김제시 간척지역 천부 지하수내 철 환원작용 특성에 대한 고찰

김지훈,정태진,류종식,김락현,Kim, Ji-Hoon,Cheong, Tae-Jin,Ryu, Jong-Sik,Kim, Rak-Hyeon 대한자원환경지질학회 2013 자원환경지질 Vol.46 No.1

간척지를 포함하고 있는 연구지역에서 육지에서 해안지역으로 근접할수록 측정된 지하수의 산화환원 전위 (Eh)와 용존 산소량 (DO)은 낮게 관찰되었다 (Eh: 0.57 V ${\rightarrow}$ 0.13 V, DO; 9.7 mg/l ${\rightarrow}$ 1.3 mg/l). 이는 연구지역 지하수의 산화환경이 육지에서 해안가로 근접할수록 호기성 환경에서 아혐기성/혐기성 환경으로 변화한다는 것을 의미한다. 또한 지하수 수질 분석 결과에 의하면 철이온 (Fe)이 지하수에 많이 포함되어 있으며 (> 20 mg/l), 대부분의 2가 철로 존재한다. 이러한 연구지역 해안가 지하수들의 특징들은 지하수들이 철의 환원작용 (Fe reduction)이 일어날 수 있는 혐기성 환경에 위치하고 있음을 지시해준다. 철 환원작용이 일어나기 위해서는 3가 철의 공급원이 필요한데, 관측정 퇴적물의 철이온 추출실험에 의하면 연구지역의 퇴적물은 철 환원작용에 필요한 3가 철이온에 대한 충분한 공급원 역할을 할 수 있다. 따라서 분석한 지하수 및 퇴적물의 결과들을 종합해석하면, 연구지역에서 일어나는 철 환원작용은 갯벌의 간척활동과 많은 관련을 가지고 있는 것으로 추정된다. The study area is located on the western coastal region of Korea, partly had been reclaimed lands. Groundwaters of the coastal area show lower Eh and DO values (Eh: 0.57 V ${\rightarrow}$ 0.13 V, DO; 9.7 mg/l ${\rightarrow}$ 1.3 mg/l), and higher Fe concentrations (> 20 mg/l) than those of the inner land (< 0.3 mg/l), indicating that the redox condition of groundwater changes from oxic into suboxic/anoxic conditions as it flows from the inland toward the coastal area. In addition, Fe speciation of groundwater from the coastal area demonstrates that the most dissolved Fe exist as $Fe^{2+}$, reflecting that groundwater is under the anoxic condition to sufficiently occur Fe reduction. According to the result of Fe extraction with the sediment samples from three wells (A, B, C), the sediments provide enough $Fe^{3+}$ to occur the Fe reduction in the groundwater. Integrated all results of the groundwater and sediment, we infer that the Fe reduction to occur in groundwater is associated with the reclamation processes of the study area.

후포분지 홀로세 퇴적물의 유기물에 대한 지화학 분석 결과 및 의미

김지훈,박명호,공기수,한현철,정태진,최지영,김진호,강무희,이치원,오재호,Kim, Ji-Hoon,Park, Myong-Ho,Kong, Gee-Soo,Han, Hyun-Chul,Cheong, Tae-Jin,Choi, Ji-Young,Kim, Jin-Ho,Kang, Moo-Hee,Lee, Chi-Won,Oh, Jae-Ho 대한자원환경지질학회 2010 자원환경지질 Vol.43 No.1

