Abstract
This report presents the results of studies of the ionic-saline and isotope composition of the unique, quite fresh, and high-alkaline waters (0.25–0.6 g/l salinity and pH 9.1–10.3) occurring within sedimentary rocks, as well as data on the calculations of equilibriums in the water-rock system. In view of these data, the concept was developed for the formation of fresh high-alkaline waters being not associated with igneous rocks. According to this concept, the water composition as such is formed at a definite stage of the development of the water-sedimentary rock system when all the chemical elements transferring to a solution may form secondary mineral products with no concentrating in the aqueous solution. The salinity of this latter does not increase, and yet the interaction with the rock is continued and, hence, the alkalinity increases.
Similar content being viewed by others
References
I. Barnes, T. S. Presser, M. Saines, and P. Dickson, “Koster Van Groos A.F,” Chem. Geol. 35(1/2), 147–154 (1982).
C. Neal and G. Stanger, Earth and Planet Sci. Lett 66, 315–320 (1983).
J. M. Marques, M. J. Matias, M. J. Basto, R. C. Graca, L. Aires-Barros, M. Andrade, P. M. Carreira, F. Goff, and L. Rocha, Proc. XI Intern. Symp. on Water-Rock Interaction. Saratoga Springs (USA), 293–297 (2004).
F. Cipolli, B. Gambardella, L. Marini, G. Ottonello, and M. V. Zuccolini, Appl. Geochem., No. (5), 787–802 (2004).
S. R. Krainov, Geochemistry of Rare Elements in Ground-waters in View of Geochemical Search for Mineral Deposits (Nedra, Moscow, 1973) [in Russian].
M. Ishikuni, R. Suzuki, and M. Tsurami, Geochemistry 16(1), 25–29 (1982).
A. M. Plyusnin, M. K. Chernyavskii, L. V. Zamana, S. L. Shvartsev, O. G. Tokarenko, Russian Geology and Geophysics. 54(5), 495–508 (2013).
A. Yu. Ozerskii, Hydrogeochemistry of Sedimentary Basins (NTL, Tomsk, 2007) [in Russian].
Hydrogeology of the USSR (Nedra, Moscow, 1972), Vol. 18, p. 479 [in Russian].
O. E. Lepokurova and O. F. Zyateva, Izv. Tomsk Polytech. Univ. 319(1), 172–177 (2011).
S. I. Golyshev and V. G. Ivanov, Geokhimiya 5, 1024–1028 (1983).
S. L. Shvartsev, B. N. Ryzhenko, V. A. Alekseev, E. M. Dutova, I. A. Kondrat’eva, O. E. Lepokurova, Geological Evolution and Self-Organization of the Water-Rock System (SO RAN, Novosibirsk, 2007), Vol. 2 [in Russian].
S. L. Shvartsev, Hydrogeochemistry of the Zone of Hypergenesis (Nedra, Moscow, 1998).
Author information
Authors and Affiliations
Corresponding author
Additional information
Original Russian Text © S.L. Shvartsev, O.E. Lepokurova, 2014, published in Doklady Akademii Nauk, 2014, Vol. 459, No. 3, pp. 357–362.
Rights and permissions
About this article
Cite this article
Shvartsev, S.L., Lepokurova, O.E. The unique alkaline waters in the Chulym basin (West Siberia). Dokl. Earth Sc. 459, 1464–1469 (2014). https://doi.org/10.1134/S1028334X14110269
Received:
Published:
Issue Date:
DOI: https://doi.org/10.1134/S1028334X14110269