• 대한기관식도과학회:학술대회논문집
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• 대한기관식도과학회 1983년도 제17차 학술대회연제순서 및 초록
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• pp.19.2-19
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• 1983

만성중이염은 이비인후과의 가장 흔한 질환 중의 하나로 이에 대한 수술요법은 여러 가지 방법이 많이 발표되고 있으나 아직까지 어려운 점이 많이 있다고 하겠다. 저자들은 1981년 2월부터 1983년 2월 까지 부산성분도병원 이비인후과에서 만성중이염이란 진단하에 수술을 받은 환자 128예에 대해서 임상적 세균학적 관찰을 실시하여 다음과 같은 결론을 얻었다. 1) 성별과 연령비는 여자가 68예(53.1%), 남자가 60예 (46.9%), 또한 연령별로는 20대가 48예(37.5%), 10대가 37예(28.9%) 그리고 30대가 27예(21.1 %) 의 순서였다. 2) 환측별은 우측이 71예(55.5 %), 좌측이 57예(44.5 %) 이었다. 3) 수술전청력검사상 중등도의 손실이 64예 (50%)로 가장 많았고 다음으로 경도손실이 32예 (25 %)이었다. 4) 고막천공의 상태는 중심성천공이 65예(50.8%), 전결손이 44예 (34.4%), 이완부천공이 12예 (9.4%) 그리고 변연성천공이 7예 (5.4%)이었다. 5) 진주종이 전체의 36.7 %인 47예에서 나타났다. 6) 피부절개 및 수술경로는 postaural incision이 123예(96.1%) 이었다. 7) 국소마취가 95예(74.2 %) 이었다. 8) 수술방법은 intact canal wall tympanoplasty with mastoidectomy 가 53예 (41.4 %), tympanoplasty without mastoidectomy가 42예(32.8%) modified radical mastoidectomy 23예 (18%) 그리고 radical mastoidectomy가 10예(7.8%) 이었다. 9) Culture를 시행하여 분리된 균주 93종 중 proteus가 29종(31.2 %), staphylococcus가 27종(28.7%), pseudomonas가 22종(23.7%) 그리고 streptococcus가 7예(7.5%)이었다.

• Journal of Chest Surgery
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• 제18권4호
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• pp.753-758
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• 1985

Hemorrhage is an important complication after operation with cardiopulmonary bypass and sometimes necessitates a further emergency operation. Between July, 1962 and June, 1985, reoperation for hemorrhage was carried out on 81 patients [3.1%] out of a total 2634 patients who had previously undergone cardiopulmonary bypass surgery at the Department of Thoracic and Cardiovascular Surgery, Yonsei University Medical Center. There were 38 males and 43 females, with an average age of 25 years [ranging 6 months to 60 years] and an average body weight of 38 kg [ranging 5 to 77 kg].There were 43 patients of cyanotic heart disease, 32 patients of acquired valvular heart disease, 4 patients of coronary artery occlusive disease, 2 patients of ascending aorta aneurysm and annuloaortic ectasia. The average amount of blood loss in the case of cyanotic heart disease was 71.7140ml/kg, in acyanotic heart disease 45.16.3ml/kg, in acquired heart disease, 56.514.4ml/kg and in coronary artery occlusive disease, 50.618.7ml/kg during first post operative day. But there was no statistical difference [p>0.05]. The mean blood loss below 10 years old was 70.412.1 ml/kg. Those below 10 years old were believed to bleed more than any other group. But there was also no statistical difference [p>0.05]. Indications for reoperation were continued excessive blood loss [74%], cardiac tamponade or hypotension [23%] and radiological evidence of a large hematoma in the thorax and pericardium [2%]. Average bypass time was 2.10.1 hours [ranging 30 minutes to 5 hours]. The interval between operation and reoperation was as follows; less than 12 hours in 49 patients [60%], 12 to 24 hours in 20 patients [25%], 24 to 48 hours in 8 patients [10%], more than 48 hours in 4 patients [5%]. The commonest sites for bleeding were chest wall [36%], heart [34%], aorta [12%], pericardium [6%], thymus [5%] and others [6%]. But no definite source was found in ll patients [31%]. Twenty seven out of 81 patients [31%] had wound problems and 5 patients [6%] were expired. [Mean SEM]. In conclusion, in order to decrease the amount of blood loss after open heart surgery with cardiopulmonary bypass, shortening of bypass time and bleeding control at the wire suture site during chest wall closure were important. If the amount of blood loss was over 45 ml/kg or 8 m/kg/hour, reoperation should be considered as soon as possible. After operating, careful wound dressings were applied to prevent wound problems.

