Electrical resistivity tomography and time-domain induced polarization field investigations of geothermal areas at Krafla, Iceland: Comparison to borehole and laboratory frequency-domain electrical observations

L. Lévy, P. K. Maurya, S. Byrdina, J. Vandemeulebrouck, F. Sigmundsson, K. Árnason, T. Ricci, D. Deldicque, M. Roger, B. Gibert, P. Labazuy

Research output: Contribution to journalArticlepeer-review

14 Citations (SciVal)

Abstract

Interaction of H2S and basaltic rocks in volcanic geothermal areas can originate from natural up-flow of magmatic fluids or H2S artificial re-injection in relation to geothermal exploitation, both causing pyrite mineralization. We study the possibility to track these processes with electrical impedance field measurements. Electrical Resistivity Tomography (ERT) and Time- Domain Induced Polarization (TDIP) measurements were performed along thirteen 1.24 km long profiles, at three different sites around the eastern caldera rim of the Krafla caldera: (i) a 'cold altered' site affected by past hydrothermal circulations, (ii) a hot active site and (iii) a 'cold un-altered' site, unaffected by hydrothermal circulations. We present 2-D inversions of direct current (DC) resistivity, maximum phase angle of the electrical impedance (MPA) and relaxation time. The maximum depth of investigation for the MPA is 200 m, obtained in zones of high resistivity, corresponding to fresh and recent unaltered basalt. At the hot and cold altered sites, the field resistivities are compared to in situ borehole logs and laboratory complex resistivity measurements on rock samples from the boreholes. The laboratory complex resistivity was measured at six different pore water conductivities, ranging from 0.02 to 5 Sm-1, and frequency in the range 10-2 - 106 Hz. The time-range investigated in our field TDIP measurements was approximately 0.01-8 s. At the cold altered site, the inverted resistivity is consistent with both borehole observations and laboratory measurements. At the hot site, resistivity from field inversion and borehole logs are consistent. Comparing inversion results and borehole logs to laboratory resistivity measured on core samples at room temperature reveals that a correction coefficient for the effect of temperature on resistivity of 6 per cent per ?C is appropriate at investigated depths. This exceptionally high temperature correction coefficient suggests a dominant influence of interface and interfoliar conduction, characteristic of smectite-rich rocks, compared to electrolyte conduction. High MPA is attributed to the presence of pyrite at the hot site and of iron-oxides at the cold unaltered site, through joint consideration of MPA together with DC resistivity and relaxation time. TDIP measurements offer the possibility to detect the presence of metallic minerals at shallow depth and distinguish between pyrite and iron-oxides. The abundance of highly conductive smectite in altered volcanic rocks represents a challenge for resolving IP parameters, because the low resistivity created by abundant smectite limits the data quality of the measured voltage discharge.

Original languageEnglish
Article numberggz240
Pages (from-to)1469-1489
Number of pages21
JournalGeophysical Journal International
Volume218
Issue number3
DOIs
Publication statusPublished - 2019 May 16
Externally publishedYes

Bibliographical note

Funding Information:
Editor Alexis Maineult and reviewers Tina Martin and Konstantyn Titov are thanked for improving the clarity and scientific quality of the manuscript, through an efficient review process. The power company Landsvirkjun is thanked for providing with on-site accommodation and facilities during the field campaign. Anthony Finizola, Renaud Trinquier and Anna Kristín Árnadóttir are thanked for helping with material transportation issues. André Revil, Svein-bjorn Steinthórsson, Daniel Juncu and Vincent Drouin are thanked for their help in the field, and Stefán Auðunn Stefánsson for the logistical support. Volker Rath is thanked for constructive discussion. LL thanks Gylfi Páll Hersir for his constructive comments on the manuscript and his general support and Lee Slater for valuable feedbacks and discussions on the manuscript. LL also thanks Pierre Briole and Ólafur G. Flóvenz for their support with the organisation of the field campaign. The company Jarðboranir is thanked for providing bentonite for field measurements. The company Aarhus GeoSoftware is thanked for providing a free trial license for Aarhus Workbench to LL. 3-D figures were made with the freeware Par-aview. This work was supported by a PhD grant from Paris Sciences et Lettres to Léa Lévy and the IMAGE FP7 EC and GEMex H2020 projects (grant agreements 608553 and 727550). Fundings for the field measurements were provided by the French Ministries of Foreign Affairs and International Development and of Education, Teaching and Research, through the PHC program Jules Verne, granted to Ecole Normale Supérieure and University of Iceland, as well as by a CNRS-INSU grant to University of Savoie-Mont Blanc. Equipment transportation expenses were covered by University of Montpellier and also supported by University of La Réunion.

Publisher Copyright:
© The Author(s) 2019.

Subject classification (UKÄ)

  • Geophysical Engineering

Keywords

  • Electrical resistivity tomography
  • Hydrogeophysics
  • Hydrothermal systems

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