• Korean Journal of Environment and Ecology
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• v.35 no.6
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• pp.579-593
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• 2021

In order to understand the types of vegetation in warm temperate-climate zones, vegetation was investigated in several island areas in Jeollanam-do (Jindo, Wando, Gangjin, Goheung, and Yeosu). The evaluation standard for degraded level of warm temperate forests were proposed based on the importance percentage (IP) in canopy layer of the evergreen broad-leaf forests and the number of arboreal evergreen broad-leaf species. Through these measurements, the restoration types and techniques for each degraded level were estimated, and it is intended to be used in establishing restoration plans for the southwest coast island area. The vegetation was analyzed using the two-way indicator species analysis (TWINSPAN) method using survey data of 307 plots. As a result, it was divided into 8 communities, and the appearance characteristics of evergreen broad-leaf species were identified in each community. Community I was located on the lower slope at an altitude of 86.6 m, and Neolitsea sericea and Castanopsis sieboldii were dominant. Communities II and III were the vegetation types that appear on the coast below an altitude of 10.5 to 22.5 m, and Machilus thunbergii, Cinnamomum japonicum, N. sericea, and C. sieboldii were dominant. Communities IV and V were vegetation types that appeared in the lower and middle slops between the altitudes of 71.9 to 153.4m, and C. sieboldii was dominant. In community VI, the N. sericea was dominant in the lower and middle slops at an altitude of 166.9 m. The last communities VII and VIII were the vegetation types that appeared on the middle slop at an altitude of 187.8 to 246.2 m. Also, Quercus acuta and Q. salicina were present. In summary, the evergreen broad-leaf forests dominated by M. thunbergii, C. japonicum, and N. sericea appeared mainly in the coastal areas of the lowlands. The community of C. sieboldii was distributed higher inland than this community. The communities that appeared mainly in the inland highlands at levels above these two communities were Q. acuta and Q. salicina. The degraded level was classified as 0 to V, according to the IP of arboreal evergreen broad-leaf species and the number of arboreal evergreen broad-leaf species. According to the degraded level, the restoration types (preservation, induction, improvement, creation) and the restoration techniques were determined.

• Applied Chemistry for Engineering
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• v.17 no.2
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• pp.210-216
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• 2006

The concentrations of 16 priority PAHs (US EPA standard) were analyzed in the surface sediments obtained from 23 sampling sites near Kwangyang Bay in Korea. There was a local variability in the total PAHs ranged from 0.01 to 171.39 mg/kg, with a mean value of $8.13{\pm}24.8mg/kg$. The major pollution sources of PAHs near Kwanyang Bay were Taeindo, Sueo stream and Wallae stream, whose concentrations were 114.81, 38.37 mg/kg and 19.05 mg/kg, respectively. It showed that PAHs concentrations were increased with the decrease of particle size and with the increase of organic carbon contents in three fractioned sediments. From the analysis of PAHs source using LMW/HMW, Phe/Ant, and Fla/Pyr, pyrolysis by-products were mostly showed in Kwangyang Bay and some place showed the mixure of pyrolysis by-products, and crude oil by-products. Besides, the toxic effects assessment on benthic ecosystem for three major pollution sources showed that the PAHs concentration of Taindo which was mainly accumulated with carcinogenic PAHs exceeds ERM value and the PAHs of Sueo and Wallae streams are the degree of ERL value.

• Proceedings of the Korean Aquaculture Society Conference
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• 2003.10a
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• pp.138-138
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• 2003