• Journal of Chest Surgery
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• 제5권2호
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• pp.87-96
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• 1972

Studies of blood gas and lung histopathology were done in 10 dogs after intrapericardlal aorto-right pulmonary arterial anastomosis with proximal ligation of the right pulmonary antery. Among the 5 expired during or after operation, in 3 cases, the causes of the death were due to surgical bleeding and, in 2 cases, acute cardiopulmonary insufficiency because of large anastomosis stoma measured respectively 7mm and 10mm. In the 5 of survivals, one was sacrificed because of empyema at postoperative 7 days and 2 were at postoperative one month and remained 2 at postoperative 3 month respectively. The following observations were made. 1.In every survival, continuous machinary murmur was auscultated and the angiograms of all long term survivals showed the good patency of the anastomosis stoma. 2.After the ligation of the right pulmonary artery, the values of $PO_2$ and $PCO_2$ in arterial and venous blood were generally decreased comparing with the preoperative values. The mean value of $P_aO_2$ noted $83.30{pm}11.875$[p<0.01]. After the shunts operation with ligation of the right pulmonary artery, the immediate values of PH, $PO_2$ and $PCO_2$showed no significant changes comparing with that of right pulmonary artery ligation only. In the cases of survivals more than one month, the values of $PO_2$ and $PCO_2$ in the arterial and venous blood were generally higher than that of ligation of the right pulmonary artery only. The $P_aO_2$ value noted $103.750{pm}7.395$[p<0.01]. The mean values of $P_aO_2$, $PCO_2$ and PH in the arterial and venous blood almost returned to that of preoperative studies. 3.In the specimens of lung from the cadavors expired due to acute cardiopulmonary insufficiency after the operation, there were massive congestion, hemorrhage in the alveolar spaces and bronchioles. In specimens obtained at postoperative one month, there were dilatation of alveolar spaces with partial rupture, slight congestion, and alveolar wall thickening in the lung parenchyme, but there was no significant changes in pulmonary vasculature except dilation of pulmonary capillaries. In the specimens obtained at postoperative three months, the alveolar walls were more thickened in the lung parenchyme than the finding of the specimens obtained at postoperative one month. In the wall of pulmonary capillaries, there was only slight thickening with connective tissue proliferatlon.

• 헤리티지:역사와 과학
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• 제49권1호
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• pp.68-83
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• 2016

본 연구는 가변적, 재료적 특성으로 인해 원형의 실체가 분명하지 않았던 판장(板墻)을 대상으로, 판장의 사용양상과 용례, 구성요소와 구조에 대한 실증 및 고찰에 목적을 두고 있다. 이에 따른 연구결과는 다음과 같이 요약될 수 있다. 첫째, 나무널로 만든 담장을 가리키는 판장은 기능, 구조, 단청색 등에 따라 다양한 용례로 사용되었다. 유사한 용례인 판장문과 목판장은 전통적인 판장과 밀접한 관계가 없다. 또한 판장과 재료적으로 유사한 중국의 목영벽과 일본의 판병도 판장과는 분명한 구조적 차이가 있다. 둘째, 판장의 변용유형은 크게 이목기판장, 살판장, 흙판장 그리고 한자어가 다른 판장(板障)으로 구분된다. 이목기판장은 두 단의 방연이 사용된 판장을 가리키며, 살판장은 살대와 널로 만든 투시형 판장을 의미한다. 흙판장은 흙담과 판장의 절충적 형태이며, 판장(板障)은 벽체의 성격을 지닌 고정형 시설로 추정된다. 셋째, 판장의 목부재로는 신방, 기둥, 도리, 중방, 인방, 널, 띠목, 초엽, 방연, 개판, 평고대, 연함 등이 조영의도와 구조형식에 따라 선별적으로 사용되었다. 목부재 외에 못, 잠금장치, 구체적인 용처를 알 수 없는 부속요소도 함께 사용되었다. 넷째, 판장의 기단부는 목부재의 종류와 결구에 따라 크게 세 가지로 구분되며, 축부는 상인방의 사용유무에 따라 두 가지로 구분된다. 지붕부 재료로는 개판과 기와가 사용되는데, 각각의 재료에 따라 명확한 구조적 차이가 나타난다.

