• 대한치과교정학회지
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• 제15권1호
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• pp.123-140
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• 1985

Variation in the facial pattern and effect of the rotational jaw growth on the facial proportion were studied in serial cephalometric radiographs of 40 Korean children (25 boys, 15 girls) ranging in age from 6 to 13 years. According to Y-axis (N-S-Gn) growth change during the 7 years of period, the subject who had exhibited 'wave-like' manner of Y-axis growth change within ${\pm}\;2^{\circ}$ was classified to the Parallelwise group and the subject who had exhibited Y-axis increase more than $+2^{\circ}$ was classified to the Clockwise rotation group and the subject who had exhibited Y-axis decrease more than $-2^{\circ}$ was classified to the Counterclockwise rotation group. For the comparison of each group, a total of 22 morphologic variables were employed and the data were analyzed by means of computer morphometrics and statistical methods. On the basis of the finding of this study, the following trends were established. 1. The Parallelwise group was $75\%$, the Clockwise rotation group was $12.5\%$ and the Counter-clockwise rotation group was $12.5\%$. 2. The growth pattern of cranial base was related to the rotation of mandible. 9. Maxillary prognathism was occured in the Counterclockwise rotation group and the rotation of palatal plane was occured in the Clockwise rotation group. 4. Mandibular prognathism was occured in the Parallelwise and the Counterclockwise rotation groups, especially in the Counterclockwise rotation group. 5. The degree of maxillo-mandibular divergency was constant in the Clockwise rotation group but decreased in the Counterclockwise rotation and the Parallelwise groups, especially in the Counterclockwise group. 6. There were no differences in the size of the anterior upper facial height (N-ANS) and the posterior lower facial height ((Go-Me)-PNS) but there were differences in the size of the anterior lower facial height (ANS-Me) and the posterior upper facial height ((S-N)-PNS) between each group. 7. The growth increment and the size of the facial depth was not related to the growth pattern of the face but the growth increment and the size of the facial height was related to the growth pattern of the face. 8. Proportional change due to the facial growth rotation was concentrated in the anterior lower face. 9. The most apparent difference between each group was happened in the size of the posterior cranial base (S-Ba) and the facial length (S-Gn).

• 자원환경지질
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• 제29권4호
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• pp.509-522
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• 1996

A total of 460 palaeomagnetic samples was collected from the Tertiary Chongja-Ulsan basins and surrounding area in the southeastern part of Korean peninsula. All samples were stepwise demagnetized by either alternating field or thermal method. It was found that most sample-sites have ChRM declination which has been rotated clockwise from the north-south reference direction of Tertiary East Asia, although other two extrusive sample-sites within the Chongja sedimentary basin show counterclockwise rotation of ChRM declination. Fold tests for the site-mean ChRMs of the latter two sites reveal insignificant result and negative result with 95% confidence level, respectively. The amount of the clockwise deflection of declination varies from about $20^{\circ}$ upto about $80^{\circ}$ according to the block to which each sample-site belongs. The amount of the counterclockwise deflection is about $20^{\circ}$. It is concluded that the clockwise ChRM rotation has been caused by dextral simple shearing accompanied by NNW-SSE spreading of the East Sea which has been active until about 16Ma, and that the counterclockwise rotation is a result of sinistral simple shearing associated with WNW-ESE contraction in the Korean Strait-SW Japan region at about 15 Ma.

• Maxillofacial Plastic and Reconstructive Surgery
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• 제35권5호
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• pp.316-324
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• 2013

This case report describes the treatment of a 23-year-old woman who had lip protrusion with gummy smile and mentalis muscle strain. Orthognathic surgery was performed in conjunction with orthodontics. Minimum dental decompensation was performed with presurgical orthodontics followed by an anterior segmental osteotomy for the majority of dental decompensation. Counterclockwise rotation of the maxillomandibular complex was applied by LeFort I osteotomy, and bilateral sagittal split ramus osteotomies with anterior segmental osteotomy to achieve overall facial balance. The active treatment period was 15 months. Stable occlusion and skeletal relationship were observed after a 10-month follow-up period.

