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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Online Access: | https://doi.org/10.1029/2019EA001007 |
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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 |
work_keys_str_mv |
AT hhguliyev onceagainonpreliminaryreferenceearthmodel AT rjjavanshir onceagainonpreliminaryreferenceearthmodel |
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