• 한국균학회지
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• 제50권4호
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• pp.291-300
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• 2022

참나무 톱밥을 이용한 표고버섯 톱밥봉지 재배는 원목재배에 비하여 많은 이점을 가지고 있어 국내 톱밥배지 재배 농가는 매년 증가하고 있는 추세이다. 그동안 표고 톱밥재배에 대한 많은 연구가 수행되어 보고된 바 있으나, 주요 연구 내용은 톱밥배지 제조 시 혼합하는 농산부산물 영양원 첨가제의 종류와 첨가효과, 톱밥 배지 재배에 적합한 신품종 개발, 참나무 발효 톱밥과 생 톱밥 간의 재배 특성 비교 등이 있으며, 배지 구성 물질 중에서 표고의 주 영양원인 참나무 톱밥의 재배 기간 중 목재 화학적 성분 변화에 대한 보고는 이루어지지 않았다. 이에 본 연구에서는 균 배양 및 버섯 수확 기간 중 배지의 물리 및 톱밥의 목재 화학 성분 변화 등에 대한 조사를 수행하였다. 그 결과, 종균 접종 후 배양 기간 중에 배지의 중량 감소가 발생하며, 이것은 배지 함유 수분의 증발이나 톱밥 목질부의 분해에 의한 현상이 아니고, 배지 중에 첨가한 저분자 수용성 물질인 쌀겨가 먼저 균사에 의해 분해, 이용되기 때문이라는 결론에 이르렀다. 또한 배양 중에 균사 생장 배지의 함수율이 꾸준히 증가하는 것을 확인하였으며, 균사 생장과 함께 유기물 분해 과정인 이화작용이 진행되어 분해 산물인 물이 생성됨으로써 배지의 함수율이 증가하는 것으로 판단하였다. 표고버섯 수확이 반복하여 진행됨에 따라 톱밥의 목재 세포벽 주성분인 홀로셀룰로오스와 리그닌 등 유기물 비율이 꾸준하게 감소하였으며, 특히 리그닌 감소 비율이 크게 나타나 백색부후균인 표고 균의 목재 세포벽 성분 분해 특징이 확인되었다. 이에 반하여 무기물 성분으로 이루어진 회분은 수확 횟수 증가와 함께 증가하는 경향을 보였는데, 이것은 홀로셀룰로오스와 리그닌의 유기물 비율이 감소함으로써 상대적으로 증가하는 결과로 나타난 것이다.

• 대한기계학회논문집B
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• 제23권10호
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• pp.1265-1273
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• 1999