Geochemical approaches on the two recovered piston cores were performed to understand the characteristics of organic matters and the influence of the sea level variation of the East Sea in the Hupo Basin since the Holocene. The analyzing results on organic components (TOC and TN), and isotopic compositions of organic matters showed the variation to core locations and sampling depths. In core 08HZP-01, their values were gradually changed with depth from 4 mbsf to seafloor. However, rapid variation was observed at the boundary of 4.71 mbsf (meter below seafloor) in core 08HZP-03. Based on TOC/TN, $\delta^{13}C_{org}$ and $\delta^{15}N_{org}$, the origin of organic matters in the Hupo Basin can be divided into three groups; 1) predominant marine algae, 2) $C_3$ land plant, and 3) mixture of $C_3$ land plant and marine/freshwater algae. It is likely that the vertical and spatial variations of organic and isotopic compositions reflect the shifts in sedimentary environment (including sediment transportation) by ocean currents and sea-level changes and others during the Holocene period. 동해안의 후포분지에서 채취한 두 개의 피스톤 코어를 이용하여 후포분지에서의 홀로세 퇴적물 내 유기물의 특징 및 동해 해수면 변화와의 관계를 규명하고자 지화학적 접근을 시도하였다. 채취한 시료에 대한 유기물 성분 분석(TOC와 TN)과 유기물 동위원소($\delta^{13}C_{org}$와 $\delta^{15}N_{org}$) 분석 결과들은 코어와 시료 채취 심도에 따라 분석값들이 특징적으로 변화한다. 코어 08HZP-01에서는 4 mbsf(meter below seafloor)에서 코어 표면까지 비교적 채취 심도가 상부로 갈수록 지화학 분석값들이 점이적으로 증가하지만, 코어 08HZP-03에서는 4.71 mbsf를 기준으로 상부와 하부에서 급격한 지화학 분석값들의 변화가 발생한다. 유기물의 TOC/TN과 $\delta^{13}C_{org}$와 $\delta^{15}N_{org}$의 값을 종합적으로 고려하였을 때, 후포분지의 유기물은 해양 조류 기원이 우세한 집단, $C_3$ 육성 식물 기원이 우세한 집단, 해성/육성 조류와 $C_3$ 육성 식물의 혼합기원이 우세한 집단으로 구분할 수 있다. 이러한 퇴적물 내 유기물의 심도에 따른 특성 및 기원 변화는 주로 홀로세 동해 해류와 해수면 등의 변화에 따른 퇴적환경 변화 (퇴적물 이동 포함)에 기인한 것으로 보인다.

족관절의 골절-탈구에 대한 임상적 고찰

김지훈,송재광,서진수,Kim, Ji Hoon,Song, Jae Gwang,Suh, Jin Soo 대한족부족관절학회 2013 대한족부족관절학회지 Vol.17 No.3

Purpose: We evaluate clinical manifestations and radiologic features of ankle fracture & dislocation, as well as the usefulness of computed tomography on posterior ankle fracture & dislocation to study factors contributing to ankle fracture & dislocation. Material and Methods: Ankle dislocation was defined as the center of talar body being translated over the cortex of tibia on AP or lateral view on simple X-ray. Surgical treatments of 30 patients from January 2007 to March 2012 were categorized according to the injury mechanism, the direction of dislocation and fracture site. Joint involvement of posterior malleoalr fracture was evaluated through simple x-ray and computed tomography. We treated surgically if posterior malleolus fracture involves more than 25% of dital tibial articular surface. Thereafter, clinical outcomes were identified through radiographs and by using the AOFAS score. Results: The mean age was 42(13-78) years old, and slip down was the most common injury mechanism (13 cases). Car accident (6 cases) and fall accident (4 cases) were the next frequently found injury mechanisms. As for the types of ankle fracture, posterior fracture and dislocation (21 cases, 43.3%) was most commonly found. Out of these 21 cases, 15 cases involved trimalleolar fracture, and 19 cases were associated with posterior malleolar fracture. Danis-weber type B and C patients were 11 cases and 10 cases respectively. Articular involvement of posterior malleolar fracture turned out to be average 27.9%(5.1%~49.1%) on simple x-ray. The rate was evaluated as average 31.7%(12.6%~55.3%) on computed tomography which was conducted 15 times, and led us to more meaningful data. Conclusion: Anterolateral fracture and dislocation often accompanied open dislocation. Posterior fracture dislocation was most commonly found. Posterior malleolus was an important factor that ensures posterior stability of the ankle joint. Computed tomograph is useful to evaluate the articular involvement of posterior malleolar fracture.

소족지 변형에서 시행한 관절 절제 성형술

김지훈,박형준,서진수,Kim, Ji Hoon,Park, Hyung Jun,Suh, Jin Soo 대한족부족관절학회 2014 대한족부족관절학회지 Vol.18 No.4

