Unveiling Informational Properties of the Chen-Ouillon-Sornette Seismo-Electrical Model

The seismo-electrical coupling is critical to understand the mechanism of geoelectrical precursors to earthquakes. A novel seismo-electrical model, called Chen–Ouillon–Sornette (COS) model, has been developed by combining the Burridge–Knopoff spring-block system with the mechanisms of stress-activat...

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Main Authors: Hong-Jia Chen, Luciano Telesca, Michele Lovallo, Chien-Chih Chen
Format: Article
Language:English
Published: MDPI AG 2021-03-01
Series:Entropy
Subjects:
Online Access:https://www.mdpi.com/1099-4300/23/3/337
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spelling doaj-ed0f451f7f974fc1aa7349ff064b0e052021-03-13T00:04:19ZengMDPI AGEntropy1099-43002021-03-012333733710.3390/e23030337Unveiling Informational Properties of the Chen-Ouillon-Sornette Seismo-Electrical ModelHong-Jia Chen0Luciano Telesca1Michele Lovallo2Chien-Chih Chen3Department of Earth Sciences, National Central University, Taoyuan 32001, TaiwanInstitute of Methodologies for Environmental Analysis, National Research Council, 85050 Tito (PZ), ItalyARPAB, 85100 Potenza, ItalyDepartment of Earth Sciences, National Central University, Taoyuan 32001, TaiwanThe seismo-electrical coupling is critical to understand the mechanism of geoelectrical precursors to earthquakes. A novel seismo-electrical model, called Chen–Ouillon–Sornette (COS) model, has been developed by combining the Burridge–Knopoff spring-block system with the mechanisms of stress-activated charge carriers (i.e., electrons and holes) and pressure-stimulated currents. Such a model, thus, can simulate fracture-induced electrical signals at a laboratory scale or earthquake-related geoelectrical signals at a geological scale. In this study, by using information measures of time series analysis, we attempt to understand the influence of diverse electrical conditions on the characteristics of the simulated electrical signals with the COS model. We employ the Fisher–Shannon method to investigate the temporal dynamics of the COS model. The result showed that the electrical parameters of the COS model, particularly for the capacitance and inductance, affect the levels of the order/disorder in the electrical time series. Compared to the field observations, we infer that the underground electrical condition has become larger capacitance or smaller inductance in seismogenic processes. Accordingly, this study may provide a better understanding of the mechanical–electrical coupling of the earth’s crust.https://www.mdpi.com/1099-4300/23/3/337Fisher informationShannon entropyseismo-electrical modelspring-block modelRLC circuit
collection DOAJ
language English
format Article
sources DOAJ
author Hong-Jia Chen
Luciano Telesca
Michele Lovallo
Chien-Chih Chen
spellingShingle Hong-Jia Chen
Luciano Telesca
Michele Lovallo
Chien-Chih Chen
Unveiling Informational Properties of the Chen-Ouillon-Sornette Seismo-Electrical Model
Entropy
Fisher information
Shannon entropy
seismo-electrical model
spring-block model
RLC circuit
author_facet Hong-Jia Chen
Luciano Telesca
Michele Lovallo
Chien-Chih Chen
author_sort Hong-Jia Chen
title Unveiling Informational Properties of the Chen-Ouillon-Sornette Seismo-Electrical Model
title_short Unveiling Informational Properties of the Chen-Ouillon-Sornette Seismo-Electrical Model
title_full Unveiling Informational Properties of the Chen-Ouillon-Sornette Seismo-Electrical Model
title_fullStr Unveiling Informational Properties of the Chen-Ouillon-Sornette Seismo-Electrical Model
title_full_unstemmed Unveiling Informational Properties of the Chen-Ouillon-Sornette Seismo-Electrical Model
title_sort unveiling informational properties of the chen-ouillon-sornette seismo-electrical model
publisher MDPI AG
series Entropy
issn 1099-4300
publishDate 2021-03-01
description The seismo-electrical coupling is critical to understand the mechanism of geoelectrical precursors to earthquakes. A novel seismo-electrical model, called Chen–Ouillon–Sornette (COS) model, has been developed by combining the Burridge–Knopoff spring-block system with the mechanisms of stress-activated charge carriers (i.e., electrons and holes) and pressure-stimulated currents. Such a model, thus, can simulate fracture-induced electrical signals at a laboratory scale or earthquake-related geoelectrical signals at a geological scale. In this study, by using information measures of time series analysis, we attempt to understand the influence of diverse electrical conditions on the characteristics of the simulated electrical signals with the COS model. We employ the Fisher–Shannon method to investigate the temporal dynamics of the COS model. The result showed that the electrical parameters of the COS model, particularly for the capacitance and inductance, affect the levels of the order/disorder in the electrical time series. Compared to the field observations, we infer that the underground electrical condition has become larger capacitance or smaller inductance in seismogenic processes. Accordingly, this study may provide a better understanding of the mechanical–electrical coupling of the earth’s crust.
topic Fisher information
Shannon entropy
seismo-electrical model
spring-block model
RLC circuit
url https://www.mdpi.com/1099-4300/23/3/337
work_keys_str_mv AT hongjiachen unveilinginformationalpropertiesofthechenouillonsornetteseismoelectricalmodel
AT lucianotelesca unveilinginformationalpropertiesofthechenouillonsornetteseismoelectricalmodel
AT michelelovallo unveilinginformationalpropertiesofthechenouillonsornetteseismoelectricalmodel
AT chienchihchen unveilinginformationalpropertiesofthechenouillonsornetteseismoelectricalmodel
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