Application of electrical tomography to study the internal structure of rock glaciers in Altai


https://doi.org/10.15356/2076-6734-2017-1-69-76

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Abstract

Internal structure of rock glaciers was investigated at two key sites in Altai by means of electric tomography. It had been found that the rock glaciers of the same type, located at different altitude levels, differ in electric resistances of ice nuclei and the degree of consolidation of the ice material inside of them. Typical characteristics of the ice core of a rock glacier in the high-mountain area are the following: electrical resistivity is about 1000–2000 kOhm∙m and a high degree of the ice consolidation, while the same for the mid-mountain region: the electrical resistivity is 150–300 kOhm∙m and the presence of the talik zones within the glacier body. Using the method of electric tomography for investigation of the internal structure of the rock-glaciers makes possible to reveal presence of frozen soils and ice and to find the upper boundary of occurrence of them from anomalously high specific electric resistance. However, it is not always possible to determine a thickness of the rock-ice formation, and to estimate a degree of its consolidation that does not allow calculating the ice content volume. Limitations of this technology can be overcome by the use of electric tomography in combination with other geophysical methods.

About the Authors

G. S. Dyakova
Altai State University
Russian Federation
Barnaul


V. V. Olenchenko
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences
Russian Federation
Novosibirsk


O. V. Ostanin
Altai State University
Russian Federation
Barnaul


References

1. Dyakova G.S., Ostanin O.V. Lichenometry method of dating: opportunities and prospects. Geografiya i prirodopolzovanie Sibiri. Geography and natural resources of Siberia. Barnaul: Publ. of Altai State University, 2013, 15: 36–44. [In Russian].

2. Solomina O.N. Gornoe oledenenie Severnoi Evrazii v golotcene. Mountain glaciation of Northern Eurasia in Holocene. Moscow: Nauchnyi Mir, 1999: 272 p. [In Russian].

3. Fukui K., Fujii Y., Mikhailov N., Ostanin O., Iwahana G. The lower limit of mountain permafrost in the Russian Altai Mountains. Permafrost and Periglacial Processes, 2007, 18 (2), April/June: 129–136.

4. Ostanin O.V., Mikhailov N.N. Sovremennye izmeneniya vysokogornykh geosistem (na primere Tcentralnogo i Yugo-Vostochnogo Altaya). Modern changes of alpine geosystems (on the example of the Central and SouthEastern Altai). Barnaul: Publ. of Altai State University, 2014: 171 p. [In Russian].

5. Lapkovskaia A.A., Olenchenkov V.V., Potapov V.V., SHein A.N., Gornostaeva E.S., Gubin D.I. The structure of the rock glaciers of the Sukorsky landslip (Altai Mountain) according electrical resistivity tomography. Arktika, Subarktika: mozaichnost, kontrastnost, variativnost kriosfery. Arctic, Subarctic: mosaic, contrast, variability of the Cryosphere: Proc. of the Intern. Conf. Tyumen: Epoha publishing house, 2015: 195–198. [In Russian].

6. Galanin A.A. Complex rock glaciers – a special type of mountain glaciers of the North-East of Russia. Vestnik DVO RAN. Herald of the Far East Branch of the RAS. 2005, 5: 59–70. [In Russian].

7. Galanin A.A., Olenchenko V.V., Khristoforov I.I. New data about the internal structure, hydrological regime and rheology of rock glaciers of the Northern Tien Shan – sources of catastrophic ice–dirtstone mudflows. Fundamentalnye i prikladnye problemy gidrogeologii. Fundamental and applied problems of hydrogeology. 2015: 369–375. [In Russian].

8. Farbrot H., Isaksen K., Eiken T., Kaab A., Sollid J.L. Composition and internal structures of a rock glacier on the strandflat of western Spitsbergen, Svalbard. Norsk Geografisk Tidsskrift – Norwegian Journ. of Geography. 2005, 59: 139–148.

9. Evin M., Fabre D., Johnson P. Electrical resistivity measurements on the rock glaciers of Grizzly Creek, St Elias Mountains, Yukon. Permafrost and Periglacial Processes. 1997, 8: 179–189.

10. Hauck C. Frozen ground monitoring using DC resistivity tomography. Geophys. Research Letters, 2016, 29 (21): 121–124.

11. Leopold M., Williams M.W., Caine N., Volkel J., Dethier D. Internal structure of the Green Lake 5 Rock Glacier, Colorado Front Range, USA. Permafrost and Periglacial Processes, 2011. doi: 10.1002/ppp.706.

12. Maurer H., Hauck C. Geophysical imaging of alpine rock glaciers. Journ. of Glaciology. 2007, 180: 110–118.

13. Dyakova G.S., Ostanin O.V. Glyatcialno-merzlotnye kamennye obrazovaniya basseina r. Chuya (Gornyi Altai). Glacial-permafrost rock formations of Chuya river basin (Altai Mountain). Barnaul: Publ. of Altai State University, 2014: 152 p. [In Russian].

14. Ostanin O.V., Dyakova G.S. Glacial-permafrost rock formations of the Central Altai. Izvestiya AGU. Proc. of the Altai State University. Barnaul: 2013, 3–2 (79): 167–170. [In Russian].

15. Sukhova M.G., Rusanov V.I. Klimaty landshaftov Gornogo Altaya i ikh otcenka dlya zhiznedeyatelnosti cheloveka. Climates of landscapes of the Altai Mountains and their assessment for human life. Novosibirsk: Publ. of Siberian Branch of the RAS, 2004: 150 p. [In Russian].

16. Loke M.H., Acworth I., Dahlin T. A comparison of smooth and blocky inversion methods in 2D electrical imaging surveys. Explorat. Geophys. 2003, 34: 182–187.

17. Frolov A.D. Elektricheskie i uprugie svoistva merzlykh porod i ldov. Electrical and elastic properties of permafrost and ice. Pushchino: ONTI PSC RAS, 1998: 515 p. [In Russian].

18. http://serc.carleton.edu/vignettes/collection/31903.html


Supplementary files

For citation: Dyakova G.S., Olenchenko V.V., Ostanin O.V. Application of electrical tomography to study the internal structure of rock glaciers in Altai. Ice and Snow. 2017;57(1):69-76. https://doi.org/10.15356/2076-6734-2017-1-69-76

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