Purpose: The objective of this study was to examine the clinical results and effectiveness of resection arthroplasty for correction of lesser toe deformity. Materials and Methods: From January 2000 to November 2012, 92 cases of resection arthroplasty for lesser toe deformity were reviewed. Hammer toe was the most common type of deformity, accounting for 44 toes (33 patients). Hallux valgus was the most common comorbid illness. Second toe was the most commonly affected toe and proximal interphalangeal joint was the most common location of resection arthroplasty (69 toes, 75.0%). We also analyzed the alignment of phalanges using the last follow-up weight bearing radiographic image. The analysis included clinical evaluation with American Orthopaedic Foot and Ankle Society (AOFAS) score as well as subjective satisfaction. Results: Flexor tenotomy (19 cases) was the most common combined surgery. Floating toe (4 cases) was the most common complication. The last follow-up alignment of phalanges was better than good in 71 toes (77.2%) in anteroposterior view and in 69 toes (75.0%) in lateral view. Sixty one cases (85.9%) resulted in better satisfaction than 'good' and the final average AOFAS score was 87.4. Conclusion: Resection arthroplasty is a valuable surgical option for treatment of lesser toe deformity, with high patient satisfaction, easy surgical technique and remarkable correction of deformity.

절단 위치에 따른 족부 절단술의 치료 결과

김지훈,고형탁,서진수,Kim, Ji Hoon,Ko, Hyeong Tak,Suh, Jin Soo 대한족부족관절학회 2015 대한족부족관절학회지 Vol.19 No.1

Purpose: The purpose of this study is to evaluate the incidence and cause of reamputation with respect to the location of foot amputation. Materials and Methods: Eighty-six patients who received amputations below the ankle level from March 2002 to September 2012 with at least 1 year follow-up were enrolled in this study. We stratified the site of the initial amputation from first to fifth ray and into either the phalanx or metatarsal bone, and investigated the cause of reamputation. Results: The reamputation rate below the ankle level was 53.5%. It was highest (62.1%) in patients with first ray amputations without statistical significance. Rays were divided into two columns, first to third rays as the medial column and others as the lateral column, and reamputation was performed in 61.2% of patients with medial column amputation. Comparing the results between phalanx and metatarsal amputations, reamputation was performed in 62.1% of patients with metatarsal bone amputation. The rate of reamputation was statistically significant in both the medial column and metatarsal amputations. The most common reamputation site, in accordance to the initial site of amputation, was the adjacent ray (57.4%), which was without statistical significance. Moreover, the most common cause of reamputation was osteomyelitis and focal infection in all rays. Conclusion: This study showed that reamputation after amputation below the ankle level was relatively common with highest rate in medial column and metatarsal amputations. Hence, surgeons should be aware of the risk of reamputation and put more preventive effort during medial column and metatarsal amputations.

울릉분지 상부 제4기 퇴적물의 유기물 기원 및 지화학적 분포

김지훈,박명호,류병재,이영주,오재호,정태진,장호완,Kim, Ji-Hoon,Park, Myong-Ho,Ryu, Byong-Jae,Lee, Young-Joo,Oh, Jae-Ho,Cheong, Tae-Jin,Chang, Ho-Wan 대한자원환경지질학회 2007 자원환경지질 Vol.40 No.5

