HomeVideoSergey Samoylenko | Russian Academy of Sciences | Russia | Earth Science 2015 | Conference Series LLC

Sergey Samoylenko | Russian Academy of Sciences | Russia | Earth Science 2015 | Conference Series LLC



Sergey Samoylenko | Russian Academy of Sciences | Russia | Earth Science 2015 | Conference Series LLC

4th International Conference on Earth Science and Climate Change June 16-18, 2015 Melia Alicante, Alicante, Spain

Scientific Talk On: On formal classification of volcanic eruption types and regimes based on the similarity theory

Click here for Abstract and Biography: http://earthscience.conferenceseries.com/abstract/2015/on-formal-classification-of-volcanic-eruption-types-and-regimes-based-on-the-similarity-theory

“Biography
Sergey B Samoylenko has completed his PhD at the age of 27 years from Yeungnam University (South Korea). He is the senior researcher at Institute of Volcanology and Seimology FEB RAS, Kamchatka, Russia, st+A55udying the active volcanism and the dynamics of volcanic eruption. He has published more than 10 papers in reputed journals and has been serving as an editorial board member of repute.

Abstract
Application of the similarity theory principles and dimentional analysis, supplemented by some orinal approaches, suggests the way to acheve following goals which are significant for understanding and modelling of the volcanic process. 1. To introduce and to define more exactly the formal classification of volcanic eruption types in the same way as it is done for the flow regimes in terms of dimensionless numbers in fluid mechanics. 2. To avoid the necessity of knowing the exact values of physical parameters which are hard or even impossible to measure (viscosity, the conduit size etc.) in modelling the volcanic processes. Instead the few number of nondimentional similarity criteria, specific to volcanology, is suggested to be used. The quanities of similarity criteria could be estimated according to observable qualitative characteristics of the process regime to be modelled. 3. To bring the variety of existing mathematical and physical models of volcanic eruptions to a uniform system. It allows to compare different models and, mostly important, to outline their applicability limits.A65”

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