PIV(Particle Image Velocimetry) velocity field measurements inside the snout of a1/10 scale model of the Zn plating process were carried out at the strip speed $V_s=1.5m/s$. Aluminum powder particles ($1{\mu}m$) and atomized olive oil ($3{\mu}m$) were used as seeding particles to simulate the molten Zinc flow and deoxidization gas flow, respectively. A pulsed Nd:Yag laser and a $2K{\times}2K$ high-resolution CCD camera were synchronized for the PIV velocity field measurement. From flow visualization study, it is found that the liquid flow in the Zn pot is dominantly governed by the uprising flow caused by the rotating sink roll, with its effect on the steel strip inside the snout largely diminished by installing of the snout. The deoxidization gas flow in front of the strip inside the snout can be characterized by a large-scale vortex rotating clockwise direction formed by the moving strip. In the rear side of the strip, a counter-clockwise vortex is formed and some of the flow entrained by the moving strip impinges on the free surface of molten zinc. The liquid flow in front of the strip is governed by the flow entering the snout, caused by the spinning sink roll. Just below the free surface a counter-clockwise vortex is formed near the snout wall. The moving strip affects dominantly the flow behind the strip inside the snout, and large amount of the liquid flow follows the moving strip toward the sink roll. The thickness of the flow following the strip is very thin in the front side due to the uprising flow, however thick boundary layer is formed in the rear side of the strip. Its thickness is increased as moving downstream toward the sink roll. Inside the snout, the deoxidization gas flow above the free surface is much faster than the liquid flow in the zinc pot. Due to the larger influx of the flow following the moving strip in the rear side of the strip, higher percentage of imperfection can be anticipated on the rear surface of the strip.

• 자원환경지질
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• 제2권1호
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• pp.1-12
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• 1969

In the Sangdong Mine area, Taebaegsan series (Pre-Cambrian) and Chosun System (Cambro-ordovician) are widely distributed. The Chosun System consists of Yangdug Series (Jangsan Quartzite and Myobong Slate) and The Great Limestone Series (Pungchon Limestone, Shesong Shale, Hwajeol Formation and Dongjeom Quartzite). The mineralized zone containing the main ore body of the Sangdong Mine was developed in the Myobong Slate formation. The result of the field and microscopic study on the mineral paragenesis and it's wall rock alteration in the tungsten ore deposit shows the following features. The orogenic movements of the Post-Chosun System in the Hambaeg Geosyncline are closely related to the tungsten ore deposition in the area, the ore minerals are composed mainly of scheelite, powelite molybdenite and sulfide minerals, and gangue minerals are hornblende, diopside, garnet, quartz, phlogopite, tremolite, biotite, muscovite, fluorite, etc., main ore body was enriched by scheelite bearing quartz vein filling into interstices of formerly mineralized zones, and the minor faults, faults of N $60^{\circ}-70^{\circ}W$, $45^{\circ}-60^{\circ}NE$ and joints, which were formed at the end of the mineralization and the slate. Country rock of the ore body was altered into the following several zones from the outside to the inside; lowgrade recrystalline aureole, silicified sericite zone, and diopside-hornblende zone. Under the microscopic observation of 195 samples taken from throughout ore body can be classified into 10 different groups by their mineral paragenesis as shown in table 2. The garnet-diopside group is primary skarn and it shows gradational change to the groups of later stage by the successive processes of metasomatism. From the stage of quartz-bearing group, the dissemination of scheelite is seen. The crystallization of scheelite in the bed started with the quartz deposition and continued to the last stage when quartz vein intruded into the main ore body. In the field and the under ground investigation a durable limestone bed in thickeness about 20 meters and their remnants in ore body are observed and under microscope calcite remnants are recognized. Hence it is posturated that the ore material moved up through the faults, shear zones or feather cracks and was assimilated with the interbeded limestone, after that the body was affected by the successive differentiated ore solution by gradational increasing in $SiO_2$, $K_2O$ and $H_2O$. Evidently this ore deposit shows the features resulted from pyrometasomatic processes.

