• Imaging Science in Dentistry
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• 제36권2호
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• pp.117-121
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• 2006

Peripheral ameloblastoma is an extremely rare odontogenic soft tissue tumor with histologic characteristics similar to those of the intraosseous ameloblastoma. It appears in the gingiva and oral mucosa. And it usually does not show any bone involvement on radiographs, except for saucer shaped erosion of underlying alveolar bone. Recurrence is considered uncommon. We report a case of peripheral ameloblastoma with bone involvement. Histologically it presented with follicles and nest of tumor cells with palisading pattern. And radiographs showed the typical saucer shaped alveolar bone erosion at the distal area of right mandibular third molar. At 6-month follow-up after operation, no local recurrence was noted.

• 한국정밀공학회:학술대회논문집
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• 한국정밀공학회 2008년도 추계학술대회 논문집
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• pp.191-192
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• 2008

• 한국암반공학회:학술대회논문집
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• 한국암반공학회 2004년도 추계학술발표 논문집
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• pp.171-180
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• 2004

Underground mining causes surface subsidence long after the mining operation had been ceased. Surface subsidence can be in the form of saucer-shaped depression or collapsed chimneys or sinkholes. Sinkhole formations are predominant over shallow-depth room and pillar mines having weak overburden strata. In this study, occurrences of sinkholes due to mining activity are assessed based on local geological conditions and mining parameters using fuzzy reasoning techniques. All input and output parameters are represented with linguistic hedges. Numerous fuzzy rules are developed to relate sinkhole occurrences with input parameters using fuzzy relational matrix. Based on the combined fuzzy rules, possibility of sinkhole occurrences can be ascertained once the geological and mining parameters of any area are known.

• Journal of Periodontal and Implant Science
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• 제34권3호
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• pp.647-657
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• 2004

A non-carious cervical lesion(NCCL) is the loss of tooth structure at the cementoenamel junction level that is unrelated to dental caries. This study was to evaluate the occlusal and periodontal status of teeth with non-carious cervical lesions. We evaluated 105 teeth with non-carious cervical lesions in 35 subjects aged 38-75 years and characterized them based on the shape and dimension, plaque retention, bleeding on probing(BOP), probing pocket depth(PPD), occlusal status, brushing type, hypersensitivity and wear facet. The results of this study were as follows 1. No significant association was observed between cervical lesions and occlusal contact in lateral excursions. 2. No significant difference occurred in plaque retention, PPD, BOP between teeth with and without cervical lesions. 3. Test teeth had a significantly higher percentage of hypersensitivity and occlusal wear facet than teeth without cervical lesions. 4. Wedge shaped lesions had a significantly higher percentage of plaque than saucer shaped lesions. 5. Teeth with plaque were found to have significantly deeper PPD than teeth without plaque retention in cervical regions. 6. Teeth with occlusal contacts were found to have significantly deeper PPD than teeth without occlusal contacts. 7. No significant association was observed between cervical lesions and PPD independent of plaque retention and occlusal contacts Although more knowledge is necessary, our results suggest that occlusal contact and bacterial plaque may influence on periodontal tissue, but NCCL is not directly associated with periodontal health

• Earthquakes and Structures
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• 제8권5호
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• pp.1255-1276
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• 2015

The importance of considering soil-structure interaction effect in the analysis and design of RC frame buildings is increasingly recognized but still not penetrated to the grass root level owing to various complexities involved. It is well established fact that the soil-structure interaction effect considerably influence the design of multi-storey buildings subjected to lateral seismic loads. The shear walls are often provided in such buildings to increase the lateral stability to resist seismic lateral loads. In the present work, the linear soil-structure analysis of a G+5 storey RC shear wall building frame resting on isolated column footings and supported by deformable soil is presented. The finite element modelling and analysis is carried out using ANSYS software under normal loads as well as under seismic loads. Various load combinations are considered as per IS-1893 (Part-1):2002. The interaction analysis is carried out with and without shear wall to investigate the effect of inclusion of shear wall on the total and differential settlements in the footings due to deformations in the soil mass. The frame and soil mass both are considered to behave in linear elastic manner. It is observed that the soil-structure interaction effect causes significant total and differential settlements in the footings. Maximum total settlement in footings occurs under vertical loads and inner footings settle more than outer footings creating a saucer shaped settlement profile of the footings. Each combination of seismic loads causes maximum differential settlement in one or more footings. Presence of shear wall decreases pulling/pushing effect of seismic forces on footings resulting in more stability to the structures.

• 한국지구과학회지
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• 제45권2호
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• pp.136-146
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• 2024

본 논문은 서해 군산분지 퇴적층 내에서 발견되는 다양한 화성암들을 탄성파 반사상에 따라 분류하고 그 공간적 분포 양상을 도시하는 과정에 대해 상술한다. 연구지역인 서해 대륙붕 군산분지의 북동소분지, 남서소분지, 남동소분지 내에서 총 6종류의 분출 화성암 반사상과 3종류의 관입 화성암 반사상이 중생대 후기 백악기, 신생대 에오세 및 전기 마이오세, 신생대 제4기 층에서 발견되었다. 분출 화성암은 그 크기, 외형, 내부 층리구조에 따라 (1) 높이 200 m 이하의 고깔형 화산체들로 1회성 단성화산 분화를 통해 형성된 것으로 추정되는 단성화산체(E.mono), (2) 단성화산체들이 모여 높이 500 m 이내의 하나의 화산체를 형성하는 단성화산복합체(E.comp), (3) 높이 1 km 이상 직경 15 km 이상으로 내부에 복수의 층이 인지되는 성층화산체(E.strato), (4) 기반암 저지대의 정단층 주변에서 고반사 특성을 보이는 열극 분출암(E.fissure), (5) 저각 사면부와 내부에 직경 약 2 km 화도 구조를 보여주는 마르-다이아트림(E.maar), (6) 퇴적층을 교란하는 직경 1 km 이내 파이프형 구조를 갖는 열수분출공(E.vent)으로 구성된다. 관입 화성암은 상부 퇴적층의 변형구조를 통해 인지되며, (1) 수평형, 계단형, 종지형 등 다양한 수직/수평 관입 기하를 나타내는 암맥 및 암상(I.dike/sill), (2) 직경 1-3 km의 뿔 또는 기둥 모양 관입암체인 화성암주(I.stock), (3) 상부 퇴적층을 광범위하게 변형시키는 폭 10 km 이상의 관입암체인 저반/병반(I.batho/lac)으로 구성된다. 분출 화성암은 주로 군산분지 남서소분지 내 백악기 및 신생대 고제3기 에오세 층 내에서 인지되며, 관입암체는 주로 남동 및 남서 소분지 내에서 발견된다. 열수분출공은 군산분지 전역에서 발견되며 활동시기는 전반적으로 중기 마이오세 이후로 일부는 현재까지 활동중인 것으로 보인다.