이 연구에서는 동해 울릉분지 북서부와 동부 해역의 상부 제4기 퇴적물의 지화학적 특징, 공간적 및 수직적 분포와 유기물 기원을 규명하기 위해 천부 퇴적물을 이용하여 원소분석, Rock-Eval 열분석 및 유기물 동위원소분석을 실시하였다. TOC, TN 및 TS 분석결과는 울릉분지 북서부 및 동부지역에서 값들의 공간적인 변화는 없지만 MIS 기간에 따른 수직적인 변화는 뚜렷하게 인지된다. 이는 동해의 퇴적환경 및 속성작용들이 해수면 변화에 따라 많은 영향을 받았다는 것을 의미한다. 코어 퇴적물의 분석 결과, TOC/N, TS/TOC, 유기물 동위원소비들(${\delta}^{13}C_{org}$와 ${\delta}^{15}N_{org}$)은 퇴적물 내 유기물이 주로 해성 조류 기원이며, 일반적인 해양 또는 정체 환경에서 퇴적되었음을 지시한다. 또한 TOC/N과 유기물 동위원소 값들(${\delta}^{13}C_{org}$와 ${\delta}^{15}N_{org}$)은 MIS 기간에 따른 변화가 없기 때문에, 동해 울릉분지에서 유기물은 MIS 기간에 상관없이 동일한 기원을 가지고 있다. 그러나 Rock-Eval 열분석 결과는 유기물 기원이 육성 식물이고, 열적 성숙단계가 미성숙단계임을 보여준다. 이러한 원소분석, 동위원소 분석과 열분석 간의 상반된 결과는 대서양, 이베리아 심해 평원 및 지중해 등에서 미성숙 단계 유기물에서도 관찰되었다 따라서 Rock-Eval은 열적으로 미성숙 단계 유기물의 특징을 잘 반영하지 못하는 것으로 추정되기 때문에, Rock-Eval을 이용하여 미성숙 단계 유기물의 특징을 규명할 때 주의가 필요하고 다른 지시자들의 결과를 종합적으로 판단하여야 한다. 즉 근지성 유형의 Cu(-Au)또는 Fe-Mo-W 광상에서는 탈가스화작용 이후에 나타나는 마그마수의 전형적인 특징을 보이는 반면, 다금속 광상과 귀금속 광상은 점이성 또는 원지성 유형으로 지표수(또는 순환수)의 혼입이 우세한 경향을 보인다.감성 마케팅의 사례를 소개하고, 그 가치를 재평가하여, 소비자 입장에서의 감성 마케팅과 디자인의 문제점을 소개하고, 앞으로 감성 디자인과 감성 마케팅의 전략적 차원에서 도입하려는 기업인이나 연구자에게 선행적 사례로 도움을 주는 것에 있다.의 실험결과 또한 control과 비교시 40% 발효주에서는 10배, 45% 고은 발효주에서는 100배 낮은 측정치가 나타났으므로 한약재의 색소성분을 휘발시키는 기술이 요구된다고 본다. 항균성실험에서 항균성 측정은 06 cm paper disk agar diffusion법을 이용하였으며, 43%의 발효주와, 45% 고온 발효주가 항균력이 가장 강력한 0.95 cm의 영향을 나타냈다. 사용한 사용한 Gram 양성, Gram 음성 균주는 Escherichia coli KCCM 11591를 제외하고는 0.8 - 0.95 cm로 항균력이 강했으며, Gram negitive의 Pseudomonas aeruginosa KCTC 1750 에서는 43% 발효주에는 0.95 cm, 45% 고은 발효주에는 0.95 cm의 항균성을 나타냈으며 관능평가에서도 가장 높게 났다. 관능평가에서는 45% 고온 발효주가 가장 높게 나타났으며, 항산화성 실험에 나타난 저온 45%의 갈색도의 측정과는 항산화성에서는 좀 다른 결과를 나타낸다. 그러나 항균성이 가장 높게 나타난 43-45%와 관능평가에서 가장 높게 나타난 45% 고온 발효주를 볼 때 본 연구에서는 고온 발효주 45%가 가장 우수한 전통주로 조사되었다. 발효주를 Elemental, Rock-Eval pyrolysis and isotopic analysis of the core sediments from the northwestern and eastern Ulleung Basin of the East were carried out to identify their geochemical characteristics, spatial and vertical variation and origin of organic matter in Upper Quaternary sediments from the northwestern and eastern Ulleung Basin of the East Sea. TOC, m and TS did not show spatial variation between the sampling locations whereas they showed systematic vertical variation associated with MIS stages related to the sea-level change of the East Sea. It is suggested that these past changes of sea-level influenced the sedimentary depositional environments and/or diagenesis which resulted the patterns observed in this study. Based on the results of TOC/N, TS/TOC, ${\delta}^{13}C_{org}\;and\;{\delta}^{15}N_{org}$ analysis, organic matters in the study area appears to be predominantly originated from the marine algae rather than land plant and deposited under normal marine oxic condition during MIS I and MIS III period, and under euxinic/anoxic condition during MIS II period. TOC/N, ${\delta}^{13}C_{org}\;and\;{\delta}^{15}N_{org}$ have a relatively constant value irrespective of MIS stages, implying that the organic matter source does not change by the sea-level fluctuations. However, the results of Rock-Eval pyrolysis indicates that the organic matter is in immature stage and originated from land-plant (Type III), locating in the immature stage land plant (Type III). Similar differences were reported from other areas such as the Atlantic Ocean, Iberia Abyssal Plain, Mediterranean Sea, suggesting that Rock-Eval method does not exactly reflect the characteristic of immature organic matters. Accordingly, the application of Rock-Eval pyrolysis for delineating the source of immature organic matters should be approached with caution and all other geochemical proxies should be considered altogether at the same time.

