• 제목/요약/키워드: Eruption state

검색결과 48건 처리시간 0.03초

하악 제3대구치의 맹출 양상과 치관주위염과의 상관관계 (CORRELATION OF PERICORONITIS AND ERUPTION STATE OF THE MANDIBULAR THIRD MOLAR)

  • 정정권
    • Journal of the Korean Association of Oral and Maxillofacial Surgeons
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    • 제32권2호
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    • pp.161-167
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    • 2006
  • Objectives: Pericoronitis was the most common indication for mandibular third molar surgery and there are no universally acceptable predictive criteria for pericoronitis occurrence. This study was designed to analyze the correlation of the pericoronitis and the eruption state of the mandibular third molar using panoramic radiographs statistically. Materials and Methods: 218 patients whose chief complaint was the extraction of the mandibular third molar were examined. The presence and absence of pericoronitis, age, sex, position of extraction site, angulation, impaction degree, position to the anterior border of mandibular ramus, distance between distal cementoenamel junction of second molar and mesial cementoenamel junction of the mandibular third molar were assessed. Then the correlation of pericoronitis and the eruption state of the mandibular third molar were analyzed by Student's t-test and chi-square test. Results: There was no correlation between Pericoronitis and age, sex, position of the mandibular third molar. The angulation(P=0.005), impaction degree(P=0.043), relation with anterior border of mandibular ramus(P=0.003), distance between distal cementoenamel junction of second molar and mesial cementoenamel junction of the mandibular third molar(P<0.05) were correlated with pericoronitis. Conclusions: The occurrence of the pericoronitis can be predicted by the eruption state of the mandibular third molar such as angulation, impaction degree, relation with anterior border of mandibular ramus, distance between distal cementoenamel junction of second molar and mesial cementoenamel junction of third molar.

영구치의 맹출 장애에 관한 조사 연구 (ERUPTION DISTURBANCES OF TEETH IN KOREAN CHILDREN)

  • 이종범;장철호;김종철;한세현;이상훈
    • 대한소아치과학회지
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    • 제34권1호
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    • pp.13-18
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    • 2007
  • 맹출 중인 치아는 오랜 기간 동안 이동하는 과정에서 주위의 여러 요인들, 즉 유치의 조기 상실, 과잉치, 국소적 병소, 혀, 입술, 저작근, 외상 등에 의해서 다양한 영향을 받을 수 있다. 이러한 여러 요인들이 작용할 경우 치아의 정상적인 맹출 과정이 방해를 받게 되어 치아의 맹출 장애를 초래할 수 있다. 본 연구에서는 서울대학교 치과병원 소아치과에 2004년 1월 2일부터 2005년 12월 31일까지 신환으로 내원한 환자들, 총 8,010명의 주소를 분석하였고, 맹출 장애를 보이는 환자는 전체의 8.79%를 보였다. 맹출 장애의 유형은 맹출 지연이나 조기 맹출, 이소 맹출로 분류할 수 있었고, 맹출 지연이 가장 많이 나타난 치아는 상악 중절치이며, 조기 맹출이 호발한 치아는 하악 유중절치이고, 이소 맹출이 가장 많이 나타난 치아는 상악 제1대구치였다.

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하악 제3대구치가 하악 우각부골절 정복술후 감염에 미치는 영향에 관한 연구 (EFFECT OF THIRD MOLAR ON POSTOPERATIVE INFECTION AFTER REDUCTION OF THE MANDIBULAR ANGLE FRACTURE)

