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Ozerov A.Yu. Experimental modeling of periodicities in the dynamics of lava fountaining // 7th Biennual workshop on Japan-Kamchatka-Alaska subduction processes: mitigating risk through international volcano, earthquake, and tsunami science (JKASP-2011). Petropavlovsk-Kamchatsky, Russia. August 25-30, 2011. 2011. P. 34-35.
Ozerov A.Yu. Experimental modeling of the basaltic eruptions mechanism // International Conference Fluxes and Structures in Fluids: Physics of Geospheres – 2009, Selected Papers. 2010. P. 269-278.
Ozerov A.Yu. Gas regime defining the mechanism of periodic lava fountaining of basaltic volcanoes (experimental modeling) // Commission on the chemistry of volcanic gases (CCVG) - IAVCEI. 11th Gas Workshop, Kamchatka, Russia. 1-10 September 2011. 2011. P. 35
Ozerov A.Yu. The mechanism of basaltic explosions: Experimental modeling // Journal of Volcanology and Seismology. 2010. V. 4. № 5. P. 295-309. doi: 10.1134/S0742046310050015.    Аннотация
An instrument package for simulating basaltic eruptions (IPSBE) with a height of 18 m has been developed for investigating the processes that occur during Strombolian eruptions. The device follows the geometrical ratio between the actual plumbing system of a volcano, with the ratio of conduit diameter to conduit height being 1 to 1000. For the first time in physical modeling studies, we created conditions in which a moving gassaturated model liquid enters the conduit; this enabled us to study bubble nucleation, expansion, and coalescence, the generation and transformation of gas structures, and the kinetic features shown by the evolution of the gas phase. These experiments revealed a novel (previously unknown) flow pattern of two phase mixtures in a vertical column, viz., a cluster flow that involves the regular alternation of compact clusters of gas bubbles that are separated by a fluid that does not involve a free gas phase. It is shown that the liquid, bubble, cluster, and slug flow patterns are mutually transformed under certain conditions; they are polymorphous modifications of a gassaturated liquid moving in a vertical pipe. The data thus acquired suggested a new model for the gas–liquid movement of a magma melt in a conduit: depending on the type of gas–liquid flow behavior at the vent, the crater will exhibit different types of explosive activity, including actual explosions.
http://repo.kscnet.ru/3530/ [связанный ресурс]
Ozerov A.Yu., Ariskin A.A., Barmina G.S. The Problem of Genetic Relations between High-Aluminous and High-Magnesian Basalts of the Klyuchevskoi Volcano, Kamchatka // Transactions (Doklady) of the Russian Academy of Sciences / Earth Science Sections. 1996. V. 350. № 7. P. 1127-1130.
http://repo.kscnet.ru/3435/ [связанный ресурс]
Ozerov A.Yu., Ariskin A.A., Kyle Ph., Bogoyavlenskaya G.E., Karpenko S.F. Petrological–Geochemical Model for Genetic Relationships between Basaltic and Andesitic Magmatism of Klyuchevskoi and Bezymyannyi Volcanoes, Kamchatka // Petrology. 1997. V. 5. № 6. P. 550–569
http://repo.kscnet.ru/463/ [связанный ресурс]
Ozerov A.Yu., Firstov P.P., Gavrilov V.A. Periodicities in the dynamics of eruptions of Klyuchevskoi Volcano, Kamchatka // Geophysical Monograph Series. // Volcanism and Subduction: The Kamchatka Region. 2007. V. 172. P. 283-291.    Аннотация
Detailed studies of volcanic tremor envelopes with frequencies ranging from 5.5⋅10-6 to 2.5⋅10-2 Hz (50 hrs - 40 sec), recorded during the Klyuchevskoi volcano eruptions of 1983 and 1984, revealed five major frequencies: 1.1⋅10-2 Hz (T1 = 1 min 34 sec), 2.5⋅10-3 Hz (T2 = 6 min 10 sec), 4.2⋅10-4 Hz (T3 = 40 min), 5.1⋅10-5 Hz (T4 = 5 hrs 30 min), 7.7⋅10-6 Hz (T5 = 36 hrs), as well as superpositions of their harmonics. In the 1993 eruption, fluctuations in the volcanic tremor envelopes have frequencies of TI = 2 hrs 48 min and TII = 6 hrs 12 min, which correspond to periodicities in the dynamics of eruptions identified by visual observations since 1932. The distribution of peak amplitudes has been found to vary in relation to eruption intensity—increasing eruption strength correlates with an increase in the amplitude of low frequency peaks, and vice versa. It is concluded that volcanic tremor allows monitoring of eruption dynamics. Possible reasons for the occurrence of periodicities are discussed, but a comprehensive model for this phenomenon has not yet been developed.
