Articles | Volume 7, issue 1
https://doi.org/10.5194/se-7-249-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-7-249-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Review article
| 
12 Feb 2016
Review article |
| 12 Feb 2016
A review on electrokinetically induced seismo-electrics, electro-seismics, and seismo-magnetics for Earth sciences
L. Jouniaux
CORRESPONDING AUTHOR
Institut de Physique du Globe de Strasbourg, CNRS and Université de Strasbourg UMR7516, Strasbourg, France
F. Zyserman
CONICET and Facultad de Ciencias Astronómicas y Geofísicas, Universidad Nacional de La Plata, La Plata, Argentina
Related subject area
Geophysics
Post-Caledonian tectonic evolution of the Precambrian and Paleozoic platform boundary zone offshore Poland based on the new and vintage multi-channel reflection seismic data
Geodynamic controls on clastic-dominated base metal deposits
Seismic wave modeling of fluid-saturated fractured porous rock: including fluid pressure diffusion effects of discretely distributed large-scale fractures
Comparison of surface-wave techniques to estimate S- and P-wave velocity models from active seismic data
Integration of automatic implicit geological modelling in deterministic geophysical inversion
Complex fault system revealed by 3-D seismic reflection data with deep learning and fault network analysis
Numerical modeling of stresses and deformation in the Zagros–Iranian Plateau region
Advanced seismic characterization of a geothermal carbonate reservoir – insight into the structure and diagenesis of a reservoir in the German Molasse Basin
Electrical conductivity of anhydrous and hydrous gabbroic melt under high temperature and high pressure: implications for the high-conductivity anomalies in the mid-ocean ridge region
Ground motion emissions due to wind turbines: observations, acoustic coupling, and attenuation relationships
Formation and geophysical character of transitional crust at the passive continental margin around Walvis Ridge, Namibia
Seismic amplitude response to internal heterogeneity of mass-transport deposits
Investigation of the effects of surrounding media on the distributed acoustic sensing of a helically wound fibre-optic cable with application to the New Afton deposit, British Columbia
Utilisation of probabilistic magnetotelluric modelling to constrain magnetic data inversion: proof-of-concept and field application
Geophysical analysis of an area affected by subsurface dissolution – case study of an inland salt marsh in northern Thuringia, Germany
Comparison of straight-ray and curved-ray surface wave tomography approaches in near-surface studies
An efficient probabilistic workflow for estimating induced earthquake parameters in 3D heterogeneous media
3D deep geothermal reservoir imaging with wireline distributed acoustic sensing in two boreholes
3D high-resolution seismic imaging of the iron oxide deposits in Ludvika (Sweden) using full-waveform inversion and reverse time migration
Three-dimensional reflection seismic imaging of the iron oxide deposits in the Ludvika mining area, Sweden, using Fresnel volume migration
Drone-based magnetic and multispectral surveys to develop a 3D model for mineral exploration at Qullissat, Disko Island, Greenland
Ambient seismic noise analysis of LARGE-N data for mineral exploration in the Central Erzgebirge, Germany
Surface-wave tomography for mineral exploration: a successful combination of passive and active data (Siilinjärvi phosphorus mine, Finland)
Reflection tomography by depth warping: a case study across the Java trench
Dynamic motion monitoring of a 3.6 km long steel rod in a borehole during cold-water injection with distributed fiber-optic sensing
Impact of Timanian thrust systems on the late Neoproterozoic–Phanerozoic tectonic evolution of the Barents Sea and Svalbard
Forearc density structure of the overriding plate in the northern area of the giant 1960 Valdivia earthquake
Imaging crustal structures through a passive seismic imaging approach in a mining area in Saxony, Germany
Investigating the effects of intersection flow localization in equivalent-continuum-based upscaling of flow in discrete fracture networks
Cross-diffusion waves resulting from multiscale, multiphysics instabilities: application to earthquakes
Reverse time migration (RTM) imaging of iron oxide deposits in the Ludvika mining area, Sweden
Near-surface structure of the Sodankylä area in Finland, obtained by passive seismic interferometry
Evolution of the Iberian Massif as deduced from its crustal thickness and geometry of a mid-crustal (Conrad) discontinuity
Four-dimensional tracer flow reconstruction in fractured rock through borehole ground-penetrating radar (GPR) monitoring
Moho topography beneath the European Eastern Alps by global-phase seismic interferometry
Seismic imaging across fault systems in the Abitibi greenstone belt – an analysis of pre- and post-stack migration approaches in the Chibougamau area, Quebec, Canada
Early Cenozoic Eurekan strain partitioning and decoupling in central Spitsbergen, Svalbard
On the comparison of strain measurements from fibre optics with a dense seismometer array at Etna volcano (Italy)
Cross-diffusion waves resulting from multiscale, multi-physics instabilities: theory
Multi-scale analysis and modelling of aeromagnetic data over the Bétaré-Oya area in eastern Cameroon, for structural evidence investigations
The impact of seismic interpretation methods on the analysis of faults: a case study from the Snøhvit field, Barents Sea
Wireline distributed acoustic sensing allows 4.2 km deep vertical seismic profiling of the Rotliegend 150 °C geothermal reservoir in the North German Basin
Integrated land and water-borne geophysical surveys shed light on the sudden drying of large karst lakes in southern Mexico
Sparse 3D reflection seismic survey for deep-targeting iron oxide deposits and their host rocks, Ludvika Mines, Sweden
Fault sealing and caprock integrity for CO2 storage: an in situ injection experiment
What can seismic noise tell us about the Alpine reactivation of the Iberian Massif? An example in the Iberian Central System
In situ hydromechanical responses during well drilling recorded by fiber-optic distributed strain sensing
Coherent diffraction imaging for enhanced fault and fracture network characterization
On the morphology and amplitude of 2D and 3D thermal anomalies induced by buoyancy-driven flow within and around fault zones
Characterizing a decametre-scale granitic reservoir using ground-penetrating radar and seismic methods
Quang Nguyen, Michal Malinowski, Stanisław Mazur, Sergiy Stovba, Małgorzata Ponikowska, and Christian Hübscher
Solid Earth, 15, 1029–1046, https://doi.org/10.5194/se-15-1029-2024, https://doi.org/10.5194/se-15-1029-2024, 2024
Short summary
Short summary
Our work demonstrates the following: (1) an efficient seismic data-processing strategy focused on suppressing shallow-water multiple reflections. (2) An improvement in the quality of legacy marine seismic data. (3) A seismic interpretation of sedimentary successions overlying the basement in the transition zone from the Precambrian to Paleozoic platforms. (4) The tectonic evolution of the Koszalin Fault and its relation to the Caledonian Deformation Front offshore Poland.
This article is included in the Encyclopedia of Geosciences
Anne C. Glerum, Sascha Brune, Joseph M. Magnall, Philipp Weis, and Sarah A. Gleeson
Solid Earth, 15, 921–944, https://doi.org/10.5194/se-15-921-2024, https://doi.org/10.5194/se-15-921-2024, 2024
Short summary
Short summary
High-value zinc–lead deposits formed in sedimentary basins created when tectonic plates rifted apart. We use computer simulations of rifting and the associated sediment erosion and deposition to understand why they formed in some basins but not in others. Basins that contain a metal source, faults that focus fluids, and rocks that can host deposits occurred in both narrow and wide rifts for ≤ 3 Myr. The largest and the most deposits form in narrow margins of narrow asymmetric rifts.
This article is included in the Encyclopedia of Geosciences
Yingkai Qi, Xuehua Chen, Qingwei Zhao, Xin Luo, and Chunqiang Feng
Solid Earth, 15, 535–554, https://doi.org/10.5194/se-15-535-2024, https://doi.org/10.5194/se-15-535-2024, 2024
Short summary
Short summary
Fractures tend to dominate the mechanical and hydraulic properties of porous rock and impact the scattering characteristics of passing waves. This study takes into account the poroelastic effects of fractures in numerical modeling. Our results demonstrate that scattered waves from complex fracture systems are strongly affected by the fractures.
This article is included in the Encyclopedia of Geosciences
Farbod Khosro Anjom, Frank Adler, and Laura Valentina Socco
Solid Earth, 15, 367–386, https://doi.org/10.5194/se-15-367-2024, https://doi.org/10.5194/se-15-367-2024, 2024
Short summary
Short summary
Most surface-wave techniques focus on estimating the S-wave velocity (VS) model and consider the P-wave velocity (VP) model as prior information in the inversion step. Here, we show the application of three surface-wave methods to estimate both VS and VP models. We apply the methods to the data from a hard-rock site that were acquired through the irregular source–receiver recording technique. We compare the outcomes and performances of the methods in detail.
This article is included in the Encyclopedia of Geosciences
Jérémie Giraud, Guillaume Caumon, Lachlan Grose, Vitaliy Ogarko, and Paul Cupillard
Solid Earth, 15, 63–89, https://doi.org/10.5194/se-15-63-2024, https://doi.org/10.5194/se-15-63-2024, 2024
Short summary
Short summary
We present and test an algorithm that integrates geological modelling into deterministic geophysical inversion. This is motivated by the need to model the Earth using all available data and to reconcile the different types of measurements. We introduce the methodology and test our algorithm using two idealised scenarios. Results suggest that the method we propose is effectively capable of improving the models recovered by geophysical inversion and may be applied in real-world scenarios.
This article is included in the Encyclopedia of Geosciences
Thilo Wrona, Indranil Pan, Rebecca E. Bell, Christopher A.-L. Jackson, Robert L. Gawthorpe, Haakon Fossen, Edoseghe E. Osagiede, and Sascha Brune
Solid Earth, 14, 1181–1195, https://doi.org/10.5194/se-14-1181-2023, https://doi.org/10.5194/se-14-1181-2023, 2023
Short summary
Short summary
We need to understand where faults are to do the following: (1) assess their seismic hazard, (2) explore for natural resources and (3) store CO2 safely in the subsurface. Currently, we still map subsurface faults primarily by hand using seismic reflection data, i.e. acoustic images of the Earth. Mapping faults this way is difficult and time-consuming. Here, we show how to use deep learning to accelerate fault mapping and how to use networks or graphs to simplify fault analyses.
This article is included in the Encyclopedia of Geosciences
Srishti Singh and Radheshyam Yadav
Solid Earth, 14, 937–959, https://doi.org/10.5194/se-14-937-2023, https://doi.org/10.5194/se-14-937-2023, 2023
Short summary
Short summary
We use numerical models to study the stresses arising from gravitational potential energy (GPE) variations and shear tractions associated with mantle convection in the Zagros–Iran region. The joint models predicted consistent deviatoric stresses that can explain most of the deformation indicators. Stresses associated with mantle convection are found to be higher than those from GPE, thus indicating the deformation in this region may primarily be caused by the mantle, except in eastern Iran.