• 미생물학회지
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• 제32권1호
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• pp.70-77
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• 1994

Streptomyces coelicolor를 화학적 방법으로 돌연변이시킨 결과, 유전적 교잡방법에 의해 bldA와 유사한 위치인 10시 방향으로 위치가 결정되는 변이주들을 찾아내었다. 이들의 자세한 위치를 점검한 결과 cysA를 중심으로 반시계 방향으로 떨어져 있는 group고가 시계방향으로 떨어져 있는 두가지로 나뉘었다. 반시계 방향으로 떨어져 있는 변이주들을 bldA와 유사한 변이주라고 생각되어 이를 확인하기 위해 정상적인 bldA 유전자가 cloning 되어 있는 phage를 이용하여 기능적인 complementation 여부를 확인하여 보았다. Complementation이 되는 것으로 미루어 보아 이 변이주들이 bldA의 allele일 가능성이 매우 높으나 이들 중 몇몇 변이주들은 기존의 bldA와 무척 다른 양상을 보였다. 즉, 고영양 배지인 $R_2$YE배지에서 왕성하게 spore를 생산하며 wild type이 생산하는 이상의 색소 생산을 보인 점이다. 이때까지 발견된 bldA 변이주들은 배지 조성에 따라 약간의 aerial mucelium을 형성하는 것이 보고되었으나 이렇게 조건에 따라서는 완전히 bld phenotype을 잃는 변이주는 보고되지 않았다. 이 색소 생산이 실지로 항생물질 유전자의 발현에 의한 것이라는 것을 xylE fusion을 이용했을 때 유전자의 전사가 일어나는 것이 확인됨으로써 증명되었다. 또 이들 bldA 유사 변이주들은 actII-ORF4가 높음 copy수로 들어있는 pasmid에 의해 act 유전자를 발현하는 것도 관찰되었다.

• 수산해양기술연구
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• 제57권3호
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• pp.214-227
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• 2021

The distribution of tidal current and tidal induced residual current, topographical eddies and tidal residual circulation in the waters surrounding the Geumo Island-An Island channel were identified through numerical model experiments and vorticity balance analysis. Tidal current flows southwest at flood and northeast at ebb along the channel. The maximum flow velocity was about 100-150 cm/s in neap and spring tide. During the flood current in the neap tide, clockwise small eddies were formed in the waters west of Sobu Island and southwest of Daebu Island, and a more grown eddy was formed in the southern waters of Geumo Island in the spring tide. A small eddy that existed in the western waters of Chosam Island during the ebb in neap tide appeared to be a more grown topographical eddy in the northeastern waters of Chosam Island in spring tide. Tidal ellipses were generally reciprocating and were almost straight in the channel. These topographical eddies are made of vorticity caused by coastal friction when tidal flow passes through the channel. They gradually grow in size as they are transported and accumulated at the end of the channel. When the current becomes stronger, the topographic eddies move, settle, spread to the outer sea and grow as a counterclockwise or clockwise tidal residual circulation depending on the surrounding terrain. In the waters surrounding the channel, there were counterclockwise small tidal residual circulations in the central part of the channel, clockwise from the northeast end of the channel to northwest inner bay of An Island, and clockwise and counterclockwise between Daebu Island and An Island. The circulation flow rate was up to 20-30 cm/s. In the future, it is necessary to conduct an experimental study to understand the growth process of the tidal residual circulation in more detail due to the convergence and divergence of seawater around the channel.

