The Method of Fundamental Solutions for Solving the Inverse Problem of Magma Source Characterization

Volcano is one of the geodynamic phenomena causing irreparable damages. As lava accumulates in reservoir and then comes to the surface, geometry of the source can be used to predict volcanic eruptions. In this study, using the inverse method of fundamental solutions (MFS) and taking into account the...

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Main Authors: Maryam Yazdanparast, Behzad Voosoghi, Farshid Mossaiby
Format: Article
Language:English
Published: Taylor & Francis Group 2019-01-01
Series:Geomatics, Natural Hazards & Risk
Subjects:
Online Access:http://dx.doi.org/10.1080/19475705.2018.1547324
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spelling doaj-6c56ff978c3148ca976c0e072424c1012020-11-25T02:19:42ZengTaylor & Francis GroupGeomatics, Natural Hazards & Risk1947-57051947-57132019-01-0110179781910.1080/19475705.2018.15473241547324The Method of Fundamental Solutions for Solving the Inverse Problem of Magma Source CharacterizationMaryam Yazdanparast0Behzad Voosoghi1Farshid Mossaiby2K. N. Toosi University of TechnologyK. N. Toosi University of TechnologyUniversity of IsfahanVolcano is one of the geodynamic phenomena causing irreparable damages. As lava accumulates in reservoir and then comes to the surface, geometry of the source can be used to predict volcanic eruptions. In this study, using the inverse method of fundamental solutions (MFS) and taking into account the effect of topography, the geometry of the source including shape, depth and centre position of the magma tank is estimated. The MFS is a numerical method for solving boundary value problems with known partial differential equations. The displacement field calculated in the previous studies using InSAR for deflation mode of Cerro Blanco volcano was utilized in this study. It was estimated that the magma source of the volcano is a sphere with a radius of 1 km located at a horizontal position of () km and the depth of about 10 km from the summit with respect to the defined coordinate system. This finding is consistent with that of recent studies in which inversion of InSAR data was used to analyse the geometry of the magma source. The RMSE between the deformation fields of the magma source calculated in the previous studies and that of the study herein via MFS was approximately 3 mm.http://dx.doi.org/10.1080/19475705.2018.1547324magma sourceinverse mfsboundary value problemmeshless methodvolcano
collection DOAJ
language English
format Article
sources DOAJ
author Maryam Yazdanparast
Behzad Voosoghi
Farshid Mossaiby
spellingShingle Maryam Yazdanparast
Behzad Voosoghi
Farshid Mossaiby
The Method of Fundamental Solutions for Solving the Inverse Problem of Magma Source Characterization
Geomatics, Natural Hazards & Risk
magma source
inverse mfs
boundary value problem
meshless method
volcano
author_facet Maryam Yazdanparast
Behzad Voosoghi
Farshid Mossaiby
author_sort Maryam Yazdanparast
title The Method of Fundamental Solutions for Solving the Inverse Problem of Magma Source Characterization
title_short The Method of Fundamental Solutions for Solving the Inverse Problem of Magma Source Characterization
title_full The Method of Fundamental Solutions for Solving the Inverse Problem of Magma Source Characterization
title_fullStr The Method of Fundamental Solutions for Solving the Inverse Problem of Magma Source Characterization
title_full_unstemmed The Method of Fundamental Solutions for Solving the Inverse Problem of Magma Source Characterization
title_sort method of fundamental solutions for solving the inverse problem of magma source characterization
publisher Taylor & Francis Group
series Geomatics, Natural Hazards & Risk
issn 1947-5705
1947-5713
publishDate 2019-01-01
description Volcano is one of the geodynamic phenomena causing irreparable damages. As lava accumulates in reservoir and then comes to the surface, geometry of the source can be used to predict volcanic eruptions. In this study, using the inverse method of fundamental solutions (MFS) and taking into account the effect of topography, the geometry of the source including shape, depth and centre position of the magma tank is estimated. The MFS is a numerical method for solving boundary value problems with known partial differential equations. The displacement field calculated in the previous studies using InSAR for deflation mode of Cerro Blanco volcano was utilized in this study. It was estimated that the magma source of the volcano is a sphere with a radius of 1 km located at a horizontal position of () km and the depth of about 10 km from the summit with respect to the defined coordinate system. This finding is consistent with that of recent studies in which inversion of InSAR data was used to analyse the geometry of the magma source. The RMSE between the deformation fields of the magma source calculated in the previous studies and that of the study herein via MFS was approximately 3 mm.
topic magma source
inverse mfs
boundary value problem
meshless method
volcano
url http://dx.doi.org/10.1080/19475705.2018.1547324
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