This article is included in the Encyclopedia of Geosciences
Sonja H. Wadas, Johanna F. Krumbholz, Vladimir Shipilin, Michael Krumbholz, David C. Tanner, and Hermann Buness
Solid Earth, 14, 871–908, https://doi.org/10.5194/se-14-871-2023, https://doi.org/10.5194/se-14-871-2023, 2023
Short summary
Short summary
The geothermal carbonate reservoir below Munich, Germany, is extremely heterogeneous because it is controlled by many factors like lithology, diagenesis, karstification, and tectonic deformation. We used a 3D seismic single- and multi-attribute analysis combined with well data and a neural-net-based lithology classification to obtain an improved reservoir concept outlining its structural and diagenetic evolution and to identify high-quality reservoir zones in the Munich area.
This article is included in the Encyclopedia of Geosciences
Mengqi Wang, Lidong Dai, Haiying Hu, Ziming Hu, Chenxin Jing, Chuanyu Yin, Song Luo, and Jinhua Lai
Solid Earth, 14, 847–858, https://doi.org/10.5194/se-14-847-2023, https://doi.org/10.5194/se-14-847-2023, 2023
Short summary
Short summary
This is the first time that the electrical conductivity of gabbroic melt was assessed at high temperature and high pressure. The dependence of electrical conductivity on the degree of depolymerization was also explored. Electrical conductivity of gabbroic melts can be employed to interpret high-conductivity anomalies in the Mohns Ridge of the Arctic Ocean. This is of widespread interest to potential readers in high-pressure rock physics, solid geophysics, and deep Earth science.
This article is included in the Encyclopedia of Geosciences
Laura Gaßner and Joachim Ritter
Solid Earth, 14, 785–803, https://doi.org/10.5194/se-14-785-2023, https://doi.org/10.5194/se-14-785-2023, 2023
Short summary
Short summary
In this work we analyze signals emitted from wind turbines. They induce sound as well as ground motion waves which propagate through the subsurface and are registered by sensitive instruments. In our data we observe when these signals are present and how strong they are. Some signals are present in ground motion and sound data, providing the opportunity to study similarities and better characterize emissions. Furthermore, we study the amplitudes with distance to improve the signal prediction.
This article is included in the Encyclopedia of Geosciences
Gesa Franz, Marion Jegen, Max Moorkamp, Christian Berndt, and Wolfgang Rabbel
Solid Earth, 14, 237–259, https://doi.org/10.5194/se-14-237-2023, https://doi.org/10.5194/se-14-237-2023, 2023
Short summary
Short summary
Our study focuses on the correlation of two geophysical parameters (electrical resistivity and density) with geological units. We use this computer-aided correlation to improve interpretation of the Earth’s formation history along the Namibian coast and the associated formation of the South Atlantic Ocean. It helps to distinguish different types of sediment cover and varieties of oceanic crust, as well as to identify typical features associated with the breakup of continents.
This article is included in the Encyclopedia of Geosciences
Jonathan Ford, Angelo Camerlenghi, Francesca Zolezzi, and Marilena Calarco
Solid Earth, 14, 137–151, https://doi.org/10.5194/se-14-137-2023, https://doi.org/10.5194/se-14-137-2023, 2023
Short summary
Short summary
Submarine landslides commonly appear as low-amplitude zones in seismic data. Previous studies have attributed this to a lack of preserved internal structure. We use seismic modelling to show that an amplitude reduction can be generated even when there is still metre-scale internal structure, by simply deforming the bedding. This has implications for interpreting failure type, for core-seismic correlation and for discriminating landslides from other "transparent" phenomena such as free gas.
This article is included in the Encyclopedia of Geosciences
Sepidehalsadat Hendi, Mostafa Gorjian, Gilles Bellefleur, Christopher D. Hawkes, and Don White
Solid Earth, 14, 89–99, https://doi.org/10.5194/se-14-89-2023, https://doi.org/10.5194/se-14-89-2023, 2023
Short summary
Short summary
In this study, the modelling results are used to help understand the performance of a helically wound fibre (HWC) from a field study at the New Afton mine, British Columbia. We introduce the numerical 3D model to model strain values in HWC to design more effective HWC system. The DAS dataset at New Afton, interpreted in the context of our modelling, serves as a practical demonstration of the extreme effects of surrounding media and coupling on HWC data quality.
This article is included in the Encyclopedia of Geosciences
Jérémie Giraud, Hoël Seillé, Mark D. Lindsay, Gerhard Visser, Vitaliy Ogarko, and Mark W. Jessell
Solid Earth, 14, 43–68, https://doi.org/10.5194/se-14-43-2023, https://doi.org/10.5194/se-14-43-2023, 2023
Short summary
Short summary
We propose and apply a workflow to combine the modelling and interpretation of magnetic anomalies and resistivity anomalies to better image the basement. We test the method on a synthetic case study and apply it to real world data from the Cloncurry area (Queensland, Australia), which is prospective for economic minerals. Results suggest a new interpretation of the composition and structure towards to east of the profile that we modelled.
This article is included in the Encyclopedia of Geosciences
Sonja H. Wadas, Hermann Buness, Raphael Rochlitz, Peter Skiba, Thomas Günther, Michael Grinat, David C. Tanner, Ulrich Polom, Gerald Gabriel, and Charlotte M. Krawczyk
Solid Earth, 13, 1673–1696, https://doi.org/10.5194/se-13-1673-2022, https://doi.org/10.5194/se-13-1673-2022, 2022
Short summary
Short summary
The dissolution of rocks poses a severe hazard because it can cause subsidence and sinkhole formation. Based on results from our study area in Thuringia, Germany, using P- and SH-wave reflection seismics, electrical resistivity and electromagnetic methods, and gravimetry, we develop a geophysical investigation workflow. This workflow enables identifying the initial triggers of subsurface dissolution and its control factors, such as structural constraints, fluid pathways, and mass movement.
This article is included in the Encyclopedia of Geosciences
Mohammadkarim Karimpour, Evert Slob, and Laura Valentina Socco
Solid Earth, 13, 1569–1583, https://doi.org/10.5194/se-13-1569-2022, https://doi.org/10.5194/se-13-1569-2022, 2022
Short summary
Short summary
Near-surface characterisation is of great importance. Surface wave tomography (SWT) is a powerful tool to model the subsurface. In this work we compare straight-ray and curved-ray SWT at near-surface scale. We apply both approaches to four datasets and compare the results in terms of the quality of the final model and the computational cost. We show that in the case of high data coverage, straight-ray SWT can produce similar results to curved-ray SWT but with less computational cost.
This article is included in the Encyclopedia of Geosciences
La Ode Marzujriban Masfara, Thomas Cullison, and Cornelis Weemstra
Solid Earth, 13, 1309–1325, https://doi.org/10.5194/se-13-1309-2022, https://doi.org/10.5194/se-13-1309-2022, 2022
Short summary
Short summary
Induced earthquakes are natural phenomena in which the events are associated with human activities. Although the magnitudes of these events are mostly smaller than tectonic events, in some cases, the magnitudes can be high enough to damage buildings near the event's location. To study these (high-magnitude) induced events, we developed a workflow in which the recorded data from an earthquake are used to describe the source and monitor the area for other (potentially high-magnitude) earthquakes.
This article is included in the Encyclopedia of Geosciences
Evgeniia Martuganova, Manfred Stiller, Ben Norden, Jan Henninges, and Charlotte M. Krawczyk
Solid Earth, 13, 1291–1307, https://doi.org/10.5194/se-13-1291-2022, https://doi.org/10.5194/se-13-1291-2022, 2022
Short summary
Short summary
We demonstrate the applicability of vertical seismic profiling (VSP) acquired using wireline distributed acoustic sensing (DAS) technology for deep geothermal reservoir imaging and characterization. Borehole DAS data provide critical input for seismic interpretation and help assess small-scale geological structures. This case study can be used as a basis for detailed structural exploration of geothermal reservoirs and provide insightful information for geothermal exploration projects.
This article is included in the Encyclopedia of Geosciences
Brij Singh, Michał Malinowski, Andrzej Górszczyk, Alireza Malehmir, Stefan Buske, Łukasz Sito, and Paul Marsden
Solid Earth, 13, 1065–1085, https://doi.org/10.5194/se-13-1065-2022, https://doi.org/10.5194/se-13-1065-2022, 2022
Short summary
Short summary
Fast depletion of shallower deposits is pushing the mining industry to look for cutting-edge technologies for deep mineral targeting. We demonstrated a joint workflow including two state-of-the-art technologies: full-waveform inversion and reverse time migration. We produced Earth images with significant details which can help with better estimation of areas with high mineralisation, better mine planning and safety measures.
This article is included in the Encyclopedia of Geosciences
Felix Hloušek, Michal Malinowski, Lena Bräunig, Stefan Buske, Alireza Malehmir, Magdalena Markovic, Lukasz Sito, Paul Marsden, and Emma Bäckström
Solid Earth, 13, 917–934, https://doi.org/10.5194/se-13-917-2022, https://doi.org/10.5194/se-13-917-2022, 2022
Short summary
Short summary
Methods for mineral exploration play an important role within the EU. Exploration must be environmentally friendly, cost effective, and feasible in populated areas. Seismic methods have the potential to deliver detailed images of mineral deposits but suffer from these demands. We show the results for a sparse 3D seismic dataset acquired in Sweden. The 3D depth image allows us to track the known mineralizations beyond the known extent and gives new insights into the geometry of the deposit.
This article is included in the Encyclopedia of Geosciences
Robert Jackisch, Björn H. Heincke, Robert Zimmermann, Erik V. Sørensen, Markku Pirttijärvi, Moritz Kirsch, Heikki Salmirinne, Stefanie Lode, Urpo Kuronen, and Richard Gloaguen
Solid Earth, 13, 793–825, https://doi.org/10.5194/se-13-793-2022, https://doi.org/10.5194/se-13-793-2022, 2022
Short summary
Short summary
We integrate UAS-based magnetic and multispectral data with legacy exploration data of a Ni–Cu–PGE prospect on Disko Island, West Greenland. The basalt unit has a complex magnetization, and we use a constrained 3D magnetic vector inversion to estimate magnetic properties and spatial dimensions of the target unit. Our 3D modelling reveals a horizontal sheet and a strong remanent magnetization component. We highlight the advantage of UAS use in rugged and remote terrain.
This article is included in the Encyclopedia of Geosciences
Trond Ryberg, Moritz Kirsch, Christian Haberland, Raimon Tolosana-Delgado, Andrea Viezzoli, and Richard Gloaguen
Solid Earth, 13, 519–533, https://doi.org/10.5194/se-13-519-2022, https://doi.org/10.5194/se-13-519-2022, 2022
Short summary
Short summary
Novel methods for mineral exploration play an important role in future resource exploration. The methods have to be environmentally friendly, socially accepted and cost effective by integrating multidisciplinary methodologies. We investigate the potential of passive, ambient noise tomography combined with 3D airborne electromagnetics for mineral exploration in Geyer, Germany. We show that the combination of the two geophysical data sets has promising potential for future mineral exploration.
This article is included in the Encyclopedia of Geosciences
Chiara Colombero, Myrto Papadopoulou, Tuomas Kauti, Pietari Skyttä, Emilia Koivisto, Mikko Savolainen, and Laura Valentina Socco
Solid Earth, 13, 417–429, https://doi.org/10.5194/se-13-417-2022, https://doi.org/10.5194/se-13-417-2022, 2022
Short summary
Short summary
Passive-source surface waves may be exploited in mineral exploration for deeper investigations. We propose a semi-automatic workflow for their processing. The geological interpretation of the results obtained at a mineral site (Siilinjärvi phosphorus mine) shows large potentialities and effectiveness of the proposed workflow.