  • 최문기;민승기;이동근;오승환
    • Maxillofacial Plastic and Reconstructive Surgery
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    • 제23권3호
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    • pp.217-225
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    • 2001
  • Any fracture passing through the socket of a teeth is compounded intraorally, even if the fracture is not displaced and the tooth is firm in its socket. Before the advent of antibiotic therapy the danger of infection in a compounded fracture posed severe problems in treatment. Infection is reduced by antibiotic therapy but prolonged use of antibiotics is not justified in an attempt to save a tooth which might eventually be sacrificed. There is still controversy in the management of third molar in mandibualr angle fracture, particulary in regard to their retention or removal at the time of fracture treatment. So we surveyed the 159 patients who were treated with open reduction of mandibular angle fracture containing third molar in fracture line, and compared with the postoperative infection rate depending on time intervals between injury and operation, eruption state of third molar, non-extraction or extraction of third molar related to eruption state, non-extraction or extraction of third molar related to condiition of third molar and its surrounding periodontium and were to propose treatment guidline of third molar in mandibular angle fracture The results obtained were as follows : 1. There were no statistical significance between the time from injury to operation and postoperative infection. 2. There were no statistical significance between eruption state of third molar and postoperative infection. 3. In case of retention of the third molar, there were no statistical significance between eruption state of third molar and postoperative infection, but in case of extraction, postoperative infection was high rate in complete impacted cases. 4. There were no statistical significance between non-extraction or extraction of third molar and postoperative infection depending on condition of third molar. There are no difference in infection rate statistically according to the time from injury to operation, eruption state and condition of third molar, but retention of third molar revealed lowered infection rate in completely impacted cases. By terms of the manegement of third molar, we should extract or preserve third molar in the line of the mandibular angle fracture according to possibility of infection.

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과잉치의 맹출에 영향을 주는 요소에 대한 후향적인 연구 (RETROSPECTIVE ANALYSIS OF FACTORS INFLUENCING THE ERUPTION OF SUPERNUMERARY TOOTH)

  • 이동걸;장인걸;홍종락
    • Journal of the Korean Association of Oral and Maxillofacial Surgeons
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    • 제34권4호
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    • pp.445-449
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    • 2008
  • Unerupted or erupted supernumerary tooth may cause crowding, diastema, cyst formation, resorption, and displacement or rotation of adjacent teeth. However, there are few studies about prognosis about the pathologic condition and expectation of spontaneous eruption. The object of this study is to evaluate factors predicting the spontaneous eruption of supernumerary tooth. 431 patients (346 males and 85 females, aged from 5 to 29 years) who visited our institution from 2002-2006 and were shown to have 471 mesiodentes was reviewed. Supernumerary teeth were classified inverted and not inverted state. In case of not inverted supernumerary tooth, eruption rate ac cording to length of supernumenary tooth, width of the tooth, angle between the tooth and incisor tooth, location (inside the incisor or not) and shape (conical or tubercle) were investigated. The regression model showed that length, width and angle were all important determinants of influencing the eruption of supernumerary tooth (p < 0.001, Pearson R: 0.619). There is no relation between shape and eruption of supernumerary tooth (p > 0.05). Location of mesiodens has an effect on eruption of supernumerary tooth (p < 0.01).

맹출장애를 가진 하악 제1대구치의 치료 : 증례 보고 (Management of Eruption Disturbances of the Mandibular First Molar : A Case Report)

  • 전현순;양연미;백병주;김재곤
    • 대한소아치과학회지
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    • 제40권4호
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    • pp.314-320
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    • 2013
  • 하악 제1대구치 맹출장애의 빈도는 전체 인구의 0.01%로 드물게 나타나며, 발생 원인과 발견 연령 등에 따라 매복, 일차적 만기잔존(primary retention), 이차적 만기잔존(secondary retention) 등으로 분류된다. 치료로는 주기적 관찰, 외과적 노출술, 외과적 노출술 후 교정적 견인술, 탈구를 동반한 교정적 견인술, 외과적 재위치술, 발치 등의 방법을 적용할 수 있다. 이 증례보고는 각각 매복, 일차적 만기잔존, 그리고 이차적 만기잔존으로 진단된 5명의 환자들에서 다양한 치료방법을 이용하여 하악 제1대구치를 성공적으로 교합유도한 증례들을 보여준다. 맹출장애를 갖는 하악 제1대구치는 치아의 평균적인 맹출시기에 임상 및 방사선검사를 통해 매복, 일차적 만기잔존, 그리고 이차적 만기잔존으로 적절하게 진단내려질 수 있으며, 치아의 맹출 정도, 대합치와 인접치와의 관계, 환자의 연령, 협조도, 경제적 상황을 종합적으로 고려하여 치료되어야 한다.

