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Remote Sensing as Tool in Geofluids Dynamics and Related Risks

A special issue of Remote Sensing (ISSN 2072-4292).

Deadline for manuscript submissions: closed (31 March 2020) | Viewed by 5236

Special Issue Editors


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Guest Editor
Department of Earth Sciences, University of Pisa, Via Santa Maria 53, Pisa, Italy
Interests: remote sensing data interpretation; geohazard monitoring; landslide mapping; building monitoring; land subsidence
Special Issues, Collections and Topics in MDPI journals

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Guest Editor
Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Vesuviano, Sezione di Napoli, 95125 Catania, Italy
Interests: geological mapping; risk management; satellite image analysis
Special Issues, Collections and Topics in MDPI journals

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Guest Editor
Roy M. Huffington Department of Earth Sciences, Southern Methodist University, Dallas, TX 75205, USA
Interests: SAR; InSAR; time-series InSAR; geophysical modeling; volcanoes; landslides; geohazards
Special Issues, Collections and Topics in MDPI journals

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Guest Editor
Istituto di Ricerca per la Protezione Idrogeologica (IRPI), National Research Council, Via della Madonna Alta 126, Perugia, Italy
Interests: remote sensing; SAR; detection and mapping; landslides; machine learning
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Fluids are fundamental to many aspects of geology. First of all, fluids are responsible for the formation of both geothermic fields and hydrocarbon deposits. The exploitation of ground water or hydrocarbon, which is a fundamental resource, can lead to subsidence or uplift phenomena that can affect the Earth’s surface. Fluids can also play an important role in natural disasters, such as floods and volcanic eruptions. Furthermore, they can modify slope stability by triggering landslides. Amongst fluids, soil moisture plays an important role in several environmental processes (interactions between the hydrosphere, atmosphere and biosphere, heat exchange, rainfall infiltration, and runoff). During the last decades, the importance of satellite and/or airborne remote sensing data and related products has increased strongly, together with sensors’ spatial and temporal resolutions. Satellite synthetic aperture radar (SAR) remote sensing products are extensively used to detect, measure, and monitor over-time ground deformation related to water extraction and aquifer recharge, hydrocarbon extraction, waste water injection, exploitation of geothermal and oil reservoirs, as well as landslide phenomena and the inflation and deflation of volcanoes. Optical (multispectral) imageries have a great potential to characterize surface physical properties. Even more, with future hyperspectral systems, it will be possible to move to a level of quantitative modelling. Thermal data can be used to evaluate top-surface temperature, emissivity, and thermal capacity. The combined use of both optical and thermal multi-temporal imageries can be thus used to map a complex terrestrial surface property, as well as to detect dynamic changes. Considering the priority of the Sendai Framework for Disaster Risk Reduction 2015–2030 (disaster risk management should be based on an understanding of disaster risk in all its dimensions of vulnerability, capacity, exposure of persons and assets, hazard characteristics, and the environment. Such knowledge can be used for risk assessment, prevention, mitigation, preparedness, and response), the above mentioned multi-sensor EO technologies can be profitably used to map and monitor wide areas affected by fluid migration-related hazards, such as landslide and subsidence dynamics, soil degradation and contamination due to anthropogenic activities, and volcanic monitoring. Manuscripts may describe new remote sensing methodologies or applications of well-known remote sensing processing techniques for the analysis of the dynamics related to subsurface fluids in the field of geology. Examples of areas covered within this research topic include but are not restricted to the following:

  • Monitoring geothermal, oil, and gas extraction and production;
  • Monitoring surface deformation related to fluid injection in the subsurface;
  • Mapping, monitoring, and forecasting subsidence phenomena induced by water extraction;
  • Assessing the effects of rainfall in slope stability;
  • Assessing the role of magmatic fluids in crustal deformation;
  • Measuring soil moisture.

Contributions related to the integration of different monitoring records with conventional field observations and new modelling frameworks for the interpretation of the observed data are welcome.

Dr. Andrea Ciampalini
Dr. Federico Di Traglia
Prof. Zhong Lu
Dr. Alessandro Mondini
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Remote Sensing is an international peer-reviewed open access semimonthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2700 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • InSAR
  • Optical images
  • Geohazards
  • Fluids dynamic
  • Volcanoes
  • Landslides
  • Machine learning
  • Floods

Published Papers (1 paper)

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Research

33 pages, 15371 KiB  
Article
Wide-Area InSAR Survey of Surface Deformation in Urban Areas and Geothermal Fields in the Eastern Trans-Mexican Volcanic Belt, Mexico
by Francesca Cigna, Deodato Tapete, Víctor Hugo Garduño-Monroy, Jesús Arturo Muñiz-Jauregui, Oscar Humberto García-Hernández and Adrián Jiménez-Haro
Remote Sens. 2019, 11(20), 2341; https://doi.org/10.3390/rs11202341 - 09 Oct 2019
Cited by 21 | Viewed by 4548
Abstract
This paper provides the first wide-area Interferometric Synthetic Aperture Radar (InSAR) survey of the whole eastern Trans-Mexican Volcanic Belt (42,200 km2). The aims are to identify ground deformation hotspots within major urbanized areas and rural valleys, establish baselines in geothermal exploration [...] Read more.
This paper provides the first wide-area Interferometric Synthetic Aperture Radar (InSAR) survey of the whole eastern Trans-Mexican Volcanic Belt (42,200 km2). The aims are to identify ground deformation hotspots within major urbanized areas and rural valleys, establish baselines in geothermal exploration sites, and analyze deformation at geothermal exploitation sites and its relationship with energy production. The whole 2003–2010 ENVISAT C-band SAR archive available over the region was processed with the Small BAseline Subset (SBAS) InSAR method to retrieve over 840,000 coherent targets and estimate their ground displacement rates and time series. Land subsidence hotspots due to aquifer drawdown are found within the city of Puebla (up to −53 mm/year vertical rates, groundwater pumping for industrial use), Tlaxcala and Apizaco (−17 mm/year, industrial and public), the valley of Tecamachalco (−22 mm/year, agricultural), Tulancingo (−55 mm/year, public, industrial and agricultural), and in the eastern Mexico City metropolitan area (−44 mm/year, agricultural). The baseline for the Acoculco caldera complex shows widespread ground stability. Conversely, localized subsidence patterns of −5 to −10 mm/year exist around Las Derrumbadas and Cerro Pinto in the Serdán-Oriental basin, due to intense groundwater pumping for agriculture. A well-defined land subsidence area with −11 mm/year maximum rates is found at Los Humeros volcanic complex within Los Potreros collapse, correlating well with energy production infrastructure location and historical steam production rates. Field surveys carried out in Acoculco and Los Humeros in 2018 provide supporting evidence for the identification of hydrothermal manifestations, and understanding of the landscape and surface deformation patterns within the geothermal fields. Full article
(This article belongs to the Special Issue Remote Sensing as Tool in Geofluids Dynamics and Related Risks)
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