This article is included in the Encyclopedia of Geosciences
Yueyang Xia, Dirk Klaeschen, Heidrun Kopp, and Michael Schnabel
Solid Earth, 13, 367–392, https://doi.org/10.5194/se-13-367-2022, https://doi.org/10.5194/se-13-367-2022, 2022
Short summary
Short summary
Geological interpretations based on seismic depth images depend on an accurate subsurface velocity model. Reflection tomography is one method to iteratively update a velocity model based on depth error analysis. We used a warping method to estimate closely spaced data-driven depth error displacement fields. The application to a multichannel seismic line across the Sunda subduction zone illustrates the approach which leads to more accurate images of complex geological structures.
This article is included in the Encyclopedia of Geosciences
Martin Peter Lipus, Felix Schölderle, Thomas Reinsch, Christopher Wollin, Charlotte Krawczyk, Daniela Pfrang, and Kai Zosseder
Solid Earth, 13, 161–176, https://doi.org/10.5194/se-13-161-2022, https://doi.org/10.5194/se-13-161-2022, 2022
Short summary
Short summary
A fiber-optic cable was installed along a freely suspended rod in a deep geothermal well in Munich, Germany. A cold-water injection test was monitored with fiber-optic distributed acoustic and temperature sensing. During injection, we observe vibrational events in the lower part of the well. On the basis of a mechanical model, we conclude that the vibrational events are caused by thermal contraction of the rod. The results illustrate potential artifacts when analyzing downhole acoustic data.
This article is included in the Encyclopedia of Geosciences
Jean-Baptiste P. Koehl, Craig Magee, and Ingrid M. Anell
Solid Earth, 13, 85–115, https://doi.org/10.5194/se-13-85-2022, https://doi.org/10.5194/se-13-85-2022, 2022
Short summary
Short summary
The present study shows evidence of fault systems (large cracks in the Earth's crust) hundreds to thousands of kilometers long and several kilometers thick extending from northwestern Russia to the northern Norwegian Barents Sea and the Svalbard Archipelago using seismic, magnetic, and gravimetric data. The study suggests that the crust in Svalbard and the Barents Sea was already attached to Norway and Russia at ca. 650–550 Ma, thus challenging existing models.
This article is included in the Encyclopedia of Geosciences
Andrei Maksymowicz, Daniela Montecinos-Cuadros, Daniel Díaz, María José Segovia, and Tomás Reyes
Solid Earth, 13, 117–136, https://doi.org/10.5194/se-13-117-2022, https://doi.org/10.5194/se-13-117-2022, 2022
Short summary
Short summary
This work analyses the density structure of the continental forearc in the northern segment of the 1960 Mw 9.6 Valdivia earthquake. Results show a segmentation of the continental wedge along and perpendicular to the margin. The extension of the less rigid basement units conforming the marine wedge and Coastal Cordillera domain could modify the process of stress loading during the interseismic periods. This analysis highlights the role of the overriding plate on the seismotectonic process.
This article is included in the Encyclopedia of Geosciences
Hossein Hassani, Felix Hloušek, Stefan Buske, and Olaf Wallner
Solid Earth, 12, 2703–2715, https://doi.org/10.5194/se-12-2703-2021, https://doi.org/10.5194/se-12-2703-2021, 2021
Short summary
Short summary
Passive seismic imaging methods use natural earthquakes as seismic sources, while in active seismic imaging methods, artificial sources (e.g. explosives) are used to generate seismic waves. We imaged some structures related to a major fault plane through a passive seismic imaging approach using microearthquakes with magnitudes smaller than 0.9 (Mw). These structures have not been illuminated by a previously conducted 3D active seismic survey due to their large dip angles.
This article is included in the Encyclopedia of Geosciences
Maximilian O. Kottwitz, Anton A. Popov, Steffen Abe, and Boris J. P. Kaus
Solid Earth, 12, 2235–2254, https://doi.org/10.5194/se-12-2235-2021, https://doi.org/10.5194/se-12-2235-2021, 2021
Short summary
Short summary
Upscaling fluid flow in fractured reservoirs is an important practice in subsurface resource utilization. In this study, we first conduct numerical simulations of direct fluid flow at locations where fractures intersect to analyze the arising hydraulic complexities. Next, we develop a model that integrates these effects into larger-scale continuum models of fracture networks to investigate their impact on the upscaling. For intensively fractured systems, these effects become important.
This article is included in the Encyclopedia of Geosciences
Klaus Regenauer-Lieb, Manman Hu, Christoph Schrank, Xiao Chen, Santiago Peña Clavijo, Ulrich Kelka, Ali Karrech, Oliver Gaede, Tomasz Blach, Hamid Roshan, Antoine B. Jacquey, Piotr Szymczak, and Qingpei Sun
Solid Earth, 12, 1829–1849, https://doi.org/10.5194/se-12-1829-2021, https://doi.org/10.5194/se-12-1829-2021, 2021
Short summary
Short summary
This paper presents a trans-disciplinary approach bridging the gap between observations of instabilities from the molecular scale to the very large scale. We show that all scales communicate via propagation of volumetric deformation waves. Similar phenomena are encountered in quantum optics where wave collisions can release sporadic bursts of light. Ocean waves show a similar phenomenon of rogue waves that seem to come from nowhere. This mechanism is proposed to be the trigger for earthquakes.
This article is included in the Encyclopedia of Geosciences
Yinshuai Ding and Alireza Malehmir
Solid Earth, 12, 1707–1718, https://doi.org/10.5194/se-12-1707-2021, https://doi.org/10.5194/se-12-1707-2021, 2021
Short summary
Short summary
In this article, we investigate the potential of reverse time migration (RTM) for deep targeting iron oxide deposits and the possible AVO effect that is potentially seen in the common image gathers from this migration algorithm. The results are promising and help to delineate the deposits and host rock structures using a 2D dataset from the Ludvika mines of central Sweden.
This article is included in the Encyclopedia of Geosciences
Nikita Afonin, Elena Kozlovskaya, Suvi Heinonen, and Stefan Buske
Solid Earth, 12, 1563–1579, https://doi.org/10.5194/se-12-1563-2021, https://doi.org/10.5194/se-12-1563-2021, 2021
Short summary
Short summary
In our study, we show the results of a passive seismic interferometry application for mapping the uppermost crust in the area of active mineral exploration in northern Finland. The obtained velocity models agree well with geological data and complement the results of reflection seismic data interpretation.
This article is included in the Encyclopedia of Geosciences
Puy Ayarza, José Ramón Martínez Catalán, Ana Martínez García, Juan Alcalde, Juvenal Andrés, José Fernando Simancas, Immaculada Palomeras, David Martí, Irene DeFelipe, Chris Juhlin, and Ramón Carbonell
Solid Earth, 12, 1515–1547, https://doi.org/10.5194/se-12-1515-2021, https://doi.org/10.5194/se-12-1515-2021, 2021
Short summary
Short summary
Vertical incidence seismic profiling on the Iberian Massif images a mid-crustal-scale discontinuity at the top of the reflective lower crust. This feature shows that upper- and lower-crustal reflections merge into it, suggesting that it has often behaved as a detachment. The orogen-scale extension of this discontinuity, present in Gondwanan and Avalonian affinity terranes into the Iberian Massif, demonstrates its relevance, leading us to interpret it as the Conrad discontinuity.
This article is included in the Encyclopedia of Geosciences
Peter-Lasse Giertzuch, Joseph Doetsch, Alexis Shakas, Mohammadreza Jalali, Bernard Brixel, and Hansruedi Maurer
Solid Earth, 12, 1497–1513, https://doi.org/10.5194/se-12-1497-2021, https://doi.org/10.5194/se-12-1497-2021, 2021
Short summary
Short summary
Two time-lapse borehole ground penetrating radar (GPR) surveys were conducted during saline tracer experiments in weakly fractured crystalline rock with sub-millimeter fractures apertures, targeting electrical conductivity changes. The combination of time-lapse reflection and transmission GPR surveys from different boreholes allowed monitoring the tracer flow and reconstructing the flow path and its temporal evolution in 3D and provided a realistic visualization of the hydrological processes.
This article is included in the Encyclopedia of Geosciences
Irene Bianchi, Elmer Ruigrok, Anne Obermann, and Edi Kissling
Solid Earth, 12, 1185–1196, https://doi.org/10.5194/se-12-1185-2021, https://doi.org/10.5194/se-12-1185-2021, 2021
Short summary
Short summary
The European Alps formed during collision between the European and Adriatic plates and are one of the most studied orogens for understanding the dynamics of mountain building. In the Eastern Alps, the contact between the colliding plates is still a matter of debate. We have used the records from distant earthquakes to highlight the geometries of the crust–mantle boundary in the Eastern Alpine area; our results suggest a complex and faulted internal crustal structure beneath the higher crests.
This article is included in the Encyclopedia of Geosciences
Saeid Cheraghi, Alireza Malehmir, Mostafa Naghizadeh, David Snyder, Lucie Mathieu, and Pierre Bedeaux
Solid Earth, 12, 1143–1164, https://doi.org/10.5194/se-12-1143-2021, https://doi.org/10.5194/se-12-1143-2021, 2021
Short summary
Short summary
High-resolution seismic profiles in 2D are acquired in the north and south of the Chibougamau area, Quebec, Canada located in the northeast of the Abitibi Greenstone belt. The area mostly includes volcanic rocks, and both profiles cross over several fault zones. The seismic method is acquired to image the subsurface down to depth of 12 km. The main aim of this study is to image major fault zones and the geological formations connected to those faults to investigate metal endowment in the area.
This article is included in the Encyclopedia of Geosciences
Jean-Baptiste P. Koehl
Solid Earth, 12, 1025–1049, https://doi.org/10.5194/se-12-1025-2021, https://doi.org/10.5194/se-12-1025-2021, 2021
Short summary
Short summary
By using seismic data and fieldwork, this contribution shows that soft, coal-rich sedimentary rocks absorbed most of early Cenozoic, Eurekan, contractional deformation in central Spitsbergen, thus suggesting that no contractional deformation event is needed in the Late Devonian to explain the deformation differences among late Paleozoic sedimentary rocks. It also shows that the Billefjorden Fault Zone, a major crack in the Earth's crust in Svalbard, is probably segmented.
This article is included in the Encyclopedia of Geosciences
Gilda Currenti, Philippe Jousset, Rosalba Napoli, Charlotte Krawczyk, and Michael Weber
Solid Earth, 12, 993–1003, https://doi.org/10.5194/se-12-993-2021, https://doi.org/10.5194/se-12-993-2021, 2021
Short summary
Short summary
We investigate the capability of distributed acoustic sensing (DAS) to record dynamic strain changes related to Etna volcano activity in 2019. To validate the DAS measurements, we compute strain estimates from seismic signals recorded by a dense broadband array. A general good agreement is found between array-derived strain and DAS measurements along the fibre optic cable. Localised short wavelength discrepancies highlight small-scale structural heterogeneities in the investigated area.