• 대한치과교정학회지
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• 제30권4호
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• pp.491-507
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• 2000

이 연구는 측두하악장애 증상을 나타내는 부정교합자를 대상으로 교합안정장치 사용 전, 후의 측모 두부방사선 사진 상의 하악골의 위치변화를 구명하는데 그 목적이 있다. 연구의 대상자는 측두하악장애증상을 나타내는 부정교합자 60명이며 남자 19명, 여자 41명으로 각각의 평균연령은 19.5세와 21.5세 이었다. 전체 대상자를 전, 후방적으로는 Angle 분류법에 따른 교합관계에 의하여 Class I, II, III로 분류하였고, 수직적으로는 Jarabak의 후안면고경과 전안면고경의 비율에 따라서 clockwise, straight downward, counterclockwise의 3군으로 구분하여 부정교합군 별로 측정했으며 하악골의 위치변화를 중심교합시의 측모 두부방사선 사진 계측치들로부터 예측할 수 있는지 알아보기 위한 분석을 시행한 것으로 다음과 같은 결과를 얻었다. 1. 전체 대상자 비교시 측두하악장애를 갖는 부정교합환자에서 교합안정장치 사용 이후 하악골은 후하방 회전을 나타내었고 overjet은 1.3mm의 증가, overbite은 1.9mm감소되어 수평변화보다 수직적인 변화의 양이 컸다. 2. 전후방 3군 분류시 하악골의 후하방 변위를 나타내는 항목의 유의성 있는 변화는 Class II군에서 가장 현저하였으며 3군중 후방변위량이 가장 컸다. 3.수직 3군 분류시 Clockwise와 counterclockwise군에서 하악골의 후하방 변위를 나타내는 항목의 유의성 있는 변화가 뚜렷하였으며, 3군 모두에서 수직적인 변화량이 수평변화량 보다 컸다. 4. 중심교합위시의 부정교합 양태 및 골격유형, 그리고 중심교합위 계측치를 통하여 중심위 계측치를 설명할 수 있는 항목은 발견되지 않았다. 이상의 결과는 기존에 시행되어 오던 중심위 전환에 의한 방법이 아니고 측두하악장애를 갖는 부정교합자에서 교합안정 장치 를 장착하여 중심위를 획득한 상태에서 하악골의 위치 변화를 계측한 것으로 측두하악장애를 동반한 부정교합환자에서 중심교합위 상태의 측모 두부방사선 사진에 의존한 진단은 부정교합의 실체를 파악할 수 없음을 확인하였으며, 통상적으로 이용되어 온 중심위 전환방법 역시 중심위 유도후 발생되는 수직적인 부조화의 양상을 나타낼 수 없음을 입증하였다. 또한 전, 후방적으로는 Class II 부정교합군, 수직적으로는 Clockwise군과 Counterclockwise군에서 교합안정장치를 사용한 중심위 회복시에 하악골의 후하방 회전과 이에 동반된 구치부의 교합간섭으로 전후방 부조화뿐 아니라 수직적부조화를 더욱 심화시키므로 이에 대한 진단 및 치료시의 고려가 요구됨을 보여주었다.

• 대한치과교정학회지
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• 제27권2호
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• pp.231-243
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• 1997

본 연구는 거대 편도를 가진 기능성 III급 부정 교합자의 구대 편도 절제술 전후의 인두강, 설골, 두부 위치의 변화 양상에 대해 알아보기 위해 단국 대학교 부속 치과 병원 교정과에 내원한 남녀 환자 42명을 대상으로 연구하여 다음과 같은 결론을 얻었다. 1. Enlarged tonsil을 보이는 기능성 3급 부정교합자는 1급 부정교합자보다 혀는 전방에 위치하고 설골은 하방에 위치한다. 2. Tonsillectomy 후에 편도 절제술전과 비교하여 혀는 후방에 위치하고, nasopharynx은 증가 양상을 보이며, 설골은상, 후방에 위치하며 counterclockwise rotation 양상을 보인다. 3. Tonsillectomy 후에 nasopharynx depth변화와 하악 전치 경사도, 혀의 수직적 변화와 cranial base에 대한 hyoid axis, hyoid의 수직적, 수평적 변화와 두경부 경사도, 두경부 경사도와 하악 전치간에 95% 유의수준으로 상관성을 보인다. 4. Tonsillectomy 후에 설골 장축의 counterclockwise rotation시 hya-NL의 감소와 nasopharyx의 증가를 보이고, 혀의 거상시 hya-NL의 감소를 보이며, 혀의 후방위치시 h-h1의 증가와 hya-ba-n의 감소를 보인다.

