• 대한치과교정학회지
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• 제28권3호
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• pp.431-440
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• 1998

치주질환에 이환된 성인환자에서 상악전치의 치간공간과 아울러 정출이 발생된 경우 기능 및 심미의 회복을 위해서는 함입이동이 필요하다. 본 연구는 골하치주낭 즉, 수직적 골결손이 있는 절치의 함입이동시 치주조직 반응을 살펴보기 위하여 시행되었다. 상악 좌우 측절치에 골결손과 함께 치주질환을 유발시킨 성견 4마리를 실험대상으로 하여 양측 모두에 치주수술을 시행하고 결손부 최하방 치근면에 notch를 형성 한 2주후 우측 제2측절치는 4주간 함입이동 후 4주간 보정을 시행한 실험측으로, 좌측 제2측절치는 구강위생관리만 시행한 대조측으로 사용한 바 조직소견을 통하여 다음과 같은 결론을 얻었다. 1. 함입이동없이 치주수술만 시행한 대조측의 조직소견은 치주낭 깊이의 감소를 보였으나 notch 부위부터 치주낭 기저부까지 긴 접합상피 상태를 보였으며 신생백악질이 형성된 일부에서만 결합조직 부착의 양상이 보였다. 2. 함입이동을 시행한 실험측은 대조측에 비하여 상피부착이 줄어든 반면 보다 넓은 신생 결합조직 부착 소견을 나타내었다. 3. 대조측과는 달리 실험측 notch근처의 결합조직내에는 다수의 세포가 관찰되었으며, 신생 백악질 생성 역시 대조측보다 많이 관찰되었다. 이상의 결과는 치주질환으로 인하여 정출된 치아에서도 철저한 염증조절과 구강위생이 유지되고 적절한 크기의 힘에 의하여 순수한 함입이동이 적용된다면 바람직한 치료결과가 가능함을 시사하였다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제7권3호
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• pp.3-17
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• 2002

본 연구는 부산시 동남해안 지역에서 해수침입의 지역적 특성과 해수침입의 범위를 파악하기 위하여 지하수 모니터링공의 자료분석과 지구통계학적 기법을 이용하였다. 강수에 의한 직접적인 지하수의 충진으로 모니터링 우물에서의 지하수위는 강수량과 비례하지만 전기전도도는 강수량과 대체로 반비례하는 것으로 나타났다. 모니터링 우물에서 전기전도도는 약 24m심도에서 급격히 증가되어 26m전후에서 20,000$\mu\textrm{s}$/cm를 초과하였고, 지하수위와 전기전도도를 비교한 결과, 지하수위가 낮아질수록 해수와 담수의 경계면이 상승하는 경향을 보인다. 교차상관성 분석에 의하면 지하수위와 강수량은 시차가 0일 때 교차상관 계수가 최대이지만, 전기전도도와 강수량의 교차상관계수는 시차가 9일 때 최대로 나타났다. 이것은 지하수위 변동이 강수에 의하여 단시간에 영향을 받고 있으나, 해수와 담수의 경계면은 강수에 의하여 매우 느리게 반응한다는 것을 나타낸다. 2개의 측선에서 실시된 수평전기탐사 자료의 역산결과, Line 1에서는 동쪽 끝에서 내륙으로 약 14m지점까지, Line 2에서는 동남쪽 끝에서 내륙으로 약 25m지점까지 해수가 침투한 것으로 나타났다 5월과 7월에 슬럼버져 배열의 수직전기탐사를 실시하여 획득한 자료는 각각 대수정규분포를 나타내었고, 크리깅에 의한 겉보기비저항 분포도와 전기비저항 분포도를 비교하면 5월보다 7월에 비저항치가 상승한 것으로 나타났다. 이것은 6, 7월에 내린 강수로 지하수의 함양량이 증가하여 대수층내 해수의 농도가 감소하였기 때문이다 겉보기비저항의 수직단면도 및 평면도 그리고 전기비저항 분포도를 분석한 결과. 지구통계학적 기법은 해안 지역에서의 전기비저항 분포 변화를 파악하는데 매우 유용하였다.