This article is included in the Encyclopedia of Geosciences
Klaus Regenauer-Lieb, Manman Hu, Christoph Schrank, Xiao Chen, Santiago Peña Clavijo, Ulrich Kelka, Ali Karrech, Oliver Gaede, Tomasz Blach, Hamid Roshan, and Antoine B. Jacquey
Solid Earth, 12, 869–883, https://doi.org/10.5194/se-12-869-2021, https://doi.org/10.5194/se-12-869-2021, 2021
Short summary
Short summary
In this paper we expand on a recent discovery of slow cross-diffusion hydromechanical waves cast into a new concise reaction–diffusion equation for THMC coupling. If waves are excited through the THMC reaction terms unbounded reactions can be captured by inclusion of statistical information from the lower scale through nonlocal reaction–diffusion equations. These cross-diffusion coefficients regularize extreme earthquake-like events (rogue waves) through a new form of quasi-soliton wave.
This article is included in the Encyclopedia of Geosciences
Christian Emile Nyaban, Théophile Ndougsa-Mbarga, Marcelin Bikoro-Bi-Alou, Stella Amina Manekeng Tadjouteu, and Stephane Patrick Assembe
Solid Earth, 12, 785–800, https://doi.org/10.5194/se-12-785-2021, https://doi.org/10.5194/se-12-785-2021, 2021
Short summary
Short summary
A multi-scale analysis of aeromagnetic data combining tilt derivative, Euler deconvolution, upward continuation, and 2.75D modelling was applied over Cameroon between the latitudes 5°30'–6° N and the longitudes 13°30'–14°45' E. Major families of faults oriented ENE–WSW, E–W, NW–SE, and N–S with a NE–SW prevalence were mapped. Depths of interpreted faults range from 1000 to 3400 m, mylonitic veins were identified, and 2.75D modelling revealed fault depths greater than 1200 m.
This article is included in the Encyclopedia of Geosciences
Jennifer E. Cunningham, Nestor Cardozo, Chris Townsend, and Richard H. T. Callow
Solid Earth, 12, 741–764, https://doi.org/10.5194/se-12-741-2021, https://doi.org/10.5194/se-12-741-2021, 2021
Short summary
Short summary
This work investigates the impact of commonly used seismic interpretation methods on the analysis of faults. Fault analysis refers to fault length, displacement, and the impact these factors have on geological modelling and hydrocarbon volume calculation workflows. This research was conducted to give geoscientists a better understanding of the importance of interpretation methods and the impact of unsuitable methology on geological analyses.
This article is included in the Encyclopedia of Geosciences
Jan Henninges, Evgeniia Martuganova, Manfred Stiller, Ben Norden, and Charlotte M. Krawczyk
Solid Earth, 12, 521–537, https://doi.org/10.5194/se-12-521-2021, https://doi.org/10.5194/se-12-521-2021, 2021
Short summary
Short summary
We performed a seismic survey in two 4.3 km deep geothermal research wells using the novel method of distributed acoustic sensing and wireline cables. The characteristics of the acquired data, methods for data processing and quality improvement, and interpretations on the geometry and structure of the sedimentary and volcanic reservoir rocks are presented. The method enables measurements at high temperatures and reduced cost compared to conventional sensors.
This article is included in the Encyclopedia of Geosciences
Matthias Bücker, Adrián Flores Orozco, Jakob Gallistl, Matthias Steiner, Lukas Aigner, Johannes Hoppenbrock, Ruth Glebe, Wendy Morales Barrera, Carlos Pita de la Paz, César Emilio García García, José Alberto Razo Pérez, Johannes Buckel, Andreas Hördt, Antje Schwalb, and Liseth Pérez
Solid Earth, 12, 439–461, https://doi.org/10.5194/se-12-439-2021, https://doi.org/10.5194/se-12-439-2021, 2021
Short summary
Short summary
We use seismic, electromagnetic, and geoelectrical methods to assess sediment thickness and lake-bottom geology of two karst lakes. An unexpected drainage event provided us with the unusual opportunity to compare water-borne measurements with measurements carried out on the dry lake floor. The resulting data set does not only provide insight into the specific lake-bottom geology of the studied lakes but also evidences the potential and limitations of the employed field methods.
This article is included in the Encyclopedia of Geosciences
Alireza Malehmir, Magdalena Markovic, Paul Marsden, Alba Gil, Stefan Buske, Lukasz Sito, Emma Bäckström, Martiya Sadeghi, and Stefan Luth
Solid Earth, 12, 483–502, https://doi.org/10.5194/se-12-483-2021, https://doi.org/10.5194/se-12-483-2021, 2021
Short summary
Short summary
A smooth transition toward decarbonization demands access to more minerals of critical importance. Europe has a good geology for many of these mineral deposits, but at a depth requiring sensitive, environmentally friendly, and cost-effective methods for their exploration. In this context, we present a sparse 3D seismic dataset that allowed identification of potential iron oxide resources at depth and helped to characterise key geological structures and a historical tailing in central Sweden.
This article is included in the Encyclopedia of Geosciences
Alba Zappone, Antonio Pio Rinaldi, Melchior Grab, Quinn C. Wenning, Clément Roques, Claudio Madonna, Anne C. Obermann, Stefano M. Bernasconi, Matthias S. Brennwald, Rolf Kipfer, Florian Soom, Paul Cook, Yves Guglielmi, Christophe Nussbaum, Domenico Giardini, Marco Mazzotti, and Stefan Wiemer
Solid Earth, 12, 319–343, https://doi.org/10.5194/se-12-319-2021, https://doi.org/10.5194/se-12-319-2021, 2021
Short summary
Short summary
The success of the geological storage of carbon dioxide is linked to the availability at depth of a capable reservoir and an impermeable caprock. The sealing capacity of the caprock is a key parameter for long-term CO2 containment. Faults crosscutting the caprock might represent preferential pathways for CO2 to escape. A decameter-scale experiment on injection in a fault, monitored by an integrated network of multiparamerter sensors, sheds light on the mobility of fluids within the fault.
This article is included in the Encyclopedia of Geosciences
Juvenal Andrés, Puy Ayarza, Martin Schimmel, Imma Palomeras, Mario Ruiz, and Ramon Carbonell
Solid Earth, 11, 2499–2513, https://doi.org/10.5194/se-11-2499-2020, https://doi.org/10.5194/se-11-2499-2020, 2020
Yi Zhang, Xinglin Lei, Tsutomu Hashimoto, and Ziqiu Xue
Solid Earth, 11, 2487–2497, https://doi.org/10.5194/se-11-2487-2020, https://doi.org/10.5194/se-11-2487-2020, 2020
Short summary
Short summary
Spatially continuous strain responses in two monitoring wells induced by a well-drilling process were monitored using high-resolution fiber-optic distributed strain sensing (DSS). The modeling results suggest that the strain polarities and magnitudes along the wellbores may be indicative of the layered-permeability structure or heterogeneous formation damage. The performance and value of DSS as a novel hydrogeophysical tool for in situ subsurface monitoring are emphasized.
This article is included in the Encyclopedia of Geosciences
Benjamin Schwarz and Charlotte M. Krawczyk
Solid Earth, 11, 1891–1907, https://doi.org/10.5194/se-11-1891-2020, https://doi.org/10.5194/se-11-1891-2020, 2020
Short summary
Short summary
Intricate fault and fracture networks cut through the upper crust, and their detailed delineation and characterization play an important role in the Earth sciences. While conventional geophysical sounding techniques only provide indirect means of detection, we present scale-spanning field data examples, in which coherent diffraction imaging – a framework inspired by optics and visual perception – enables the direct imaging of these crustal features at an unprecedented spatial resolution.
This article is included in the Encyclopedia of Geosciences
Laurent Guillou-Frottier, Hugo Duwiquet, Gaëtan Launay, Audrey Taillefer, Vincent Roche, and Gaétan Link
Solid Earth, 11, 1571–1595, https://doi.org/10.5194/se-11-1571-2020, https://doi.org/10.5194/se-11-1571-2020, 2020
Short summary
Short summary
In the first kilometers of the subsurface, temperature anomalies due to heat conduction rarely exceed 20–30°C. However, when deep hot fluids in the shallow crust flow upwards, for example through permeable fault zones, hydrothermal convection can form high-temperature geothermal reservoirs. Numerical modeling of hydrothermal convection shows that vertical fault zones may host funnel-shaped, kilometer-sized geothermal reservoirs whose exploitation would not need drilling at depths below 2–3 km.
This article is included in the Encyclopedia of Geosciences
Joseph Doetsch, Hannes Krietsch, Cedric Schmelzbach, Mohammadreza Jalali, Valentin Gischig, Linus Villiger, Florian Amann, and Hansruedi Maurer
Solid Earth, 11, 1441–1455, https://doi.org/10.5194/se-11-1441-2020, https://doi.org/10.5194/se-11-1441-2020, 2020
Cited articles
Adamson, A. W.: Physical
Chemistry of Surfaces, John Wiley and sons, New York, 1976.
Ageeva, O. A., Svetov, B. S., Sherman, G. K.,
and Shipulin, V.: E-effect in rocks, Russ. Geol. Geophys., 64,
1349–1356, 1999.
Ahmad, M.: A laboratory study of streaming potentials, Geophys. Prospect.,
XII, 49–64, 1964.
Aki K. and Richards, P. G.: Quantitative Seismology, University Science,
Sausalito, CA, 2002.
Alkafeef, S. and Alajmi, A.: Streaming potentials and conductivities of
reservoir rock cores in aqueous and non-aqueous liquids, Colloid. Surface. A,
289, 141–148, https://doi.org/10.1016/j.colsurfa.2006.04.023, 2006.
Allègre, V., Jouniaux, L., Lehmann, F., and Sailhac, P.: Streaming
potential dependence on water-content in Fontainebleau sand, Geophys. J.
Int., 182, 1248–1266, https://doi.org/10.1111/j.1365-246X.2010.04716.x, 2010.
Allègre, V., Jouniaux, L., Lehmann, F., and Sailhac, P.: Reply to the
comment by A. Revil and N. Linde on: “Streaming potential
dependence on water-content in Fontainebleau sand”, edited by: Allègre,
V., Jouniaux, L., Lehmann, F., and Sailhac, P., Geophys. J. Int., 186,
115–117, 2011.
Allègre, V., Lehmann, F., Ackerer, P., Jouniaux, L., and Sailhac, P.:
Modelling the streaming potential dependence on water content during
drainage: 1. A 1D modelling of SP using finite element method,
Geophys. J. Int., 189, 285–295, https://doi.org/10.1111/j.1365-246X.2012.05371.x, 2012.
Allègre, V., Jouniaux, L., Lehmann, F., Sailhac, P., and Toussaint, R.:
Influence of water pressure dynamics and fluid flow on the
streaming-potential response for unsaturated conditions, Geophys. Prospect.,
63, 694–712, https://doi.org/10.1111/1365-2478.12206, 2015.
