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Physical Characterization of Long‐Lasting Hybrid Eruptions: The 2021 Tajogaite Eruption of Cumbre Vieja (La Palma, Canary Islands)
Long‐lasting, hybrid eruptions can be of complex description and classification, especially when associated with multiple eruptive styles and multiple products. The 2021 Tajogaite eruption of La Palma, Canary Islands, was associated with a magma‐gas decoupled system that resulted in the simultaneous...
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Published in: | Journal of geophysical research. Solid earth 2022-11, Vol.127 (11), p.n/a |
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creator | Bonadonna, Costanza Pistolesi, Marco Biass, Sébastien Voloschina, Marija Romero, Jorge Coppola, Diego Folch, Arnau D’Auria, Luca Martin‐Lorenzo, Alba Dominguez, Lucia Pastore, Camille Reyes Hardy, Maria‐Paz Rodríguez, Fátima |
description | Long‐lasting, hybrid eruptions can be of complex description and classification, especially when associated with multiple eruptive styles and multiple products. The 2021 Tajogaite eruption of La Palma, Canary Islands, was associated with a magma‐gas decoupled system that resulted in the simultaneous emission of lava flows and tephra plumes from various vents. Even though the tephra blanket (∼2 × 107 m3) represents only 7%–16% of the total erupted volume, it provides fundamental insights into the overall eruptive dynamics. Tephra was mostly dispersed NE‐SW due to a complex regional and local wind patterns and was subdivided into 3 units and 11 layers that well correlate at different distances from the vent and with both tremor data and lava emission rate. While plume height varied at the temporal scale of a few hours, the average mass eruption rate associated with the tephra blanket of the different units remained relatively constant (∼3–4 × 103 kg s−1). In contrast, the emission rate of lava largely increased after the first week and remained higher than the overall emission of tephra throughout the whole eruption (average value of ∼6 × 104 kg s−1). Based on a detailed characterization of the tephra blanket in combination with atmospheric wind, tremor, and lava emission trend, we demonstrate the need of (a) multidisciplinary strategies for the description of hybrid eruptions that account for both the duration of individual phases and the quantification of the mass of multiple products, and of (b) dedicated ash dispersal forecasting strategies that account for the frequent variations of eruptive and atmospheric conditions.
Plain Language Summary
Volcanic eruptions are mostly subdivided into effusive and explosive when they are associated with the emission of lava flows or with the fragmentation of magma that results in the generation of widespread deposits (i.e., tephra). The September–December 2021 Tajogaite eruption of La Palma Island (Spain) represents a typical example of long‐lasting, hybrid eruption with alternation, or, more often, contemporaneous emission of lava flows and tephra. The lava field extended toward the western sector of the island, while the tephra blanket was mostly dispersed NE‐SW due to a complex regional and local wind pattern. Even though the tephra blanket represents only 7%–16% of the total erupted volume, it provides fundamental insights into the overall eruptive dynamics. Based on a detailed characterization of the tephra blank |
doi_str_mv | 10.1029/2022JB025302 |
format | article |
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Plain Language Summary
Volcanic eruptions are mostly subdivided into effusive and explosive when they are associated with the emission of lava flows or with the fragmentation of magma that results in the generation of widespread deposits (i.e., tephra). The September–December 2021 Tajogaite eruption of La Palma Island (Spain) represents a typical example of long‐lasting, hybrid eruption with alternation, or, more often, contemporaneous emission of lava flows and tephra. The lava field extended toward the western sector of the island, while the tephra blanket was mostly dispersed NE‐SW due to a complex regional and local wind pattern. Even though the tephra blanket represents only 7%–16% of the total erupted volume, it provides fundamental insights into the overall eruptive dynamics. Based on a detailed characterization of the tephra blanket, in combination with wind, seismic tremor, and lava emission trend, we demonstrate the need of dedicated strategies for the description of hybrid, long‐lasting eruptions that account for both eruption duration and for the quantification of multiple products (tephra blanket, tephra cone, lava flows). We also show the need of dedicated strategies of short‐range ash dispersal forecasting that account for the frequent variations of eruptive and atmospheric conditions.
