Equilibrium-nonequilibrium state of the water-rock system

S. L. Shvartsev

    Research output: Chapter in Book/Report/Conference proceedingChapter

    9 Citations (Scopus)

    Abstract

    The study of the saturation states of various underground waters (from ultra-fresh to strong brines) with different minerals show, that the water-rock system is in the equilibrium-nonequilibrium state. This internally contradictory state allows spontaneous, continuous evolution over geologically long time with the formation of principally new mineral phases and new geochemical types of water.

    Original languageEnglish
    Title of host publicationWater-rock interaction. Proc. symposium, Vladivostok, 1995
    Pages751-754
    Number of pages4
    Publication statusPublished - 1995

    Fingerprint

    rock
    new mineral
    water
    saturation
    mineral

    ASJC Scopus subject areas

    • Earth and Planetary Sciences(all)
    • Environmental Science(all)

    Cite this

    Shvartsev, S. L. (1995). Equilibrium-nonequilibrium state of the water-rock system. In Water-rock interaction. Proc. symposium, Vladivostok, 1995 (pp. 751-754)

    Equilibrium-nonequilibrium state of the water-rock system. / Shvartsev, S. L.

    Water-rock interaction. Proc. symposium, Vladivostok, 1995. 1995. p. 751-754.

    Research output: Chapter in Book/Report/Conference proceedingChapter

    Shvartsev, SL 1995, Equilibrium-nonequilibrium state of the water-rock system. in Water-rock interaction. Proc. symposium, Vladivostok, 1995. pp. 751-754.
    Shvartsev SL. Equilibrium-nonequilibrium state of the water-rock system. In Water-rock interaction. Proc. symposium, Vladivostok, 1995. 1995. p. 751-754
    Shvartsev, S. L. / Equilibrium-nonequilibrium state of the water-rock system. Water-rock interaction. Proc. symposium, Vladivostok, 1995. 1995. pp. 751-754
    @inbook{8b2c147bbbc9492188b08f81bb610c75,
    title = "Equilibrium-nonequilibrium state of the water-rock system",
    abstract = "The study of the saturation states of various underground waters (from ultra-fresh to strong brines) with different minerals show, that the water-rock system is in the equilibrium-nonequilibrium state. This internally contradictory state allows spontaneous, continuous evolution over geologically long time with the formation of principally new mineral phases and new geochemical types of water.",
    author = "Shvartsev, {S. L.}",
    year = "1995",
    language = "English",
    pages = "751--754",
    booktitle = "Water-rock interaction. Proc. symposium, Vladivostok, 1995",

    }

    TY - CHAP

    T1 - Equilibrium-nonequilibrium state of the water-rock system

    AU - Shvartsev, S. L.

    PY - 1995

    Y1 - 1995

    N2 - The study of the saturation states of various underground waters (from ultra-fresh to strong brines) with different minerals show, that the water-rock system is in the equilibrium-nonequilibrium state. This internally contradictory state allows spontaneous, continuous evolution over geologically long time with the formation of principally new mineral phases and new geochemical types of water.

    AB - The study of the saturation states of various underground waters (from ultra-fresh to strong brines) with different minerals show, that the water-rock system is in the equilibrium-nonequilibrium state. This internally contradictory state allows spontaneous, continuous evolution over geologically long time with the formation of principally new mineral phases and new geochemical types of water.

    UR - http://www.scopus.com/inward/record.url?scp=0029419696&partnerID=8YFLogxK

    UR - http://www.scopus.com/inward/citedby.url?scp=0029419696&partnerID=8YFLogxK

    M3 - Chapter

    SP - 751

    EP - 754

    BT - Water-rock interaction. Proc. symposium, Vladivostok, 1995

    ER -