Archie, G. E.: The electrical resistivity log as an aid in determining some
reservoir characteristics, Trans. AIME, 146, 54–62, 1942.
Auriault, J. and Strzelecki, T.: On the electro-osmotic flow in saturated
porous media, Int. J. Engrg. Sci., 19, 915–928, 1981.
Barrière, J., Bordes, C., Brito, D., Sénéchal, P., and Perroud, H.:
Laboratory monitoring of P waves in partially saturated sand, Geophys. J.
Int., 191, 1152–1170, 2012.
Beamish, D.: Characteristics of near surface electrokinetic coupling,
Geophys. J. Int., 137, 231–242, 1999.
Beamish, D. and Peart, R. J.: Electrokinetic geophysics – a review, Terra
Nova, 10, 48–55, 1998.
Beddiar, K., Berthaud, Y., and Dupas, A.: Experimental verification of the
Onsager's reciprocal relations for electro-osmosis and electro-filtration
phenomena on a saturated clay, CR Mecanique, 330, 893–898, 2002.
Biot, M. A.: Theory of propagation of elastic waves in a fluid-saturated
porous solid: I. Low frequency range, J. Acoust. Soc. Am., 28, 168–178,
1956a.
Biot, M. A.: Theory of
propagation of elastic waves in a fluid-saturated porous solid: II. High
frequency range, J. Acoust. Soc. Am., 28, 178–191, 1956b.
Biot, M. A.: Mechanics of deformation
and acoustic propagation in porous media, J. Appl. Phys., 34,
36–40, 1962.
Block, G. I. and Harris, J. G.: Conductivity dependence of seismoelectric
wave phenomena in fluid-saturated sediments, J. Geophys. Res., 111, B01304,
https://doi.org/10.1029/2005JB003798, 2006.
Bolève, A., Revil, A., Janod, F., Mattiuzzo, J. L., and Jardani, A.:
Forward Modeling and validation of a new formulation to compute
self-potential signals associated with ground water flow, Hydrol. Earth Syst.
Sci., 11, 1661–1671, https://doi.org/10.5194/hess-11-1661-2007, 2007.
Bordes, C., Jouniaux, L., Dietrich, M., Pozzi, J.-P., and Garambois, S.:
First laboratory measurements of seismo-magnetic conversions in fluid-filled
Fontainebleau sand, Geophys. Res. Lett., 33, L01302,
https://doi.org/10.1029/2005GL024582, 2006.
Bordes, C., Jouniaux, L., Garambois, S., Dietrich, M., Pozzi, J.-P., and
Gaffet, S.: Evidence of the theoretically predicted seismo-magnetic
conversion, Geophys. J. Int., 174, 489–504, 2008.
Bordes, C., Sénéchal, P., Barrière, J., Brito, D., Normandin, E., and
Jougnot, D.: Impact of water saturation on seismoelectric transfer
functions:a laboratory study of coseismic phenomenon, Geophys. J. Int., 200,
1317–1335, https://doi.org/10.1093/gji/ggu464, 2015.
Brekhovskikh, L. M.: Waves in Layered Media, Academic, New York, 1960.
Briggs, D.: The detemination of the zeta-potential on cellulose-a method, J.
Phys. Chem., 32, 641–675, 1928.
Butler, K.: Seismoelectrics effects of electrokinetic origin, PhD thesis,
Univ. B. C., Vancouver, Canada, 1996.
Butler, K., Russell, R., Kepic, A., and
Maxwell, M.: Measurements of the seismoelectric response from a
shallow boundary, Geophysics, 61, 1769–1778, 1996.
Butler, K., Dupuis, J., and Kepic, A.: Signal to noise improvements
in seismoelectrics data acquisition, J. Phys. Chem. C, 111,
3753–3755,
https://doi.org/10.1021/jp070060s, 2007.
Butler, K. E. and
Russell, R. D.: Substraction of powerline harmonics from geophysical
records, Geophysics, 58, 898–903, 1993.
Butler, K. E. and
Russell, R. D.: Cancellation of multiple harmonic noise series in
geophysical records, Geophysics, 68, 1083–1090, 2003.
Chandler, R.: Transient
streaming potential measurements on fluid-saturated porous
structures: an experimental verification of Biot's slow wave in
the quasi-static limit, J. Acoust. Soc. Am., 70, 116–121,
1981.
Chen, B. and Mu, Y.:
Experimental studies of seismoelectric effects in fluid-saturated
porous media, J. Geophys. Eng., 2, 222–230,
https://doi.org/10.1088/1742-2132/2/3/006, 2005.
Cooke, C. E.: Study of electrokinetic
effects using sinusoidal pressure and voltage, J. Chem. Phys., 23,
2299–2303, 1955.
Davis, J. and Kent, D.:
Surface complexation modeling in aqueous geochemistry, Reviews in Mineralogy
and Geochemistry, 23, 177–260, 1990.
Davis, J. A., James, R. O., and Leckie, J.: Surface ionization and
complexation at the oxide/water interface, J. Colloid Interf. Sci.,
63, 480–499, 1978.
Dean, T., Dupuis, C., Herrmann, R., and
Valuri, J.: A brute-strength approach to improving the quality of
seismoelectric data, SEG Annual meeting, 4–9 November, Las Vegas, 1–4,
https://doi.org/10.1190/segam2012-0222.1, 2012.
Debye, P. and Huckel, E.:
On the theory of electrolytes. I. Freezing point depression and
related phenomena, Phys. Z., 24, 185–206, 1923.
Dukhin, S. S. and
Derjaguin, B. V.: Surface and Colloid Science, edited by:
Matijevic, E., John Wiley and Sons, New York, 1974.
Dupuis, J. C. and
Butler, K. E.: Vertical seismoelectric profiling in a borehole
penetrating glaciofluvial sediments, Geophys. Res. Lett., 33, L16301,
https://doi.org/10.1029/2006GL026385, 2006.
Dupuis, J. C., Butler, K. E., and Kepic, A. W.: Seismoelectric imaging of the
vadose zone of a sand aquifer, Geophysics, 72, A81–A85,
https://doi.org/10.1190/1.2773780, 2007.
Dupuis, J. C., Butler, K. E., Kepic, A. W., and Harris, B. D.:
Anatomy of a seismoelectric conversion: measurements and conceptual modeling
in boreholes penetrating a sandy aquifer, J. Geophys. Res.-Sol. Ea., 114,
B10306, https://doi.org/10.1029/2008JB005939, 2009.
Dutta, N. C. and Odé, H.: Seismic reflection from a gas water contact,
Geophysics, 48, 148–162, 1983.
Fourie, F.: Aspects of the lateral
and vertical resolution of surface electroseismic data with
implications for groundwater exploration in fractured Karoo rocks,
S. Afr. J. Geol., 109, 571–584, 2006.
Fourie, F. and
Botha, J.: The failure of the sounding assumption in electroseismic
investigations, in: Proceedings of the 7th SAGA Biennial Technical
Meeting and Exhibition, 9–12 October, Drakensberg, 2001.
Fourie, F., Botha, J., Grobbelaar, R., and van
Tonder, G.: Application of the electrokinetic sounding technique for
geohydrological investigations in a fractured rock aquifer system,
in: Proceedings of the XXX IAH Congress on groundwater: past
achievements and future challenges, edited by: Sililo, O., Cape
Town, 26 November– 1 December, A. A. Balkema,
135–140, 2000.
Frenkel, J.: On the theory of
seismic and electroseismic phenomena in a moist
soil, J. Phys., 8,
230–241, 1944.
Frenkel, J.: On the theory of
seismic and seismoelectric phenomena in a moist
soil, J. Eng. Mech.-ASCE, 131, 879–887,
2005.
Gao, Y. and Hu, H.:
Seismoelectromagnetic waves radiated by a double couple source in a
saturated porous medium, Geophys. J. Int., 181, 873–896,
https://doi.org/10.1111/j.1365-246X.2010.04526.x, 2010.
Garambois, S. and
Dietrich, M.: Seismoelectric wave conversions in porous media: field
measurements and transfer function analysis, Geophysics, 66,
1417–1430, 2001.
Garambois, S. and
Dietrich, M.: Full waveform numerical simulations of
seismoelectromagnetic wave conversions in fluid-saturated stratified
porous media, J. Geophys. Res., 107, ESE 5–1,
https://doi.org/10.1029/2001JB000316, 2002.
Gaskarov, I. and Parkhomenko, E.: The seismoelectric effect in rocks
and the preconditions for its application in geological prospecting
work, Izv.-Phys. Solid. Earth., 1, 71–74,
1974.
Gershenzon, N., Bambakidis, G., and Ternovskiy, I.: Coseismic electromagnetic
field due to the electrokinetic effect, Geophysics, 79, E217–E229,
https://doi.org/10.1190/GEO2014-0125.1, 2014.
Gharibi, M., Bentley, L., Muller, J., and
Stewart, R.: Seismoelectric monitoring of producing oilfields: a
review, CREWES Research report, 15, 1–13, 2003.
Glover, P., Walker, E., Ruel, J., and Tardif, E.: Frequency-dependent
streaming potential of porous media
– Part 2: Experimental mesurement of unconsolidated materials,
Int. J. Geophys., 2012, 728495,
https://doi.org/10.1155/2012/728495, 2012.
Gouy, G.: About the electric charge on the surface of an electrolyte, J.
Phys. Radium A, 9, 457–468, 1910.
Grobbe, N. and Slob, E.: Validation of an electroseismic and seismoelectric
modeling code, for layered earth models, by the explicit homogeneous space
solutions, SEG Technical Program Expanded Abstracts 2013, 1847–1851,
https://doi.org/10.1190/segam2013-1208.1, 2013.
Grobbe, N. and Slob, E.: Seismoelectric interface response signal behaviour
in thin-bed geological settings, SEG Technical Program Expanded Abstracts
2014, 3428–3432, https://doi.org/10.1190/segam2014-0744.1, 2014.
Grobbe, N., Hunziker, J., and Slob, E.: Seismoelectric wave propagation
modeling for typical laboratory configurations: A numerical validation, SEG
Technical Program Expanded Abstracts 2014, 2072–2077,
https://doi.org/10.1190/segam2014-0689.1, 2014.
Grobbe, N., van der Neut, J., Slob, E., Wapenaar, K., Vidal, C., and
Drijkoningen, G.: Unified multi-depth-level field decomposition, Geophys.
Prospect., https://doi.org/10.1111/1365-2478.12290 online first, 2015.
Groves, J. and Sears, A.:
Alternating streaming current measurements, J. Colloid Interf. Sci.,
53, 83–89, 1975.
Guan, W. and Hu, H.:
Finite-difference modeling of the electroseismic logging in a
fluid-saturated porous formation, J. Comput. Phys., 227, 5633–5648,
2008.
Guan, W., Hu, H., and Wang, Z.: Permeability inversion from low-frequency
seismoelectric logs in fluid-saturated porous formations, Geophys. Prospect.,
61, 120–133, https://doi.org/10.1111/j.1365-2478.2012.01053.x, 2013.
