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- 저자 : 김창성 ( Chang Seong Kim ) (검색결과 145 건)
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김성준(Seong-Jun Kim),김창성(Chang-Sung Kim) 응용생태공학회 2020 Ecology and resilient infrastructure Vol.7 No.4
본 연구에서는 낙동강을 대상으로 HEC-RAS를 이용하여 보 개방에 따른 하상변동 특성을 분석하였다. 연구 대상 지역은 낙동강 구담교 하류부터 하구둑까지 292.37 km 구간이다. 하상변동 모의를 위하여 1차원 수치해석모델인 HEC-RAS 프로그램을 사용하였으며 2017년도부터 2019년도까지 2가지의 시나리오로 모의를 수행하였다. 시나리오 1은 수문 전면 개방의 조건으로 구축하였으며 시나리오 2는 수문이 설치된 조건으로 모의를 수행하였다. 모의결과, 시나리오 1의 조건에서 합천창녕보 – 창녕함안보 대부분의 구간 (약 40 km)에서 퇴적이 발생한 것을 확인하였다. 또한 낙동강 본류 내의 유사를 포함한 흐름이 보 구조물로 인해 단절되지 않고 연속적으로 하상을 변동시키는 것으로 예측되었다. In this study, the characteristics of bed elevation changes of the Nakdong River when weir gates are opened were analyzed using the Hydrologic Engineering Center-River Analysis System (HEC-RAS). The study area was 292.37 km downstream of the Gudam Bridge to the Nakdong estuary of the Nakdong River. The HEC-RAS program, which is a 1D numerical analysis model, was used to simulate bed elevation changes. Simulations were conducted under two scenarios from 2017 to 2019. Scenarios 1 and 2 were devised under the conditions of a fully opened gate and during gate installation, respectively. Results confirmed that, under the conditions of Scenario 1, deposition occurred in most sections from the Hapcheon-Changnyeong weir to the Changnyeong-Haman weir (a distance of approximately 40 km). In addition, it was predicted that the flow that included sediments in the main stream of the Nakdong River was not interrupted by the weir structure and regularly produced changes in the river bed.
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이승범,연제영,채경준,정의원,김창성,이용근,조규성,채중규,김종관,최성호,Lee, Seung-Bum,Yon, Je-Young,Chae, Gyung-Joon,Jung, Ui-Won,Kim, Chang-Sung,Lee, Yong-Geun,Cho, Kyoo-Sung,Chai, Jung-Kiu,Kim, Chong-Kwan,Choi, Seong-Ho 대한치주과학회 2007 Journal of Periodontal & Implant Science Vol.37 No.4
Purpose: Various bone graft materials are being used for periodontal tissue regeneration. Th materials are being developed continuously for ideal clinical effects. Therefore, it is necessary to identify the clinical characteristics of each bone graft material through comparing the various bone graft materials statistically and in doing so, proposing a more efficient bone graft material. In this study, the following results were attained through comparing the clinical effects among the bone graft materials, using the statistical method based on the clinical studies published at the department of periodontology of Yonsei hospital. Materials and Method: 6 selected studies of department of Periodontology at Yonsei University Hospital were based on clinical study of bone grafting in intrabony defects. It was compared the clinical parameters among the 6 clinical studies, using the statistical META analysis. Result: When comparing the probing depth reduction, there was a relatively great amount of decease when using the xenograft, Anorganic Bovine Derived Hydroxapatite Bone Matrix/Cell Binding Peptide(ABM/P-15: PepGen $P-15^{(R)}$) and the autogenous bone and absorbable membrane, d, 1-alctide/glycolide copolymer(GC: $Biomesh^{(R)}$). The allogfrafts showed a relatively low decrease in the probing depth and clinical attachment change. It also showed a slight decrease in the bone probing depth. The allografts showed various results according to different bone graft materials. When comparing the ABM/P-15 and bovine bone $powder(BBP^{(R)})$, ABM/P-15 showed a relatively high clinical attachment level and the bovine bone powder showed a relatively high clinical attachment level. The probing depth change and gingival recession change showed a lower value than the mean value between the two bone graft materials. The synthetic bone showed a relatively high decrease in clinical attachment level and periodontal probing depth change. There was a relatively larger amount of gingival recession when using Bioactive Glass(BG) but a relatively low bone regeneration effect was seen. Conclusion: Good restorative results of the periodontal tissue can be attained by applying the various bone graft materials being used today after identifying the accurate clinical effects.
