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Journal ArticleDOI

Recent developments in the direct-current geoelectrical imaging method

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TLDR
There have been major improvements in instrumentation, field survey design and data inversion techniques for the geoelectrical method over the past 25 years as mentioned in this paper, which has made it possible to conduct large 2D, 3D and even 4D surveys efficiently to resolve complex geological structures that were not possible with traditional 1-D surveys.
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This article is published in Journal of Applied Geophysics.The article was published on 2013-08-01. It has received 702 citations till now. The article focuses on the topics: Computer technology.

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Citations
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On the spatio-temporal dynamics of soil moisture at the field scale

TL;DR: In this paper, the authors review the state of the art of characterizing and analyzing spatio-temporal dynamics of soil moisture content at the field scale and discuss measurement techniques that have become available in recent years and that provide unique opportunities to characterize field scale soil moisture variability with high spatial and temporal resolution.
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Electrical resistivity tomography technique for landslide investigation: A review

TL;DR: A review of the main results obtained by applying 2D and 3D Electrical Resistivity Tomography (ERT) for the investigation of a wide spectrum of landslide phenomena which affected various geological formations and occurred in different geographic areas is presented in this paper.
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Geophysical Monitoring of Moisture-Induced Landslides: A Review

TL;DR: Whiteley et al. as discussed by the authors presented a review of the state of the art of geophysical monitoring applied to moisture-induced landslides, focusing on technical and practical uses of time-lapse methods in geophysics applied to monitoring moistureinduced landslide.
Journal ArticleDOI

Life and death of slow-moving landslides

TL;DR: In the most destructive and catastrophic landslide events, rocks, soil and fluids can travel at speeds approaching several tens of metres per second as discussed by the authors, but slow-moving landslides rarely claim lives, they can cause major damage to infrastructure and sometimes fail catastrophically, transitioning into fast moving landslides that can result in thousands of casualties.
References
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Journal ArticleDOI

Aquatic electrical resistivity imaging of shallow-water wetlands

TL;DR: In this article, the authors used aquatic electrical resistivity imaging (ERI) to predict spatial and temporal patterns of porefluid conductivity in wetland soils of a shallow-water wetland.
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Potential of Electrical Resistivity Tomography to Detect Fault Zones in Limestone and Argillaceous Formations in the Experimental Platform of Tournemire, France

TL;DR: In this article, a 2D electrical resistivity survey was carried out along a 2.5 km baseline, and a takeout of 40 m was used to assess the potential of this method to detect faults from the ground surface.
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A complex geo-scientific strategy for landslide hazard mitigation – from airborne mapping to ground monitoring

TL;DR: In this article, the authors evaluated several exploration methods on their applicability to investigate and monitor landslide areas and the resulting optimised strategy consists of the combined application of airborne electromagnetics, ground geoelectrical measurements and geoeLECTrical monitoring combined with hydrological and geological mapping and geotechnical modelling.
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Electrical imaging of sliding geometry and fluids associated with a deep seated landslide (La Clapière, France)

TL;DR: In this article, the applicability of electrical resistivity tomography (ERT) for the recognition of large landslide structures at depths, which have never previously been imaged accurately, is discussed.
Journal ArticleDOI

Non‐destructive DC resistivity surveying using flat‐base electrodes

TL;DR: In this paper, the application of flat-base electrodes to geoelectrical measurements is examined, motivated by the inability to apply conventional spike electrodes in environments where conventional spikes cannot be inserted into the ground.
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