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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.
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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

Time-lapse ERT monitoring of an injection/withdrawal experiment in a shallow unconfined aquifer

TL;DR: In this paper, a sequential injection/withdrawal experiment was designed for monitoring the pump-and-capture remediation of a conductive solute in an unconfined alluvial aquifer.
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Application of multivariate geostatistics in delineating management zones within a gravelly vineyard using geo-electrical sensors

TL;DR: In this article, the potential use of electro-magnetic induction scans (EMI) to measure apparent electrical conductivity and improve the estimate accuracy of sparsely sampled primary variables was assessed in a 5-ha gravelly soil vineyard in Valpolicella, north-eastern Italy.
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Temperature‐calibrated imaging of seasonal changes in permafrost rock walls by quantitative electrical resistivity tomography (Zugspitze, German/Austrian Alps)

TL;DR: In this paper, electrical resistivity tomography (ERT) was applied to gain insight into spatial thaw and refreezing behavior of permafrost rocks and presents the first approach to calibrating ERT with frozen rock temperature.
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Forensic Geoscience: applications of geology, geomorphology and geophysics to criminal investigations

TL;DR: A review of geoscience applications to criminal investigation can be found in this paper, where the authors use the concept of scales of investigation, from large-scale landforms through to microscopic particles.
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Snowmelt infiltration: monitoring temporal and spatial variability using time-lapse electrical resistivity

TL;DR: In this paper, a series of electrical resistivity surveys were carried out using electrodes installed below the ground surface and in shallow boreholes, and the results from this time-lapse survey reveal significant changes over time, and suggest that localised infiltration takes place.
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