Once Again on Preliminary Reference Earth Model

Abstract We studied the isotropic ball using data of Preliminary Reference Earth Model (PREM). It is shown that such a ball should be either destructed or gone into a more stable equilibrium state with uneven distributed deformation under thermobaric condition of the inner core. Body elastic waves w...

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Main Authors: H. H. Guliyev, R. J. Javanshir
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2020-03-01
Series:Earth and Space Science
Subjects:
Online Access:https://doi.org/10.1029/2019EA001007
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spelling doaj-e2a8e6e8409e49128c3d66655e33db7d2020-11-25T02:01:48ZengAmerican Geophysical Union (AGU)Earth and Space Science2333-50842020-03-0173n/an/a10.1029/2019EA001007Once Again on Preliminary Reference Earth ModelH. H. Guliyev0R. J. Javanshir1Institute of Geology and Geophysics Azerbaijan National Academy of Sciences Baku AzerbaijanInstitute of Geology and Geophysics Azerbaijan National Academy of Sciences Baku AzerbaijanAbstract We studied the isotropic ball using data of Preliminary Reference Earth Model (PREM). It is shown that such a ball should be either destructed or gone into a more stable equilibrium state with uneven distributed deformation under thermobaric condition of the inner core. Body elastic waves with real velocities cannot propagate in it. This manuscript is devoted to study the situation from the standpoint of nonlinear geomechanics. A number of necessary principles of Mechanics of Deformable Solid Body (MDSB) is given at the beginning of the analysis. A brief review of the published latest experimental work is performed. It is established that proper attention to the role of the MDSB principles in micro‐scale (nano) experiments of the physical level has not been given. Deformation properties of solid bodies are emphasized in microscale and macroscale. Application of linear acoustoelasticity and extrapolation of Birch's linear law of the inner core and use of an idea on variability of elasticity moduli with the increase of pressure and temperature have contributed to obtained pseudo data for the geological medium of the Earth's core instead of linear data on the physicomechanical properties. It is proposed that parallel to elimination of the indicated disadvantages, collection, processing and interpretation should be performed using nonclassically linearized approach. This set of necessary actions is offered as the “key” of geomechanical analysis. The proper application will allow conducting similar analysis concerning other solid‐state structures of the Earth.https://doi.org/10.1029/2019EA001007Earth's inner coregeomechanicsnonlinear elastodynamicsBirchs's diagramtheoretical models of the Earth
collection DOAJ
language English
format Article
sources DOAJ
author H. H. Guliyev
R. J. Javanshir
spellingShingle H. H. Guliyev
R. J. Javanshir
Once Again on Preliminary Reference Earth Model
Earth and Space Science
Earth's inner core
geomechanics
nonlinear elastodynamics
Birchs's diagram
theoretical models of the Earth
author_facet H. H. Guliyev
R. J. Javanshir
author_sort H. H. Guliyev
title Once Again on Preliminary Reference Earth Model
title_short Once Again on Preliminary Reference Earth Model
title_full Once Again on Preliminary Reference Earth Model
title_fullStr Once Again on Preliminary Reference Earth Model
title_full_unstemmed Once Again on Preliminary Reference Earth Model
title_sort once again on preliminary reference earth model
publisher American Geophysical Union (AGU)
series Earth and Space Science
issn 2333-5084
publishDate 2020-03-01
description Abstract We studied the isotropic ball using data of Preliminary Reference Earth Model (PREM). It is shown that such a ball should be either destructed or gone into a more stable equilibrium state with uneven distributed deformation under thermobaric condition of the inner core. Body elastic waves with real velocities cannot propagate in it. This manuscript is devoted to study the situation from the standpoint of nonlinear geomechanics. A number of necessary principles of Mechanics of Deformable Solid Body (MDSB) is given at the beginning of the analysis. A brief review of the published latest experimental work is performed. It is established that proper attention to the role of the MDSB principles in micro‐scale (nano) experiments of the physical level has not been given. Deformation properties of solid bodies are emphasized in microscale and macroscale. Application of linear acoustoelasticity and extrapolation of Birch's linear law of the inner core and use of an idea on variability of elasticity moduli with the increase of pressure and temperature have contributed to obtained pseudo data for the geological medium of the Earth's core instead of linear data on the physicomechanical properties. It is proposed that parallel to elimination of the indicated disadvantages, collection, processing and interpretation should be performed using nonclassically linearized approach. This set of necessary actions is offered as the “key” of geomechanical analysis. The proper application will allow conducting similar analysis concerning other solid‐state structures of the Earth.
topic Earth's inner core
geomechanics
nonlinear elastodynamics
Birchs's diagram
theoretical models of the Earth
url https://doi.org/10.1029/2019EA001007
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