Key Points
Tephra blanket of the 2021 Tajogaite eruption is only 7%–16% of the total volume but is key to decipher the variable eruptive dynamics
Tephra blanket shows distinct layers and units at different distances from vents that well correlate with tremor and lava emission rate
Hybrid eruptions are best described based on both event duration and mass associated with multiple products (tephra blanket, cone, lava)</description><identifier>ISSN: 2169-9313</identifier><identifier>EISSN: 2169-9356</identifier><identifier>DOI: 10.1029/2022JB025302</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>ash dispersal ; ash forecasting ; Ashes ; Atmospheric conditions ; Dispersion ; Dynamics ; Emission ; Emissions ; eruption classification ; Forecasting ; Geophysics ; Islands ; Lava ; Lava flows ; Local winds ; Magma ; Plumes ; Tephra ; tephra cones ; tephra deposits ; Tremors ; Volcanic eruptions ; Wind</subject><ispartof>Journal of geophysical research. Solid earth, 2022-11, Vol.127 (11), p.n/a</ispartof><rights>2022. The Authors.</rights><rights>2022. This article is published under http://creativecommons.org/licenses/by-nc-nd/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3683-4478ee8a2e312d7fb4f2844e2d7c832f0ef1ed0bf44b529fb2fb22cbd025479b3</citedby><cites>FETCH-LOGICAL-a3683-4478ee8a2e312d7fb4f2844e2d7c832f0ef1ed0bf44b529fb2fb22cbd025479b3</cites><orcidid>0000-0002-7568-6495 ; 0000-0002-7664-2216 ; 0000-0001-8919-702X ; 0000-0002-5096-3708 ; 0000-0002-2368-2193 ; 0000-0001-9383-9830 ; 0000-0001-7181-4122 ; 0000-0002-0677-6366 ; 0000-0002-1919-9473 ; 0000-0003-4659-7810</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Bonadonna, Costanza</creatorcontrib><creatorcontrib>Pistolesi, Marco</creatorcontrib><creatorcontrib>Biass, Sébastien</creatorcontrib><creatorcontrib>Voloschina, Marija</creatorcontrib><creatorcontrib>Romero, Jorge</creatorcontrib><creatorcontrib>Coppola, Diego</creatorcontrib><creatorcontrib>Folch, Arnau</creatorcontrib><creatorcontrib>D’Auria, Luca</creatorcontrib><creatorcontrib>Martin‐Lorenzo, Alba</creatorcontrib><creatorcontrib>Dominguez, Lucia</creatorcontrib><creatorcontrib>Pastore, Camille</creatorcontrib><creatorcontrib>Reyes Hardy, Maria‐Paz</creatorcontrib><creatorcontrib>Rodríguez, Fátima</creatorcontrib><title>Physical Characterization of Long‐Lasting Hybrid Eruptions: The 2021 Tajogaite Eruption of Cumbre Vieja (La Palma, Canary Islands)</title><title>Journal of geophysical research. Solid earth</title><description>Long‐lasting, hybrid eruptions can be of complex description and classification, especially when associated with multiple eruptive styles and multiple products. The 2021 Tajogaite eruption of La Palma, Canary Islands, was associated with a magma‐gas decoupled system that resulted in the simultaneous emission of lava flows and tephra plumes from various vents. Even though the tephra blanket (∼2 × 107 m3) represents only 7%–16% of the total erupted volume, it provides fundamental insights into the overall eruptive dynamics. Tephra was mostly dispersed NE‐SW due to a complex regional and local wind patterns and was subdivided into 3 units and 11 layers that well correlate at different distances from the vent and with both tremor data and lava emission rate. While plume height varied at the temporal scale of a few hours, the average mass eruption rate associated with the tephra blanket of the different units remained relatively constant (∼3–4 × 103 kg s−1). In contrast, the emission rate of lava largely increased after the first week and remained higher than the overall emission of tephra throughout the whole eruption (average value of ∼6 × 104 kg s−1). Based on a detailed characterization of the tephra blanket in combination with atmospheric wind, tremor, and lava emission trend, we demonstrate the need of (a) multidisciplinary strategies for the description of hybrid eruptions that account for both the duration of individual phases and the quantification of the mass of multiple products, and of (b) dedicated ash dispersal forecasting strategies that account for the frequent variations of eruptive and atmospheric conditions.
