6734",
publisher = "Институт географии РАН",
number = "3",

}

RIS

TY - JOUR

T1 - Изотопный состав атмосферных осадков и природных вод в районе Баренцбурга (Шпицберген)

AU - Скакун, А.А.

AU - Чихачев, К.Б.

AU - Екайкин, А.А.

AU - Козачек, А.В.

AU - Владимирова, Д.О.

AU - Верес, А.Н.

AU - Веркулич, С.Р.

AU - Сидорова, О.С.

AU - Демидов, Н.Э.

PY - 2020

Y1 - 2020

N2 - In 2016-2017, during Russian Arctic Expedition on Svalbard (RAE-S) we have collected the samples of atmospheric precipitation, terrestrial waters, snow and ice on Spitsbergen island in the vicinity of Grønfjorden. The measurements of stable water isotope content (δ18O and δD) in the atmospheric precipitation has allowed to draw the Local Meteoric Water Line (δD = 6,93δ18O - 0,35) and to analyze the relationship between the isotopic content and condensation temperature. Aside from this, the d-excess values in precipitation (dexc = δD - 8δ18O) was interpreted as a marker of the moisture source. It has been demonstrated that the isotopic content of the surface waters (lakes and rivers) clearly pointsto the dominating type of feeding (atmospheric, ground) of these hydrological objects. We have discovered the interannual variability of the isotopic composition of Lake Kongress water during 2 years and defined the sources of water in its tributes: 13 of them have atmospheric source and 9 - ground source. In general, isotopic content of water in the vicinity of Grønfjorden (mean values are: δ18O = -10,3 ‰, δD = -72,5 ‰) is higher than in other regions of Svalbard.

AB - In 2016-2017, during Russian Arctic Expedition on Svalbard (RAE-S) we have collected the samples of atmospheric precipitation, terrestrial waters, snow and ice on Spitsbergen island in the vicinity of Grønfjorden. The measurements of stable water isotope content (δ18O and δD) in the atmospheric precipitation has allowed to draw the Local Meteoric Water Line (δD = 6,93δ18O - 0,35) and to analyze the relationship between the isotopic content and condensation temperature. Aside from this, the d-excess values in precipitation (dexc = δD - 8δ18O) was interpreted as a marker of the moisture source. It has been demonstrated that the isotopic content of the surface waters (lakes and rivers) clearly pointsto the dominating type of feeding (atmospheric, ground) of these hydrological objects. We have discovered the interannual variability of the isotopic composition of Lake Kongress water during 2 years and defined the sources of water in its tributes: 13 of them have atmospheric source and 9 - ground source. In general, isotopic content of water in the vicinity of Grønfjorden (mean values are: δ18O = -10,3 ‰, δD = -72,5 ‰) is higher than in other regions of Svalbard.

KW - ICE

KW - Svalbard

KW - atmospheric precipitation

KW - isotopic composition

KW - natural waters

UR - https://www.mendeley.com/catalogue/7c96bc39-855f-3081-b387-c45bb7d532aa/

U2 - 10.31857/S2076673420030046

DO - 10.31857/S2076673420030046

M3 - статья

VL - 60

SP - 379

EP - 394

JO - Лед и Снег

JF - Лед и Снег

SN - 2076-6734

IS - 3

ER -

ID: 61461900