FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4322005793> ?p ?o ?g. }

• W4322005793 abstract "Tenerife is the largest (2,034 km2) and highest (3,718 m) island of the Canarian archipelago and is the only one hosting an active stratovolcano (Teide-Pico Viejo volcanic system). Its structure is controlled by a volcanotectonic rift-system with NW, NE and NS directions, with the Teide-Pico Viejo volcanic system located in the intersection. The last eruption Teide-Pico Viejo volcanic system occurred in 1798 through an adventive cone. Although Teide volcano shows a weak fumarolic system, volcanic gas emissions observed in the summit cone consist mostly of diffuse CO2 degassing (Hern&#225;ndez et al., 1998; Mori et al., 2001).More than 200 diffuse CO2 efflux surveys have been performed in the summit crater of Teide Volcano during the period 1999-2023. During each survey, diffuse CO2 emission was estimated in 38 sampling sites, homogeneously distributed inside the crater, by means of a portable non dispersive infrared (NDIR) CO2 fluxmeter using the accumulation chamber method. CO2 emission rates was estimated after spatial distribution maps constructed by sequential Gaussian simulation (sGs) algorithm. During 23 years of the studied period, CO2 emissions ranged from 2.0 to 346 t/d. The most remarkable feature of the temporal evolution of diffuse CO2 emission rate was an important increase that began few weeks after the occurrence of a seismic swarm of long period events was recorded on Tenerife in 2 October 2, 2016, a followed by a general increase of the seismic activity in and around the island (D&#8217;Auria et al., 2019). Several geochemical parameters showed significant changes during &#8764;June&#8211;August of 2016 and 1&#8211;2 months before the occurrence of the October 2, 2016, long-period seismic swarm (Padr&#243;n et al., 2021). Since then, anomalously high diffuse CO2 emission rates has remained in the crater of Teide. This change might be explained as an input of magmatic fluids triggered by an injection of fresh magma and convective mixing after the 2 October 2016 seismic swarm (D'Auria et al., 2019; Padr&#243;n et al., 2021). This work reflects how useful are the diffuse studies to understand the behaviour of the volcanic system and to forecast future volcanic activity. Monitoring the diffuse degassing rates has demonstrated to be an essential tool for the prediction of future seismic&#8211;volcanic unrest and has become an important monitoring tool to reduce volcanic risk in Tenerife.D'Auria, L., et al. (2019). J. Geophys. Res.124,8739-8752Hern&#225;ndez, P., et al. (1998). Geophys. Res. Lett. 25, (17) 3311-3314Mori, T., et al. (2001). Chem. Geol. 177, 85&#8211;99Padr&#243;n, E., et al. (2021). J. Geophys. Res.126,e2020JB020318" @default.
• W4322005793 created "2023-02-26" @default.
• W4322005793 creator A5003165094 @default.
• W4322005793 creator A5028121122 @default.
• W4322005793 creator A5041308926 @default.
• W4322005793 creator A5057012442 @default.
• W4322005793 creator A5067748429 @default.
• W4322005793 creator A5075009688 @default.
• W4322005793 creator A5076852837 @default.
• W4322005793 creator A5079215077 @default.
• W4322005793 creator A5079636633 @default.
• W4322005793 creator A5087202100 @default.
• W4322005793 date "2023-05-15" @default.
• W4322005793 modified "2023-10-12" @default.
• W4322005793 title "Anomalous diffuse CO2 emission from the summit crater of Teide volcano and changes of seismic activity in and around Tenerife, Canary Islands" @default.
• W4322005793 doi "https://doi.org/10.5194/egusphere-egu23-7410" @default.
• W4322005793 hasPublicationYear "2023" @default.
• W4322005793 type Work @default.
• W4322005793 citedByCount "0" @default.
• W4322005793 crossrefType "posted-content" @default.
• W4322005793 hasAuthorship W4322005793A5003165094 @default.
• W4322005793 hasAuthorship W4322005793A5028121122 @default.
• W4322005793 hasAuthorship W4322005793A5041308926 @default.
• W4322005793 hasAuthorship W4322005793A5057012442 @default.
• W4322005793 hasAuthorship W4322005793A5067748429 @default.
• W4322005793 hasAuthorship W4322005793A5075009688 @default.
• W4322005793 hasAuthorship W4322005793A5076852837 @default.
• W4322005793 hasAuthorship W4322005793A5079215077 @default.
• W4322005793 hasAuthorship W4322005793A5079636633 @default.
• W4322005793 hasAuthorship W4322005793A5087202100 @default.
• W4322005793 hasConcept C114793014 @default.
• W4322005793 hasConcept C120806208 @default.
• W4322005793 hasConcept C121332964 @default.
• W4322005793 hasConcept C127313418 @default.
• W4322005793 hasConcept C1276947 @default.
• W4322005793 hasConcept C165205528 @default.
• W4322005793 hasConcept C179537507 @default.
• W4322005793 hasConceptScore W4322005793C114793014 @default.
• W4322005793 hasConceptScore W4322005793C120806208 @default.
• W4322005793 hasConceptScore W4322005793C121332964 @default.
• W4322005793 hasConceptScore W4322005793C127313418 @default.
• W4322005793 hasConceptScore W4322005793C1276947 @default.
• W4322005793 hasConceptScore W4322005793C165205528 @default.
• W4322005793 hasConceptScore W4322005793C179537507 @default.
• W4322005793 hasLocation W43220057931 @default.
• W4322005793 hasOpenAccess W4322005793 @default.
• W4322005793 hasPrimaryLocation W43220057931 @default.
• W4322005793 hasRelatedWork W1984872911 @default.
• W4322005793 hasRelatedWork W2034727470 @default.
• W4322005793 hasRelatedWork W2060680501 @default.
• W4322005793 hasRelatedWork W2091270751 @default.
• W4322005793 hasRelatedWork W2167536656 @default.
• W4322005793 hasRelatedWork W2318468411 @default.
• W4322005793 hasRelatedWork W2343561287 @default.
• W4322005793 hasRelatedWork W2909005903 @default.
• W4322005793 hasRelatedWork W4200257457 @default.
• W4322005793 hasRelatedWork W988014797 @default.
• W4322005793 isParatext "false" @default.
• W4322005793 isRetracted "false" @default.
• W4322005793 workType "article" @default.