Plain Language Summary
Volcanic eruptions are mostly subdivided into effusive and explosive when they are associated with the emission of lava flows or with the fragmentation of magma that results in the generation of widespread deposits (i.e., tephra). The September–December 2021 Tajogaite eruption of La Palma Island (Spain) represents a typical example of long‐lasting, hybrid eruption with alternation, or, more often, contemporaneous emission of lava flows and tephra. The lava field extended toward the western sector of the island, while the tephra blanket was mostly dispersed NE‐SW due to a complex regional and local wind pattern. Even though the tephra blanket represents only 7%–16% of the total erupted volume, it provides fundamental insights into the overall eruptive dynamics. Based on a detailed characterization of the tephra blanket, in combination with wind, seismic tremor, and lava emission trend, we demonstrate the need of dedicated strategies for the description of hybrid, long‐lasting eruptions that account for both eruption duration and for the quantification of multiple products (tephra blanket, tephra cone, lava flows). We also show the need of dedicated strategies of short‐range ash dispersal forecasting that account for the frequent variations of eruptive and atmospheric conditions.
Key Points
Tephra blanket of the 2021 Tajogaite eruption is only 7%–16% of the total volume but is key to decipher the variable eruptive dynamics
Tephra blanket shows distinct layers and units at different distances from vents that well correlate with tremor and lava emission rate
Hybrid eruptions are best described based on both event duration and mass associated with multiple products (tephra blanket, cone, lava)</description><subject>ash dispersal</subject><subject>ash forecasting</subject><subject>Ashes</subject><subject>Atmospheric conditions</subject><subject>Dispersion</subject><subject>Dynamics</subject><subject>Emission</subject><subject>Emissions</subject><subject>eruption classification</subject><subject>Forecasting</subject><subject>Geophysics</subject><subject>Islands</subject><subject>Lava</subject><subject>Lava flows</subject><subject>Local winds</subject><subject>Magma</subject><subject>Plumes</subject><subject>Tephra</subject><subject>tephra cones</subject><subject>tephra deposits</subject><subject>Tremors</subject><subject>Volcanic eruptions</subject><subject>Wind</subject><issn>2169-9313</issn><issn>2169-9356</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><recordid>eNp9kM1Kw0AQx4MoWGpvPsCCFwWj-5Um8WZD7QcBi1SvYZLsthvSpO4mSDx58AF8Rp_ELZXiyWFghpnffPB3nHOCbwim4S3FlM5HmHoM0yOnR8kwdEPmDY8POWGnzsCYAlsLbInwnvO5WHdGZVCiaA0askZo9Q6NqitUSxTX1er74ysG06hqhaZdqlWOxrrd7ghzh5ZrgexhgpZQ1CtQjTh0d_NRu0m1QC9KFIAuY0ALKDdwjSKoQHdoZkqocnN15pxIKI0Y_Ma-8_wwXkZTN36czKL72AU2DJjLuR8IEQAVjNDclymXNOBc2DwLGJVYSCJynErOU4-GMqXWaZbmVhTuhynrOxf7vVtdv7bCNElRt7qyJxPqc-x5QeATS13vqUzXxmghk61WG_tvQnCykzr5K7XF2R5_U6Xo_mWT-eRp5Hmhx9gP1aF_iQ</recordid><startdate>202211</startdate><enddate>202211</enddate><creator>Bonadonna, Costanza</creator><creator>Pistolesi, Marco</creator><creator>Biass, Sébastien</creator><creator>Voloschina, Marija</creator><creator>Romero, Jorge</creator><creator>Coppola, Diego</creator><creator>Folch, Arnau</creator><creator>D’Auria, Luca</creator><creator>Martin‐Lorenzo, Alba</creator><creator>Dominguez, Lucia</creator><creator>Pastore, Camille</creator><creator>Reyes Hardy, Maria‐Paz</creator><creator>Rodríguez, Fátima</creator><general>Blackwell Publishing Ltd</general><scope>24P</scope><scope>WIN</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TG</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-7568-6495</orcidid><orcidid>https://orcid.org/0000-0002-7664-2216</orcidid><orcidid>https://orcid.org/0000-0001-8919-702X</orcidid><orcidid>https://orcid.org/0000-0002-5096-3708</orcidid><orcidid>https://orcid.org/0000-0002-2368-2193</orcidid><orcidid>https://orcid.org/0000-0001-9383-9830</orcidid><orcidid>https://orcid.org/0000-0001-7181-4122</orcidid><orcidid>https://orcid.org/0000-0002-0677-6366</orcidid><orcidid>https://orcid.org/0000-0002-1919-9473</orcidid><orcidid>https://orcid.org/0000-0003-4659-7810</orcidid></search><sort><creationdate>202211</creationdate><title>Physical Characterization of Long‐Lasting Hybrid Eruptions: The 2021 Tajogaite Eruption of Cumbre Vieja (La Palma, Canary