• 대한치과교정학회지
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• 제18권2호
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• pp.367-385
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• 1988

In case of skeletal Class III malocclusion with underdeveloped maxilla, the extraoral orthopedic force for the stimulation of maxillary growth or anterior reposition of the maxilla has been used clinically for the improvement of facial skeletal relationship. The purpose of this investigation was to examine the initial reaction of maxillofacial complex to the maxillary protraction by using extraoral orthopedic force. The dried human skull was used and this investigation was done by means of double exposure holographic interferometry. The protraction forces placed on the canine or the first molar were parallel, $10^{\circ}$ downward, $20^{\circ}$ downward to the occlusal plane. Fringe pattern of each protraction condition was compared and analized. The results were as follows: 1. Each maxillofacial bone displaced saparately. 2. More displacement was shown at the area of the teeth and the alveolar bone. 3. A counterclockwise rotation of the maxilla wa decreased by downward protraction and especially 20 degree downward protraction from the canine showed least rotation. 4. On the zygomatic arch, outward bend was observed and this effect was decreased by downward protraction. 5. On the zygomatic bone, the counter clockwise rotation was increased by the downward protraction. 6. When maxillary expansion was applied at the same time, outward and upward displacement with counterclockwise rotation was observed on the maxilla. 7. The lateral pterygoid plate of sphenoid bone was affected by maxillary protraction.

• 대한치과교정학회지
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• 제21권2호
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• pp.419-432
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• 1991

The purpose of this study is to observe how the Class III intermaxillary elastics act upon the craniofacial structures of mixed dentition with anterior crossbites. The cephalometric headplafes of 16 childrens treated only with Class III elastics (C III elastics group) and 23 childrens treated with Class III elastics and Reverse pull headgear simultaneously (C III elastics + RPHG group) were traced, digitized and statistically analyzed. The results were as follows. 1 . Anterior displacement of maxilla was observed in both groups. 2. Simultaneous Class III elastics and reverse pull headgear group showed the counterclockwise rotation of maxilla, however Class III elastics group manifested no rotational change of maxilla. 3. Simultaneous Class III elastics and reverse pull headgear group showed the downward and backward rotation of mandible, however Class III elastics group manifested no rotational change of mandible. 4. Counterclockwise canting of occlusal plane, labial tipping of upper incisor and lingual tipping of lower incisor and mesial displacement of upper molar to pterygoid root vertical were observed in both groups.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume I
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• pp.352-355
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• 2006

In this study, the seasonal and inter-annual variation of sea surface current in the Gulf of Thailand were revealed through the use of WOD temperature and salinity data and monthly sea surface dynamic heights (SSDH) from TOPEX/Poseidon and ERS-2 altimetry data during 1995-2001. The mean dynamic height and mean geostrohic current were derived from the climatological data while SSDH data gave monthly dynamic heights and their geopstrophic currents. The mean geostrophic current showed strong southward and westward flow of South China Sea water along the gulf entrance. Counterclockwise eddy in the inner gulf and the western side of the gulf entrance associated with upwelling in the area. Seasonal geostrophic currents show basin-wide counterclockwise circulation during the southwest monsoon season and clockwise circulation during the northeast monsoon season. Upwelling was enhanced during the southwest monsoon season. The circulation patterns varied seasonally and inter-annually probably due to the variation in wind regime. And finally we found that congregation, spawning, and migration routes of short-bodied mackerel conform well with coastal upwelling and surface circulation in the gulf.