METADATA IN ENGLISH
About the journal
NAUKA I
TEKHNOLOGICHESKIE RAZRABOTKI (SCIENCE AND TECHNOLOGICAL DEVELOPMENTS), ISSN:
2079-5165, eISSN: 2410-7948, DOI: 10.21455/std; https://elibrary.ru/title_about.asp?id=32295; http://std.ifz.ru/.
The journal was founded in 1992.
NATURAL EXPLOSIVE PROCESSES
IN THE PERMAFROST AREA
© 2017 A.N. Vlasov1, A.N. Khimenkov2, D.B. Volkov-Bogorodskiy1, Yu.K. Levin1
1Institute
of Applied Mechanics of the Russian Academy of Sciences, Moscow, Russia
2Sergeev
Institute of Environmental Geoscience of the Russian Academy of Sciences,
Moscow, Russia
Corresponding
author: A.N. Khimenkov, e-mail: a_khimenkov@mail.ru
Highlights
‒ Two types
of natural explosive processes in the permafrost are described
‒ Explosions of blisters and icing
mound are caused by water freezing in closed volumes
‒ The second
type is release of gases during dissociation of gas hydrates in permafrost
‒ Stages of the natural explosive
processes are considered
‒ Features of gas hydrate dissociation
before impended explosions are shown
Abstract. The
aim of the paper is the consideration of the group’s natural explosive
processes on the area of permafrost, which have not been allocated. The first
group described the long and associated with freezing of water in closed
environments (explosions of blisters and icing mound). The second was allocated
in the last 3 years. It is associated with the release of underground gases
formed during dissociation of gas hydrate contained in permafrost. The cause of
the explosion in both cases is formation overpressure in the soil mass
containing free water or gas. Once pressure exceeds the strength of the roof of
permafrost occurs her release. It can identify a number of common features of preparation
of the explosive processes in the permafrost. First, there is a local zone
where is concentrated substance forming explosion: over-freezing streambed
ground water flow, water concentration zone in over-freezing soil mass, gas
hydrates in frozen soil. Second, there is the pressure of a compressive the
substance. Third, there are deformations in overlying soils. If pressure
increases slowly and the roof have time to deform, then there is plastic
deformation. In this case mounds are formed. It is expressed in the topography.
If the pressure increases quickly then plastic deformation may not occur.
Fourth, it is the explosion itself. As many authors described the explosion
effect on the objects of various origins has common characteristics. It is a gas-saturated
water and gas ejection, also ground and ice debris, which are launched on ten
and sometimes on hundred meters. During dissociation of the gas hydrate in
frozen ground first micro-cracks are arising. Then they make up ascended
subvertical channels and elongate pores growing under sufficiently high
pressure. Gas hydrat cropout on the soil surface and gas evaporation is
prevented by the durable monolithic overlying ice-soil “cover”. As a result of
this impossibility the crack-pore structure of the frozen ground is formed
under “cover”. Then the width of crack opening and the pore size are increased
with pressure grow by gas filtration from the source. They merge together
founded cavity in which continue gas leakage. In the moment of exceeding the ultimate
strength limit, the “cover” could not bear stresses and accumulated potential
gas energy is released (i.e. transformed to the kinetic one) by the explosion.
During Arctic development the hazard of explosion processes for engineering
constructions will be increased. Nevertheless this group of risk is not only
not considering under designing and prediction, but even not including in the
group of danger geological processes.
Keywords:
permafrost, gas hydrates, blister, explosion, crater, stages, dissociation.
Cite this
article as: Vlasov A.N.,
Khimenkov A.N., Volkov-Bogorodskiy D.B., Levin Yu.K. Natural explosive processes in
the permafrost area, Nauka i
Tekhnologicheskie Razrabotki (Science and Technological Developments).
2017. Vol. 96, No. 3. P. 41–56. [Special issue “Applied
Geophysics: New Developments and Results. Part. 1.
Seismology and Seismic Exploration”]. [in Russian]. DOI:
10.21455/std2017.3-4
References
Andreev V.I.
Hydrolakkolites (Bulgunnyakhs) in the West Siberian Tundra, Izvestiya Gosudarstvennogo geograficheskogo
obshchestva (Izvestia of the State Geographical Society), 1936,
Vol. 68, No. 2, pp. 186–210.
Bazhenova O.I.
Modern dynamics of lake-fluvial systems of the Onon-Torean high plain (Southern
Transbaikalia), Vestnik Tomskogo gosudarstvennogo
universiteta (Bulletin of Tomsk State University), 2013, No. 371,
pp. 171–177.
Bogomolov N.S., Sklyarevskaya A.N.
On the explosions of hydrolakkolites in the southern part of the Chita region, Naledi Sibiri, Moscow, Nauka, 1969,
pp. 127–130.
Bogoyavlenskiy V.I.
Oil and gas emissions on land and offshore areas of the Arctic and the World
Ocean, Bureniye i neft’ (Drilling and
Oil), 2015, No. 6, pp.4–10.
Bogoyavlenskiy V.I., Garagash I.A. Mathematical modeling of
the formation process of craters of gas ejection in the Arctic, Arktika. Ekologiya i ekonomika (Arctic. Ecology
and Economics), 2015, No. 3. pp. 12–17.
GOST R
22.0.08-96. Safety in Emergency Situations.
Man-Caused Emergency Situations. Explosions.
Terms and Definitions. Moscow: IPK Publishing House of
Standards, 1996.
Griva G.I.
