Rodyti trumpą aprašą

dc.contributor.authorPuzienė, Rūta
dc.contributor.authorAnikėnienė, Asta
dc.date.accessioned2023-12-22T07:06:13Z
dc.date.available2023-12-22T07:06:13Z
dc.date.issued2023
dc.identifier.issn1866-7511
dc.identifier.urihttps://etalpykla.vilniustech.lt/xmlui/handle/123456789/153602
dc.description.abstractThe levelling network is arranged in separate lines that together form levelling polygons. When determining the vertical movements of the Earth’s surface based on the results of levelling measurements, the results are obtained only at the location of the geodetic network. During the compilation of the vertical movements of the Earth’s surface, a significant part of the studied area lacks measurement-based results, and the movement values are obtained by interpolation. Therefore, measurements of movement obtained inside levelling polygons are relatively inaccurate, and active centres of movement are concentrated only on the levelling lines. The present article introduces a methodology that allows determining the vertical surface movements in the entire area. The methodology holistically employs statistical methods, geoindexes, and levelling measurement data. Movement values are calculated for points evenly spaced throughout the entire area. The vertical movement map compiled based on this methodology is not subject to such significant influence by the interpretations of the interpolation algorithm, moreover, it avoids the concentration of movements in the levelling lines. During the study, three maps of vertical movements of the Earth’s surface are compiled: one is created on the basis of the levelling results, and two other maps — using the proposed methodology. The comparison of the maps reveals that the main rising/sinking tendencies of the Earth’s surface match, and simultaneously the concentration of movements in geodetic points is avoided.eng
dc.formatPDF
dc.format.extentp. 1-22
dc.format.mediumtekstas / txt
dc.language.isoeng
dc.relation.isreferencedbyDimensions
dc.relation.isreferencedbyGeoRef
dc.relation.isreferencedbyGEOBASE
dc.source.urihttps://link.springer.com/article/10.1007/s12517-023-11527-6
dc.titleEstimating vertical movement of the earth’s crust in Lithuania using different methods
dc.typeStraipsnis kitoje DB / Article in other DB
dcterms.references41
dc.type.pubtypeS3 - Straipsnis kitoje DB / Article in other DB
dc.contributor.institutionVilniaus Gedimino technikos universitetas
dc.contributor.institutionVilniaus technologijų ir dizaino kolegija
dc.contributor.facultyAplinkos inžinerijos fakultetas / Faculty of Environmental Engineering
dc.subject.researchfieldT 010 - Matavimų inžinerija / Measurement engineering
dc.subject.vgtuprioritizedfieldsSD05 - Geodezinės technologijos / Geodetic technologies
dc.subject.ltspecializationsL104 - Nauji gamybos procesai, medžiagos ir technologijos / New production processes, materials and technologies
dc.subject.envertical earth’s crust movements
dc.subject.encrustal rising/sinking
dc.subject.enprecise levelling
dc.subject.encorrelation analysis
dc.subject.enforecast applying regressive models
dcterms.sourcetitleArabian journal of geosciences
dc.description.issueiss. 7
dc.description.volumevol. 16
dc.publisher.nameSpringer Heidelberg
dc.publisher.cityHeidelberg
dc.identifier.doiCrossref citavimo ID
dc.identifier.doi10.1007/s12517-023-11527-6
dc.identifier.elaba176765791


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