• 대한소아치과학회지
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• 제1권1호
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• pp.35-39
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• 1974

505 girls were studied on the eruption of second molar clinically. 1. Eruption rate was 9.04% earlier in mandible than in maxilla. 2. Average age of eruption was 12.53 years old in maxilla and 11.73 in mandible. 3. There is no significant right and left arch, 4. Generally, period of eruption in Korean was slightly retarded as compared to that of foreigners.

• Journal of Korean Society for Atmospheric Environment
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• 제22권E2호
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• pp.69-77
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• 2006

Combined gas and aerosol measurements at a downwind area of the volcanic plume would be essential for helping to access the impact of the volcanic eruption on the local ecosystem and residents. An intensive and the fine time resolution measurement of $SO_2$, sulfate and PM2.5 was made to estimate their distribution in the Kanto area of Japan during the Miyakejima volcanic eruption period. In Tokyo, the 1 hr average $SO_2$ concentration observed before the eruption was 23.9 ppbv, while that of after eruption was 140.4 ppbv. In the Saitama Prefecture, the average concentration of $SO_2$ marked in the present study was two times higher than the average before the volcanic eruption. The PM2.5 mass concentrations in Sitama ranged from 3.8 to $136{\mu}g\;m^{-3}$. Sulfate accounts for $4.4{\sim}39.6%$ of PM2.5 in Sitama. The good correlationship between the concentrations of $SO_2$ and sulfate was obtained. The results of the VAFTAD and HYSPLIT models indicate that $SO_2$, sulfate, and PM2.5 measured in the present study would be expected to be significantly affected by the Miyakejima volcanic plume.

• 구강회복응용과학지
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• 제33권2호
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• pp.127-134
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• 2017

전신적 혹은 국소적 원인에 의해 발생하는 치아맹출지연은 대부분 소아기에 발견되어 교정적 정출을 이용한 치료를 진행한다. 하지만 소아기때 치료를 받지 못하고 성인기로 될 경우, 교정에 의한 치아이동이 어려워지기 때문에 보철수복으로 치료를 변경할 수 있다. 보철계획을 결정하기 전 고려사항으로는 치아상실이 나타난 범위, 치아사이 근원심공간 및 악간공간, 환자의 연령대 등이 있다. 이 논문에서는 상하악 구치부 맹출지연환자를 지르코니아 부분 고정성 보철물을 통해 구강회복한 증례를 소개하고자 한다.

• 대한치과교정학회지
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• 제23권4호
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• pp.493-501
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• 1993

It is the aim of this study to determine the impacts of radicular development of lower third molars on its eruption/impaction and to grope the prediction for eruption and/or impaction in advance. Three hundred and thirty cases of orthopantomogram were employed and classified as mesial root-dominant group, distal root-dominant group and Identical group according to the radicular development of lower third molars. This presentation has carried out the incipient mesial inclination, radicular development, impaction/eruption rate and changes of mesial inclination of the very teeth. Consequently the following summary and conclusions were drawn; Radicular development dominated mesial root than the distal and dominant mesial root invited higher potentialities for normal eruption. The mesial or honzontal impactions were detected on the distal root-dominant group. This analysis has been suggested the potential eruption/impaction of lower third molars were dependent upon the radicular development and the incipient mesial inclination.

• 천문학회보
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• 제35권2호
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• pp.50.1-50.1
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• 2010

The New Solar Telescope (NST) at Big Bear Solar Observatory (BBSO) is the recently constructed world largest 1.6 m optical solar telescope on the ground. We took an observation of the north polar limb in H-alpha line center wavelength on 2009 August 26 with the instrument at Nasmyth focus of the NST and found a remarkable small-scale H-alpha eruption from 18:20 UT and 18:45 UT. The eruption occurred with a relatively slow speed of about 10 km/s in early stage and a slight acceleration up to 20-30 km/s in later stage. We also found that the eruption shows a deflection along the pre-existing magnetic field as well as several interesting features such as bifurcation, rotation, horizontal oscillation, and direction and thickness change of its structure during the eruption. In this talk, we will report the observational properties of the small-scale eruption observed by the NST and discuss their implication on magnetic reconnection.

• 대한소아치과학회지
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• 제11권1호
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• pp.91-101
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• 1984

The purpose of this study is to determine what influence the lesion and the premature loss of mandibular 1st deciduous molar have on the eruption of its successor, and the author devided 580 cases of orthopantomograms from age 3 to 9 years old children into 3 groups: Control Group: both side normal Study I Group: one normal and the other lesion. Study II Group: one normal and the other premature loss before 8 years old. and observed the amount of differences and the relative position in eruption between study-tooth successor and normal-tooth successor, The following results were obtained: 1. The differences in eruption between right and left mandibular 1st primary molars of Study Group were greater than those of Control Group. 2. The successors of lesioned-teeth showed more accelerated eruption than the antimeres in 40.9% and more delayed, in 22.7%. 3. The successors of premature lost-teeth showed more accelerated eruption than the antimeres in 61.7% and more delayed, in 4.3%.