• 지질공학
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• 제18권3호
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• pp.331-338
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• 2008

다양한 조건의 관정에 지하수를 채수할 수 있는 샘플러를 개발하고 평가하였다. 이 샘플러는 공압 튜브, 공압 실린더, 주사기 바늘 그리고 샘플병으로 구성되며, 공기압을 동력원으로 사용한다. 공압 실린더는 주사기 바늘을 샘플병의 고무마개에 관통시키는 기능을 담당하며, 샘플병 고무마개를 관통한 주사기 바늘은 샘플병으로의 지하수 유입 통로 역할을 담당한다. 샘플러 현장시험은 해수의 영향으로 수질이 주기적으로 변화하는 제주 한동지역의 해수침투 관측정을 대상으로 하였다. 샘플러의 내부와 외부에 CTD Diver를 장착하고 관정내 동일 심도에서의 샘플링을 여러 차례 반복하면서 샘플링 단계별 전기전도도와 압력 변화를 측정하였다. 시험 결과, 샘플러를 작동시킬 때에만 지하수가 샘플러로 유입되며, 샘플러 내부와 외부에서 측정한 지하수의 전기전도도와 압력은 거의 일치하는 것이 확인되었다. 이러한 결과는 이 연구에서 제시한 샘플러를 이용하여 채수한 지하수 시료들이 샘플러 설치 심도의 샘플링 시간대의 지하수 수질을 정확하게 반영하고 있음을 지시한다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2005년도 총회 및 춘계학술발표회
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• pp.271-275
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• 2005

The horizontal heat-pulse flowmeter was used to measure grounwater flow in volcanic rocks at sites in eastern part of Jeju Island, Korea. Three boreholes, Handong-1, Jongdal-1, and Susan-1, which are located at close distance from the coastline, were selected from the sea water intrusion monitoring wells. To evaluate the direction and velocity of the groundwater flow, 6 to 8 measuring points for each borehole were chosen. There are two major flow directions at Handong-1, which are toward north-east and south-east directions and velocity ranges from $2.2{\sim}3.0cm/hr\;and\;0.6{\sim}1.0cm/hr$, respectively. For Jongdal-1, two major flow directions were detected that are east and north-west and velocity ranges from $1.2{\sim}2.0cm/hr$. For Susan-1, major flow is toward east direction and the ,velocity ranges from $2.2{\sim}2.7cm/hr$ at depth $60{\sim}70m$,\;and\;0.8{\sim}0.9cm/hr$ at depth $70{\sim}80m$. In order to evaluate the tidal effect on groundwater flow, direction and velocity were measured at specific depth with time, At depth 57m of Susan-1, the velocity increased during the tidal variation, The flow direction and velocity varies with different depths, and they are also affected by tidal fluctuation. Thereafter, care must be taken when flow direction and velociy is estimated indirectly by using hydraulic head at monitoring wells.

• 자원환경지질
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• 제19권spc호
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• pp.103-112
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• 1986

The geology of the mine consists of Cretaceous lower andesitic breccia member, tuffaceous black shale, upper tuffaceous sandstone member and andesitic dike. Ore bodies are two parallel veins of breccia originated from hydrothermal activity of later acidic igneous intrusion. First two periods of mineralization, gold and silver, and copper, and later copper enrichment was identified. The first two might have been occurred during boiling of hydrothermal solution that formed breccia and copper enrichment was accomplished by enhancement of $CO_2$ fugacity from the organic material contained in the black shale. With all the geologic and mineralogic data and inferences attained from other investigators it was estimated that the optimum depth of the ore mineralization was between 500m and 300m below the surface of Kyong-Sang series.

• 한국콘크리트학회:학술대회논문집
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• 한국콘크리트학회 2004년도 춘계 학술발표회 제16권1호
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• pp.838-841
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• 2004

This paper presents the experimental results on the penetration of chloride. ions to ordinary portland cement concrete which is subjected to 2 different artificial environments; consecutive digestion, wetting at $3\%$ NaCl for 1 day and then drying at $40^{\circ}C$ oven for 4 days. The water-cement ratio was $35\%,\;45\%,\;55\%$. Test results showed that the intrusion depth and concentration of chloride ions penetrated into concrete in repeated wetting-drying environments were respectively deeper and higher than those of consecutive digestion environment. The penetration of chloride ions deeply depend on the effect of water to cement ratio.

• 한국농업기계학회:학술대회논문집
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• 한국농업기계학회 1993년도 Proceedings of International Conference for Agricultural Machinery and Process Engineering
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• pp.556-564
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• 1993

The response of salt affected rice soils to salinity reclaimation by flushings and chemical amelioration by lime and gypsum were evaluated . Soils with good drainage system responded well to simple reclimation . The effects of seawater intrusion were reduced efficiently in a very short time. Yields of rice crops recovered to their potential level within one to two seasons of cropping. Soil profile strength was also improved under well drained areas. However, when drainage system was ineffective the problems of salinity and soil strength remained unsolved. Under both condition, water depth management played important role in the survival of rice crop under the sline soil conditions.

