Abstract:Abstract. In order to investigate the complex nature of landslides triggered by rainfall, dynamic muon radiography of the motion of the underground water table is planned in a drainage tunnel drilled underneath an estimated fault plane. However, the humidity inside the tunnel is almost 100 %. In order to suppress moisture effects, a scintillation counter with Cockcroft-Walton photomultipler tubes (CW-MPT) was developed and tested at the observation site located in Shizuoka Prefecture, Japan. The counter was st… Show more
“…There are several potential applications of muographic imagery (Figure 7A). These include (A) geological investigation of volcanoes 1 , landslides 69 , mines 70 , glaciers 71 , etc., (B) non-destructive testing, evaluation and monitoring of industrial plants and civil engineering structures such as electric furnace 72 , blast furnace 73 , nuclear reactors 74,75 , railway tunnels 76 , underground pillars 77 , check valve 78 , etc., and (C) non-destructive surveys of cultural heritage, such as pyramids 44,79 . Although it is impossible to introduce all of these applications here, several successful examples will be briefly explained in this section.…”
Section: Muographic Imagerymentioning
confidence: 99%
“…In 2011, groundwater dynamics (as a response to heavy rainfall events) were first captured within a mechanically fractured zone inside a seismic fault 114 . Since then, muographic survey and monitoring activities have been conducted to search for water resources 115 , for prevention of landslides (most respond slowly to rainfall and move at low speeds, but have substantial impacts on landscapes after several years) 69 , and monitoring of debris flows that are gravity-driven, rapid movements of material composed of a mixture of rock debris and water 97,98 . The main goal of the Tomographic Research of Underground and large STructures with Muographic Expertise (TRUST-ME) project, carried out by the Low Background Noise Underground Research Laboratory of Rustrel (LSBB), is to characterize the dynamics of the water transfer processes in the critical zone, and the cycles of these processes within the region of the Fontaine-de-Vaucluse in particular.…”
Muography is a technique that takes advantage of the specific properties of a relativistic lepton called the cosmic-ray muon that is much heavier than the electron. Due mainly to their strong penetrating power and relativistic nature, cosmic-ray muons can be utilized for a wide range of technologies including imagery, positioning, navigation, timing (PNT), and secured communication in environments where most conventional techniques are unavailable. Cosmic-ray muons are universally present everywhere on the Earth and thus, muographic measurements can be conducted in the same manner globally and therefore have reproduced similar results regardless of the countries where researchers conduct these measurements. This feature has enabled the muographic field to expand and grow, developing into a powerful tool to investigate natural phenomena, cultural heritage, and PNT worldwide. This Primer is intended as an introductory article to introduce new and established muographic techniques, case studies with some of the results obtained and some recent interdisciplinary advances. Data reproducibility and limitations are also discussed; additionally, there is a presentation of the outlook of developments in the future of muography.
