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dc.contributor.authorDølven, Knut Ola
dc.contributor.authorVierinen, Juha
dc.contributor.authorGrilli, Roberto
dc.contributor.authorTriest, Jack
dc.contributor.authorFerré, Benedicte
dc.date.accessioned2022-08-30T12:59:14Z
dc.date.available2022-08-30T12:59:14Z
dc.date.issued2022-08-11
dc.description.abstractAccurate high-resolution measurements are essential to improve our understanding of environmental processes. Several chemical sensors relying on membrane separation extraction techniques have slow response times due to a dependence on equilibrium partitioning across the membrane separating the measured medium (i.e., a measuring chamber) and the medium of interest (i.e., a solvent). We present a new technique for deconvolving slow-sensorresponse signals using statistical inverse theory; applying a weighted linear least-squares estimator with the growth law as a measurement model. The solution is regularized using model sparsity, assuming changes in the measured quantity occur with a certain time step, which can be selected based on domain-specific knowledge or L-curve analysis. The advantage of this method is that it (1) models error propagation, providing an explicit uncertainty estimate of the responsetime-corrected signal; (2) enables evaluation of the solution self consistency; and (3) only requires instrument accuracy, response time, and data as input parameters. Functionality of the technique is demonstrated using simulated, laboratory, and field measurements. In the field experiment, the coefficient of determination (<i>R</i><sup>2</sup>) of a slow-response methane sensor in comparison with an alternative fast-response sensor significantly improved from 0.18 to 0.91 after signal deconvolution. This shows how the proposed method can open up a considerably wider set of applications for sensors and methods suffering from slow response times due to a reliance on the efficacy of diffusion processes.en_US
dc.identifier.citationDølven KO, Vierinen J, Grilli R, Triest J, Ferré B. Response time correction of slow-response sensor data by deconvolution of the growth-law equation. Geoscientific Instrumentation, Methods and Data Systems. 2022;11:292-306en_US
dc.identifier.cristinIDFRIDAID 2037379
dc.identifier.doi10.5194/gi-11-293-2022
dc.identifier.issn2193-0856
dc.identifier.issn2193-0864
dc.identifier.urihttps://hdl.handle.net/10037/26477
dc.language.isoengen_US
dc.publisherEuropean Geosciences Unionen_US
dc.relation.journalGeoscientific Instrumentation, Methods and Data Systems
dc.relation.projectIDNorges forskningsråd: 223259en_US
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/FP7/713619/EU/OCEAN in-situ Isotope and Dissolved gas sensing/OCEAN-IDsen_US
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/FP7/291062/EU/Innovative Concepts for Extracting climate and atmospheric composition records from polar ice cores using new LASER Sensors/ICE&LASERS/en_US
dc.rights.accessRightsopenAccessen_US
dc.rights.holderCopyright 2022 The Author(s)en_US
dc.titleResponse time correction of slow-response sensor data by deconvolution of the growth-law equationen_US
dc.type.versionpublishedVersionen_US
dc.typeJournal articleen_US
dc.typeTidsskriftartikkelen_US
dc.typePeer revieweden_US


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