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dc.contributor.authorBüyük, Ersin
dc.date.accessioned2024-02-29T07:44:24Z
dc.date.available2024-02-29T07:44:24Z
dc.date.issued2024en_US
dc.identifier.citationErsin Büyük ebuyuk@gumushane.edu.tr orcid.org/0000-0001-9440-0918 Department of Geophysical Engineering, Faculty of Engineering and Natural Sciences, Gümüşhane University, Gümüşhane, Turkey TUBİTAK, Marmara Research Center, Earth Sciences Research Group, Gebze, Kocaeli, Turkeyen_US
dc.identifier.urihttps://onlinelibrary.wiley.com/doi/10.1111/1365-2478.13485
dc.identifier.urihttps://hdl.handle.net/20.500.12440/6167
dc.description.abstractParticle swarm optimization, one of the modern global optimization methods, is attracting widespread interest because it overcomes the difficulties of conventional inversion techniques, such as trapping at a local minimum and/or initial model dependence. The main characteristic of particle swarm optimization is the large search space of parameters, which in a sense allows the exploration of the entire objective function space if the input parameters are properly chosen. However, in the case of a high-dimensional model space, the numerical instability of the solution may increase and lead to unrealistic models and misinterpretations due to the sampling problem of particle swarm optimization. Therefore, smoothness-constrained regularization techniques used for the objective function or model reduction techniques are required to stabilize the solution. However, weighting and combining objective function terms is partly a subjective process, as the regularization parameter is generally chosen based on some kind of criteria of how the smoothing constraints affect the data misfits. This means that it cannot be completely predefined but needs to be adjusted during the inversion process, which begins with the response of an initial model. In this paper, a new modelling approach is proposed to obtain a smoothness-constrained model from magnetotelluric data utilizing multi-objective particle swarm optimization based on the Pareto optimality approach without using a regularization parameter and combining several objective function terms. The presented approach was verified on synthetic models and an application with field data set from the Çanakkale–Tuzla geothermal field in Turkey. Findings from these analyses confirm the usefulness of the method as a new approach for all constrained inversions of geophysical data without the need to combine the objective function terms weighted by a regularization parameter. © 2024 The Authors. Geophysical Prospecting published by John Wiley & Sons Ltd on behalf of European Association of Geoscientists & Engineers.en_US
dc.language.isoengen_US
dc.publisherJohn Wiley and Sons Incen_US
dc.relation.ispartofGeophysical Prospectingen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectelectromagnetical modellingen_US
dc.subjectmagnetotelluric modellingen_US
dc.subjectmulti-objective particle swarm optimizationen_US
dc.subjectPareto optimalityen_US
dc.subjectregularizationen_US
dc.subjectsmoothness constrainten_US
dc.titleA new method of smoothness-constrained magnetotelluric modelling with the utility of Pareto-optimal multi-objective particle swarm optimizationen_US
dc.typearticleen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.departmentFakülteler, Mühendislik ve Doğa Bilimleri Fakültesi, Jeofizik Mühendisliği Bölümüen_US
dc.authorid0000-0001-9440-0918en_US
dc.contributor.institutionauthorBüyük, Ersin
dc.identifier.doi10.1111/1365-2478.13485en_US
dc.authorwosidABB-1185-2020en_US
dc.authorscopusid57216708730en_US


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