“…There are several potential applications of muographic imagery (Figure 7A). These include (A) geological investigation of volcanoes 1 , landslides 69 , mines 70 , glaciers 71 , etc., (B) non-destructive testing, evaluation and monitoring of industrial plants and civil engineering structures such as electric furnace 72 , blast furnace 73 , nuclear reactors 74,75 , railway tunnels 76 , underground pillars 77 , check valve 78 , etc., and (C) non-destructive surveys of cultural heritage, such as pyramids 44,79 . Although it is impossible to introduce all of these applications here, several successful examples will be briefly explained in this section.…”
Section: Muographic Imagerymentioning
confidence: 99%
“…In 2011, groundwater dynamics (as a response to heavy rainfall events) were first captured within a mechanically fractured zone inside a seismic fault 114 . Since then, muographic survey and monitoring activities have been conducted to search for water resources 115 , for prevention of landslides (most respond slowly to rainfall and move at low speeds, but have substantial impacts on landscapes after several years) 69 , and monitoring of debris flows that are gravity-driven, rapid movements of material composed of a mixture of rock debris and water 97,98 . The main goal of the Tomographic Research of Underground and large STructures with Muographic Expertise (TRUST-ME) project, carried out by the Low Background Noise Underground Research Laboratory of Rustrel (LSBB), is to characterize the dynamics of the water transfer processes in the critical zone, and the cycles of these processes within the region of the Fontaine-de-Vaucluse in particular.…”
Muography is a technique that takes advantage of the specific properties of a relativistic lepton called the cosmic-ray muon that is much heavier than the electron. Due mainly to their strong penetrating power and relativistic nature, cosmic-ray muons can be utilized for a wide range of technologies including imagery, positioning, navigation, timing (PNT), and secured communication in environments where most conventional techniques are unavailable. Cosmic-ray muons are universally present everywhere on the Earth and thus, muographic measurements can be conducted in the same manner globally and therefore have reproduced similar results regardless of the countries where researchers conduct these measurements. This feature has enabled the muographic field to expand and grow, developing into a powerful tool to investigate natural phenomena, cultural heritage, and PNT worldwide. This Primer is intended as an introductory article to introduce new and established muographic techniques, case studies with some of the results obtained and some recent interdisciplinary advances. Data reproducibility and limitations are also discussed; additionally, there is a presentation of the outlook of developments in the future of muography.
“…In muography, most scintillation counters are designed as thin strips (e.g., Tanaka et al 2001Tanaka et al , 2003Tanaka et al , 2005Basset et al 2006;Menichelli et al 2007;Beauducel et al 2010;Gibert et al 2010;Taira & Tanaka 2010;Tanaka & Sannomiya 2013). Particle trajectories can be tracked by connecting two or more vertex points (muon passing points) determined by the geometrical address of the strips that are hit by the particle and their corresponding timings.…”
Section: Real-time Detectorsmentioning
confidence: 99%
“…Currently, muography observations are becoming more active than before. In addition to the presently running experiments [fault zones in Japan (Tanaka et al 2011, Tanaka & Sannomiya 2013 and Spain (Cumbre Vieja; Hernández et al 2013); volcanoes in Japan (Unzen; Miyamoto et al 2012), Italy (Stromboli and Etna;Aleksandrov et al 2012, Anastasio et al 2013, Carbone et al 2013Hernández et al 2013)], new projects to explore small Solar System bodies (Prettyman 2013) and to monitor a carbon storage (Kudryavtsev et al 2012) have begun.…”
Geophysics research has long been dominated by classical mechanics, largely disregarding the potential of particle physics to augment existing techniques. The purpose of this article is to review recent progress in probing Earth's interior with muons and neutrinos. Existing results for various volcanological targets are reviewed. Geoneutrinos are also highlighted as examples in which the neutrino probes elucidate the composition of Earth's deep interior. Particle geophysics has the potential to serve as a useful paradigm to transform our understanding of Earth as dramatically as the X-ray transformed our understanding of medicine and the body.
“…1). However, this problem could be solved with borehole/tunnel observations from underground muon detectors (Tanaka and Sannomiya, 2013). Secondly, this technique only resolves the average density distribution along individual muon paths.…”
Abstract. Rainfall-triggered fluid flow in a mechanical fracture zone associated with a seismic fault has been estimated (Tanaka et al., 2011) using muon radiography by measuring the water position over time in response to rainfall events. In this report, the data taken by Tanaka et al. (2011) are reanalyzed to estimate the porosity distribution as a function of a distance from the fault gouge. The result shows a similar pattern of the porosity distribution as measured by borehole sampling at Nojima fault. There is a low porosity shear zone axis surrounded by porous damaged areas with density increasing with the distance from the fault gouge. The dynamic muon radiography (Tanaka et al., 2011) provides a new method to delineate both the recharge and discharge zones along the fault segment, an entire hydrothermal circulation system. This might dramatically raise the success rate for drilling of geothermal exploration wells, and it might open a new horizon in the geothermal exploration and monitoring.
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