Guglielmi, A., Tsegmed, B., Potapov, A., Kultima, I., and Raita, T.:
Seismomagnetic signals from the strong earthquake of Sumatra, Izvestiya,
Physics Solid Earth, 42, 921–927, 2006.
Guichet, X., Jouniaux, L., and Pozzi, J.-P.: Streaming potential of a sand
column in partial saturation conditions, J. Geophys. Res., 108, 2141,
https://doi.org/10.1029/2001JB001517, 2003.
Guichet, X., Jouniaux, L., and Catel, N.:
Modification of streaming potential by precipitation of calcite in a
sand-water system: laboratory measurements in the pH range from 4
to 12, Geophys. J. Int., 166, 445–460,
https://doi.org/10.1111/j.1365-246X.2006.02922.x, 2006.
Haartsen, M. W. and
Pride, S.: Electroseismic waves from point sources in layered
media, J. Geophys. Res., 102, 24745–24769, 1997.
Haartsen, M. W., Dong, W., and Toksöz, M. N.: Dynamic streaming
currents from seismic point sources in homogeneous poroelastic
media, Geophys. J. Int., 132, 256–274, 1998.
Haines, S.: Seismoelectric imaging
of shallow targets, PhD thesis, Stanford University,
2004.
Haines, S. H. and
Pride, S. R.: Seismoelectric numerical modeling on a grid,
Geophysics, 71, 57–65, 2006.
Haines, S. S., Guitton, A., Biondi, B., and Pride, S.: Development of
experimental methods in electroseismics, SEG Technical Program Expanded
Abstracts 2003, 560–563, https://doi.org/10.1190/1.1817987, 2003.
Haines, S. S., Guitton, A., and Biondi, B.:
Seismoelectric data processing for surface surveys of shallow
targets, Geophysics, 72, G1–G8,
https://doi.org/10.1190/1.2424542, 2007a.
Haines, S. S., Pride, S. R.,
Klemperer, S. L., and Biondi, B.: Seismoelectric imaging of shallow
targets, Geophysics, 72, G9–G20,
https://doi.org/10.1190/1.2428267, 2007b.
Han, Q. and Wang, Z.:
Time-domain simulation of SH-wave-induced electromagnetic field in
heterogeneous porous media: A fast finite element algorithm,
Geophysics, 66, 448–461, https://doi.org/10.1190/1.1444936, 2001.
Honkura, Y., Matsushima, M., Oshiman, N., Tuncer, M., Baris, S., Ito, A., and
Iio, Y.: Small electric and magnetic signals observed before the arrival of
seismic wave, Earth Planets Space, 54, e9–e12, 2002.
Hornbostel, S. and Thompson, A.: Waveform design for electroseismic
exploration, 75th SEG Annual International Meeting, Nov6-11, Houston, Expanded Abstract, 1–4, 2005.
Hornbostel, S. and Thompson, A.: Waveform design for electroseismic
exploration, Geophysics, 72, Q1–Q10. 2007.
Hu, H. and Gao, Y.: Electromagnetic
field generated by a finite fault due to electrokinetic
effect, J. Geophys. Res., 116, 1132–1143, 2011.
Hu, H. and Liu, J.: Simulation of
the converted electric field during acoustoelectric logging, 72nd
SEG Annual International Meeting,Salt Lake City, 6–11 October, Expanded Abstracts, 21, 348–351,
https://doi.org/10.1029/2001JB001517, 2002.
Hu, H. and Wang, K.: Simulation of
an acoustically induced electromagnetic field in a borehole embedded
in a porous formation, Borehole Acoustics and Logging Reservoir
Delineation consortis, Annual Report, Earth Resources Laboratory Industry Consortia Annual Report 2000–13, MIT,
available at: http://hdl.handle.net/1721.1/75724 (last access: 20 August 2015), 13-1–13-20,
2000.
Hu, H.,
Guan, W., and Harris, J.: Theoretical simulation of electroacoustic
borehole logging in a fluid-saturated porous
formation, J. Acoust. Soc. Am., 122, 135–145, 2007.
Hunt, C. W. and Worthington, M. H.: Borehole elektrokinetic
responses in fracture dominated hydraulically conductive zones,
Geophys. Res. Lett., 27, 1315–1318, 2000.
Hunter, R.: Zeta Potential in
Colloid Science: Principles and Applications, Academic Press, New
York, 1981.
Ishido, T. and
Mizutani, H.: Experimental and theoretical basis of electrokinetic
phenomena in rock water systems and its applications to
geophysics, J. Geophys. Res., 86, 1763–1775, 1981.
Ivanov, A.: Effect of electrization
of earth layers by elastic waves passing through them, Doklady
Akademii Nauk SSSR, 24, 42–45, 1939 (in Russian).
Jaafar, M. Z., Vinogradov, J., and
Jackson, M. D.: Measurement of streaming potential coupling
coefficient in sandstones saturated with high salinity NaCl brine,
Geophys. Res. Lett., 36, L21306,
https://doi.org/10.1029/2009GL040549,
2009.
Jackson, M. D.: Characterization
of multiphase electrokinetic coupling using a bundle of capillary
tubes model, J. Geophys. Res., 113, B04201,
https://doi.org/10.1029/2007JB005490, 2008.
Jackson, M. D.: Multiphase
electrokinetic coupling: insights into the impact of fluid and
charge distribution at the pore scale from a bundle of capillary
tubes model, J. Geophys. Res., 115, B07206,
https://doi.org/10.1029/2009JB007092, 2010.
Jardani, A., Revil, A., Slob, E., and
Söllner, W.: Stochastic joint inversion of 2D seismic and
seismoelectric signals in linear poroelastic materials: a numerical
investigation, Geophysics, 75, N19–N31,
https://doi.org/10.1190/1.3279833, 2010.
Johnson, D. L., Koplik, J., and Dashen, R.: Theory of dynamic
permeability in fluid saturated porous media, J. Fluid Mech., 176,
379–402, 1987.
Johnston, M., Sasai, Y., Egbert, G., and Mueller, R.: Seismomagnetic effects
from the long-awaited 28 September 2004 M 6.0 Parkfield earthquake,
B. Seismol. Soc. Am., 96, S206–S220, https://doi.org/10.1785/0120050810, 2006.
Jouniaux, L.: Electrokinetic
techniques for the determination of hydraulic conductivity, in:
Hydraulic Conductivity – Issues, Determination and Applications,
edited by: Elango, L., In Tech Publisher, Rijeka, ISBN 978-953-307-288-3, 307–328,
2011.
Jouniaux, L. and
Bordes, C.: Frequency-dependent streaming potentials: a
review, Int. J. Geophys., 2012, 648781,
https://doi.org/10.1155/2012/648781, 2012.
Jouniaux, L. and
Ishido, T.: Electrokinetics in earth sciences: a tutorial,
Int. J. Geophys., 2012, 286107,
https://doi.org/10.1155/2012/286107, 2012.
Jouniaux, L. and Pozzi, J.-P.: Permeability dependence of streaming potential
in rocks for various fluid conductivity, Geophys. Res. Lett., 22, 485–488,
1995.
Jouniaux, L. and
Pozzi, J.-P.: Laboratory measurements anomalous 0.1–0.5 Hz
streaming potential under geochemical changes: implications for
electrotelluric precursors to earthquakes, J. Geophys. Res., 102,
15335–15343, 1997.
Jouniaux, L. and Zyserman, F.: Interactive comment on “Seismo-electrics,
electro-seismics, and seismo-magnetics for earth
sciences”, Author reply to comment of A. Revil, Solid Earth Discuss., 7,
C1274–C1274, http://www.solid-earth-discuss.net/7/C1274/2015/sed-7-C1274-2015.pdf, 2015.
Jouniaux, L., Lallemant, S., and Pozzi, J.:
Changes in the permeability, streaming potential and resistivity of
a claystone from the Nankai prism under stress,
Geophys. Res. Lett., 21, 149–152, 1994.
Jouniaux, L., Pozzi, J.-P., Berthier, J., and
Massé, P.: Detection of fluid flow variations at the Nankai
Trough by electric and magnetic measurements in boreholes or at the
seafloor, J. Geophys. Res., 104, 29293–29309, 1999.
Jouniaux, L., Bernard, M.-L., Zamora, M., and
Pozzi, J.-P.: Streaming potential in volcanic rocks from Mount
Peleé, J. Geophys. Res., 105, 8391–8401, 2000.
Jouniaux, L., Maineult, A., Naudet, V.,
Pessel, M., and Sailhac, P.: Review of self-potential methods in
Hydrogeophysics, C. R. Geosci., 341, 928–936,
https://doi.org/10.1016/j.crte.2009.08.008, 2009.
Kepic, A. and Rosid, M.:
Enhancing the seismoelectric method via a virtual shot gather, 74th SEG
Technical Program Expanded Abstracts, Denver, October, 1337–1340,
https://doi.org/10.1190/1.2428267, 2004.
Kröger, B., Yaramanci, U., and Kemna, A.:
Numerical analysis of seismoelectric wave propagation in spatially
confined geological units, Geophys. Prospect., 62, 133–147,
https://doi.org/10.1111/1365-2478.12020, 2014.
Kulessa, B., Murray, T., and Rippin, D.: Active seismoelectric
exploration of glaciers, Geophys. Res. Lett., 33, L07503,
https://doi.org/10.1029/2006GL025758, 2006.
Li, S.,
Pengra, D., and Wong, P.: Onsager's reciprocal relation and the
hydraulic permeability of porous media, Phys. Rev. E, 51,
5748–5751, 1995.
Liu, Z., Yuan, L., Zhang, X., Liu, Z., and Wu, H.: A laboratory
seismoelectric measurement for the permafrost model with a
frozen–unfrozen interface, Geophys. Res. Lett., 35, L21404,
https://doi.org/10.1029/2008GL035724, 2008.
Long, L. T. and
Rivers, W. K.: Field measurement of the electroseismic response,
Geophysics, 40, 233–245, 1975.
Lorne, B., Perrier, F., and Avouac, J.-P.: Streaming potential
measurements. 1. Properties of the electrical double layer from
crushed rock samples, J. Geophys. Res., 104, 17857–17877, 1999.
Løseth, L., Pedersen, H., Ursin, B., Amundsen, L., and Ellingsrud, S.:
Low-frequency electromagnetic fields in applied geophysics: Waves or
diffusion?, Geophysics, 71, W29–W40, 2006.
Luong, D. and Sprik, R.: Examination of a theoretical model of streaming
potential coupling coefficient, Int. J. Geophys., 2014,
471819, https://doi.org/10.1155/2014/471819, 2014.
Maas, P., Grobbe, N., Slob, E., and Mulder, W.: Electromagnetic and
seismoelectric sensitivity analysis using resolution functions,
edited by: Hellmich, C., Pichler, B., and Adam, D.,
77th EAGE Conference & Exhibition, Madrid, Spain, 1 June 2015, https://doi.org/10.3997/2214-4609.201413076, 2015.
Mahardika, H., Revil, A., and
Jardani, A.: Waveform joint inversion of seismograms and
electrograms for moment tensor characterization of fracking events,
Geophysics, 77, ID23–ID39, 2012.