Islands)</title><author>Bonadonna, Costanza ; Pistolesi, Marco ; Biass, Sébastien ; Voloschina, Marija ; Romero, Jorge ; Coppola, Diego ; Folch, Arnau ; D’Auria, Luca ; Martin‐Lorenzo, Alba ; Dominguez, Lucia ; Pastore, Camille ; Reyes Hardy, Maria‐Paz ; Rodríguez, Fátima</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3683-4478ee8a2e312d7fb4f2844e2d7c832f0ef1ed0bf44b529fb2fb22cbd025479b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>ash dispersal</topic><topic>ash forecasting</topic><topic>Ashes</topic><topic>Atmospheric conditions</topic><topic>Dispersion</topic><topic>Dynamics</topic><topic>Emission</topic><topic>Emissions</topic><topic>eruption classification</topic><topic>Forecasting</topic><topic>Geophysics</topic><topic>Islands</topic><topic>Lava</topic><topic>Lava flows</topic><topic>Local winds</topic><topic>Magma</topic><topic>Plumes</topic><topic>Tephra</topic><topic>tephra cones</topic><topic>tephra deposits</topic><topic>Tremors</topic><topic>Volcanic eruptions</topic><topic>Wind</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bonadonna, Costanza</creatorcontrib><creatorcontrib>Pistolesi, Marco</creatorcontrib><creatorcontrib>Biass, Sébastien</creatorcontrib><creatorcontrib>Voloschina, Marija</creatorcontrib><creatorcontrib>Romero, Jorge</creatorcontrib><creatorcontrib>Coppola, Diego</creatorcontrib><creatorcontrib>Folch, Arnau</creatorcontrib><creatorcontrib>D’Auria, Luca</creatorcontrib><creatorcontrib>Martin‐Lorenzo, Alba</creatorcontrib><creatorcontrib>Dominguez, Lucia</creatorcontrib><creatorcontrib>Pastore, Camille</creatorcontrib><creatorcontrib>Reyes Hardy, Maria‐Paz</creatorcontrib><creatorcontrib>Rodríguez, Fátima</creatorcontrib><collection>Wiley Open Access Journals</collection><collection>Wiley-Blackwell Backfiles (Open access)</collection><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Environment Abstracts</collection><jtitle>Journal of geophysical research. Solid earth</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bonadonna, Costanza</au><au>Pistolesi, Marco</au><au>Biass, Sébastien</au><au>Voloschina, Marija</au><au>Romero, Jorge</au><au>Coppola, Diego</au><au>Folch, Arnau</au><au>D’Auria, Luca</au><au>Martin‐Lorenzo, Alba</au><au>Dominguez, Lucia</au><au>Pastore, Camille</au><au>Reyes Hardy, Maria‐Paz</au><au>Rodríguez, Fátima</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Physical Characterization of Long‐Lasting Hybrid Eruptions: The 2021 Tajogaite Eruption of Cumbre Vieja (La Palma, Canary Islands)</atitle><jtitle>Journal of geophysical research. Solid earth</jtitle><date>2022-11</date><risdate>2022</risdate><volume>127</volume><issue>11</issue><epage>n/a</epage><issn>2169-9313</issn><eissn>2169-9356</eissn><abstract>Long‐lasting, hybrid eruptions can be of complex description and classification, especially when associated with multiple eruptive styles and multiple products. The 2021 Tajogaite eruption of La Palma, Canary Islands, was associated with a magma‐gas decoupled system that resulted in the simultaneous emission of lava flows and tephra plumes from various vents. Even though the tephra blanket (∼2 × 107 m3) represents only 7%–16% of the total erupted volume, it provides fundamental insights into the overall eruptive dynamics. Tephra was mostly dispersed NE‐SW due to a complex regional and local wind patterns and was subdivided into 3 units and 11 layers that well correlate at different distances from the vent and with both tremor data and lava emission rate. While plume height varied at the temporal scale of a few hours, the average mass eruption rate associated with the tephra blanket of the different units remained relatively constant (∼3–4 × 103 kg s−1). In contrast, the emission rate of lava largely increased after the first week and remained higher than the overall emission of tephra throughout the whole eruption (average value of ∼6 × 104 kg s−1). Based on a detailed characterization of the tephra blanket in combination with atmospheric wind, tremor, and lava emission trend, we demonstrate the need of (a) multidisciplinary strategies for the description of hybrid eruptions that account for both the duration of individual phases and the quantification of the mass of multiple products, and of (b) dedicated ash dispersal forecasting strategies that account for the frequent variations of eruptive and atmospheric conditions.
