• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 1999.04a
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• pp.16-17
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• 1999

• KOMUNHWA
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• no.70
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• pp.109-132
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• 2007

Taking the Yosu Peninsula where prestige goods were prevalent and more dolmen were excavated and surveyed than other regions as object of the research, this dissertation investigated the hierarchy of dolmen society. The dolmen groups were excavated and surveyed at some 20 positions in Yosu Peninsula Analyzing the number, weight of upper stone, location, the buried relics of dolmen, the hierarchy for each dolmen group can be summarized as follows. It seems that the large group with a lot of dolmen and big upper stone which is located on the plane with stream or on the lower part of hill might be the central group with abundant buried relics. However, the size of individual upper stone does not coincide with buried relics sometimes. Thus, it is required to review the entirety of dolmen group rather than individual upper stone in the relation between the scale of upper stone and buried relics. Then the scale of tomb is proportionate to the prestige goods. Meanwhile, the discrepancy between dolmens can be verified by the difference among upper stone, tomb, burial accessories, etc in the unit dolmen group. Since dolmen is the tomb of some inhabitants in the Bronze Age, the existence of stone coffin tomb with buried bronze sword, jade or stone sword compared to the stone coffin with no relics means that there was powerful representative of one generation even in one kindred group on the basis of wealth or authority. It can be concluded that the upper stone or large tomb or prestige goods among the persons buried in dolmen were fixed as high class, those with relatively small stone coffin with no or scanty burial accessories were fixed as medium class and multitudinous class who were not buried in dolmen were fixed as low class. Therefore, the dolmen society in Yosu Peninsula shows that there was division of class in the unit dolmen group as well as hierarchy in the group.

• The Journal of Engineering Geology
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• v.9 no.1
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• pp.31-43
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• 1999

This study aims to quantify the distribution characteristics of the fracture system for the numerical modeling of groundwater flow in the north-eastern area of Yosu peninsula. The study area is composed mainly of volcanic rocks and granite. The regional and site scale lineament in the range of magnitude Order 1 to Order 3 were analyzed from the geologic map, air-photograph and shaded relief map. The geometric parameter of Order 4 fracture system was acquired from the scanline survey on the ground surface. There is a similar trend in the preferred orientation between the regional lineament and the Order 4 fracture system except the Set 4 of Order 4 fracture system which is not prominent in the type. That is classified to three fracture sat of high dip angle and one of ow dip angle. From the lineament trend. The orientation of Order 4 fracture system has similar characteristics in each rock termination mode analysis, it is considered that the fracture system was developed systematically and sequentially from Set 1 to Set 4 Filling materials are distinct relatively in low dip angle set. The fracture spacing follows to lognoral distribution and the fracture frequency corrected by the modified Terzaghi correction ranges from 0.38 to 1.01 per mater in each fracture set. The fracture trace lenght also follows to lognormal distribution and ranges from 2.9m to 3.7m in each fracture set.

• The Safety technology
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• no.146
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• pp.18-19
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• 2010

전남 여수시 화치동에 위치한 금호석유화학(주) 여수정밀화학에 안전관리자로 근무하고 있는 이재섭 과장은 이곳의 총체적 안전관리를 위해 방화관리자, 고압가스안전관리책임자, 냉동안전관리책임자, 위험물안전관리자 등 사업장 전반적인 분야에서 중요한 역할을 다하고 있다. 24년 반평생 안전과 함께 걸어온 그는 이제 그 동안 쌓아온 경험과 지식을 전하고자 후학 양성이라는 새로운 목표로 제2의 도약기를 준비하고 있다.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.5 no.2
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• pp.131-140
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• 2000

Heavy metals (Fe, Mn, Cr, Co, Cu, Ni, Zn, Pb) were determined in ninety-one surface sediments collected from Kwangyang Bay, south coast of Korea. The data show that the Fe, Cr, Ni, and Zn distribution in the bay can be described by metal vs. grain size relationship. However, the distribution pattern of Mn, Co, Cu and Pb were found to be changed because they are anthropogenically enriched to sediment. Correlation matrix and R-mode factor analyses revealed that two important factors controlling the distribution of metals in the bay are grain size and anthropogenic input.

• Proceedings of the Korean Society of Fisheries Technology Conference
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• 2000.05a
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• pp.393-394
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• 2000

여수반도 남단에 위치한 소리도 주변해역에서는 1995년 7월 23일에 유조선 Sea Prince호에 의한 유류 유출사고로 인하여 약5,000톤의 연료유와 원유가 유출되어 극심한 유류 오염이 발생하였다. 또한 1995년 11월 17일에는 인근 광양만 입구에서 호남 싸파이어호의 부두충돌 사고로 인하여 약 1,402 kl의 아라비아산 원유가 유출되는 사고가 발생하였다. 그 결과 남해안의 여수, 여천 일대의 해역에서 수산업에 막대한 피해가 생겼고, 또한 유류오염으로 인한 생태계 변화를 파악하기 위한 필요성이 사회적인 문제로 대두되었다. 따라서 본 연구는 광양만 입구에서 소리도 주변 해역에 이르는 해역에서 저서동물 군집 구조와 주요 우점종의 분포패턴을 밝힘으로서 유류오염 이후 저서생태계 변동을 파악하는 기초자료를 제공하는데 주 목적을 두고자 하였다. (중략)

