Damage and consequences of mudflows in Central Tajikistan

Journals

Title：
Damage and consequences of mudflows in Central Tajikistan
Author：
Karimov Alihon Akhmedovich
Author Affiliation：
The Scientific Research State Unitary Enterprise "Tabiat", the Committee for the Protection of the Environment under the Government, Dushanbe, The Republic of Tajikistan
Received：Mar.6, 2023
Accepted：Apr.11, 2023
Published：Apr.26, 2023

Abstract

Mudflows are typical not only for most of the mountainous regions of Tajikistan, but also for all regions of Central Asia. When passing, they led to casualties and destruction. This process has been studied since the second half of the 19th century. Significant research experience has been accumulated, especially in the field of identifying the parameters of mudflows and measures to protect against them. In the history of the study of mudflows in Central Tajikistan, two periods can be distinguished - the stage of episodic studies from the middle of the 19th to the middle of the 20th century and the modern stage of systematic studies. A number of summaries works and monographs have been written about the mudflows of Central Tajikistan, and bibliographic summaries have been compiled. The evolution of glaciation and mudflow activity was considered in the book by I.B. Seinova and E.A. Zolotarev (2001).

Keywords

Mudflow basin, flow, rescuers of the CoES, mudflow masses, deposition, generation, transit, accumulation, lithodynamic criterion.

Doi

https://doi.org/10.58396/gges020101

References

[1] Valiev, Sh.F. (2014). Engineering and economic transformation of the roof of the lithosphere in Tajikistan. Scientific journal Science and Innovation No. 1 Str–219. Dushanbe Tajikistan:

[2] Chernomorets S.S. (2003). Features of morpholithodynamics of mudflow centers of the Central Caucasus after catastrophic mudflows. Abstract of the dissertation for the degree of candidate of geographical sciences. Russia Moscow.

[3] Golosov V.N. (1987). Scree processes. Modern exogenous processes in the foothills of the Western Tien Shan. dep. VINITI No. 6388, p. 40-58. Russia

[4] Karimov A.A., Ospanova N.K. (2020). About Engineering-Geonomic Research in the Zeravshan River Pool (Southern Tien Shan) in Connection with Climate Oscillations. 8: #5; ISSN: 2327-4336. https://www.scirp.org/journal/gep. DOI: 10.4236/gep.2020.85024

[5] Karimov A.A., Valiev Sh.F., Andamov R.Sh., Nabiev N.F. (20117). Glacial formations and climate change are the source of manifestation and development of natural georisks in central Tajikistan. Journal of Izvestia of universities of Kyrgyzstan. No. 1, p. 70-73.

[6] Tukeev O.V. (2002). Mudflow phenomena in the Pamirs catastrophe patterns. forecast. Page 176. Moscow. Russia.

[7] Krylenko I.V., Krylenko I.N. (2003). Epicatastrophic limnogenesis: Lake Saniban after the Genaldon disaster of 2002. - Sat. m-catching 3rd scientific-practical. "Problems of Forecasting Emergency Situations". Page 95. Moscow. Russia.

[8] Karimov A. A. (2018) Engineering-geonomic assessment of the development and typification of sources of solid runoff of mudflows in the Zeravshan river basin. Bishkek. Kyrgyz scientific journal Science, new technology and innovation. No. 2, pp. 77-81.

[9] Usupaev Sh. E., Valiev Sh. F. (2017). IGN model of typification and forecast of glacio-permafrost georisks in mountainous regions and the world. Mat. Intern. Scientific and Practical Conf. “Climate Change and Water Resources of Central Asia”, Tajikistan Dushanbe Journal of Science and Innovation. Natural Sciences Series, No. 1. Pp. 159-165.

[10] Sheko A.I. (1980) Patterns of formation and forecast of mudflows. Nedra–296 s Russia Moscow.

[11] 11. Karimov A.A., Valiev Sh.F. (2019). Monitoring of natural georisks in the Zeravshan river basin. Science and innovation #2. Series of Geological and Technical Sciences. Pp 52-58. (UDC: 556.33.632). Dushanbe Tajikistan.

[12] Karimov A. A., Andamov R. Sh., Fayzaliev. (2019). Sources of formation and development of mudflow processes in the Zeravshan river basin. Science and innovation #2. pp 169-175. (UDC: 551.3.053). Dushanbe Tajikistan.

[13] Karimov A.A. (2019). Monitoring of natural georisks in the Zeravshan river basin. Science and innovation. Series of geological and technical sciences. No. 2. Pg. 52-58. Dushanbe Tajikistan.

[14] Karimov A.A. (2019). Anti-mudflow structures of some sections of the Zeravshan river basin and measures to prevent georisks Kishovarz. - No. 2. - S. 147-149. Dushanbe Tajikistan.

[15] Valiev Sh.F., Karimov A.A., Usupaev Sh.E. (2016) Potential georisks as a consequence of the construction of the Zeravshan cascade of hydroelectric power plants and their expected scale. Science, new technologies and innovations №7. pp. 32-35. Kyrgyzstan.

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