Ozerov A.Yu., Gordeev E.I., Dvigalo V.N. Modern volcanism of Kamchatka, Russia // Proceeding of the 3-rd International symposium. Jeju Volcanological Institute. Korea. 2005. С. 33-41.
Ozerov A.Yu., Karpov G.A., Droznin V.A., Dvigalo V.N., Demyanchuk Yu.V., Ivanov V.V., Belousov A.B., Firstov P.P., Gavrilov V.A., Yaschuk V.V., Okrugina A.I. The September 7 - October 2, 1994 Eruption of Klyuchevskoi Volcano, Kamchatka // Volcanology and Seismology. 1997. № 18. P. 501-516.
http://repo.kscnet.ru/1466/ [связанный ресурс]
Ozerov A.Yu., Khubunaya S.A. High-magnesian olivines and pyroxens as a criterion of petrogenetic relationship of calc-alkaline magmas from Klyuchevskoy volcano // Abstracts of 29th International Geological Congress. Kyoto: 1992. P. 639
Ozerov A.Yu., Konov A.S. Regularities in the dynamics of the Klyuchevskoy volcano eruptions // Proceeding Kagoshima International Conference on Volcanoes. Japan: 1988. P. 63-65.
Ozerov A.Yu., Murav’ev Ya.D., Frisbie A.J. The 1996 Eruption of Karymsky Volcano and the Composition of its Products, Kamchatka, Russia // AGU Spring Meeting 1997 Abstracts. Baltimore, Maryland: AGU. 1997. P. V22A-04.
Ozerov Alexei Y. The evolution of high-alumina basalts of the Klyuchevskoy volcano, Kamchatka, Russia, based on microprobe analyses of mineral inclusions // Journal of Volcanology and Geothermal Research. 2000. V. 95. № 1–4. P. 65 - 79. doi: 10.1016/S0377-0273(99)00118-3.    Аннотация
The origin of calc-alkaline high-alumina basalts (HAB) of the Klyuchevskoy volcano, Kamchatka, was examined using electron microprobe analyses of phenocrysts and mineral phases included in the phenocrysts. Continuous trends on major-element variation diagrams suggest the HAB were derived from high-magnesia basalt (HMB) by fractional crystallization. Phenocrysts in the HAB are strongly zoned: olivine (Mg# 91–64), clinopyroxene (Wo45–38En40–51Fs5–20) and chrome—spinel/magnetite inclusions in them (Cr2O3 45–0 wt.%, TiO2 0.5–11%). Microprobe analyses of minerals included in the phenocrysts provide additional constraints on the mineral crystallization trends in the HAB. Fe/Mg partitioning data, when applied to the phenocrysts cores, show they crystallized from a HMB. The similarity of phenocryst core compositions in HAB with those in HMB strongly suggests a genetic relationship between the two magma types.
Ozerova N., Ozerov A. Atmochemical halos of mercury (Hg) within the area of active volcanic edifices in Kamchatka // IAVCEI 2008 - General Assembly, Reykjavik, Iceland. Abstracts. 2008. P. 7
Ozerova N., Ozerov A. Mercury (Hg) in the near-ground atmosphere of active volcanic edifices in Kamchatka // 33rd International Geological Congress. Oslo, Norway. Abstracts. 2008.
Ozerova N.A., Ozerov A.Yu. Mercury in vapor-gas fumarole jets and products of their sedimentation at the Mutnovsky volcano // Commission on the chemistry of volcanic gases (CCVG) - IAVCEI. 11th Gas Workshop, Kamchatka, Russia. 1-10 September 2011. 2011. P. 36
Panov V.K., Slezin Yu.B. The mechanism of the lava field formation at the Predskazanny parasitic eruption (Klyuchevskoy volcano, 1983) // Volcanology and Seismology. 1988. V. 7. P. 321-335.
Panov V.K., Slezin Yu.B., Storcheus A.V. Mechanical properties of lava extruded in the 1983 Predskazanny eruption (Klyuchevskoi volcano) // Volcanology and Seismology. 1988. V. 7. P. 25-37.
Paris Raphaël, Switzer Adam D., Belousova Marina, Belousov Alexander, Ontowirjo Budianto, Whelley Patrick L., Ulvrova Martina Volcanic tsunami: a review of source mechanisms, past events and hazards in Southeast Asia (Indonesia, Philippines, Papua New Guinea) // Natural Hazards. 2014. V. 70. № 1. P. 447-470. doi:10.1007/s11069-013-0822-8.
Paris Raphaël, Wassmer Patrick, Lavigne Franck, Belousov Alexander, Belousova Marina, Iskandarsyah Yan, Benbakkar Mhammed, Ontowirjo Budianto, Mazzoni Nelly Coupling eruption and tsunami records: the Krakatau 1883 case study, Indonesia // Bulletin of Volcanology. 2014. V. 76. № 4. doi:10.1007/s00445-014-0814-x.


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