• Journal of Advanced Marine Engineering and Technology
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• 제40권3호
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• pp.165-173
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• 2016

2011년 3월 11일 리히터 스케일 9.0의 강진과 10-14m파도로 인해 Fukushima Daiichi(FD) 원자력 단지의 주전력과 보조전력이 끊어져 냉각장치가 작동하지 않았고 노심의 열이 제거되지 못해 폭발이 일어나는 사고가 발생했다. 노심의 열이 제거되지 못하면 핵연료 피복재인 지르칼로이(zircaloy)와 같은 금속이 고온 상태에서 수증기와 산화 반응하여 수소를 발생시킨다. 발생된 수소는 격납건물로 방출되는데 방출된 수소가 연소하는 경우 격납건물의 안정성에 영향을 줄 정도의 큰 충격을 유발할 수 있는 수소폭발로 이어질 수 있다. 본 연구에서는 격납건물 내부의 수소 분포를 분석한 연구 [1]에서 제시한 폭발의 위해도가 높은 영역에 대하여 폭발해석을 수행하였으며 수소 폭발이 격납건물의 건전성에 미치는 영향에 대하여 분석하였다. 격납건물 중앙부를 제외하고 수소폭발이 발생하였고 상부에 전체 수소의 40%이상이 모였을 때와 하부 좌측, 우측의 격벽사이에 수소가 모였을 때 큰 폭발이 발생했으며 격납건물 벽면에 큰 응력을 동반하였다.

• Journal of Microbiology and Biotechnology
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• 제26권1호
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• pp.130-138
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• 2016

The use of antibiotics in aquaculture raises environmental and food safety concerns because chronic exposure of an aquatic ecosystem to antibiotics can result in the spread of antibiotic resistance, bioaccumulation of antibiotics in the organisms, and transfer of antibiotics to humans. In an attempt to overcome these problems, high-concentration red clay was applied as an alternative antibiotic against the following common fish pathogens: Aeromonas salmonicida, Vibrio alginolyticus, and Streptococcus equinus. The growth of A. salmonicida and V. alginolyticus was retarded by red clay, whereas that of S. equinus was promoted. Phase contrast and scanning electron microscopy analyses confirmed the attachment of red clay on cell surfaces, resulting in rapid gravitational removal and cell surface damage in both A. salmonicida and V. alginolyticus, but not in S. equinus. Different cell wall properties of grampositive species may explain the unharmed cell surface of S. equinus. Significant levels of oxidative stress were generated in only the former two species, whereas significant changes in membrane permeability were found only in S. equinus, probably because of its physiological adaptation. The bacterial communities in water samples from Oncorhynchus mykiss aquacultures supplemented with red clay showed similar structure and diversity as those from oxytetracycline-treated water. Taken together, the antibiotic effects of high concentrations of red clay in aquaculture can be attributed to gravitational removal, cell surface damage, and oxidative stress production, and suggest that red clay may be used as an alternative for antibiotics in aquaculture.

• 자원환경지질
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• 제23권2호
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• pp.161-181
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• 1990

The lead-zinc-silver-iron deposits from the Janggun mine are of hydrothermal-metasomatic origin, characterized by the marked hydrothermal alteration of the wallrocks, such as hydrothermal manganese enrichment of carbonate rocks, silicification, chloritization, sericitization, montmorillonitization and argillic alteration. The ore deposits have been emplaced within the Janggun Limestone of Cambro-Ordovician age at the immediate contacts with apophyses injected from the Chunyang Granite plutons of Late Jurrasic age. They have been structurally controlled by fractures in the carbonate rocks and the irregular intrusive contacts of granitic rocks, and are closely associated with hypogene manganese carbonate deposits. In the mine nine seperate orebodies are being mined. On the basis of the petrological study, hydrothermal alteration zone of this mine may be divided into the following four zones from wallrock to orebody. (I) Primary calcite and dolomite zone${\rightarrow}$(II) dolomitic limestone zone${\rightarrow}$(III) dolomitic zone${\rightarrow}$(IV) rhodochrosite zone${\rightarrow}$ orebody. There was not recongnized Mn and Fe elements in the primary calcite and dolomite zone. But, in the dolomitic limestone and dolomite zone, calcite and dolomite were subjected to weak hydrothermal manganese enrichment and the grade of the manganese enrichment increase oreward. By means of electron probe microanalysis, it was found that manganoan dolomite occured between primary dolomite grains, cross the cleavage of the primary dolomite and around the dolomite grains. Above these result supports that the Janggun manganese carbonate deposits are of hydrothermal metasomatic origin.