우리나라 전남 동부 연안에서 확인된 해마 서식지를 대상으로 해마 이외의 혼재 유영 어류에 대한 생태 조사를 실시하였다. 조사는 전남 동부 연안의 해마의 서식이 확인된 수역에서 임의의 3 정점 (A, B, C)을 지정하여 채집하였다. 해마 채집 및 혼재 어류상 조사에는 소형 선박을 이용하였으며, 길이 45m, 폭 5m, 망목 크기 6~8mm의 어구를 사용하여 서식 생물을 채포하였다. 그리고 1회에 어획된 전 어종을 한 조사군으로 설정하였고 채집된 해마와 혼재 어종에 대해서는 각 어종별 분류키를 이용하여 분류하였다. 그리고 해마와 혼재 어류에 대해서는 0.1mm 범위에서 전장과 체장을 측정하였으며, 1mg 범위에서 체중을 측정하였다. 임의로 선정한 각 조사 정점별 채집된 해마와 혼재 어류상은 다음과 같다. 확인된 서식지는 전남 동부의 여수와 고흥 연안으로 각 지역별로 서식하고 있는 해마의 종류는 다소 차이가 있었는데 조사 정점 A와 B에서는 산호 해마 hippocampus sp. of. japonicus만이 관찰된 반면, 정점 c에서는 산호해마, 가시해마 Hippocampus sp. of. histrix, (참)해마 Hippocampus sp. cf. coronatus의 3종이 모두 관찰되었고 채집된 개체수도 정점 A와 B에서 1개체씩만이 관찰된 반면 정점 C에서는 5개체가 채집되어 다른 조사 정점에 비교하여 종의 수 및 개체수에서 매우 높은 결과를 나타내었다. 각 조사 정점별 관찰된 유영 어류상은 정점 A에서는 7종, 정점 B에서는 6종 그리고 정점 C에서는 12종의 어류가 관찰되었고, 이들 중 해마를 제외한 혼재 어종 수는 정점 A, B 및 C에서 각각 6종, 5종, 9종이 관찰되었다. 혼재 어종 중 감성돔, 복섬, 두줄 망둑, 실비늘치, 주둥치는 조사정점 A, B, C 모두에서 관찰되었다. 이 결과는 해마의 서식장 또는 산란장이 되는 조사 정점 C (36개체)가 다른 조사 정점 A (53개체)와 B (67개체)에 비교하여 해마의 어린 치어 또는 해마 성체를 포식할 수 있는 포식자의 개체수가 현격하게 낮기 때문인 것으로 판단된다. 그러나, 임의의 3 조사 정점에서 혼재 어종의 출현 종 수를 비교한 결과에서는 오히려 정점 A에서 6종, 정점 5에서 5종 그리고 정점 C에서 8종으로 나타나 정점 C에서 다소 높은 혼재 어종 수가 관찰되었다. 결국 해마의 서식지 주변 혼재 어종 특히, 혼재 어종의 개체수가 많을수록 해마의 서식 밀도를 감소시킬 가능성이 있는 것을 알 수 있었다. 한편, 다른 조사 정점에 비교하여 정점 C에서 출현 종 수가 높음에도 불구하고 출현 개체수가 매우 낮은 이유로 혼재 어종도 자어 또는 치어 시기에 해마 성체의 먹이로서 이용되었을 가능성도 배제할 수 없을 것으로 판단된다. 2003년 9월 (2일간)에 우리나라 전라남도 동부 연안에서 채집된 해마는 하루 오전과 오후 조석에 맞추어 4회에 걸쳐서 총 30여회 투망 작업한 결과 3종 62개체가 채집되었다.

• Proceedings of the Korea Technical Association of the Pulp and Paper Industry Conference
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• 2001.11a
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• pp.54-54
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• 2001