• Maxillofacial Plastic and Reconstructive Surgery
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• 제31권2호
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• pp.173-179
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• 2009

Dentigerous cyst is an odontogenic cyst which occurs in unerupted tooth crown. After the crown formation, enamel epithelium remnants surrounded continuously proliferates and it forms effusionfluid cyst and expands due to increased internal osmotic pressure. Treatments of cysts are mainly enucleation, marsupialization and de-compression. When deciding the way of treatment, the age of a patient, the anatomical circumstances, the region of lesion and the size of cyst should be considered. Marsupialization is that some parts of internal cystic wall would be converted into oral mucosa if the cyst is large size and is concerned about neighboring anatomic structure. It can be accompanied by enucleation later and eruption of related tooth can be possible. If there is a limitation of spontaneous tooth eruption, eruption of tooth can be induced by orthodontic apparatus. There were 3 patients had dentigerous cyst and underwent marsupialization, their impacted teeth had preserved and had induced eruption, all showing satisfactory results.

• 대한심미치과학회지
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• 제28권2호
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• pp.86-94
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• 2019

치아의 매복은 병리적인 변화, 기능적 결손, 심미적인 문제 등 다양한 문제점을 만든다. 이러한 매복치를 때론 제거하기도 하지만 매복치를 구강내로 노출시켜주는 수술적인 치료와 교정적인 forced eruption을 통해서 향후 발생할 수 있는 많은 문제점들을 해결할 수 있다. 교정적 forced eruption을 위해서 매복치아를 노출시킬 때 매복치아가 치조골 안에 완전하게 매복되어있지 않으면서 단지 연조직에만 덮혀있는 매복양상과 치조골 내부에 완전하게 매복되어있는 두가지의 양상으로 존재한다. 교정정 forced eruption을 위해서 매보되어있는 치아를 수술적으로 노출시키는 방법에관해 다양한 증례와 문헌과 함께 알아보고자 한다.

• 대한소아치과학회지
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• 제6권1호
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• pp.43-52
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• 1979

The purpose of this study was to finding out the relationship between the tooth calcification and eruption of the mandibular permanent teeth in Korean. This study was undertaken in 592 children at ages from 3 to 13 years who had good oral condition by means of panoramic roentgenographic analysis. The following results were obtained. 1. The mean ages of crown completion were as follows; Canine 1st. Premolar 2nd. Premolar 1st. Molar Male 6yrs. 4mos. 6yrs. 8mos. 7yrs. 6mos. 7yrs. 6mos. Female 5yrs. 11mos. 6yrs. 5mos. 7yrs. 2mos. 3yrs. 3mos. 2. Each tooth started to move toward occlusion at approximately stage 6 or after crown completion. 3. The highest increment in eruption rate was at about 1/3~1/2 completion of root and ages at 10-11 years in male, 9-10 years in female. 4. Eruption period of both sexes were as follows; Canine: 6-12years 1st. Premolar: 7-12 years 2nd. Premolar: 7-13 years 1st. Molar: 3-7 years 5. The eruption was completed before the root completion. 6. The sequence of eruption and calcification was 1st. Molar-Canine-1st. Premolar-2nd. Premolar in both sexes.

• Geosciences Journal
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• 제22권6호
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• pp.1069-1080
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• 2018

The Alaskan Aleutian Islands form one of the world's largest volcanic island chains. The islands are exposed to both direct and indirect damage from continuous volcanic eruptions. Surface deformation is mostly observed before volcanic eruption, but with some volcanoes, such as Ontake Volcano, deformations cannot be detected. In this study, we analyzed volcanic eruptions in the Alaskan Aleutian Islands, which is a region of frequent volcanic eruptions. Based on our results, we predicted the type of eruption that would occur on Baekdusan Volcano according to the presence or absence of surface deformation. For this purpose, 10 sites were selected from areas where recent volcanic activity had occurred in the Aleutian Islands. Additionally, Advanced Land Observing Satellite Phased Array-type L-band Synthetic Aperture Radar (ALOS-PALSAR) and European Remote Sensing (ERS)-1/2 satellite data were obtained from 10 experimental sites. Based on the radar satellite data, the volcanic surface deformations were identified, and the characteristics of the volcanic eruption were quantitatively calculated by determining the presence of surface deformation. The results of this study should facilitate the process of correlation between volcanic eruption and surface deformation.