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Надмерзлотные субаэральные талики в бассейне реки шестаковка (Центральная Якутия). / Lebedeva, L. S.; Bazhin, K. I.; Khristoforov, I. I.; Abramov, A. A.; Pavlova, N. A.; Efremov, V. S.; Ogonerov, V. V.; Tarbeeva, A. M.; Fedorov, M. P.; Nesterova, N. V.; Makarieva, O. M.

In: Earth's Cryosphere, Vol. 23, No. 1, 01.01.2019, p. 40-50.

Research output: Contribution to journal › Article › peer-review

Harvard

Lebedeva, LS, Bazhin, KI, Khristoforov, II, Abramov, AA, Pavlova, NA, Efremov, VS, Ogonerov, VV, Tarbeeva, AM, Fedorov, MP, Nesterova, NV & Makarieva, OM 2019, 'Надмерзлотные субаэральные талики в бассейне реки шестаковка (Центральная Якутия)', Earth's Cryosphere, vol. 23, no. 1, pp. 40-50. https://doi.org/10.21782/KZ1560-7496-2019-140-50

APA

Lebedeva, L. S., Bazhin, K. I., Khristoforov, I. I., Abramov, A. A., Pavlova, N. A., Efremov, V. S., Ogonerov, V. V., Tarbeeva, A. M., Fedorov, M. P., Nesterova, N. V., & Makarieva, O. M. (2019). Надмерзлотные субаэральные талики в бассейне реки шестаковка (Центральная Якутия). Earth's Cryosphere, 23(1), 40-50. https://doi.org/10.21782/KZ1560-7496-2019-140-50

Vancouver

Lebedeva LS, Bazhin KI, Khristoforov II, Abramov AA, Pavlova NA, Efremov VS et al. Надмерзлотные субаэральные талики в бассейне реки шестаковка (Центральная Якутия). Earth's Cryosphere. 2019 Jan 1;23(1):40-50. https://doi.org/10.21782/KZ1560-7496-2019-140-50

Author

Lebedeva, L. S. ; Bazhin, K. I. ; Khristoforov, I. I. ; Abramov, A. A. ; Pavlova, N. A. ; Efremov, V. S. ; Ogonerov, V. V. ; Tarbeeva, A. M. ; Fedorov, M. P. ; Nesterova, N. V. ; Makarieva, O. M. / Надмерзлотные субаэральные талики в бассейне реки шестаковка (Центральная Якутия). In: Earth's Cryosphere. 2019 ; Vol. 23, No. 1. pp. 40-50.

BibTeX

@article{c7bd1bf48e3a422ea33304ad0d7d7671,
title = "Надмерзлотные субаэральные талики в бассейне реки шестаковка (Центральная Якутия)",
abstract = "The study presents the results of drilling, geophysical survey and ground temperature monitoring in the area of suprapermafrost subaerial water-bearing talik that is associated with sandy deposits in the sparsely vegetated gentle slope of the Levaya Shestakovka River terrace covered by pine forest. The talik is 180–200 m wide and more than 500 m long, has a complicated contour and consists of several water-conducting channels. The configuration of unfrozen zones assessed with a ground penetrating radar and electrical resistivity tomography is similar, thus confirming the efficiency of the applied geophysical methods. The mean value of ground temperature and its amplitude for one year at the talik area are much higher than outside of the talik. The depth of the zero annual amplitude does not exceed 6 m due to the constant yearly temperature of the water-saturated deposits equal to 0 °С.",
keywords = "Electrical resistivity tomography, Ground penetrating radar, Permafrost, Soil temperature, Water-bearing talik, Electrical resistivity tomography, Ground penetrating radar, Permafrost, Soil temperature, Water-bearing talik",
author = "Lebedeva, {L. S.} and Bazhin, {K. I.} and Khristoforov, {I. I.} and Abramov, {A. A.} and Pavlova, {N. A.} and Efremov, {V. S.} and Ogonerov, {V. V.} and Tarbeeva, {A. M.} and Fedorov, {M. P.} and Nesterova, {N. V.} and Makarieva, {O. M.}",
year = "2019",
month = jan,
day = "1",
doi = "10.21782/KZ1560-7496-2019-140-50",
language = "русский",
volume = "23",
pages = "40--50",
journal = "КРИОСФЕРА ЗЕМЛИ",
issn = "1560-7496",
publisher = "Российская академия наук",
number = "1",

}

RIS

TY - JOUR

T1 - Надмерзлотные субаэральные талики в бассейне реки шестаковка (Центральная Якутия)

AU - Lebedeva, L. S.

AU - Bazhin, K. I.

AU - Khristoforov, I. I.

AU - Abramov, A. A.

AU - Pavlova, N. A.

AU - Efremov, V. S.

AU - Ogonerov, V. V.

AU - Tarbeeva, A. M.

AU - Fedorov, M. P.

AU - Nesterova, N. V.

AU - Makarieva, O. M.

PY - 2019/1/1

Y1 - 2019/1/1

N2 - The study presents the results of drilling, geophysical survey and ground temperature monitoring in the area of suprapermafrost subaerial water-bearing talik that is associated with sandy deposits in the sparsely vegetated gentle slope of the Levaya Shestakovka River terrace covered by pine forest. The talik is 180–200 m wide and more than 500 m long, has a complicated contour and consists of several water-conducting channels. The configuration of unfrozen zones assessed with a ground penetrating radar and electrical resistivity tomography is similar, thus confirming the efficiency of the applied geophysical methods. The mean value of ground temperature and its amplitude for one year at the talik area are much higher than outside of the talik. The depth of the zero annual amplitude does not exceed 6 m due to the constant yearly temperature of the water-saturated deposits equal to 0 °С.

AB - The study presents the results of drilling, geophysical survey and ground temperature monitoring in the area of suprapermafrost subaerial water-bearing talik that is associated with sandy deposits in the sparsely vegetated gentle slope of the Levaya Shestakovka River terrace covered by pine forest. The talik is 180–200 m wide and more than 500 m long, has a complicated contour and consists of several water-conducting channels. The configuration of unfrozen zones assessed with a ground penetrating radar and electrical resistivity tomography is similar, thus confirming the efficiency of the applied geophysical methods. The mean value of ground temperature and its amplitude for one year at the talik area are much higher than outside of the talik. The depth of the zero annual amplitude does not exceed 6 m due to the constant yearly temperature of the water-saturated deposits equal to 0 °С.

KW - Electrical resistivity tomography

KW - Ground penetrating radar

KW - Permafrost

KW - Soil temperature

KW - Water-bearing talik

KW - Electrical resistivity tomography

KW - Ground penetrating radar

KW - Permafrost

KW - Soil temperature

KW - Water-bearing talik

UR - http://www.scopus.com/inward/record.url?scp=85061900707&partnerID=8YFLogxK

UR - http://www.mendeley.com/research/suprapermafrost-subaerial-taliks-central-yakutia-shestakovka-river-basin

U2 - 10.21782/KZ1560-7496-2019-140-50

DO - 10.21782/KZ1560-7496-2019-140-50

M3 - статья

AN - SCOPUS:85061900707

VL - 23

SP - 40

EP - 50

JO - КРИОСФЕРА ЗЕМЛИ

JF - КРИОСФЕРА ЗЕМЛИ

SN - 1560-7496

IS - 1

ER -

ID: 41099938