지필의 수축 현상은 섬유의 특성, Forming 공정에서 섬유배향Drying, 온도조건, Size P Press Y- Coating 공정 에서 Rewetting, 공정 중의 Tension, Draw등에 의 해 영 향을 받게 된다. 특히 Drying 공정에서는 지필 수분이 증발하면서 섬유의 자체 수축 및 섬유결합 부의 Micro compression이 발생하게 된다. 그리고 Draw, Canvas Tension, Cylinder 온도둥과 같은 공정 조건의 변동에 따라 지필 수축률의 차이가 발생하며 제품의 M MD/CD의 강도적 특성 및 칫수안정성 컬등의 품질과 상관성을 갖는다. 일반적으로 제 품의 신축률을 측정하는 일반적인 방법은 Reel 샘플을 일정시간 침수하여 종이 내부의 응력을 제거한 후 전후의 치수 차이를 비교하는 것이다. 그러나 이 방법을 통해서는 실 질적으로 Dryer 내부의 어느 단계에서 어느 정도의 수축이 발생하는지를 판단할 수는 없다. 본 연구는 Dryer에서 Reel 까지의 종이 수축 변화를 On - Line상에서 직접 측정한 적 용 사례와 공정 조건에 따른 지필 수축의 변화를 측정한 결과에 대한 것이다. 여기서 사용된 On-Line 지필 수축기는 직진성의 레이저를 이동식 지지대에 설치하여 전/후측 의 지필과 Cy linder 양끝의 거리 차이를 측정하여 지필의 폭을 계산할 수 있도록 자체 개발하였다. 이 설비를 이용하여 Dryer 내부에서 지필 수축이 급격이 일어나는 C Cylinder 군을 찾아 스팀압력과 Bel Run의 진공도, Canvas Tension, Draw 공정조건을 조정하였고 결과적으로 제품의 신축률 개선 효과를 가져올 수 있었다. 본 연구에서 개발한 On-Line 지필 수축 측정 기법은 종이 칫수 안정성과 관련하여 향후 공정 최적화 작업의 진단 도구로서 적극적으로 활용할 수 있을 것으로 기대된다.었다. 특히 지분의 경우, 참여한 회사의 지분관련 complain이 약 80% 정도 감소하는 결과를 나타 내었다. 또한 백상지의 경우 ink jet 프린터에 많이 사용됨으로 ink jet 프린터의 인쇄 적성을 image analyzer로 측정한 결과 산화전분 보다 향상된 결과를 나타내었다. 있다 고 사료되었다.칼비터에 의한 고해나 큰 물성적으로 큰 차이를 보이지는 않고 있 었다. 단지 섬유의 차이가 고해방식의 차이보다 월등히 크다는 사실을 보이고 있다 이러한 점은 섬유장의 길이에서도 볼 수 있다. 칼비터가 섬유를 절단하기만 하고 닥방망이 고해가 섬유장의 변화를 일으키지 않는다면 틀림없이 평균 섬유장의 차이가 생길것이다.의 여수도가 7 70% 이상 개선되는 것으로 나타났다.측정하였다. 또한 카르복실기 정량과 종이의 pH 측정 및 X -ray Diffractometer를 이용하여 결정화도를 측정하였다. 본 연구의 결과, 시간의 경과에 따라서 탄소의 결합에너지는 분포가 C-H에서 COO-, 또는 C=O로 달라짐으로써 종 이가 산화되고 있다는 것을 알 수 있었다. 또한 이 결합에너지 분포의 변화가 펄프의 종류 에 따라서 다르게 이동함으로써 제조된 시트의 표면 산화반응이 서로 다르게 일어나고 있음 을 알 수 있었으며, 이는 사용한 펄프의 화학 조성분의 차이에 기인한 것이라 사료된다.>NW 단열군이 연구지역 내에서 지하수 유동성이 가장 높은 단열군으로 추정된다. 이러한 사실은 3개 시추공을 대상으로 실시한 시추공 내 물리검층과 정압주입시험에서도 확인된다.. It was resulted from increase of weight of single cocoon. "Manta"2.5ppm produced 22.2kg of cocoon. It is equal to 9% increase in index, as compared to that of control.

• Journal of the Korean GEO-environmental Society
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• v.11 no.1
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• pp.13-18
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• 2010

It is crucial to decide reasonably the parameters necessary for design through research on the characteristics of rock in order to analyze stability of rock structure. This article has conducted both pressure meter test, uniaxial and triaxial compression test to the areas of andesite or tuff located in local regions such as Yeosu, Gwangju, Yangsan, Busan, and Daejeon and has comparatively analyzed previously proposed estimative formulas. According to the result of estimating the deformation modulus through using the damping coefficient suggested by Nicholson & Bieniawski, when RMR is less than 60, it is desirable to use the result of the pressure meter test considering the damping coefficient. If the RMR value is over 60, however, the formula suggested by Kim Gyo-won has been proved to be the most applicable. Moreover, according to the result of comparing the RMR, adhesion, and angle of internal friction, both the adhesion and angle of internal friction best correspond to the formula proposed by Tsuchiya. Comparatively analyzing the relations between the rock deformation modulus and RMR and also suggesting the formula of calculating the shear strength parameter to use the RMR value, this study did not include the deformation modulus and shear strength parameter as factors to decide the RMR index. Since result can differ by several factors, it will be necessary afterwards to suggest practical estimative formulas applicable to the actual spots of Korea.

• 한국해양학회지
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• v.20 no.2
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• pp.10-21
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• 1985

The sound velocity (compressional wave) and attenuation coefficient in the marine surface sediments in the nearshore areas off the Pohang, Pusan, Yeosu and Kunsan were investigated in terms of the geotechnical properties of the marine surface sediments in the water depth range of 10-50 meters. The marine surface sediments in the study areas are variable, that is, sand to clay. Due to the various four different study area, the sound velocities and attenuation coefficients in the surface sediment facies vary 1,44m/sec to 1,510m/sec in velocity and 0.82dB/m to 3.70dB/m in coefficient respectively. In fact, the sound velocity increases with increasing of density and mean grain sizes of the sediments, and however, with decreasing of porosith. The correlation equations between the sound velocith and geotechnical properties of mean grain size, density, and porosity were expressed as the following: Vp=1512.28406-9.16083(Mz)＋0.20795(Mz)$\^$2/, Vp=1876.15527-597.50397(d)＋210.48375(d)$\^$2/, Vp=1559.47217-2.09266(n)$\^$2/. where Vp is sound velocity, Mz is mean grain size, d is density, and m is porosity, respectively. However, the relationship between the attenuation and geotechnical properties were different from that of sound velocity and geotchnical properties. Furthermore, the correlation equations between attenuation coefficient and geotechnical properties were expressed as the following: a=1.85217＋0.67197(Mz)-0.09035 (Mz)$\^$2/, a=48.87859＋58.21721(d)-16.3.143(d)$\^$2/, a=2.06765＋0.07215(n)-0.00111(n)$\^$2/, where a is attenuation coefficient. The high attenuation appeared in the silty sand through fine sand facies in sediment and k values in these facies were in the range of 0.86 to 0.89 dB/m/KHz.