Maineult, A., Jouniaux, L., and
Bernabé, Y.: Influence of the mineralogical composition on the
self-potential response to advection of KCl concentration fronts
through sand, Geophys. Res. Lett., 33, L24311, https://doi.org/10.1029/2006GL028048,
2006.
Markov, M. and
Verzhbitskiy, V.: Simulation of the electroseismic effect produced
by an acoustic multipole source in a fluid-filled borehole, SPWLA
45th Annual Logging Symposium, Society of Petrophysicists and
Well-Log Analysts (Pubs), 6–9 June, Noordwijk, 1–11, 2004.
Markov, M. and
Verzhbitskiy, V.: Electroseismic waves from acoustic source in a
fluid-filled borehole, in: Poromechanics II Biot Centennial
(1905–2005), edited by: Abousleiman, Y. N., Cheng, A. I. D., and Ulm, F. J.,
A. A. Balkema, Taylor and Francis Group, London, UK, 283–288, 2005.
Martner, S. T. and
Sparks, N. R.: The electroseismic effect, Geophysics, 24, 297–308,
1959.
Matsushima, M., Y.Honkura, Oshiman, N., Baris, S., Tuncer, M., Tank, S.,
Celik, C., Takahashi, F., Nakanishi, M., Yoshimura, R., Pektas, R., Komut,
T., Tolak, E., Ito, A., Iio, Y., and Isikara, A.: Seismoelectromagnetic
effect associated with the Izmit earthquake and its aftershocks, B.
Seismol. Soc. Am., 92, 350–360, 2002.
McBain, J., Peaker, C., and King, A.: Absolute measurements of the
surface conductivity near the boundary of optically polished glass
ans solutions of potassium chloride, J. Am. Chem. Soc., 51,
3294–3312, 1929.
Migunov, N. and
Kokorev, A.: Dynamic properties of the seismoelectric effect of
water-saturated rocks, Izvestiya, Earth Physics, 13, 443–445, 1977.
Mikhailov, O. V., Haartsen, M. W., and
Toksöz, M. N.: Electroseismic investigation of the shallow
subsurface: field measurements and numerical modeling, Geophysics,
62, 97–105, 1997.
Mikhailov, O. V., Queen, J., and Toksöz, M. N.: Using borehole
electroseismic measurements to detect and characterize fractured (permeable)
zones, Geophysics, 65, 1098–1112, 2000.
Miller, D.: Thermodynamics of irreversible processes, The experimental
verification of Onsager reciprocal relations, Chem. Rev., 60, 15–37, 1960.
Mogi, T., Tanaka, D., Widarto, E., Arsadi, N., Puspito, T., Nagao, W., and
Uyeda, S.: Geoelectric potential difference monitoring in southern Sumatra,
Indonesia – Coseismic change, Earth, Planets and Space, 52, 245–252,
2000.
Morgan, F. D., Williams, E. R., and Madden, T. R.: Streaming
potential properties of westerly granite with
applications, J. Geophys. Res., 94, 12449–12461, 1989.
Mualem, Y.: A new model for predicting the hydraulic conductivity of
unsaturated porous media, Water Resour. Res., 12, 513–522, 1976.
Neev, J. and Yeatts, F. R.:
Electrokinetic effects in fluid-saturated poroelastic media,
Phys. Rev. B, 40, 9135–9141,
1989.
Neishtadt, N. M., Eppelbaum, L. V., and
Levitski, A. G.: Case History. Application of piezoelectric and
seismoelectrokinetic phenomena in exploration geophysics: review of
Russian and Israeli experiences, Geophysics, 71, B41–B53,
2006.
Onsager, L.: Reciprocal relations
in irreversible processes: I, Phys. Rev., 37, 405–426,
1931.
Overbeek, J. T. G.:
Electrochemistry of the double layer, in: Colloid Science,
Irreversible Systems, edited by: Kruyt, H. R., Elsevier, Amsterdam, 115–193,
1952.
Packard, R. G.: Streaming
potentials across capillaries for sinusoidal
pressure, J. Chem. Phys., 1, 303–307, 1953.
Pain, C.,
Saunders, J. H., Worthington, M. H., Singer, J. M.,
Stuart-Bruges, C. W., Mason, G., and Goddard, A.: A mixed
finite-element method for solving the poroelastic Biot equations
with electrokinetic coupling, Geophys. J. Int., 160, 592–608,
2005.
Parkhomenko, E. and Gaskarov, I.: Borehole and laboratory studies of
the seismoelectric effect of the second kind in rocks,
Izv. Akad. Sci. USSR, Physics Solid Earth, 9, 663–666, 1971.
Parkhomenko, E. and Topchyan, K.: Influence of high-conducting
component on the magnitude os seismoelectric effect, Physics of the Solid Earth, 30,
727–732, 1995.
Parkhomenko, I. and Tsze-San, C.: A study of the influence of
moisture on the magnitude of the seismoelectric effect in
sedimentary rocks by a laboratory method, Bull. (Izv.) Acad. Sci.,
USSR, Geophys. Ser., 115–118, 1964.
Parks, G.: The isoelectric points of
solid oxides, solid hydroxides, and aqueous hydroxo-complex,
Chem. Rev., 65, 177–198, 1965.
Paterson, M.: The equivalent channel model for permeability and resistivity
in fluid-saturated rock – a re-appraisal, Mech. Mater., 2, 345–352, 1983.
Pengra, D. B., Li, S. X., and Wong, P.-Z.: Determination of rock
properties by low frequency AC electrokinetics, J. Geophys. Res.,
104, 29485–29508, 1999.
Perrier, F. and
Froidefond, T.: Electrical conductivity and streaming potential
coefficient in a moderately alkaline lava series, Earth
Planet. Sc. Lett., 210, 351–363,
https://doi.org/10.1016/S0012-821X(03)00105-5, 2003.
Perrier, F. and Morat, P.: Characterization of electrical daily variations
induced by capillary flow in the non-saturated zone, Pure Appl. Geophys.,
157, 785–810, 2000.
Pozzi, J.-P. and Jouniaux, L.: Electrical effects of fluid circulation in
sediments and seismic prediction, C. R. Acad. Sci. Paris, serie II, 318,
73–77, 1994.
Pride, S.: Governing equations for the coupled electromagnetics and
acoustics of porous media, Phys. Rev. B, 50, 15678–15695,
1994.
Pride, S. and Garambois, S.: Electroseismic wave theory of Frenkel and more
recent developments, J. Eng. Mech.-ASCE, 131, 697–706, 2005.
Pride, S. and Haartsen, M. W.: Electroseismic wave
properties, J. Acoust. Soc. Am., 100, 1301–1315, 1996.
Pride, S. and
Morgan, F. D.: Electrokinetic dissipation induced by seismic waves,
Geophysics, 56, 914–925, 1991.
Quincke, G.: Uber die
Fortfuhrung materieller Teilchen durch stromende Elektricitat,
Annalen der Physik und Chemie 113, 513–598, 1861.
Ren, H.,
Huang, Q., and Chen, X.: A new numerical technique for simulating
the coupled seismic and electromagnetic waves in layered porous
media, Earthquake Science, 23, 167–176, 2010.
Ren, H.,
Chen, X., and Huang, Q.: Numerical simulation of coseismic
electromagnetic fields associated with seismic waves due to finite
faulting in porous media, Geophys. J. Int., 188, 925–944,
2012.
Ren, H., Wen, J., Huang, Q., and Chen, X.: Electrokinetic effect combined
with surface-charge assumption: a possible generation mechanism of coseismic
EM signals, Geophys. J. Int., 200, 837–850, https://doi.org/10.1093/gji/ggu435,
2015.
Reppert, P. and Morgan, F.: Temperature-dependent streaming
potentials: 1. Theory, J. Geophys. Res., 108, 2546,
https://doi.org/10.1029/2002JB001754, 2003a.
Reppert, P. and Morgan, F.: Temperature-dependent streaming
potentials: 2. Laboratory, J. Geophys. Res., 108, 2547,
https://doi.org/10.1029/2002JB001755, 2003b.
Reppert, P. M., Morgan, F. D.,
Lesmes, D. P., and Jouniaux, L.: Frequency-dependent streaming
potentials, J. Colloid Interf. Sci., 234, 194–203,
https://doi.org/10.1006/jcis.2000.7294, 2001.
Reuss, F.: Sur un nouvel effet de
l'éléctricité galvanique, Mémoires de la société
impériale des naturalistes de Moscou, 2, 326–337, 1809.
Revil, A. and Cerepi, A.:
Streaming potentials in two-phase flow conditions,
Geophys. Res. Lett., 31, L11605, https://doi.org/10.1029/2004GL020140, 2004.
Revil, A. and Glover, P.:
Nature of surface electrical conductivity in natural sands,
sandstones, and clays, Geophys. Res. Lett., 25, 691–694,
1998.
Revil, A. and Jardani, A.: Seismoelectric response of heavy oil reservoirs:
theory and numerical modelling, Geophys. J. Int., 180, 781–797,
https://doi.org/10.1111/j.1365-246X.2009.04439.x, 2010.
Revil, A. and Linde, N.: Chemico-electromechanical coupling in microporous
media, J. Colloid Interface Sci., 302, 682–694, 2006.
Revil, A. and Mahardika, H.: Coupled hydromechanical and electromagnetic
disturbances in unsaturated porous materials, Water Resour. Res., 49,
744–766, 2013.
Revil, A., Linde, N., Cerepi, A.,
Jougnot, D., Matthäi, S., and Finsterle, S.: Electrokinetic
coupling in unsaturated porous media, J. Colloid Interf. Sci., 313,
315–327, 2007.
Russell, R. D., Butler, K. E., Kepic, A. W., and
Maxwell, M.: Seismoelectric exploration, Leading
Edge, 16, 1611–1615, 1997.
Rutgers, A.: Streaming effects
and surface conduction. Streaming potentials and surface
conductance, T. Faraday Soc., 35, 69–80,
https://doi.org/10.1039/TF9403500069, 1940.
Santos, J., Zyserman, F., and
Gauzellino, P.: Numerical electroseismic modeling: a finite
element approach, Appl. Math. Comput., 218, 6351–6374,
2012.
Santos, J. E.: Finite element
approximation of coupled seismic and electromagnetic waves in
fluid-saturated poroviscoelastic media, Numer. Meth. Part. D. E.,
27, 351–386, 2009.
Schakel, M. and
Smeulders, D.: Seismoelectric reflection and transmission at a
fluid/porous-medium interface, J. Acoust. Soc. Am., 127, 13–21,
2010.
Schakel, M., Smeulders, D., Slob, E., and
Heller, H.: Seismoelectric interface response: experimental results
and forward model, Geophysics, 76, N29–N36,
https://doi.org/10.1190/1.3592984, 2011.
Schakel, M., Smeulders, D., Slob, E., and
Heller, H.: Seismoelectric fluid/porous-medium interface response
model and measurements, Transport Porous Med., 93, 271–282,
https://doi.org/10.1007/s11242-011-9869-8, 2012.