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김창성,김용휘,최선규,고광범,한경수,Kim, Chang Seong,Kim, Yong-Hwi,Choi, Seon-Gyu,Ko, Kwang-Beom,Han, Kyeong-Soo 대한자원환경지질학회 2017 자원환경지질 Vol.50 No.1
단파장적외선 분광분석법을 현장에 적용하여 일정한 스펙트럼을 획득할 수 있는 시료의 표면상태, 수분함유 정도 및 분석조건에 대하여 검토하였다. 자연면, 절단면, 분말의 표면상태 중 자연면과 절단면은 거의 유사한 스펙트럼이 획득되었으며, 분말상태의 시료에서는 스펙트럼의 변화가 인지된다. 수분이 함유된 시료는 24시간 이상 상온 건조 후 측정 시 일정한 스펙트럼을 얻을 수 있으므로, 현장에서의 여건에 따라 24 ~ 48시간의 건조시간이 필요할 것이다. 밝은 색 광물의 경우 기기의 기본 값인 10회 반복측정으로도 안정적인 스펙트럼의 획득이 가능하였으나, 어두운 색의 광물은 100회에 해당하는 10초 정도의 분석시간이 필요할 것으로 판단된다. 열수변질대 탐사 시, 2,160 ~ 2,330 nm 영역에서의 흡수피크 위치 및 형태를 기준으로, 그 외의 스펙트럼 특징들을 이용하면 대략적인 열수변질대 분대가 현장에서도 가능할 것으로 판단된다. 2,160 ~ 2,180 nm는 고령석, 딕카이트, 엽납석 및 명반석에 의해 (고)점토대((advanced) argillic zone)로, 2,180 ~ 2,230 nm의 흡수피크는 백운모, 견운모 및 스멕타이트에 의해 견운모대(phyllic zone), 2,230 ~ 2,270 nm 영역의 흡수피크는 녹니석 및 녹염석에 의해 프로필리틱대(prophylitic zone)로 구분 가능하다. 2,270 ~ 2,330 nm 영역에서는 명반석, 활석, 사문석, 각섬석, 탄산염광물 등 다양한 광물의 흡수피크가 나타나므로, 보다 더 세밀한 스펙트럼 해석이 요구된다. The analytical conditions including surface state, moisture effect, and device condition were investigated for applying Short Wave Infrared(SWIR) spectroscopy to the field survey. Among the three surface state of samples (exposed surface, cutting face and powder), both spectra from the exposed surface and cutting face are almost identical whereas spectral variation was detected in powder sample. Over 24-hours-dryring of the wet sample at room temperature, the samples show a similar spectrum with that of dry condition. The result suggests that outcrop samples mighty be dried for 24 ~ 48 hours depending on the wetness of outcrop. The bright minerals could produce stable spectra with 10 times measurements as default value of the device under SWIR spectroscopy but the dark minerals would require about 10 seconds, which corresponds to 100 times measurements to get the reliable spectra. The position and shape 2,160 ~ 2,330 nm and/or other spectral features of hydrothermal alteration minerals by SWIR spectroscopy could be used for a classification of hydrothermal alteration zone in the field. Absorption peaks in 2,160 ~ 2180 nm are useful for identifying (advanced) argillic zone by spectral characteristics of kaoline, dickite, pyrophyllite, and alunite. Absorption peaks in 2,180 ~ 2,230 nm are able to define muscovite, sericite, and smectite, which are key alteration minerals in phyllic zone. Absorption peaks in 2,230 ~ 2,270 nm can be used to recognize prophylitic zone where chlorite and epidote occur. Absorption peaks of other principle minerals such as talc, serpentine, amphibole, and carbonate group are mainly detected within the wave length of 2,270 ~ 2,330 nm. This result indicates that the spectra of these minerals need to be carefully interpreted.
