Zobrazeno 1 - 10
of 25
pro vyhledávání: '"V V Malakhova"'
Autor:
V. V. Malakhova, A. V. Eliseev
Publikováno v:
Лëд и снег, Vol 60, Iss 4, Pp 533-546 (2020)
Salt transport in shelf sediments can affect the state of the submarine permafrost and the thermodynamic stability of hydrates. To estimate the effect of salt transport, we used a model analysis of salinization of underwater sediments. It is assumed
Externí odkaz:
https://doaj.org/article/b9e4b1a7a1fb49c5a6c543eb0d8e7fb0
Autor:
V. V. Malakhova, A. V. Eliseev
Publikováno v:
Лëд и снег, Vol 58, Iss 2, Pp 231-242 (2018)
This paper presents results of the analysis of the influence of talik zones associated with thermokarst lakes and processes in rift zones on the dynamics of subaqueous permafrost and zones of stability of methane hydrates for conditions of theLaptev
Externí odkaz:
https://doaj.org/article/92a691738faa44dd8d526c8f9955277c
Autor:
V. A. Cheverda, D. S. Bratchikov, K. G. Gadylshin, E. N. Golubeva, V. V. Malakhova, G. V. Reshetova
Publikováno v:
Doklady Earth Sciences. 507:S424-S430
Publikováno v:
Doklady Earth Sciences. 506:782-789
Autor:
V. V. Malakhova, E. N. Golubeva
Publikováno v:
Лëд и снег, Vol 56, Iss 1, Pp 61-72 (2016)
A state of permafrost in the Arctic is the key to understanding whether methane, stored in the permafrost related gas hydrate, can release into the atmosphere. The global warming can lead to destabilization of the submarine permafrost and, thus, caus
Externí odkaz:
https://doaj.org/article/4da7c22b3aa94a7a8dd0cdfebf3e815c
Publikováno v:
Permafrost and Periglacial Processes. 31:487-496
Autor:
V. V. Malakhova, A. V. Eliseev
Publikováno v:
Ice and Snow. 60:533-546
Autor:
V V Malakhova
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 1040:012022
In this study, we evaluate the sensitivity of gas hydrate reservoirs associated with submarine permafrost conditions to changes in global climate. We apply numerical simulations to assess the timings of methane hydrate dissociation on the East Siberi
Publikováno v:
Doklady Earth Sciences. 480:826-830
The thermobaric conditions of the formation, stability, and dissociation of continental gas hydrates were determined by simulation of the thermal state of the permafrost. The calculations covered the period over the last 130 000 years, taking into ac
Publikováno v:
25th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics.
The dissociation of the pore metastable relict gas hydrates in permafrost as a consequence of the observed climate changes is one the possible reasons for the formation of gas craters in the northern part of West Siberia. Using the heat transfer mode