Impact of Volcanic Gas and Ash Emissions: Perspectives in Hazards Assessment

A special issue of Geosciences (ISSN 2076-3263). This special issue belongs to the section "Natural Hazards".

Deadline for manuscript submissions: closed (25 January 2024) | Viewed by 1449

Special Issue Editors


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Guest Editor
ASI - Agenzia Spaziale Italiana, Rome, Italy
Interests: geochemistry; gas monitoring and modelling; ash leachates; earth and planetary sciences; volcanism and cryo-volcanism; salt–water solutions; hydrothermal systems; in situ and remote sensing; natural hazards

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Guest Editor
Instituto de Geofísica, Universidad Nacional Autónoma de México, Mexico City, Mexico
Interests: volcano monitoring; volcanic gas measurements; remote sensing of ash plumes; natural hazards; petrology

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Guest Editor
Italian Spatial Agency, ASI, Via del Politecnico, 00133 Rome, Italy
Interests: mineralogy; hyperspectral data; laboratory; remote spectroscopy; earth and planetary sciences

Special Issue Information

Dear Colleagues,

This Special Issue of Geosciences aims to gather original research articles, reviews, and technical notes on Natural Hazard assessment, applied to geological systems, based on the collection of data and/or numerical modelling derived from in situ and remote sensing (including from satellites) measurements.

In volcanic systems, the passive release of fluids from hydrothermal and magmatic sources marks the inter-eruptive periods. The diffuse soil degassing activity can generate gas hazard, asphyxiation, or poisoning, allowing the accumulation of harmful gases, especially under low wind conditions or in depressed areas. In addition to the catastrophic events, attention would be focused on the long-term (active and passive) release which may affect human health and may increase the knowledge in terms of forecasting. Critical gas hazard conditions occur in volcanic areas: large plumes, weakly degassing sites, fumarolic fields, mud volcanoes, but they can occur also in other geological systems. Studies focusing on the natural gas quantification and dispersion numerical modelling are welcome. The articles must give an important contribution to improve the monitoring (that is not easy) and the forecasting of natural events.

In addition, also the ash release and dispersal are crucial considering the effects of ash amounts into the high troposphere-low stratosphere. Characterizing the pyroclastic fragments injected into the atmosphere during volcanic eruptions is crucial to the forecasting of plume dispersal. The main hazards connected to the tephra release are: 1) the fast in-plume heterogeneous reactions and 2) the deposition and the leaching of fresh-fallen ash.

This Special Issue will examine the state of the art of monitoring, including the complete range of aspects: the acquisition of the data, its interpretation, its application to generate models and forecasts. We would appreciate multidisciplinary research studies, including expertise from various fields of physics, chemistry, and geology, and as well as computer science and statistics. We welcome papers aiming to understand natural events using in situ, proximal, and remote sensing observations, laboratory analyses, numerical modelling, geophysical/geochemical techniques.

Dr. Maria Pedone
Dr. Hugo Delgado-Granados
Dr. Paola Manzari
Guest Editors

Manuscript Submission Information

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Keywords

  • forecast
  • risk evaluation and communication
  • gas emissions
  • ash dispersion and leachates
  • in situ measurements
  • remote sensing
  • data from satellites
  • laboratory
  • numerical modelling

Published Papers (1 paper)

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Research

19 pages, 12210 KiB  
Article
Applications of Ground-Based Infrared Cameras for Remote Sensing of Volcanic Plumes
by Fred Prata, Stefano Corradini, Riccardo Biondi, Lorenzo Guerrieri, Luca Merucci, Andrew Prata and Dario Stelitano
Geosciences 2024, 14(3), 82; https://doi.org/10.3390/geosciences14030082 - 17 Mar 2024
Viewed by 940
Abstract
Ground-based infrared cameras can be used effectively and safely to provide quantitative information about small to moderate-sized volcanic eruptions. This study describes an infrared camera that has been used to measure emissions from the Mt. Etna and Stromboli (Sicily, Italy) volcanoes. The camera [...] Read more.
Ground-based infrared cameras can be used effectively and safely to provide quantitative information about small to moderate-sized volcanic eruptions. This study describes an infrared camera that has been used to measure emissions from the Mt. Etna and Stromboli (Sicily, Italy) volcanoes. The camera provides calibrated brightness temperature images in a broadband (8–14 µm) channel that is used to determine height, plume ascent rate and volcanic cloud/plume temperature and emissivity at temporal sampling rates of up to 1 Hz. The camera can be operated in the field using a portable battery and includes a microprocessor, data storage and WiFi. The processing and analyses of the data are described with examples from the field experiments. The updraft speeds of the small eruptions at Stromboli are found to decay with a timescale of ∼10 min and the volcanic plumes reach thermal equilibrium within ∼2 min. A strong eruption of Mt. Etna on 1 April 2021 was found to reach ∼9 km, with ascent speeds of 10–20 ms−1. The plume, mostly composed of the gases CO2, water vapour and SO2, became bent over by the prevailing winds at high levels, demonstrating the need for multiple cameras to accurately infer plume heights. Full article
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