• Proceedings of the Korean Institute of Industrial Safety Conference
• /
• 2000.06a
• /
• pp.101-107
• /
• 2000

가연성 가스가 누출함에 따른 화재 및 폭발 재해는 공업화 사회에 있어서 방치될 수 없는 매우 중요한 문제이다. 기체, 액체, 분체가 단면적이 작은 분출구를 통해 공기중으로 분출될 때 분출하는 물질과 분출구와의 마찰로 인해 정전기가 발생한다. 분출되는 물질과 분출구를 구성하는 물질의 직접적인 마찰에 의해서도 정전기가 발생하고, 분출되는 물질 구성입자들간 상호충돌에 의해서도 정전기가 발생된다. 배관 내에 순수천연가스가 이송ㆍ분출할 때의 대전량은 매우 작다. (중략)

• Bulletin of the Korean Space Science Society
• /
• 2003.10a
• /
• pp.32-32
• /
• 2003

1999년 Nitta & Akiyama는 17개의 limb 플레어와 연관된 X-선 플라즈마 분출(X-ray plasma ejection)과 코로나질량방출(Coronal Mass Ejection; CME) 사이에 일반적인 상관관계가 있음을 제안하였다. 즉, 관련 CME가 관측되는 플레어의 경우, X-선 플라즈마 분출 역시 관측이 되고 비록 잘 관측된 현상이라 하더라도 관련 CME가 없는 경우에는 X-선 플라즈마 분출 역시 확인되지 않았다. 본 연구에서는 1999년 4월부터 2001년 3월까지 2년간의 281개의 limb 플레어 관측자료를 이용하여 CME와 X-선 플라즈마 분출간의 물리적 관계를 통계적으로 연구하였다. 아울러 플레어, X-선 플라즈마 분출, CME 사이의 물리적 관계를 알아보기 위하여 관련 현상들 간의 시간적 관련성을 조사하였다. 우리의 결과는 X-선 플라즈마 분출과 CM 사이에 밀접한 상관관계가 있으며 일부 X-선 플라즈마 분출은 X-선에서 관측되는 CME의 전조일 가능성을 보여준다.

• Economic and Environmental Geology
• /
• v.53 no.6
• /
• pp.715-727
• /
• 2020

Volcanostratigraphy in Ulleung Island is divided into 4 stratigraphic groups: Dodong Basaltic Rocks, Ulleung Group, Seonginbong Group and NariGroup. The main pyroclastics in them includes lapilli tuff intercalated within the Dodong Basaltic Rocks, lapilli tuff at the top of Sadong Breccia, Sataegam Tuff, Gombawi Welded Tuff, Bongrae Scoria Deposits, Maljandeung Tuff, Nari Scoria Deposits and Jugam Scoria Deposits. Analysing eruption types, The lapilli tuff in the Dodong Basaltic Rocks is derived from Surtseyan eruption, and the Bongrae, Nari and Jugam Scoria Deposits are caused by Strombolian eruptions or/and sub-Plinion eruptions, but the Sataegam Tuff and Maljandeung Tuff are derived from Plinian and phreatoplinian eruptions. Among them the large-scaled eruptions. In particular, the eruptions of Maljandeung were large enough to result in caldera collapse, and had falled out tephras to the eastern Korean peninsula but even Japan Islands. The magma with high potential to be still alive is judged to be trachyandesitic and phonolitic in composition. If the trachyandesitic magma explodes, it will probably result in a strombolian eruption and have a fairly low explosivity, but if the phonolitic magma explodes, it will probably result in a plinian eruption and have a much higher explosivity. If the eruption had a high explosivity, there is a possibility that it could easily be converted into a phreatoplinian eruption due to the influx of groundwater by the easy generation of fractures. These large-scaled eruptions could fall out tephras to the eastern Korean peninsula but even Japan Islands.

• Proceedings of the Korean Institute of Industrial Safety Conference
• /
• 2000.11a
• /
• pp.333-339
• /
• 2000

현대사회의 공업화 및 도시화에 따라 NG(Natural Gas)를 포함하는 일반 가연성 가스의 누출에 의한 화재 및 폭발 재해는 매우 중요한 문제이다. 기체, 액체 및 분체가 단면적이 작은 분출구를 통해 공기중으로 이송 및 분출될 때 분출물질과 분출구와의 마찰로 인해 정전기가 발생한다./sup 1)/ 배관 내에 순수 NG가 이송·분출될 때의 대전량은 매우 작다./sup 2,3)/ 그러나, 배관 내에는 벤트스텍 등 외부에서 유입되는 먼지 또는 배관내의 부식에 의한 산화철(Fe₂O₃) 등의 분체가 포함될 수 있으며 이러한 분체가 천연가스 등과 함께 분출될 때 배관과의 마찰로 인해 대전량이 크게 상승된다./sup 3,4)/ 또한 분출되는 물질 구성입자들간 상호충돌에 의해서도 대전량은 더욱 증가하게 된다./sup 5)/(중략)