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한국 포천 철(-동) 스카른 광상의 지질, 광화작용 및 생성연대
김창성,고지수,최선규,김상태,Kim, Chang Seong,Go, Ji Su,Choi, Seon-Gyu,Kim, Sang-Tae 대한자원환경지질학회 2014 자원환경지질 Vol.47 No.4
선캄브리아기 경기육괴의 북서부에 위치한 포천 철(-동)광상은 다양한 이론이 제시되어 논쟁 대상이 되었으며, 성인적 측면에서 변성(-배기형) 퇴적 광상이 주된 생성이론으로 인지되었다. 본 논문에서는 포천 스카른화작용/철광화작용의 핵심 증거를 통하여 공간적으로 인접한 명성산 화강암이 관계화성암의 가능성을 제시하였다. 포천 스카른은 석회암과 백운암의 다양한 탄산염암을 모암으로 하여 Ca계열, Mg계열 및 Na-Ca계열 스카른이 형성되었다. 철광화작용은 주로 Na-Ca계열 스카른대를 따라 배태되고 있으며, 후퇴 스카른 단계에 국부적으로 동 광화작용이 중첩된다. 포천 후퇴 스카른 단계에 정출된 금운모의 Ar-Ar과 K-Ar연대측정 결과는 $110.3{\pm}1.0{\sim}108.3{\pm}2.8Ma$이며, 스카른 철(-동) 광화작용은 천부 관입암체인 명성산 화강암의 관입시기(112 Ma)와 일치하여 관계화성암으로 추정된다. 주변 탄산염암, 스카른 및 맥상의 탄산염광물간 산소-탄소 동위원소 빈화된 경향성은 개방계 조건($XCO_2=0.1$)에서 열수의 탈탄산염화 작용과 침투작용에서 유도되었다. 한편 황화광물(황동석-황철석 혼합물)과 경석고에서 매우 높은 황 동위원소 값은 황근원물질이 주변 탄산염암에 함유되어 있던 황산염광물로부터 공급되었을 가능성을 지시한다. 포천 광상 주변의 전단대에서는 파쇄대가 중첩되어 발달하여 있으며, 백악기 화강암으로부터 공급된 고온성 광화유체가 이러한 약선대를 따라 유입되어 약 $500^{\circ}{\sim}400^{\circ}C$의 온도범위에서 강력한 근지성 스카른화작용과 함께 광화작용이 유도되었다. The Pocheon iron (-copper) deposit, located at the northwestern part of the Precambrian Gyeonggi massif in South Korea, genetically remains controversial. Previous researchers advocated a metamorphosed (-exhalative) sedimentary origin for iron enrichment. In this study, we present strong evidences for skarnification and Fe mineralization, spatially associated with the Myeongseongsan granite. The Pocheon deposit is composed of diverse carbonate rocks such as dolostone and limestone which are partially overprinted by various hydrothermal skarns such as sodic-calcic, calcic and magnesian skarn. Iron (-copper) mineralization occurs mainly in the sodic-calcic skarn zone, locally superimposed by copper mineralization during retrograde stage of skarn. Age data determined on phlogopites from retrograde skarn stage by Ar-Ar and K-Ar methods range from $110.3{\pm}1.0Ma$ to $108.3{\pm}2.8Ma$, showing that skarn iron mineralization in the Pocheon is closely related to the shallow-depth Myeongseongsan granite (ca. 112 Ma). Carbon-oxygen isotopic depletions of carbonates in marbles, diverse skarns, and veins can be explained by decarbonation and interaction with an infiltrating hydrothermal fluids in open system ($XCO_2=0.1$). The results of sulfur isotope analyses indicate that both of sulfide (chalcopyrite-pyrite composite) and anhydrites in skarn have very high sulfur isotope values, suggesting the $^{34}S$ enrichment of the Pocheon sulfide and sulfate sulfur was derived from sulfate in the carbonate protolith. Shear zones with fractures in the Pocheon area channeled the saline, high $fO_2$ hydrothermal fluids, resulting in locally developed intense skarn alteration at temperature range of about $500^{\circ}$ to $400^{\circ}C$.
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성견의 치조 연상 임플란트주위 결손부에서의 탈회냉동건조골과 e-PTEE막의 효과
김창성,최성호,조규성,Kim, Chang-Sung,Choi, Seong-Ho,Cho, Kyoo-Sung 대한치주과학회 2001 Journal of Periodontal & Implant Science Vol.31 No.1
The purpose of this study was to evaluate the adjunctive combined effect of demineralized freeze-dried bone allograft(DFDB) in guided bone regeneration on supra-alveo-lar peri-implant defect. Supra-alveolar perio-implant defects, 3mm in height, each including 4 IMZ titanium plasma-sprayed implants were surgically created in two mongrel dogs. Subsequently, the defects were treated with 1 of the following 3 modalities: Control) no membrane or graft application, Group1) DFDB application, Group2) guided bone regeneration using an expanded polytetra-fluoroethylene membrane, Group3) guided bone regeneration using membrane and DFDB. After a healing period of 12-week, the animals were sacrificed, tissue blocks were harvested and prepared for histological analysis. Histologic examination were as follows; 1. New bon formation was minimal in control and Group 1, but considerable new bone formation was observed in Group 2 and Group 3. 2. There was no osteointegration at the implant-bone interface in the high-polished area of group2 and Group 3. 3. In fluorescent microscopic examination, remodeling of new bone was most active during week 4 and week 8. There was no significant difference in remodeling rate between group 2 and group 3. 4. DFDB particles were observed, invested in a connective tissue matrix. Osteoblast activity in the area was minimal. The results suggest that guided bone regeneration shows promising results in supra-alveolar peri-implant defects during the 12 week healing period although it has a limited potential in promoting alveolar bone regeneration in the high-polished area. There seems to be no significant adjunctive effect when DFDB is combined with GBR.
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