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Assessment of the long-term safety of radioactive waste disposal. 2. Isotopic study of water exchange in a multilayer system. / Tokarev, I. V.; Zubkov, A. A.; Rumynin, V. G.; поздняков, сергей павлович.

In: Water Resources, Vol. 36, No. 3, 2009, p. 345-356.

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

Harvard

Tokarev, IV, Zubkov, AA, Rumynin, VG & поздняков, СП 2009, 'Assessment of the long-term safety of radioactive waste disposal. 2. Isotopic study of water exchange in a multilayer system', Water Resources, vol. 36, no. 3, pp. 345-356. https://doi.org/10.1134/S0097807809030105

APA

Tokarev, I. V., Zubkov, A. A., Rumynin, V. G., & поздняков, С. П. (2009). Assessment of the long-term safety of radioactive waste disposal. 2. Isotopic study of water exchange in a multilayer system. Water Resources, 36(3), 345-356. https://doi.org/10.1134/S0097807809030105

Vancouver

Tokarev IV, Zubkov AA, Rumynin VG, поздняков СП. Assessment of the long-term safety of radioactive waste disposal. 2. Isotopic study of water exchange in a multilayer system. Water Resources. 2009;36(3):345-356. https://doi.org/10.1134/S0097807809030105

Author

Tokarev, I. V. ; Zubkov, A. A. ; Rumynin, V. G. ; поздняков, сергей павлович. / Assessment of the long-term safety of radioactive waste disposal. 2. Isotopic study of water exchange in a multilayer system. In: Water Resources. 2009 ; Vol. 36, No. 3. pp. 345-356.

BibTeX

@article{6fbe38cab3e043298573717c8730804e,
title = "Assessment of the long-term safety of radioactive waste disposal. 2. Isotopic study of water exchange in a multilayer system",
abstract = "As a continuation of previous studies of 3H, δ2H, δ18O, Ar, 40Ar/ 36Ar, and 234U/238U isotope systems, data of uranium-helium dating of groundwater at the radioactive waste repository of Siberian Chemical Works are quantitatively interpreted. The interpretation is based on analytical models taking into account the inflow of deep-earth helium and the diffusion-advection exchange between layers. Estimated flow velocities in reservoir beds and buffer horizons are in agreement with previous hydrodynamic estimates. The obtained velocities of horizontal mass transfer were used to evaluate the age of groundwater in sampling points. Water age varies from 7 to 14 (with a mean of ∼9) in the lower (II and III) aquifers, into which the radioactive wastes are pumped, from 2 to 4 in buffer horizon IV, and from 1 to 2 thousand years in the upper V horizon.",
author = "Tokarev, {I. V.} and Zubkov, {A. A.} and Rumynin, {V. G.} and поздняков, {сергей павлович}",
note = "Funding Information: ACKNOWLEDGMENTS This study was supported by the Russian Foundation for Basic Research (project nos. 04–5-97508r_ofi and 07-05-00796-a), International Research and Development Center (projects 3193 and 3590), and Civil Research and Development Foundation (project RUG2-2821-MO-06). Copyright: Copyright 2009 Elsevier B.V., All rights reserved.",
year = "2009",
doi = "10.1134/S0097807809030105",
language = "English",
volume = "36",
pages = "345--356",
journal = "Water Resources",
issn = "0097-8078",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "3",

}

RIS

TY - JOUR

T1 - Assessment of the long-term safety of radioactive waste disposal. 2. Isotopic study of water exchange in a multilayer system

AU - Tokarev, I. V.

AU - Zubkov, A. A.

AU - Rumynin, V. G.

AU - поздняков, сергей павлович

N1 - Funding Information: ACKNOWLEDGMENTS This study was supported by the Russian Foundation for Basic Research (project nos. 04–5-97508r_ofi and 07-05-00796-a), International Research and Development Center (projects 3193 and 3590), and Civil Research and Development Foundation (project RUG2-2821-MO-06). Copyright: Copyright 2009 Elsevier B.V., All rights reserved.

PY - 2009

Y1 - 2009

N2 - As a continuation of previous studies of 3H, δ2H, δ18O, Ar, 40Ar/ 36Ar, and 234U/238U isotope systems, data of uranium-helium dating of groundwater at the radioactive waste repository of Siberian Chemical Works are quantitatively interpreted. The interpretation is based on analytical models taking into account the inflow of deep-earth helium and the diffusion-advection exchange between layers. Estimated flow velocities in reservoir beds and buffer horizons are in agreement with previous hydrodynamic estimates. The obtained velocities of horizontal mass transfer were used to evaluate the age of groundwater in sampling points. Water age varies from 7 to 14 (with a mean of ∼9) in the lower (II and III) aquifers, into which the radioactive wastes are pumped, from 2 to 4 in buffer horizon IV, and from 1 to 2 thousand years in the upper V horizon.

AB - As a continuation of previous studies of 3H, δ2H, δ18O, Ar, 40Ar/ 36Ar, and 234U/238U isotope systems, data of uranium-helium dating of groundwater at the radioactive waste repository of Siberian Chemical Works are quantitatively interpreted. The interpretation is based on analytical models taking into account the inflow of deep-earth helium and the diffusion-advection exchange between layers. Estimated flow velocities in reservoir beds and buffer horizons are in agreement with previous hydrodynamic estimates. The obtained velocities of horizontal mass transfer were used to evaluate the age of groundwater in sampling points. Water age varies from 7 to 14 (with a mean of ∼9) in the lower (II and III) aquifers, into which the radioactive wastes are pumped, from 2 to 4 in buffer horizon IV, and from 1 to 2 thousand years in the upper V horizon.

UR - http://www.scopus.com/inward/record.url?scp=65849302658&partnerID=8YFLogxK

U2 - 10.1134/S0097807809030105

DO - 10.1134/S0097807809030105

M3 - Article

AN - SCOPUS:65849302658

VL - 36

SP - 345

EP - 356

JO - Water Resources

JF - Water Resources

SN - 0097-8078

IS - 3

ER -

ID: 70199628