• The Journal of the Petrological Society of Korea
• /
• v.14 no.4 s.42
• /
• pp.251-263
• /
• 2005

Modern volcanoes, Laoheishan and Huoshaoshan, have erupted during $1720\~1721$ in the Wudalianchi volcanic group, NE china. They comprise scoria and spatter cones that consist of potassium-rich phono-tephritic pyroclastic deposits and lavas, and include wide lava flow fields. The Laoheishan scoria cone is a polygenetic multiple volcano that overlaps earlier and later edifices with more complicated internal structures produced in greater scale and in earlier time than the Huoshaoshan. There is a funnel-shaped crater in the center of the later edifice of the Laoheishan scoria cone. The Huoshaoshan spatter cone is a monogenetic simple volcano with a central pit crater. The volcanic sequences indicate eruption processes that followed a repeated pattern that progressed through 5 stages of explosive and effusive eruption including lava fountains and Strombolian eruptions in the Laoheishan, and a recognizable pattern of 2 stages that started with Strombolian eruption and progressed through lava effusion in the Huoshaoshan.

• The Journal of the Petrological Society of Korea
• /
• v.7 no.1
• /
• pp.1-14
• /
• 1998

Dangsanbong volcano, which is located on the coast of the western promontory of Cheju Island, occurs in such a regular pattern on the sequences which represent an excellent example of an eruptive cycle. The volcano comprises a horseshoe-shaped tuff cone and a younger nested cinder cone on the crater floor, which are overlain by a lava cap at the top of the cinder cone, and wide lava plateau in the moat between two cones and in the northern part. The volcanic sequences suggest volcanic processes that start with Surtseyan eruption, progress through Strombolian eruption and end with Hawaiian eruption, and then are followed by rock fall from sea cliff of the tuff cone and by air fall from another crater. It is thought that the eruptive environments of the tuff cone could be mainly emergent because the present cone is located on the coast, and standing body of sea water could play a great role. It is thought that the now emergent part of the tuff cone was costructed subaerially because there is no evidence of marine reworking. The emergent tuff cone is characterized by distinctive steam-explosivity that results primarily from a bulk interaction between rapidly ascending magma and external water. The sea water gets into the vent by flooding accross or through the top or breach of northern tephra cone. Dangsanbong tuff cone was constructed from Surtseyan eruption which went into with tephra finger jetting explosion in the early stage, late interspersed with continuous upruch activities, and from ultra-Surtseyan jetting explosions producting base surges in the last. When the enclosure of the vent by a long-lived tephra barrier would prevent the flooding and thus allow the vent to dry out, the phreatomagmatic activities ceased to transmit into magmatic activity of Strombolian eruption, which constructed a cinder cone on the crater floor of the tuff cone Strombolian eruption ceased when magma in the conduit gradually became depleted in gas. In the Dangsanbong volcano, the last magmatic activity was Hawaiian eruption which went into with foundation and effusion of basalt lava.

• Proceedings of the Korea Water Resources Association Conference
• /
• 2016.05a
• /
• pp.352-357
• /
• 2016

광역상수관은 원수 또는 정수를 자체 수자원확보가 어려운 지자체에 적기에 공급해주는 중요한 역할을 하고 있다. 최근 자연재해에 및 관 노후, 공사 중 사고 등의 원인으로 광역상수관이 파손되는 사례가 발생되었다. 이와 같은 광역상수관의 파손은 상수 보급 수혜지역에 대한 단수피해가 발생될 뿐만 아니라 파손지점에서 상수유량의 분출으로 침수피해를 야기 시킬 수 있게 된다. 본 연구에서는 광역상수관 파손에 따른 파손지역 주변부에서 유량 분출에 의한 침수양상 및 분출지점에 위치하고 있는 지하시설물(지하철 정거장)에 대한 침수피해 영향을 검토하였다. 침수양상 분석 방법은 광역상수관 파손시 분출유량 산정, 지형자료 구축, 표면류 흐름 계산, 침수범람도 작성 순으로 검토를 수행하였다. 광역상수관 파손에 따른 분출유량은 상수관 공급량 $770,000m^3/day$를 기준으로 초당 흐르는 유량(2차원 부정류 흐름 해석)으로 환산하여 유입조건으로 선정하고, 파손위치 및 분출유량에 따른 시나리오를 설정하였다. 광역상수관 파손에 따른 침수양상을 살펴본 결과, 파손 지점의 위치의 지형적 여건에 따라 최대 침수심 및 최대 침수 위치가 상이한 결과가 나타나는 것을 확인할 수 있다. 정거장 주변부 최대 침수심은 0.50m로 정거장 노출부 최소 높이 0.65m(노출부 높이 - 지반고)보다 작은 수치이므로 광역상수관 파손에 따른 분출유량의 정거장 내부 유입은 없는 것으로 분석 되었다.