• Journal of the korean society of oceanography
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• 제33권4호
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• pp.146-156
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• 1998

Hydrographic data retrieved in the southwestern part of the East Sea in 1992-1993 were analyzed to investigate the probability of southward intrusion of the East Sea Intermediate Water (ESIW) into the Ulleung Basin. The ESIW showed the ranges of 1 to 4$^{\circ}$C in potential temperature, 33.80-34.06 psu in salinity, and 26.9-27.3 kg/m$^3$ in potential density (${\sigma}$$_{\theta}$). The mean depth occupied by the ESIW was 170 m, where the characteristic values of the above three were 2.64$^{\circ}$C , 34.02 psu, and 27.13 kg/m$^3$, respectively. One of the most prominent features of the ESIW was that its salinity changed not only seasonally but also interannually. It was low in summer and high in winter. The salinity within the isopycnal layer of 26.9-27.3 kg/m$^3$ was closely related with the potential vorticity (${\rho}$$_{\theta}^{-1}$ f ${\varrho}$${\rho}_{\theta}$/${\varrho}$z), being in direct proportion to the salinity. This implies that the low-salinity water was thicker than the high-salinity water. The flow path of the ESIW was investigated by tracking the low-salinity or the low-potential vorticity water and by referring to acceleration potential. Careful analysis of the flow path proves that the ESIW intrudes from the north between the Korean coast and Ulleung Island into the Ulleung Basin in summer. Existence of the high-potential vorticity water in the Ulleung Basin is associated with the interruption of the inflow of low-salinity water.

• 대한치과교정학회지
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• 제45권6호
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• pp.289-298
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• 2015

Objective: To evaluate and compare the effects of two appliances on the en masse retraction of the anterior teeth anchored by temporary skeletal anchorage devices (TSADs). Methods: The sample comprised 46 nongrowing hyperdivergent adult patients who planned to undergo upper first premolar extraction using lingual retractors. They were divided into three groups, based on the lingual appliance used: the C-lingual retractor (CLR) group (group 1, n = 16) and two antero-posterior lingual retractor (APLR) groups (n = 30, groups 2 and 3). The APLR group was divided by the posterior tube angulation; posterior tube parallel to the occlusal plane (group 2, n = 15) and distally tipped tube (group 3, n = 15). A retrospective clinical investigation of the skeletal, dental, and soft tissue relationships was performed using lateral cephalometric radiographs obtained pretreatment and post en masse retraction of the anterior teeth. Results: All groups achieved significant incisor and canine retraction. The upper posterior teeth did not drift significantly during the retraction period. The APLR group had less angulation change in the anterior dentition, compared to the CLR group. By changing the tube angulation in the APLR, the intrusive force significantly increased in the distally tipped tube of group 3 patients and remarkably reduced the occlusal plane angle. Conclusions: Compared to the CLR, the APLR provides better anterior torque control and canine tipping while achieving bodily translation. Furthermore, changing the tube angulation will affect the amount of incisor intrusion, even in patients with similar palatal vault depth, without the need for additional TSADs.

• 대한치과교정학회지
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• 제45권3호
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• pp.121-129
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• 2015

Objective: This study aimed to assess three-dimensional changes in the temporomandibular joint positions and mandibular dimensions after correction of dental factors restricting mandibular growth in patients with Class II division 1 or division 2 malocclusion in the pubertal growth period. Methods: This prospective clinical study included 14 patients each with Class II division 1 (group I) and Class II division 2 (group II) malocclusions. The quad-helix was used for maxillary expansion, while utility arches were used for intrusion (group I) or protrusion and intrusion (group II) of the maxillary incisors. After approximately 2 months of treatment, an adequate maxillary arch width and acceptable maxillary incisor inclination were obtained. The patients were followed for an average of 6 months. Intraoral and extraoral photographs, plaster models, and cone-beam computed tomography (CBCT) images were obtained before and after treatment. Lateral cephalometric and temporomandibular joint measurements were made from the CBCT images. Results: The mandibular dimensions increased in both groups, although mandibular positional changes were also found in group II. There were no differences in the condylar position within the mandibular fossa or the condylar dimensions. The mandibular fossa depth and condylar positions were symmetrical at treatment initiation and completion. Conclusions: Class II malocclusion can be partially corrected by achieving an ideal maxillary arch form, particularly in patients with Class II division 2 malocclusion. Restrictions of the mandible in the transverse or sagittal plane do not affect the temporomandibular joint positions in these patients because of the high adaptability of this joint.