Schoemaker, F., Smeulders, D., and Slob, E.:
Simultaneous determination of dynamic permeability and streaming
potential, SEG expanded abstracts, 26, 1555–1559, 2007.
Schoemaker, F., Smeulders, D., and Slob, E.:
Electrokinetic effect: theory and measurement, SEG Technical Program
Expanded Abstracts, 9–14 November, Las Vegas, 1645–1649,
2008.
Schoemaker, F., Grobbe, N., Schakel, M., de Ridder, S., Slob, E., and
Smeulders, D.: Experimental validation of the electrokinetic theory and
development of seismoelectric interferometry by cross-correlation,
International J. Geophys., 2012, 514242,
https://doi.org/10.1155/2012/514242, 2012.
Sears, A. and Groves, J.:
The use of oscillating laminar flow streaming potential measurements
to determine the zeta potential of a capillary surface, J. Colloid
Interf. Sci., 65, 479–482, 1978.
Sénéchal, P., Garambois, S., and
Bordes, C.: Feasibility of acoustic imaging for in-situ
characterization of subsurface soil injected with fresh
mortar, J. Appl. Geophys., 72, 184–193, 2010.
Singarimbun, A., Srigutomo, W.,
Fauzi, U., and Sunarya, A.: An application of numerical simulation
in a seismoelectric phenomena by using transfer function, in:
Proceedings of the Third Asian Physics Symposium
APS, 22–23 July, Bandung,
189–193, 2009.
Singer, J., Saunders, J., Holloway, L., Stoll, J., Pain, C.,
Stuart-Bruges, W., and Mason, G.: Electrokinetic logging has the
potential to measure the permeability, Society of Petrophysicists
and Well Log Analysts, 46th Annual Logging
Symposium, 26–29 June New Orleans, 2005.
Smeulders, D., Eggels, R., and van
Dongen, M.: Dynamic permeability: reformulation of theory and new
experimental and numerical data, J. Fluid Mech., 245, 211–227,
1992.
Smeulders, D., Grobbe, N., Heller, H., and
Schakel, M.: Seismoelectric conversion for the detection of porous
medium interfaces between wetting and nonwetting fluids, Vadose
Zone J., 13, https://doi.org/10.2136/vzj2013.06.0106, 2014.
Sposito, G.: The Chemistry of
Soils, Oxford University, Oxford, 1989.
Stern, O.: Zur Theorie der electrolytischen Doppelschicht,
Z. Electrochem., 30, 508–516, 1924 (in German).
Strahser, M., Jouniaux, L., Sailhac, P.,
Matthey, P.-D., and Zillmer, M.: Dependence of seismoelectric
amplitudes on water-content, Geophys. J. Int., 187, 1378–1392,
2011.
Strahser, M. H. P., Rabbel, W., and
Schildknecht, F.: Polarisation and slowness of seismoelectric
signals: a case study, Near Surf. Geophys., 5, 97–114, 2007.
Szarka, L.: Geophysical aspects of
man-made electromagnetic noise in the earth – a review,
Surv. Geophys., 9, 287–318, 1987.
Tardif, E., Glover, P., and Ruel, J.: Frequency-dependent streaming
potential of Ottawa sand, J. Geophys. Res., 116, B04206,
https://doi.org/10.1029/2010JB008053, 2011.
Thompson, A., Hornbostel, S., Burns, J.,
Murray, T., Raschke, R., Wride, J., McCammon, P., Sumner, J.,
Haake, G., Bixby, M., Ross, W., White, B., Zhou, M., and Peczak, P.:
Field tests of electroseismic hydrocarbon detection, SEG Technical
Program Expanded Abstracts, 565–568, 2005.
Thompson, A., Sumner, J., and
Hornbostel, S.: Electromagnetic-to-seismic conversion: a new direct
hydrocarbon indicator, Leading Edge, 26, 428–435, 2007.
Thompson, A. H. and
Gist, G. A.: Geophysical applications of electrokinetic conversion,
Leading Edge, 12, 1169–1173, 1993.
Thompson, R. R.: A note on the
seismic-electric effect, Geophysics, 4, 102–103, 1939.
Thyssen, S. V., Hummel, J., and Rülke, O.:
Die Ursachen des seismisch-elektrischen
Effektes, Z. Geophs., 13, 112–119, 1937.
Tosha, T., Matsushima, N., and Ishido, T.: Zeta potential measured
for an intact granite sample at temperatures to 200° C,
Geophys. Res. Lett., 30, 1295, https://doi.org/10.1029/2002GL016608, 2003.
Urban, F. and White, H.:
Application of the double layer theory of Otto
Stern. I, J. Phys. Chem., 36, 3157–3161, 1932.
Valuri, J., Dean, T., and Dupuis, J.: Seismoelectric acquisition in
an arid environment, 22nd International Geophysical Conference and
Exhibition, 26–29 February 2012, Brisbane, 2012.
VanCappellen, P., Charlet, L.,
Stumm, W., and Wersin, P.: A surface complexation model of the
carbonate mineral-aqueous solution interface,
Geochim. Cosmochim. Acta, 57, 3505–3518, 1993.
Vinogradov, J., Jaafar, M., and
Jackson, M. D.: Measurement of streaming potential coupling
coefficient in sandstones saturated with natural and artificial
brines at high salinity, J. Geophys. Res., 115, B12204,
https://doi.org/10.1029/2010JB007593, 2010.
von Helmholtz, H.:
Studien uber elektrische Grenzschichten, Annalen der Physik und
Chemie, Neue Folge, 7, 337–382, 1879 (in German).
Walker, E. and
Glover, P. W. J.: Permeability models of porous media:
characteristic length scales, scaling constants and time-dependent
electrokinetic coupling, Geophysics, 75, E235–E246,
https://doi.org/10.1190/1.3506561, 2010.
Wang, J. and Hu, H.: The
determination of electrokinetic coupling coefficient and zeta
potential of rock samples by electrokinetic measurements,
Adv. Mat. Res., 516–517, 1870–1873, 2012.
Wang, Z.,
Hu, H., and Guan, W.: Three-dimensional finite-difference
time-domain computation of the seismoelectric field generated by a
slipping fault, in: Poromechanics V: Proceedings of the Fifth Biot
Conference on Poromechanics, edited by: Hellmich, C., Pichler, B.,
and Adam, D., 2032–2041, 10–12 July, Vienna, 2013.
Warden, S., Garambois, S., Sailhac, P.,
Jouniaux, L., and Bano, M.: Curvelet-based seismoelectric data
processing, Geophys. J. Int., 190, 1533–1550,
https://doi.org/10.1111/j.1365-246X.2012.05587.x, 2012.
Warden, S., Garambois, S.,
Jouniaux, L., Brito, D., Sailhac, P., and Bordes, C.: Seismoelectric
wave propagation numerical modeling in partially saturated
materials, Geophys. J. Int., 194, 1498–1513,
https://doi.org/10.1093/gji/ggt198, 2013.
White, B. and Zhou, M.:
Electroseismic prospecting in layered media, SIAM J. Appl. Math.,
67, 69–98, 2006.
White, B. S.: Asymptotic theory of
electroseismic prospecting, SIAM J. Appl. Math., 65, 1443–1462,
2005.
White, H., Urban, F., and Monaghan, B.: The magnitude of surface
conductivity at aqueous-glass
interfaces, J. Phys. Chem., 45, 560–570, 1941.
Wiedemann, G.: Uber die Bewegung von Flüssigkeiten im Kreise der
geschlossenen galvanischen Saule, Annalen der Physik und
Chemie, 87, 321–352, 1852 (in German).
Xia, J. and Miler, D.: Design of a hum filter for suppressing
power-noise in seismic data, J. Environ. Eng. Geoph., 5, 31–38,
2000.
Yeh, C.,
Chen, S., Teng, T., and Lee, Y.: On formulation of a transition
matrix for electroporoelastic medium and application to analysis of
scattered electroseismic wave, J. Acoust. Soc. Am., 120, 3672,
2006.
Zhan, X., Chi, S., and Toksöz, M.:
Simulation of the converted electric field during multipole logging
while drilling (LWD), 76th SEG Annual International Meeting,
Expanded Abstracts, New Orleans, 1–6 October, 25, 446–450, 2006a.
Zhan, X., Zhu, Z., Chi, S., Rao, R.,
Burns, D., and Toksöz, M.: Elimination of LWD (Logging While
Drilling) Tool Modes, Technical Report MIT, Cambridge, United States, 1–32,
2006b.
Zhang, Y., Xiao, L., Chu, Z., and Li, J.: The converted
electromagnetic wave characteristics of seismoelectric conversion
effect in borehole, Chinese J. Geophys., 48, 501–508, 2005.
Zhou, J.,
Cui, Z., and Lü, W.: Seismoelectric waves in a borehole excited by
an external explosive source, Chinese Phys. B, 23,
014301-1–014301-6, 2014.
Zhu, Z. and Toksöz, M.:
Experimental measurements of the streaming potential and
seismoelectric conversion in Berea sandstone, Geophys. Prospect.,
61, 688–700, https://doi.org/10.1111/j.1365-2478.2012.01110.x,
2013.
Zhu, Z. and Toksöz, M. N.:
Crosshole seismoelectric measurements in borehole models with
fractures, Geophysics, 68, 1519–1524, 2003.
Zhu, Z., Haartsen, M. W., and Toksöz, M. N.: Experimental studies
of electrokinetic conversions in fluid-saturated borehole models,
Geophysics, 64, 1349–1356, 1999.
Zhu, Z., Haartsen, M. W., and Toksöz, M. N.: Experimental studies
of seismoelectric conversions in fluid-saturated porous
media, J. Geophys. Res., 105, 28055–28064, 2000.
Zhu, Z.,
Toksöz, M., and Burns, D.: Electroseismic and seismoelectric
measurements of rock sample in a water tank, Geophysics, 73,
E153–E164, https://doi.org/10.1190/1.2952570, 2008.
Zyserman, F., Gauzellino, P., and Santos, J.: Finite element
modeling of SHTE and PSVTM electroseismics, J. Appl. Geophys.,
72, 79–91, https://doi.org/10.1016/j.jappgeo.2010.07.004, 2010.
Zyserman, F., Gauzellino, P., and
Santos, J.: Numerical evidence of gas hydrate detection by means of
electroseismics, J. Appl. Geophys., 86, 98–108, 2012.
Zyserman, F., Jouniaux, L., Warden, S.,
and Garambois, S.: Borehole seismoelectric logging using a
shear-wave source: possible application to CO2 disposal?,
Int. J. Greenh. Gas Con., 33, 82–102,
https://doi.org/10.1016/j.ijggc.2014.12.009, 2015.
Short summary
The seismo-electromagnetic method is used for non-invasive subsurface exploration, showing interesting results for detecting fluids such as water, oil, gas, CO2, or ice, and to better characterize the subsurface in terms of porosity, permeability, and fractures. We describe theoretical background, the role of key parameters, recent theoretical and numerical developments, and field and laboratory observations to show that this method can bring advantages compared to classical geophysical method.
The seismo-electromagnetic method is used for non-invasive subsurface exploration, showing...
