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Implementation of the Kalman Filter for a Geostatistical Bivariate Spatiotemporal Estimation of Hydraulic Conductivity in Aquifers

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dc.contributor 271445 es_ES
dc.coverage.spatial Global es_ES
dc.creator Junez Ferreira, Hugo Enrique
dc.creator González Trinidad, Julian
dc.creator Junez Ferreira, Carlos Alberto
dc.creator Robles Rovelo, Cruz Octavio
dc.creator Herrera, G.S.
dc.creator Olmos Trujillo, Edith
dc.creator Bautista Capetillo, Carlos Francisco
dc.creator Contreras Rodríguez, Ada Rebeca
dc.creator Pacheco Guerrero, Anuard Isaac
dc.date.accessioned 2021-12-14T18:05:47Z
dc.date.available 2021-12-14T18:05:47Z
dc.date.issued 2020-11
dc.identifier info:eu-repo/semantics/publishedVersion es_ES
dc.identifier.issn 2073-4441 es_ES
dc.identifier.uri http://ricaxcan.uaz.edu.mx/jspui/handle/20.500.11845/2877
dc.description.abstract The estimation of the hydraulic parameters of an aquifer such as the hydraulic conductivity is somehow complicated due to its heterogeneity, on the other hand field and laboratory tests are both time consuming and costly. The use of geostatistical-based techniques for data assimilation could represent an alternative tool that allows the use of space-time aquifer behaviour to characterize hydraulic conductivity heterogeneity. In this paper, a spatiotemporal bivariate methodology was implemented combining historical hydraulic head data with hydraulic conductivity sparse data in order to obtain an estimate of the spatial distribution of the latter variable. This approach takes advantage of the correlation between the hydraulic conductivity (K) and the hydraulic head (H) behaviour through time. In order to evaluate this approach, a synthetic experiment was constructed through a transitory numerical flow-model that simulates hydraulic head values in a horizontally-heterogeneous aquifer. Geostatistical tools were used to describe the correlation between simulated spatiotemporal data of hydraulic head and the spatial distribution of the hydraulic conductivity in a group of model nodes. Subsequently, the Kalman filter was used to estimate the hydraulic conductivity values at nonsampled sites. The results showed acceptable differences between estimated and synthetic hydraulic conductivity data, with low estimate error variances (predominating the 1 m2/day2 value for K for all the cases, however, the smallest number of cells with values above 2 m2/day2 correspond to the bivariate spatiotemporal case) and the best agreement between the estimated errors and the selected model variance (SMSE values of 0.574 and 0.469) were found for the bivariate cases, which suggests that the implemented methodology could be used for reducing calibration efforts, particularly when the hydraulic parameters data are scarce. es_ES
dc.language.iso eng es_ES
dc.publisher MDPI es_ES
dc.relation https://www.mdpi.com/2073-4441/12/11/3136 es_ES
dc.relation.uri generalPublic es_ES
dc.rights Attribution-NonCommercial-ShareAlike 3.0 United States *
dc.rights.uri http://creativecommons.org/licenses/by-nc-sa/3.0/us/ *
dc.source Water 2020, 12, 3136 es_ES
dc.subject.classification CIENCIAS FISICO MATEMATICAS Y CIENCIAS DE LA TIERRA [1] es_ES
dc.subject.other hydraulic conductivity es_ES
dc.subject.other groundwater numerical modelling es_ES
dc.subject.other bivariate spatiotemporal geostatistics es_ES
dc.subject.other Kalman filter es_ES
dc.title Implementation of the Kalman Filter for a Geostatistical Bivariate Spatiotemporal Estimation of Hydraulic Conductivity in Aquifers es_ES
dc.type info:eu-repo/semantics/article es_ES


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