22-27 September 2019
Trade Fairs and Congress Center (FYCMA)
Europe/Madrid timezone

Chemical and isotopic signatures of the thermal groundwaters from Kuldur spa (Russia)

24 Sep 2019, 16:00
Trade Fairs and Congress Center (FYCMA)

Trade Fairs and Congress Center (FYCMA)

Av. de José Ortega y Gasset, 201 29006 Malaga, Spain
Poster Topic 5 - Tools, methods and models to study groundwater Poster with refreshments


Ms Larisa Lyamina (MSU)


Kuldur spa is the most famous and great resort located in the Russian Far East, Amur River region. The geological structure is defined by the contact zone of Paleozoic granites and Proterozoic gneiss. The granite country rocks are intensive altered and fractured. The typical feature of studied waters is a high temperature (up to 100 °C), low TDS (< 0.5 g/l), high pH (> 9). The cations are mostly Na+, less Ca2+ and a few Mg2+. The main anion is HCO3, the second - SO4. Water is usually enriched with F-, Si, Al, W, Mo, etc. All waters content high amount of radon ( up to 32.4 kBq/l).

The purpose of this work is to study the chemical and isotopic signatures of nitric thermal waters from Kuldur spa and characterize their circulation processes. For solving this task, multiple isotopes δD, δ18O, 3H, 3He/4He, 4He/20Ne, δ13C, 234U/238U together with geothermometer calculation were utilized.

The main gas component is N2 (up to 98 vol.% ) with a trace amount of noble gases (Ar, Kr, Xe, He and Ne), in both dissolved and escaping gas. The methane, carbon dioxide and oxygen contents are minor. The 3He/4He ratio is low 0,19-0,25 and can be considered as dominated by a crustal source. The δ13СDIC values vary from -30 to -18.1 ‰ and testify on the biogenic origin of carbonate specimens. The δ18O and δD are parallel with GMWL showing that the recharge source of thermal water is local meteoric precipitation. Value of 3H are very low up to 0.7 TE which indicate the long circulation time and also confirm no dilution of deep thermal waters with shallow cold water. Our calculation based on Na-K and SiO2 geothermometers indicates that these thermal waters are reached 130oC and the corresponding circulation depth is about 5 km. According to the 234U/238U dating, the circulation time of the studied thermal groundwater is at about 400,000 years.

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