Dynamics of natural discharge of the hydrothermal system and geyser eruption regime in the Valley of Geysers, Kamchatka. (January 2022)

• Record Type: Journal Article
• Authors: Kiryukhin, A.V.; Polyakov, A.Y.; Zhuravlev, N.B.; Tsuchiya, N.; Rychkova, T.V.; Usacheva, O.O.; Dubrovskaya, I.K.
• Is Part Of: Applied geochemistry. Volume 136(2022)
• Publication Date: 2022-01
• Subjects: Environmental geochemistry -- Periodicals; Water chemistry -- Periodicals; Geochemistry -- Social aspects -- Periodicals; Geochemistry -- Periodicals; 551.9
• DOI: 10.1016/j.apgeochem.2021.105166
• Languages: English
• ISSNs: 0883-2927

Abstract

Abstract: The total deep component natural mass discharge Qd (defined in terms of chloride mass discharge Qcl ) of the Valley of Geysers, on an average ranges from 280 kg/s from 1961 to 1984, to 230 kg/s after 2015. Post 2012, discharge measurements reveal a seasonal variation: the discharge increases (340–370 kg/s) during the winter-frozen period, and decreases during the summer flooding period (≈100 kg/s). Long term annually averaged Qd is 274 kg/s, Qcl is 0.247 kg/s and heat flow is 265 MW. In the course of using high-frequency (min −1 ) observations specific conductance measurements from 2017 to 2020, the total natural discharge was found to be cycling due to the internal cycling of geysers. It was mostly sensitive to the Bolshoy and Velikan geysers with averaged intervals between eruptions of 60 min and 70 min, respectively. The tracer chloride method estimates the volume of hot water erupted from geysers. This method yielded the following estimates: 5–34 m 3 of hot water cyclically erupted from the Bolshoy geyser; 0.5–4.5 m 3 erupted from the Velikan geyser between 2018 and 2020, and 24–144 m 3 erupted before the 2014 mud-flow disaster; and 289–330 m 3 erupted from the Grot geyser between May–June 2012. The seasonal features of natural discharge mentioned above may be explained in terms of cold-water infiltration into a two-phase geyser geothermal reservoir, especially if gas-phase condensation induces vacuum conditions, which may further reduce some thermal discharge features. Highlights: High-frequency (min −1 ) tracer chloride method was used to define Valley of Geysers deep component water natural discharges. The total Qd significantly decreases during flooding periods, possibly due to cold water inflow into the geyser reservoir. The tracer chloride method estimates the volumes of hot water erupted from geysers. Up to 34 m 3 (Bolshoy), 144 m 3 (Velikan, before the 2014), and 330 m 3 (Grot) of hot water have erupted from geysers.