제1대구치의 맹출 연령에 관한 분석 연구 (Study on the Eruption Age of the First Molar)

  • Hong-Chan Rah;Chong-Youl Kim
    • Journal of Oral Medicine and Pain
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    • 제19권1호
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    • pp.57-72
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    • 1994
  • This study was undertaken to obtain the data age determination following the eruption of individual cusps of the first molars in the point of forensic odontology. 532 children (294 male and 238 female, born between April, 1989 and March, 1986) from a kindergarten and a primary school in a reesidential district in Seoul were studied. The eruption state of the first molar was divides into 6 stages according to the degree of exposure of individual cusps, and correlation between the stage and age was stastically analysed. The results of the study lead to following conclusions : 1. The most frequently seen eruption sequence of cusps for the upper first molar was mesibuccal cusp, mesiopalatal cusp, distobuccal cusp, mesiodistal cusp, distopalatal cusp. As for the lower first molar : mesiobuccal cusp, mcsiolingual cusp, distobuccal cusp, distolingual cusp. 2. The time of eruption was earlier in the female ethan in the male, but it was stastically remarkable only in upper and lower parts of the right and the left teeth of subjects age between 6.0 and 6.5 and upper part of the right and the left teeth of subjects age over 7.5 3. The eruption of the lower first molar was comparatively earlier than that of the upper first molar and there was no significant stastical difference between the right and the left first molars in the time of eruption. 4. There was no noticeable difference in the eruption sequence of cusps, irrespective of sex and side. 5. The eruption of the upper first molar is started at the age of about 6.4 and complete the age of about 7.1 and as for the lower first molar, it is from 6.3 to 7.0

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A model of a solar eruption affected by a solar wind

  • Lee, Hwanhee;Magara, Tetsuya;Kang, Jihye;Satoshi, Inoue;An, Jun-Mo
    • 천문학회보
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    • 제39권2호
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    • pp.99.2-99.2
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    • 2014
  • We investigate how a solar eruption occurs in an environment where a solar wind exists during a pre-eruptive phase. To understand it, we have performed three-dimensional simulations based on a zero-beta magnetohydrodynamic (MHD) equations in various ways to drive an eruption with a solar wind. A pre-eruptive state is derived by applying a nonlinear force-free reconstruction method to a flux emergence full MHD simulation. We discuss what is the most appropriate way to drive a solar wind-related eruption.

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Ionospheric Responses to the Earthquake in the Gulf of Alaska and the Kusatsu-Shiranesan Volcanic Eruption on 23 January 2018

  • Shahbazi, Anahita;Park, Jihye
    • Journal of Positioning, Navigation, and Timing
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    • 제11권4호
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    • pp.305-316
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    • 2022
  • Numerous research revealed a strong association between the ionospheric perturbations and various natural hazards. The ionospheric measurements from Global Navigation Satellite System (GNSS) observations provide the state of electron contents in the ionosphere that contributes to investigate the source events. In this study, two geophysical events occurred on 23 January 2018, the 7.9 Mw earthquake in Alaska and Kusatsu-Shiranesan volcanic eruption in Japan, are examined to characterize the fingerprint of each event in the ionosphere. Firstly, we extracted the Total Electron Content (TEC) from GNSS measurements, then isolated disturbed wave signatures from the TEC measurements that is referred to as a traveling ionospheric disturbance (TID). As TIDs are short-term ionospheric variations, the major trend of GNSS TEC measurements should be properly removed. We applied a natural neighbor interpolation method together with a leave-one-out cross validation technique for detrending. After detrending the TEC, the remaining signals are further enhanced by applying a band-pass filter and TIDs are detected from them. Finally, the detected TIDs are verified as the response of the ionosphere to Kusatsu-Shiranesan volcanic eruption and Gulf of Alaska earthquake which propagated through the ionosphere with an average velocity of 530 m/s and 724 m/s, respectively. In addition, a coherence analysis is conducted to discriminate between the signatures from a volcanic explosion and an earthquake. The analysis reveals the TID waveforms from each single event are highly correlated, while a low correlation is found between the TIDs from the earthquake and explosion. This study supports the claim that different geophysical events induce the distinctive characteristics of TIDs that are detectable by the ionospheric measurements of GNSS.

