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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10280
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dc.contributor.authorallYun, S.; Earth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.authorallLee, J.; Earth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.authorallKim, S.; Earth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.authorallChang, C.; Earth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.authorallCho, E.; Earth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.authorallYang, I.; Earth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.authorallKim, Y.; Earth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.authorallKim, S.; Environmental Engineering, Pusan National University, Busan 609-735, Koreaen
dc.contributor.authorallLee, K.; Civil Engineering, Daegu University, Gyeongbuk 712-714, Koreaen
dc.contributor.authorallKim, S; GI Co. Ltd., Busan 611-839, Koreaen
dc.contributor.authorallMacedonio, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.date.accessioned2016-03-18T09:22:41Zen
dc.date.available2016-03-18T09:22:41Zen
dc.date.issued2013-12en
dc.identifier.urihttp://hdl.handle.net/2122/10280en
dc.description.abstractMany eruptions of Mt. Baekdusan volcano have been recorded in the historical literatures, and there were unrest precursors in 2002. Based on the geological survey results, it has been recognized that Mt. Baekdusan’s Plinian eruptions had caused ashfall, followed by the occurrence of pyroclastic flows, which were caused by the collapse of eruption column. Therefore, we simulated the range of the impacts of pyroclastic flows, which were caused by small eruptions from a specific crater. Based on the simulation results, it can be interpreted that, when the pyroclastic flows are caused by the eruption column collapse from an eruption with less than VEI 3, the impacts will range from the outer rim of the caldera to the mountain slope 7 km at the maximum distance. Furthermore, it is interpreted that, when the eruption column occurs by the crater located inside the caldera, most will be deposited inside the caldera and what overflows will be deposited thickly mostly in the north valley, the upper stream region of Erdaobaihe.en
dc.language.isoEnglishen
dc.relation.ispartofJour. Korean Earth Science Societyen
dc.relation.ispartofseries34en
dc.subjectBaekdusanen
dc.subjectpyroclastic flowen
dc.subjectsmall-scale eruptionen
dc.subjectvolcanic disasteren
dc.subjectimpact zoneen
dc.titleTITAN2D Simulations of Pyroclastic Flows from Small Scale Eruption at Mt. Baekdusanen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber615-625en
dc.subject.INGV05. General::05.01. Computational geophysics::05.01.99. General or miscellaneousen
dc.identifier.doi10.5467/JKESS.2013.34.7.615en
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dc.description.obiettivoSpecifico3V. Dinamiche e scenari eruttivien
dc.description.journalTypeN/A or not JCRen
dc.description.fulltextrestricteden
dc.relation.issn1225-6692en
dc.relation.eissn2287-4518en
dc.contributor.authorYun, S.en
dc.contributor.authorLee, J.en
dc.contributor.authorKim, S.en
dc.contributor.authorChang, C.en
dc.contributor.authorCho, E.en
dc.contributor.authorYang, I.en
dc.contributor.authorKim, Y.en
dc.contributor.authorKim, S.en
dc.contributor.authorLee, K.en
dc.contributor.authorKim, Sen
dc.contributor.authorMacedonio, G.en
dc.contributor.departmentEarth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.departmentEarth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.departmentEarth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.departmentEarth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.departmentEarth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.departmentEarth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.departmentEarth Science Education, Pusan National University, Busan 609-735, Koreaen
dc.contributor.departmentEnvironmental Engineering, Pusan National University, Busan 609-735, Koreaen
dc.contributor.departmentCivil Engineering, Daegu University, Gyeongbuk 712-714, Koreaen
dc.contributor.departmentGI Co. Ltd., Busan 611-839, Koreaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptEarth Science Education, Pusan National University, Busan 609-735, Korea-
crisitem.author.deptPusan National University, Busan, South Korea-
crisitem.author.deptEnvironmental Engineering, Pusan National University, Busan 609-735, Korea-
crisitem.author.deptEarth Science Education, Pusan National University, Busan 609-735, Korea-
crisitem.author.deptEarth Science Education, Pusan National University, Busan 609-735, Korea-
crisitem.author.deptEarth Science Education, Pusan National University, Busan 609-735, Korea-
crisitem.author.deptEarth Science Education, Pusan National University, Busan 609-735, Korea-
crisitem.author.deptEnvironmental Engineering, Pusan National University, Busan 609-735, Korea-
crisitem.author.deptCivil Engineering, Daegu University, Gyeongbuk 712-714, Korea-
crisitem.author.deptEnvironmental Engineering, Pusan National University, Busan 609-735, Korea-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.orcid0000-0001-6604-1479-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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