Plain Language Summary
Volcanic eruptions are mostly subdivided into effusive and explosive when they are associated with the emission of lava flows or with the fragmentation of magma that results in the generation of widespread deposits (i.e., tephra). The September–December 2021 Tajogaite eruption of La Palma Island (Spain) represents a typical example of long‐lasting, hybrid eruption with alternation, or, more often, contemporaneous emission of lava flows and tephra. The lava field extended toward the western sector of the island, while the tephra blanket was mostly dispersed NE‐SW due to a complex regional and local wind pattern. Even though the tephra blanket represents only 7%–16% of the total erupted volume, it provides fundamental insights into the overall eruptive dynamics. Based on a detailed characterization of the tephra blanket, in combination with wind, seismic tremor, and lava emission trend, we demonstrate the need of dedicated strategies for the description of hybrid, long‐lasting eruptions that account for both eruption duration and for the quantification of multiple products (tephra blanket, tephra cone, lava flows). We also show the need of dedicated strategies of short‐range ash dispersal forecasting that account for the frequent variations of eruptive and atmospheric conditions.
Key Points
Tephra blanket of the 2021 Tajogaite eruption is only 7%–16% of the total volume but is key to decipher the variable eruptive dynamics
Tephra blanket shows distinct layers and units at different distances from vents that well correlate with tremor and lava emission rate
Hybrid eruptions are best described based on both event duration and mass associated with multiple products (tephra blanket, cone, lava)</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2022JB025302</doi><tpages>31</tpages><orcidid>https://orcid.org/0000-0002-7568-6495</orcidid><orcidid>https://orcid.org/0000-0002-7664-2216</orcidid><orcidid>https://orcid.org/0000-0001-8919-702X</orcidid><orcidid>https://orcid.org/0000-0002-5096-3708</orcidid><orcidid>https://orcid.org/0000-0002-2368-2193</orcidid><orcidid>https://orcid.org/0000-0001-9383-9830</orcidid><orcidid>https://orcid.org/0000-0001-7181-4122</orcidid><orcidid>https://orcid.org/0000-0002-0677-6366</orcidid><orcidid>https://orcid.org/0000-0002-1919-9473</orcidid><orcidid>https://orcid.org/0000-0003-4659-7810</orcidid><oa>free_for_read</oa></addata></record> |
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language | eng |
recordid | cdi_proquest_journals_2740558871 |
source | Wiley-Blackwell Read & Publish Collection; Alma/SFX Local Collection |
subjects | ash dispersal ash forecasting Ashes Atmospheric conditions Dispersion Dynamics Emission Emissions eruption classification Forecasting Geophysics Islands Lava Lava flows Local winds Magma Plumes Tephra tephra cones tephra deposits Tremors Volcanic eruptions Wind |
title | Physical Characterization of Long‐Lasting Hybrid Eruptions: The 2021 Tajogaite Eruption of Cumbre Vieja (La Palma, Canary Islands) |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-27T20%3A54%3A38IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Physical%20Characterization%20of%20Long%E2%80%90Lasting%20Hybrid%20Eruptions:%20The%202021%20Tajogaite%20Eruption%20of%20Cumbre%20Vieja%20(La%20Palma,%20Canary%20Islands)&rft.jtitle=Journal%20of%20geophysical%20research.%20Solid%20earth&rft.au=Bonadonna,%20Costanza&rft.date=2022-11&rft.volume=127&rft.issue=11&rft.epage=n/a&rft.issn=2169-9313&rft.eissn=2169-9356&rft_id=info:doi/10.1029/2022JB025302&rft_dat=%3Cproquest_cross%3E2740558871%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a3683-4478ee8a2e312d7fb4f2844e2d7c832f0ef1ed0bf44b529fb2fb22cbd025479b3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2740558871&rft_id=info:pmid/&rfr_iscdi=true |