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dc.contributor.authorMacchioli Grande, Franco-
dc.contributor.authorZyserman, Fabio-
dc.contributor.authorMonachesi, Leonardo Bruno-
dc.contributor.authorJouniaux, Laurence-
dc.contributor.authorRosas Carbajal, Marina-
dc.date.accessioned2020-09-10T16:05:25Z-
dc.date.available2020-09-10T16:05:25Z-
dc.date.issued2020-
dc.identifier.citationMacchioli Grande, F., Zyserman, F., Monachesi, L.B., Jouniaux, L. and Rosas Carbajal, M., (2020). Bayesian inversion of joint SH seismic and seismoelectric data to infer glacier system properties. Geophysical prospecting; European Association of Geoscientists & Engineers; 68 (5); 1633-1656es_ES
dc.identifier.issn0016-8025es_ES
dc.identifier.issn1365-2478es_ES
dc.identifier.urihttps://onlinelibrary.wiley.com/doi/abs/10.1111/1365-2478.12940-
dc.identifier.urihttp://rid.unrn.edu.ar/handle/20.500.12049/5796-
dc.description.abstractIn glacial studies, properties such as glacier thickness and the basement permeability and porosity are key to understand the hydrological and mechanical behaviour of the system. The seismoelectric method could potentially be used to determine key properties of glacial environments. Here we analytically model the generation of seismic and seismoelectric signals by means of a shear horizontal seismic wave source on top of a glacier overlying a porous basement. Considering a one-dimensional setting, we compute the seismic waves and the electrokinetically induced electric field. We then analyse the sensitivity of the seismic and electromagnetic data to relevant model parameters, namely depth of the glacier bottom, porosity, permeability, shear modulus and saturating water salinity of the glacier basement. Moreover, we study the possibility of inferring these key parameters from a set of very low noise synthetic data, adopting a Bayesian framework to pay particular attention to the uncertainty of the model parameters mentioned above. We tackle the resolution of the probabilistic inverse problem with two strategies: (1) we compute the marginal posterior distributions of each model parameter solving multidimensional integrals numerically and (2) we use a Markov chain Monte Carlo algorithm to retrieve a collection of model parameters that follows the posterior probability density function of the model parameters, given the synthetic data set. Both methodologies are able to obtain the marginal distributions of the parameters and estimate their mean and standard deviation. The Markov chain Monte Carlo algorithm performs better in terms of numerical stability and number of iterations needed to characterize the distributions. The inversion of seismic data alone is not able to constrain the values of porosity and permeability further than the prior distribution. In turn, the inversion of the electric data alone, and the joint inversion of seismic and electric data are useful to constrain these parameters as well as other glacial system properties. Furthermore, the joint inversion reduces the uncertainty of the model parameters estimates and provides more accurate results.es_ES
dc.format.extentp. 1633–1656es_ES
dc.format.mediumdigitales_ES
dc.language.isoenes_ES
dc.publisherEuropean Association of Geoscientists & Engineerses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/-
dc.titleBayesian inversion of joint SH seismic and seismoelectric data to infer glacier system propertieses_ES
dc.typeArticuloes_ES
dc.rights.licenseCreative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)-
dc.description.filiationMacchioli Grande, Franco. CONICET, Facultad de Ciencias Astronómicas y Geofísicas, Universidad Nacional de La Plata; Argentina.es_ES
dc.description.filiationZyserman, Fabio. CONICET, Facultad de Ciencias Astronómicas y Geofísicas, Universidad Nacional de La Plata; Argentina.es_ES
dc.description.filiationMonachesi, Leonardo. Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Río Negro, Argentina.es_ES
dc.description.filiationJouniaux, Laurence. Institut de Physique du Globe de Strasbourg (UMR 7516), Université de Strasbourg et CNRS, Strasbourg; Francia.es_ES
dc.description.filiationRosas Carbajal, Marina. Institut de Physique du Globe de Paris; Francia.es_ES
dc.subject.keywordElectromagneticses_ES
dc.subject.keywordInversiones_ES
dc.subject.keywordModellinges_ES
dc.subject.keywordParameter Estimationes_ES
dc.subject.keywordSeismicses_ES
dc.type.versioninfo:eu-repo/semantics/publishedVersiones_ES
dc.subject.materia.::Ciencias Exactas y Naturaleses_ES
dc.origin.lugarDesarrolloUniversidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología.es_ES
dc.relation.journalissue68 (5)es_ES
dc.description.reviewtruees_ES
dc.description.resumen-es_ES
dc.identifier.doihttps://doi.org/10.1111/1365-2478.12940-
dc.relation.journalTitleGeophysical Prospectinges_ES
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