Geoecological Conditions for the Development of Gas Fields in the Yamal
Peninsula: author’s abstract. Diss. ... Dr. Geol.-Min. Sciences. Nadym, 2006.
41 p.
Devisilov V.A., Drozdova T.I., Timofeeva S.S. Theory of Combustion and
Explosion. Workshop: A Training Manual. Moscow: FORUM, 2012, 352 p.
Dyadin Yu.A.,
Gushchin A.L. Gas hydrates, Sorosovskiy
Obrazovatel’nyy zhurnal (Soros Educational Magazine). 1998,
Issue. 3, pp. 55–64.
Epov M.I., Eltsov I.N., Olenchenko V.V., Potapov V.V., Kushnarenko O.N., Plotnikov A.E., Sinitsky A.I. Bermuda Triangle of
Yamal, Nauka iz pervykh ruk (Science
from the First-Hand), 2014. Vol. 59, No. 5.
pp. 14–23.
Khimenkov A.N., Sergeev D.O., Stanilovskaya Yu.V., Vlasov A.N., Volkov-Bogorodskiy D.B. Trans-formation
of permafrost during the dissociation of gas hydrates, Proceedings of the International Conference on
Permafrost “Earth’s Cryosphere: Past, Present and Future”, Pushchino,
2017. pp. 131–132.
Kizyakov A.I., Sonyushkin A.V., Leibman M.O., Zimin M.V., Khomutov A.V. Geomorphological
conditions for the formation of a gas discharge funnel and the dynamics of this
shape in central Yamal // Kriosfera Zemli,
(Cryosphere of the Earth), 2015, Vol. XIX, No. 2, pp. 15–25.
Leibman M.O.,
Kizyakov A.I., Plekhanov A.V., Streletskaya I.D.
New permafrost feature — deep crater in central Yamal (West Siberia,
Russia) as a response to local climate fluctuations, Geography Environment, 2014, Vol. 7,
No. 4, pp. 68–80. DOI: 10.15356/2071-9388_04v07_2014_05
Mackay J.R.
Pingos of the Tuktoyaktuk Peninsula Area, Northwest Territories, Géographie Physique et Quaternaire, 1979,
Vol. 33, No. 1. pp. 3–61. DOI :
10.7202/1000322ar
Mackay J.R.
Pingo Growth and collapse, Tuktoyaktuk Peninsula Area,
Western Arctic Coast, Canada: a long-term field study, Géographie Physique et
Quaternaire, Volume, 1998, Vol. 52, No. 3, pp. 271–323. DOI
10.7202/004847ar
Natural
Hazards of Russia. Geocryological Hazards /
Garagulya L.S., Buldovich S.N., Romanovsky V.E. et al.
Moscow: KRUK, 2000, 315 p.
Petrov V.G.
Naledi on the Amur-Yakutian Highway, Leningrad, Publishing House of the USSR
Academy of Sciences, 1930, 177 p.
Strugov A.S. The explosion of the hydro-laccolith (Chita Region), Priroda (Nature), 1955, No. 6,
p. 117.
Savatorova V.L.,
Talonov A.V., Vlasov A.N., Volkov-Bogorodskiy D.B.
Brinkman’s filtration of fluid in rigid porous media: multiscale analysis and
investigation of effective permeability, Composites:
Mechanics, Computations, Applications: An International Journal, 2015. Vol. 6, No. 3. P. 239–264. DOI:
10.1615/CompMechComputApplIntJ.v6.i3.50
Savatorova V.L.,
Talonov A.V., Vlasov A.N.,
Volkov-Bogorodskiy D.B.
Multiscale modeling of gas flow through organic-rich shale matrix, Composites: Mechanics, Computations, Applications:
An International Journal, 2016, Vol. 7, No. 1, pp. 45–70.
DOI: 10.1615/CompMechComputApplIntJ.v7.i1.40
Vlasov A.N., Savatorova V.L., Talonov A.V. The use of the multiscale
averaging method for describing mass transfer processes in organic materials of
geomaterials, Mekhanika kompozitsionnykh
materialov i konstruktsiy (Mechanics of Composite Materials and
Structures), 2016, Vol. 22, No. 3, pp. 362–377.
About the authors
VLASOV Alexander Nikolaevich — Doctor of Technical Sciences, Director, Institute of
Applied Mechanics of the Russian Academy of Sciences (IPRIM RAS). 125040, Russia, Moscow, Leningradskii prospekt 7, stroenie 1.
E-mail: iam@iam.ras.ru
KHIMENKOV Alexander Nikolaevich — Candidate
of Geological and Mineralogical Sciences, Leading Researcher, Sergeeva
Institute of Geoecology of the Russian Academy of Sciences (IGE RAS). 101000, Moscow, Ulansky pereulok 13, stroenie 2, PO Box 145.
E-mail: a_khimenkov@mail.ru ((corresponding author).
VOLKOV-BOGORODSKIY Dmitry
Borisovich — Candidate of
Physical and Mathematical Sciences, Leading Researcher, Institute of Applied
Mechanics of the Russian Academy of Sciences (IPRIM RAS). 125040,
Moscow, Leningradskii prospekt 7, stroenie 1. E-mail: v-b1957@yandex.ru.
LEVIN Yuri Konstantinovich — Candidate of Technical Sciences, Head of Laboratory,
Institute of Applied Mechanics of the Russian Academy of Sciences (IPRIM RAS). 125040, Moscow, Leningradskii prospekt 7, stroenie 1. E-mail:
iam-ras@mail.ru