Gravity field modelling for the Hannover 10 m atom interferometer

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dc.identifier.uri http://dx.doi.org/10.15488/10717
dc.identifier.uri https://www.repo.uni-hannover.de/handle/123456789/10795
dc.contributor.author Schilling, Manuel
dc.contributor.author Wodey, Étienne
dc.contributor.author Timmen, Ludger
dc.contributor.author Tell, Dorothee
dc.contributor.author Zipfel, Klaus H.
dc.contributor.author Schlippert, Dennis
dc.contributor.author Schubert, Christian
dc.contributor.author Rasel, Ernst M.
dc.contributor.author Müller, Jürgen
dc.date.accessioned 2021-03-31T06:01:23Z
dc.date.available 2021-03-31T06:01:23Z
dc.date.issued 2020
dc.identifier.citation Schilling, M.; Wodey, É.; Timmen, L.; Tell, D.; Zipfel, K.H. et al.: Gravity field modelling for the Hannover 10 m atom interferometer. In: Journal of Geodesy 94 (2020), Nr. 12, 122. DOI: https://doi.org/10.1007/s00190-020-01451-y
dc.description.abstract Absolute gravimeters are used in geodesy, geophysics and physics for a wide spectrum of applications. Stable gravimetric measurements over timescales from several days to decades are required to provide relevant insight into geophysical processes. Users of absolute gravimeters participate in comparisons with a metrological reference in order to monitor the temporal stability of the instruments and determine the bias to that reference. However, since no measurement standard of higher-order accuracy currently exists, users of absolute gravimeters participate in key comparisons led by the International Committee for Weights and Measures. These comparisons provide the reference values of highest accuracy compared to the calibration against a single gravimeter operated at a metrological institute. The construction of stationary, large-scale atom interferometers paves the way for a new measurement standard in absolute gravimetry used as a reference with a potential stability up to 1nm/s2 at 1 s integration time. At the Leibniz University Hannover, we are currently building such a very long baseline atom interferometer with a 10-m-long interaction zone. The knowledge of local gravity and its gradient along and around the baseline is required to establish the instrument’s uncertainty budget and enable transfers of gravimetric measurements to nearby devices for comparison and calibration purposes. We therefore established a control network for relative gravimeters and repeatedly measured its connections during the construction of the atom interferometer. We additionally developed a 3D model of the host building to investigate the self-attraction effect and studied the impact of mass changes due to groundwater hydrology on the gravity field around the reference instrument. The gravitational effect from the building 3D model is in excellent agreement with the latest gravimetric measurement campaign which opens the possibility to transfer gravity values with an uncertainty below the 10nm/s2 level. © 2020, The Author(s). eng
dc.language.iso eng
dc.publisher Berlin [u.a.] : Springer
dc.relation.ispartofseries Journal of Geodesy 94 (2020), Nr. 12
dc.rights CC BY 4.0 Unported
dc.rights.uri https://creativecommons.org/licenses/by/4.0/
dc.subject absolute gravimetry eng
dc.subject atom interferometry eng
dc.subject gravimeter reference eng
dc.subject gravity acceleration eng
dc.subject.ddc 550 | Geowissenschaften ger
dc.subject.ddc 530 | Physik ger
dc.title Gravity field modelling for the Hannover 10 m atom interferometer
dc.type Article
dc.type Text
dc.relation.essn 1432-1394
dc.relation.issn 0007-4632
dc.relation.issn 0949-7714
dc.relation.doi https://doi.org/10.1007/s00190-020-01451-y
dc.bibliographicCitation.issue 12
dc.bibliographicCitation.volume 94
dc.bibliographicCitation.firstPage 122
dc.description.version publishedVersion
tib.accessRights frei zug�nglich


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