Vestnik КRAUNC. Fiz.-Mat. nauki. 2024. vol. 47. no. 2. P. 129 – 142. ISSN 2079-6641

INSTRUMENTS AND MEASUREMENT METHODS
https://doi.org/10.26117/2079-6641-2024-47-2-129-142
Research Article
Full text in Russian
MSC 86-11

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Experience with the «Triton-M» georadar device in the Petropavlovsk-Kamchatsky city (Kamchatka)

V.Yu. Pavlova^\ast

Vitus Bering Kamchatka State University, 683032, Petropavlovsk-Kamchatsky, st. Pogranichnaya, 4, Russia

Abstract. Determining the possibilities of using the ground penetrating radar method, which is a method of shallow geophysics, in seismically active areas will increase the information content and reliability of the results, especially in engineering and geological surveys to ensure seismic-resistant construction in geodynamically active areas, which include Kamchatka. To optimize the ground penetrating radar method, it is necessary to compare and analyze the results of observations in various geological conditions. Since the ground penetrating radar method has been intensively developing in recent years, theoretical research in the field of data processing must be illustrated by numerous examples of the practical use of ground penetrating radars at various research sites. The purpose of the research is to create a scientific and methodological basis for the georadar method in relation to Kamchatka, including methods for processing and interpreting data, taking into account practical experience of application at various sites. The object of the research is the geological features and soil conditions of the territory of the Petropavlovsk-Kamchatsky city, requiring clarification and detailed study. The article describes the experience and features of working with the «Triton-M» georadar device in the Petropavlovsk-Kamchatsky city. Some results of ground penetrating radar profiling are characterized. Recommended values of measurement parameters during work are given. From a practical point of view, the most important parameters of the ground penetrating radar are the probing depth and the depth resolution. The «Triton-M» ground penetrating radar device is applicable for solving geological problems in the territory of the Petropavlovsk-Kamchatsky city, while optimally selected values of measurement parameters minimize the recording of interference and provide more accurate useful information about the probed environment. For accurate interpretation of radargrams, it is necessary to use information about the geological structure of the studied territory.

Key words: Kamchatka, the Petropavlovsk-Kamchatsky city, georadar, the GPR method, radargrams, data processing.

Received: 28.06.2024; Revised: 15.08.2024; Accepted: 19.08.2024; First online: 26.08.2024

For citation. Pavlova V.Yu. Experience with the «Triton-M» georadar device in the Petropavlovsk Kamchatsky city (Kamchatka). Vestnik KRAUNC. Fiz.-mat. nauki. 2024, 47: 2, 129-142. EDN: OKEVKJ. https://doi.org/10.26117/2079-6641-2024-47-2-129-142.

Funding. The work was carried out as part of the realization of the Strategic Academic Leadership Program «Priority 2030. The Far East» and as part of the implementation of the grant of the Federal State Budgetary Educational Institution of Higher Education «KamSU. Vitus Bering» №124020800006-9 on the topic of the scientific project «Clarification of soil conditions and the geological structure of the territory of Petropavlovsk-Kamchatsky using the method of geolocation» (head Pavlova V.Yu.).

Competing interests. There are no conflicts of interest regarding authorship and publication.

Contribution and Responsibility. The author participated in the writing of the article and is fully responsible for submitting the final version of the article to the press.

^\astCorrespondence: E-mail: verpavlova88@gmail.com

The content is published under the terms of the Creative Commons Attribution 4.0 International License

© Pavlova V.Yu., 2024

© Institute of Cosmophysical Research and Radio Wave Propagation, 2024 (original layout, design, compilation)

References

1. SP 14.13330.2018. Construction in seismic areas. Updated edition of SNiP II-7-81*. Moscow, Standartinform, 2018, 115 p. (In Russian)
2. Sheimovich V. S. State geological map of the Russian Federation 1:200000. South Kamchatka series. Sheets N-57-XXI (Northern Koryaks), N-57–XXVII (Petropavlovsk-Kamchatsky), N-57-XXXIII (Mount Mutnovskaya), 2000, 302 p. (In Russian)
3. Savelyev D.P., Palechek T. N., Portnyagin M. V. Campanian oceanic siliceous-volcanogenic deposits in the basement of the eastern Kamchatka volcanic belt, Pacific Geology, 2005, vol. 24, no. 2, pp. 46–54. (In Russian)
4. Bergal-Kuvikas O., Bindeman I., Chugaev A., Larionova Y., Perepelov A., Khubaeva O. Pleistocene-Holocene Monogenetic Volcanism at the Malko-Petropavlovsk Zone of Transverse Dislocations on Kamchatka: Geochemical Features and Genesis, Pure and Applied Geophysics, 2022, vol. 179, pp. 3989–4011. DOI: 10.1007/s00024-022-02956-7.
5. Konstantinova T. G. Behavior of soils and buildings during strong earthquakes. Obninsk, FRC EGS RAS, 2020, 188 p. (In Russian)
6. Esin E. I., Vasilevskiy A. N., Bushenkova N. A. Spatial correlations between the terrain features, gravitational field and seismic velocity anomalies in the central Kamchatka region. Russian Geology and Geophysics, 2024, vol. 65, no. 2, pp. 285-298 (In Russian)
7. Gontovaya L.I., Popruzhenko S.V., Nizkous I.V., Aprelkov S.E. Upper Kamchatka mantle: Depth model and relationship with tectonics, Pacific Geology, 2008, vol. 27, no 2, pp. 80–91. (In Russian)
8. Seliverstov N. I. Stroyeniye dna kamchatskikh vod i geodinamika zony sochleneniya Kurilo Kamchatskoy i Aleutskoy ostrovnykh dug [Structure of the bottom of the Kamchatka waters and geodynamics of the articulation zone of the Kuril-Kamchatsky and Aleutian island arcs]. Moscow: Scientific World, 1998, 164 p. (In Russian)
9. Avdeyko G.P., Bergal-Kuvikas O. V. Geodynamic conditions of formation of adakites and Nb-enriched basalts (NEAB) in Kamchatka, Volcanology and Seismology, 2015, no 5, p. 1–13. (In Russian)
10. Agibalov A. O., Bergal-Kuvikas O.V., Zaitsev V.A., Makeev V.M., Sentsov A.A. The relationship between morphometric parameters of the relief characterizing the cracking of the upper part of the lithosphere and manifestations of volcanism of the Malko-Petropavlovsk Zone, Geophysical Processes and Biosphere, 2023, vol.22, no2, pp. 122-133. (In Russian)
11. Pavlova V.Yu., Delemen I. F. Primeneniye metoda georadiolokatsii na Kamchatke [Application of the ground penetrating radar method in Kamchatka]. Moscow, Publishing House of the Academy of Natural Sciences, 2024, 144 p. (In Russian)
12. Vladov M. L., Starovoytov A. V. Vvedeniye v georadar [Introduction to ground penetrating radar]. Moscow, Moscow State University Publishing House, 2004, 153 p. (In Russian)
13. Starovoytov A. V. Interpretatsiya dannykh georadara [Interpretation of ground penetrating radar data]. Moscow, Moscow State University Publishing House, 2008, 192 p. (In Russian)
14. Operating manual: Triton-M kit. Ramenskoye, Logical Systems LLC, 2021, 13 p. (In Russian)
15. CartScan software package: Operator’s manual. Moscow: LogiS LLC, 2022, 94 p. (In Russian)

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