• Proceedings of the Korean Environmental Sciences Society Conference
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• 2007.05a
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• pp.289-291
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• 2007

본 연구의 대상해역은 여수반도 남단에 위치한 가막만은 굴을 비롯한 패류양식 생산활동에 기여하는 자연환경의 실질적인 가치와 인간경제 시스템에 대한 EMERGY 분석법으로 평가하고자 한다. 이를 기초로 넙치생산의 지속적인 발전방향을 제시하고자 했다. 2004년 통계를 기준으로 가막만 양식에 유입되는 총 EMERGY의 양은 33.42E+19 sej/yr이고, 이 중 자연환경으로부터 영속성 에너지는 2.95E+20 sej/yr 이며, 주 경제로부터 유입되는 비영속성 에너지는 3.92E+19 sej/yr이다. 자연환경으로부터의 유입이 전체 에너지원의 88%이고, 주 경제로부터의 유입은 12%로서 환경자원에 대한 의존도가 높은 1차 산업의 구조적 특징을 나타내고 있다. Net EMERTY yield ratio는 8.52으로 이는 주 경제로부터 투입된 에너지(비영속성 에너지)에 대해 8배 만큼 수산물을 얻을 수 있는 자원으로서의 가치를 가진다. EMERGY Investment Ratio 0.13은 주 경제로부터 유입된 에너지의 약 7배에 해당하는 에너지를 자연환경에서 얻을 수 있음을 의미한다. EMERGY량이 모두 현재의 EMERGY 생산비대로 생산이 된다는 가정하면 가막만의 패류(굴) 생산량은 환경수용량의 50%정도에도 못 미치는 것으로 나타났다.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.28 no.1B
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• pp.11-20
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• 2008

The spillway type of small and midsize dams in Korea is almost overflow weir. To examine flood control capacity of overflow spillway, FLOW-3D was applied to Daesuho dam and analysis was focused on the discharge of dam spillway by changing weir shape. Overflow phases and discharges of linear labyrinth weir and curved labyrinth weir were compared with those of existing linear ogee weir. Hydraulic model experiment was performed to verify numerical result. Verification results showed that overflow behaviors and flow characteristics in the side channel by hydraulic model experiment and numerical simulation are well matched, and water surface elevation at side wall coincides with each other. When the reservoir elevation was increased up to design flood level, in case of the linear ogee weir the flow over the crest ran through smoothly in the side channel, whereas in cases of linear labyrinth weir and curved labyrinth weirs, the flow discharge was increased by 40 cms, and the flow over the weir crest, rotating counter-clockwise, was submerged in the side channel. The results of the water level-discharge curve revealed that labyrinth weir can increase discharge by 71% compared to the discharge of linear ogee weir at low reservoir elevation since it can have longer effective length. But as water surface elevation rises, the slope of water level-discharge curve of labyrinth weir becomes milder by submergence and nappe interference in the side channel.

• The Journal of Engineering Geology
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• v.9 no.3
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• pp.227-241
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• 1999

Groundwater flow in a fractured rock mass is related to the geometric characteristics of the fracture system. The objective of this study aims to analyze the probabilistic density function of fracture properties md their relations to the hydraulic conductivity in volcanic rocks of the northern Yosu area. Fracture characteristics were investigated by core logging and acoustic televiewer logging in four boreholes and the hydraulic conductivity was obtained from the constant pressure injection and fall-off tests. The 303 fractures were grouped into three sets by their orientation and three fracture types by the degree of opening in aperture. As a result of the study, the hydraulic conductivity in the test section intersected by open and semi-open fractures, conductive fractures, and set 1 fractures was very high, while closed fractures did rarely affect the hydraulic conductivity. It was recognized that the hydraulic conductivity in a fractured rock mass was preferentially affected by the aperture size of conductive fractures and fracture intersection frequency and size, secondly.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 1999.10a
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• pp.420-421
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• 1999

여천지역은 화학물질 누출사고 등 안전 사고 발생의 잠재적 위험이 높으나 (김영성 등, 1999), 복잡한 해안선의 여수 반도 해안지역에 산을 등지고 있어 해륙풍에 의한 일 변화와 지형 조건에 따른 국지 변화등 복잡한 형태의 바람장이 예상되는 지역이다. 이러한 지역에서의 확산현상은 환경영향평가에서 흔히 이용되고 있는 균일한 바람장 분포를 가정한 대기화산 예측과는 다른 결과를 보이며 (오현선, 김영성, 1999), 따라서 단순한 가우시안 플룸 모델을 이용한 확산 예측은 적용범위가 매우 제한적일 수밖에 없다.(중략)