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dc.contributor.authorZikmund A.
dc.contributor.authorJanošek M.
dc.contributor.authorUlvr M.
dc.contributor.authorKupec J.
dc.date.accessioned2024-06-18T08:58:11Z
dc.date.available2024-06-18T08:58:11Z
dc.date.issued2015
dc.identifierV3S-224304
dc.identifier.citationZIKMUND, A., et al. Precise calibration method for triaxial magnetometers not requiring Earth's field compensation. IEEE Transactions on Instrumentation and Measurement. 2015, 64(5), 1250-1255. ISSN 0018-9456. DOI 10.1109/TIM.2015.2395531.
dc.identifier.issn0018-9456 (print)
dc.identifier.issn1557-9662 (online)
dc.identifier.urihttp://hdl.handle.net/10467/114517
dc.description.abstractA calibration procedure for calibrations of triaxial magnetometers is presented. The procedure uses a triaxial Helmholtz coil system and an Overhauser scalar magnetometer and is performed in the an Earth's field range. The triaxial coils are firstly calibrated with the help of the Overhauser magnetometer and subsequently a calibration of a digital triaxial magnetometer calibration is performed. As opposed to other approaches, neither Earth’s field nulling system is needed, nor are movements of the magnetometer are needed. A real calibration test was carried out and the extended uncertainty was better than 430 ppm in sensitivity and 0.06 degrees in orthogonality.eng
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.publisherIEEE
dc.relation.ispartofIEEE Transactions on Instrumentation and Measurement
dc.subjectcalibrationeng
dc.subjectmagnetometereng
dc.subjectcoileng
dc.titlePrecise calibration method for triaxial magnetometers not requiring Earth's field compensationeng
dc.typečlánek v časopisecze
dc.typejournal articleeng
dc.identifier.doi10.1109/TIM.2015.2395531
dc.relation.projectidinfo:eu-repo/grantAgreement/Technology Agency of the Czech Republic/TA/TA01010298/CZ/Fluxgate gradiometer for space application/
dc.rights.accessopenAccess
dc.identifier.wos000352492900018
dc.type.statusPeer-reviewed
dc.type.versionacceptedVersion
dc.identifier.scopus2-s2.0-85027946105


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