부산 주변 해역 해저 퇴적물 내 공기층 가스 기원

김지훈,한현철,정태진,이영주,Kim, Ji-Hoon,Han, Hyun-Chul,Cheong, Tae-Jin,Lee, Young-Joo 한국석유지질학회 2007 한국석유지질학회지 Vol.13 No.1

본 연구의 주요 목적은 대한해협 대륙붕 이토대 지역의 천부 공기층 가스의 기원을 규명하는데 있다. 채취한 시료의 공기층 가스 분석 결과에 의하면 천부 공기층 가스의 대부분은 메탄으로 구성되어 있으며, 메탄 내 탄소 및 수소 동위원소 값은 각각 $-93.4%o{\sim}-70.9%o{\sim}\;-228%o{\sim}-199%o$ 가진다. 이러한 분석결과는 천부 공기층 가스 내 메탄가스가 열기원(thermogenic) 가스보다는 이산화탄소 환원작용($CO_2$ reduction)에 의한 생물 기원(biogenic) 가스임을 지시한다. 또한 메탄과 이산화탄소의 탄소 동위원소비 차는 54.4에서 72.2의 범위를 가지고 있으며, 이러한 결과 역시 전기한 결과를 뒷받침하는 또 다른 증거이다. The main purpose of this study is to identify the shallow gas origin in the KSSM zone. Based on the results of gas composition and isotope in the headsapace gas, the shallow gas is mainly composed of methane and carbon and deuterium isotopes (${\delta}^{13}CCH_4$ and ${\delta}DCH_4$) of methane has ranged from -93.4%o to -70.9%, and from -228%o to -199%o in each. These results imply that shallow gas has predominately biogenic source by $CO_2$ reduction rather than thermogenic. The carbon isotopic separation (${\varepsilon}_c$) between methane and carbon dioxide $(CO_2)$ has a range of 54.4 to 72.2, it also supports biogenic origin of shallow gas.

장막침범이 없는 진행성 위암의 2년 이내 재발과 연관된 E-cadherin, β-catenin, Cdx2, MMP7 발현양상

김지훈(Ji Hoon Kim),엄대운(Dae Yoon Eom),김찬욱(Chan Wook Kim),최남규(Nam Kyu Choi),곽진호(Jin Ho Kwak),최건무(Gun Moo Choi),장혁재(Hyuck Jae Jang),한명식(Myung Sik Han) 대한외과학회 2011 Annals of Surgical Treatment and Research(ASRT) Vol.80 No.1

Purpose: The aim of this study was to examine the expression of E-cadherin, β-catenin, Cdx2, MMP7 in gastric cancer and to evaluate the clinical significance of these molecules in tumor recurrence within 2 years of pT2 and N1/N2 gastric cancer. Methods: In 122 patients who underwent radical resection of gastric cancer, we investigated the association between the expression of these molecules and clinicopathologic factors by immunohistochemistry. The included criteria were pT2 and N1 or N2 (6th AJCC TNM). Results: The expression of MMP7 was significantly associated with N stage (N1 vs. N2) (P=0.011). The negative expression of β-catenin was strongly correlated with tumor recurrence within a 2-year period. However, the expression of these molecules was not related with recurrent sites. Multivariate analysis demonstrated that negative expression of β-catenin was an independent predictor for tumor recurrence within 2 years (OR 2.366; 95%CI 1.056∼5.297; P=0.036). Conclusion: Negative expression of β-catenin may serve as a significant indicator for predicting tumor recurrence within a 2-year period in pT2 and N1/N2 gastric cancer.

척치해 아라온 마운드 메탄 생성 기작 및 속성 작용

김지훈(Ji-Hoon Kim),이동헌(Dong-Hun Lee),진영근(Young Keun Jin),류종식(Jong-Sik Ryu),이영미(Yong Mi Lee),허진(Jin Hur),박명호(Myong-Ho Park),김영균(Young-Gyun Kim),강무희(Moo-Hee Kang),박상희(Sanghee Park),강승구(Seung-Goo Kang),김수관 대한지질학회 2020 대한지질학회 학술대회 Vol.2020 No.10

중공사막을 이용한 정수처리용 정밀여과 Pilot 시스템의 성능 평가

김지훈(Ji Hoon Kim),김관엽(Kwan Yeop Kim),김진모(Jin Mo Kim),김형수(Hyung Soo Kim),한기봉(Gee Bong Han) 大韓環境工學會 2003 대한환경공학회지 Vol.25 No.2