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ISSN : 1225-6692(Print)
ISSN : 2287-4518(Online)
Journal of the Korean earth science society Vol.34 No.7 pp.615-625

백두산에서 소규모 분화로 발생 가능한 화쇄류에 대한 TITAN2D 시뮬레이션 연구

윤성효1,*, 이정현1, 김선경1, 장철우1, 조은일1, 양인숙1, 김윤정1, 김상현2, 이길하3, 김성욱4, 지오바니 마케도니오5
1부산대학교 지구과학교육과, 609-735, 부산광역시 금정구 부산대학로 63번길 2
2부산대학교 사회환경시스템공학부, 609-735, 부산광역시 금정구 부산대학로 63번길 2
3대구대학교 토목공학과, 712-714, 경상북도 경산시 진량읍 대구대로 201
4주식회사 GI, 611-839, 부산광역시 연제구 중앙대로 1048번길 11
5이탈리아 국립지구물리화산연구원 베수비우스 화산관측소
백두산은 역사시대에 다수의 분화 기록이 있으며, 2002년도에 불안정한 전조를 나타내었다. 지질조사 결과 백두산에서는 플리니안 분화로 인하여 강하화산재 발생 후 분연주의 붕괴로 화쇄류가 발생한 것이 인지되므로, 특정 분화구로부터 소규모 분화에 의한 화쇄류의 영향 범위에 대하여 시뮬레이션 하였다. 화산폭발지수(VEI) 3 이하의 분화가 발생하여 분연주의 붕괴에 의하여 화쇄류가 발생하면 칼데라 외륜산으로부터 백두산 사면을 따라 최대 7 km까지 영향을 미칠 것으로 해석되었으며, 칼데라 내의 분화구에 의한 분연주 발생 시 대부분이 칼데라 내부에 퇴적되거나, 흘러넘칠 경우에는 주로 북쪽 이도백하 상류 계곡에 두껍게 퇴적될 것으로 파악된다.

TITAN2D Simulations of Pyroclastic Flows from Small Scale Eruption at Mt. Baekdusan

*Corresponding author:

*Tel: +82-51-510-2723

*Fax: +82-51-513-7495
, Sung-Hyo Yun1,*, Jeong-hyun Lee1, Sunkyeong Kim1, Cheolwoo Chang1, Eunil Cho1, Innsook Yang1, Yunjeong Kim1, Sanghyun Kim2, Kilha Lee3, Seongwook Kim4, Giovanni Macedonio5

1Earth Science Education, Pusan National University, Busan 609-735, Korea
2Environmental Engineering, Pusan National University, Busan 609-735, Korea
3Civil Engineering, Daegu University, Gyeongbuk 712-714, Korea
4GI Co. Ltd., Busan 611-839, Korea
5Osservatiorio Vesuviano, Instituto Nazionale di Geofisica e Vulcanologia, Napoli, Italy


Many eruptions of Mt. Baekdusan volcano have been recorded in the historical literatures, and there wereunrest precursors in 2002. Based on the geological survey results, it has been recognized that Mt. Baekdusan’s Plinianeruptions had caused ashfall, followed by the occurrence of pyroclastic flows, which were caused by the collapse oferuption column. Therefore, we simulated the range of the impacts of pyroclastic flows, which were caused by smalleruptions from a specific crater. Based on the simulation results, it can be interpreted that, when the pyroclastic flows arecaused by the eruption column collapse from an eruption with less than VEI 3, the impacts will range from the outer rimof the caldera to the mountain slope 7 km at the maximum distance. Furthermore, it is interpreted that, when the eruptioncolumn occurs by the crater located inside the caldera, most will be deposited inside the caldera and what overflows willbe deposited thickly mostly in the north valley, the upper stream region of Erdaobaihe.


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