Experience of application surface thermometry in hydrogeological survey

The paper examines in detail the methodological aspects of measuring the temperature field on watercourses when mapping sheet O-41-XXV (Ekaterinburg). A series of thermometric and hydrometric observations was conducted to identify areas of subaquatic discharge of groundwater in the lower reaches of the Mochalovka River, in the area where the Murzinka and Mochalovka rivers converge, and in the middle reaches of the Murzinka River. According to the results of the analysis of the collected data, the most contrasting negative anomalies in groundwater temperature are observed at a depth of 0.5 m. These anomalies are associated with subaquatic discharge into the river of an underground stream with a temperature of 6–7 °C, which differs from the background temperature by a factor of 1.8. The results of the studies revealed three areas with abnormally low temperatures in the range of 6.1–7.2 °C. Experiments and modeling have shown that the discharge points of colder groundwater form local stable temperature anomalies with lower values. Spatial analysis showed that in areas of temperature reduction, the anomaly is associated with cracks surrounding the main fault zone, which are controlled in the relief by a sublatitudinal log, proving the connection between temperature anomalies and active hydrogeological processes and their influence on the dynamics of underground flow.

Keywords: thermometry, groundwater discharge, hydrogeological survey, geophysics on water areas, temperature profile, water flow, tectonic disturbances, Ural, modeling.
For citation:

Zyryanova E. S., Kindler A. A., Elokhina S. N., Elokhin V. A. Experience of application surface thermometry in hydrogeological survey. MIAB. Mining Inf. Anal. Bull. 2025;(12-1):157-169. [In Russ]. DOI: 10.25018/0236_1493_2025_121_0_157.

Acknowledgements:
Issue number: 12-1
Year: 2025
Page number: 157-169
ISBN: 0236-1493
UDK: 553.8: 550.8.08
DOI: 10.25018/0236_1493_2025_121_0_157
Article receipt date: 24.07.2025
Date of review receipt: 09.10.2025
Date of the editorial board′s decision on the article′s publishing: 10.11.2025
About authors:

E.S. Zyryanova1,2, Graduate Student; Leading Specialist, e-mail: katrin.zyrian@mail.ru, ORCID ID: 0000-0003-3394-078X,
A.A. Kindler2, Leading Specialist, e-mail: kindler@gmsn-ural.ru, ORCID ID: 0000-0003-1082-5164,
S.N. Elokhina1,2, Dr. Sci. (Geol. Mineral.); Director, e-mail: elohina.s@mail.ru, ORCID ID: 0000-0002-8641-5439,
V.A. Elokhin1, Dr. Sci. (Geol. Mineral.), Professor, Head of Chair, e-mail: elokhin.v.a@mail.ru, ORCID ID: 0000-0003-4355-5156,
1 Ural State Mining University, 620144, Ekaterinburg, Russia,
2 Hydrospetsgeology «Urals Regional Center GMSN», 620014, Ekaterinburg, Russia.

For contacts:

E.S. Zyryanova, e-mail: katrin.zyrian@mail.ru.

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