Hydroacoustic Records and Numerical Models of the Source Mechanisms from the First Historical Eruption of Anatahan Volcano, Mariana Islands

  • Park M.;Dziak R.P.;Matsumoto H.
    • 한국지구물리탐사학회:학술대회논문집
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    • 한국지구물리탐사학회 2004년도 대한지구물리학회.한국지구물리탐사학회 공동학술대회 초록집
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    • pp.232-237
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    • 2004
  • Anatahan Volcano in the Commonwealth of the Northern Mariana Islands (CNMI) erupted for the first time in recorded history on 10 May 2003. The underwater acoustic records of earthquakes, explosions, and tremor produced during the eruption were recorded on a sound-channel hydrophone deployed in February 2003. Acoustic propagation models show the seismic to acoustic conversion at Anatahan is particularly efficient, aided by the slope of the seamount toward the hydrophone. The hydrophone records confirm the onset of earthquake activity at 01:53Z on 10 May, as well as the onset (at ${\~}$06:20Z) of continuous, low-frequency (5-40 Hz) acoustic energy that is likely volcanic tremor related to magma intrusion. The hydrophone recorded a total of 458 earthquakes associated with the eruption. To predict the character of acoustic signals generated from Anatahan, we developed a moment-tensor representation of a volcano-seismic source that is governed by the geometry of the source and the physical properties of the magma. A buried magmatic pipe model was adopted, and numerically modeling source parameters such as the pipe radius and magma viscosity enable us to grasp the inward nature of Anatahan Volcano.

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역위 매복된 상악 중절치의 자발적 맹출유도 (CASE REPORT : FOR SPONTANEOUS ERUPTION GUIDANCE OF INVERTED MAXILLARY CENTRAL INCISOR TEETH)

  • 최선아;이난영;이상호;이창섭
    • 대한소아치과학회지
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    • 제31권3호
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    • pp.406-411
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    • 2004
  • 영구 상악 절치의 매복은 매복이 흔한 제3대구치와 상악 견치에 비해서 드물지만 상악 중절치 미맹출을 주소로 내원한 학동기 아동에서 종종 관찰된다. 매복을 유발시키는 원인에 대해서는 많은 논란이 있으나 주 요인으로는 유치의 외상과 유치의 치근단 감염이 보고되고 있다. 특히 유치의 치근단 감염에 의한 매복설이 유력한데 병소의 압력에 의한 계승영구치의 회전, 변위등의 위치변화가 일어날 수 있다고 보고되고 있다. 매복치는 무엇보다도 조기에 발견하여 치료하는 것이 이로 인해 발생되는 부정교합이나 그 밖의 부작용을 예방할 수 있다. 일단 매복이 진단되면 방사선 검사를 통하여 위치 확인을 정확히 하는 것이 중요하며 치료에 앞서 전반적인 공간분석과 치료계획을 세워야 한다. 치료로는 교정적 견인, 또는 자가이식등이 있으며, 역위 매복된 경우가 아니라면 공간 확보만으로도 50%의 자발적 맹출을 보고하고 있다. 본 증례는 유치의 치근단 감염에 의해 역위 매복된 것으로 보이는 상악 중절치를 교정력을 이용해 정상적인 맹출로 바로 잡아준 결과 4-5개월만에 자발적으로 맹출하였기에 이에 보고하는 바이다.

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