Aarhus University Seal

Heterodox transients in time-domain-induced polarization

Research output: Contribution to journal/Conference contribution in journal/Contribution to newspaperJournal articleResearchpeer-review


Negative-induced polarization (IP) time-domain transients, sign-changing or nonmonotonically decaying transients, are currently often considered as measurement errors and are removed in data processing. These transients, here called heterodox in the sense of other than generally accepted signals, might originate from measurement errors, inductive effects, or poor signal processing, but synthetic modeling and field measurements indicate that these transients are physically possible. A simple theoretical explanation of the basic mechanism for their origin can be found through the superposition of contributions from regions with different sensitivities, and such heterodox transients can be identified through the processing of full-waveform IP data. A mathematical classification of orthodox and heterodox IP transients into six different types is evaluated based on the temporal development of the sign of their amplitude and derivative. The basic mechanism for IP transients with heterodox shapes is further investigated by considering the subsurface Cole-Cole parameter sensitivities and time-varying IP potential for 2D synthetic models. The time-domain forward response and sensitivities are computed through a time transformation that accounts for the current waveform. This approach allows for quantitative unbiased estimates of the time-domain transients and sensitivities, different from the estimates obtained when using multiple direct-current forward computations, as is often done in the inversion of time-domain IP data. Time-domain IP transients may differ from the traditionally expected decaying-like transients when the electrode geometry has IP potential sensitivities with different signs for areas with different IP parameters. Hence, previously disregarded IP transients containing valuable information of the subsurface can be kept for inversion and contribute to the final parameter distribution. An increased understanding of theoretically possible IP transients makes way for more accurate processing of data in the future, reducing the time and resources needed for spectral inversion of time-domain data.

Original languageEnglish
Pages (from-to)E35-E47
Publication statusPublished - 1 Jan 2022

Bibliographical note

Funding Information:
Funding for the work was provided by Formas — The Swedish Research Council for Environment, Agricultural Sciences and Spatial Planning (ref. 2012-1931), BeFo — Swedish Rock Engineering Research Foundation (ref. 331), and SBUF — The Development Fund of the Swedish Construction Industry (ref. 13232). The project is part of the Geoinfra-TRUST framework (http://trust-geoinfra.se/). The Innovation Fund Denmark provided additional funding via the GEOCON project (http://www.geocon.env.dtu.dk/). Furthermore, the work is jointly funded by the European Union, Eurostars Programme, Central Region Denmark, Innovation Fund Denmark, and The Swedish innovation agency Vinnova under the project “Mapping Geology in Cities” (E10096 MAGIC).

Publisher Copyright:
© 2022 Society of Exploration Geophysicists.

    Research areas

  • induced polarization, signal processing, time domain

See relations at Aarhus University Citationformats

ID: 228150426