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Origin of high 234U/238U ratio in post-permafrost aquifers. / Tokarev, I.V.; Zubkov, A.A.; Rumynin, V.G.; Polyakov, V.A.; Kuznetsov, V.Yu.; Maksimov, F.E.

Uranium in the Environment: Mining Impact and Consequences. ed. / Broder J. Merkel; Andrea Hasche-Berger. Berlin, Heidelberg : Springer Nature, 2006. p. 847-856.

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review

Harvard

Tokarev, IV, Zubkov, AA, Rumynin, VG, Polyakov, VA, Kuznetsov, VY & Maksimov, FE 2006, Origin of high 234U/238U ratio in post-permafrost aquifers. in BJ Merkel & A Hasche-Berger (eds), Uranium in the Environment: Mining Impact and Consequences. Springer Nature, Berlin, Heidelberg, pp. 847-856, 4th International conference on Uranium Mining and Hydrogeology, UMH 2005, Freiberg, Germany, 1/09/05. https://doi.org/10.1007/3-540-28367-6_88, https://doi.org/10.1007/3-540-28367-6

APA

Tokarev, I. V., Zubkov, A. A., Rumynin, V. G., Polyakov, V. A., Kuznetsov, V. Y., & Maksimov, F. E. (2006). Origin of high 234U/238U ratio in post-permafrost aquifers. In B. J. Merkel, & A. Hasche-Berger (Eds.), Uranium in the Environment: Mining Impact and Consequences (pp. 847-856). Springer Nature. https://doi.org/10.1007/3-540-28367-6_88, https://doi.org/10.1007/3-540-28367-6

Vancouver

Tokarev IV, Zubkov AA, Rumynin VG, Polyakov VA, Kuznetsov VY, Maksimov FE. Origin of high 234U/238U ratio in post-permafrost aquifers. In Merkel BJ, Hasche-Berger A, editors, Uranium in the Environment: Mining Impact and Consequences. Berlin, Heidelberg: Springer Nature. 2006. p. 847-856 https://doi.org/10.1007/3-540-28367-6_88, https://doi.org/10.1007/3-540-28367-6

Author

Tokarev, I.V. ; Zubkov, A.A. ; Rumynin, V.G. ; Polyakov, V.A. ; Kuznetsov, V.Yu. ; Maksimov, F.E. / Origin of high 234U/238U ratio in post-permafrost aquifers. Uranium in the Environment: Mining Impact and Consequences. editor / Broder J. Merkel ; Andrea Hasche-Berger. Berlin, Heidelberg : Springer Nature, 2006. pp. 847-856

BibTeX

@inproceedings{9ae36ba45ca24ee599da1ebb16ec2056,
title = "Origin of high 234U/238U ratio in post-permafrost aquifers",
abstract = "Isotope composition and concentration (δ2H, δ18O, 234U/238U, Ar, 40Ar/ 36Ar, 3He/4He and 20Ne/ 4He) were measured in the ground waters (Tomsk-7). Water has a distinct cold climate isotope signature δ2H = -127..-140, δ18O = -17.0.. -18.2 in contrast of modern meteoric water δ2H = -117, δ18O = -15.9. Stable isotopes are in concord with noble gas temperature tNGT = 0..+4 °C and helium model ages t = 7-14 ka. Disequilibrium uranium 234U/238U up to 16 (activity ratio) obtained and explained of 234U leaching by the melt water during the permafrost degradation.",
author = "I.V. Tokarev and A.A. Zubkov and V.G. Rumynin and V.A. Polyakov and V.Yu. Kuznetsov and F.E. Maksimov",
year = "2006",
month = jan,
day = "1",
doi = "10.1007/3-540-28367-6_88",
language = "English",
isbn = "978-3-540-28363-8",
pages = "847--856",
editor = "Merkel, {Broder J. } and Andrea Hasche-Berger",
booktitle = "Uranium in the Environment",
publisher = "Springer Nature",
address = "Germany",
note = "4th International conference on Uranium Mining and Hydrogeology, UMH 2005 ; Conference date: 01-09-2005 Through 01-09-2005",

}

RIS

TY - GEN

T1 - Origin of high 234U/238U ratio in post-permafrost aquifers

AU - Tokarev, I.V.

AU - Zubkov, A.A.

AU - Rumynin, V.G.

AU - Polyakov, V.A.

AU - Kuznetsov, V.Yu.

AU - Maksimov, F.E.

PY - 2006/1/1

Y1 - 2006/1/1

N2 - Isotope composition and concentration (δ2H, δ18O, 234U/238U, Ar, 40Ar/ 36Ar, 3He/4He and 20Ne/ 4He) were measured in the ground waters (Tomsk-7). Water has a distinct cold climate isotope signature δ2H = -127..-140, δ18O = -17.0.. -18.2 in contrast of modern meteoric water δ2H = -117, δ18O = -15.9. Stable isotopes are in concord with noble gas temperature tNGT = 0..+4 °C and helium model ages t = 7-14 ka. Disequilibrium uranium 234U/238U up to 16 (activity ratio) obtained and explained of 234U leaching by the melt water during the permafrost degradation.

AB - Isotope composition and concentration (δ2H, δ18O, 234U/238U, Ar, 40Ar/ 36Ar, 3He/4He and 20Ne/ 4He) were measured in the ground waters (Tomsk-7). Water has a distinct cold climate isotope signature δ2H = -127..-140, δ18O = -17.0.. -18.2 in contrast of modern meteoric water δ2H = -117, δ18O = -15.9. Stable isotopes are in concord with noble gas temperature tNGT = 0..+4 °C and helium model ages t = 7-14 ka. Disequilibrium uranium 234U/238U up to 16 (activity ratio) obtained and explained of 234U leaching by the melt water during the permafrost degradation.

UR - http://www.scopus.com/inward/record.url?scp=84896593290&partnerID=8YFLogxK

U2 - 10.1007/3-540-28367-6_88

DO - 10.1007/3-540-28367-6_88

M3 - Conference contribution

SN - 978-3-540-28363-8

SN - 978-3-662-51793-2

SP - 847

EP - 856

BT - Uranium in the Environment

A2 - Merkel, Broder J.

A2 - Hasche-Berger, Andrea

PB - Springer Nature

CY - Berlin, Heidelberg

T2 - 4th International conference on Uranium Mining and Hydrogeology, UMH 2005

Y2 - 1 September 2005 through 1 September 2005

ER -

ID: 4629567