• Journal of the korean Society of Automotive Engineers
• /
• v.10 no.6
• /
• pp.61-71
• /
• 1988

본 논문에서는 Laser Rayleigh Pyrometer에 의한 광학계의 개조와 측정기술을 발전시켜 지금까지의 측정이 불가능한 밀폐용기내에서 분출화염의 온도측정을 시도하여 분출화염에 의한 착화나 소염의 연구에 중요한 자료를 얻고자 하는데 있다. 밀폐용기내에서의 온도측정은 대기개방형에서와 같이 Laser의 에너지를 증대시키기 위해 이용한는 다중반사 Mirror가 사용될 수 없을 뿐만 아니라 약한 Rayleigh산란빛에 의하여 입사창이란 Laser Trap으로 발생하는 강한 배경광 및 분출화염 뿐만 아니고 착화된 화염에서 대량의 화학발광은 피할 수 없다. 본 논문은 이와 같은 영향을 제거하는데 노력하여 밀폐용기내의 연소장에서 온도를 측정하였으며 또 측정가능성을 시사하였다.

• The Journal of the Petrological Society of Korea
• /
• v.22 no.1
• /
• pp.49-62
• /
• 2013

The Dongmakgol Tuff is divided into 8 lithofacies based on their grain size and depositional structures: massive tuff breccia(TBm), welded tuff and lapilli tuff(LTw), rheomorphic tuff and lapilli tuff(LTr), massive lapilli tuff(LTm), stratified lapilli tuff(LTs), gradedly bedded lapilli tuff(LTg), crudely bedded lapilli tuff(LTb) and massive fine tuff(Tm). They can be divided into 3 pyroclastic rock group based on their constituents of the lithofacies. The lower group(LI) is composed of LTm, LTw and LTr, which are interpreted to have resulted from emplacement of voluminous pyroclastic flows due to ignimbrite-form eruption to boiling-over eruption. The middle group(LT+MI) consists of LTs, LTg and LTm associated with Tm in the lower part, and of LTm, LTw and LTr in the middle and upper parts; these suggest that started with deposition of pyroclastic surges from phreatoplinian eruption by poor eternal water, passed through emplacement of pyroclastic flows from ignimbrite-form eruption and ended with deposition of voluminous pyroclastic flows from boiling-over eruption. The upper group(lUT+uUT+UI) is composed of LTs, LTg and Tm in the lowermost, TBm, LTb, LTb and Tm in the lower part, and LTm and LTw in the middle and upper part, suggesting that began with deposition of surges from phreatoplinian eruption, passed through deposition of pumice- and ash-fallouts from plinian eruption and transformed into emplacement of pyroclastic flows due to boiling-over eruption. As result, eruptive processes in the Dongmakgol Tuff approximately began with phreatoplinian or/and plinian eruption, transformed into ignimbrite-forming eruption and proceeded into boiling-over eruption in each volcanism, but proceeded presumably without phreatoplinian or plinian eruption in the earlier stage of 1st volcanism.

• Economic and Environmental Geology
• /
• v.53 no.5
• /
• pp.553-564
• /
• 2020

Transition between explosive and effusive eruption in Ulleung Island is observed in the Nari Scoria Deposits and Albong Trachyandesite (lava dome) origined by dome-building eruption and may be related to factors such as magma influx, ascent rate and degassing. However, the interpretation of them has not been resolved yet because the interaction between these factors is not complex but also the resulting behaviour during eruption is unpredictable. This paper focuses on the explosive and effusive activity perceived during building the Albong lava dome in Nari caldera. Samples were collected along with time from the scoria deposits and lava dome, linked to eruption stage and style of activity. Textures of groundmass feldspar microlites from these samples are quantitatively analyzed, including measurements of areal number density, mean microlite size, crystal aspect ratio, groundmass crystallinity and crystal size. The microlite textures show that shallow pre- and syn-eruptive magmatic processes acted to govern the changing behaviour during the eruption. Transition between explosive and effusive eruption was driven by the dynamics of magma ascent in the conduit, with degassing and crystallisation acting via feedback mechanisms, resulting in a cycle of effusive and explosive eruption.