• Journal of the Korea Institute of Information and Communication Engineering
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• v.7 no.4
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• pp.845-852
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• 2003

This study deals with the relationship between the red tide occurrence and the meteorological and marine factors, the prediction of areas where the red tide is likely to occur based on the information, and the satellite monitoring for the red tide in mid-South Sea of Korea. From 1990 to 2001, the red tide was observed every year and the number of occurrences increased as well. The red tide mostly occurred in July, August, and September. The most important meteorological factor governing the mechanisms of the increase in the number of red tide occurrences is found to be a heavy precipitation. It was found that the favorable marine environmental conditions for the red tide formation are some of marine factors such as the warm water temperature, the low salinity, the high suspended solid, the low phosphorus, and the low nitrogen. The necessary conditions for the red tide occurrence are found to be the heavy precipitation (23.4-54.5 mm) for 2∼4 days, the warm temperature $(24.6∼25.9^{\circ}C)$, proper sunshine (2∼10.3 h), and light winds (2∼4.6 m/s & SW) for the day in red tide occurrence. It was possible to monitor the spatial distributions and concentration of the red tide using the satellite images. It was found that the likely areas for red tide occurrence in August 2000 were Yosu - Dolsan coast, Gamak bay, Namhae coast, Marado coast, Goheung coast, and Deukryang bay.

• Proceedings of the Korean Institute of Information and Commucation Sciences Conference
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• 2003.05a
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• pp.323-328
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• 2003

This study deals with the relationship between the red tide occurrence and the meteorological and marine factors, the prediction of areas where the red tide is likely to occur based on the information, and the satellite monitoring for the red tide in mid-South Sea of Korea. From 1990 to 2001, the red tide was observed every year and the number of occurrences increased as well. The red tide mostly occurred in July, August, and September. The most important meteorological factor governing the mechanisms of the increase in the number of red tide occurrences is found to be a heavy precipitation. It was found that the favorable marine environmental conditions for the red tide formation are some of marine factors such as the warm water temperature, the low salinity, the high suspended solid, the low phosphorus, and the low nitrogen. The necessary conditions for the red tide occurrence are found to be the heavy precipitation (23.4∼54.5 mm) for 2∼4 days, the warm temperature (24.64-25.85 $^{\circ}C$), proper sunshine (2∼10.3 h), and light winds (2∼4.6 m/s & SW) for the day in red tide occurrence. It was possible to monitor the spatial distributions and concentration of the red tide using the satellite images. It was found from this study that the likely areas for red tide occurrence in August 2000 were Yosu ∼ Dolsan coast, Gamak bay, Namhae coast, Marado coast, Goheung coast, and Deukryang bay.

• Journal of Korean Ophthalmic Optics Society
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• v.9 no.2
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• pp.257-267
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• 2004

Our study investigated the association between solvent exposure and acquired color vision loss using the Lanthony D-15 desaturated panel in petrochemical industry. Since neurotoxic effects associated with chronic solvent exposure, subjects with more than 6 months of exposure were included. Exposure assesment was estimated mean, maximum and cumulative 8hr TWA from individual 8-hour sampling. Exposure status were classified into two groups, occupationally exposed group to solvent and a non-exposed group. The results showed that CCI was positively related for age. According to the results of qualitative analysis, there was no significant difference in the prevalence of specific Type of dyschromatopsia the two examined group. However, the prevalence showed a higher proportion of dyschromatopsia to solvent exposure. It was affect with acquired dyschromatopsia(Type II, III and Complex) in exposed worker group(5.9%,7.86%,14.99%, respectively) than in the nonexposed group(6.16%,7.55%,13.71%, respectively). After each variable was adjusted for age, alcohol and tobacco consumption, a relationship between acquired dyschromatopsia and exposure showed an increase in the Odds ratio as compared to the nonexposed group at only left. The results showed that acquired dyschromatopsia was positively related to age (p<0.001). The results showed that solvent exposure, although not significant, could cause the acquired dyschromatopsia and visual system can serve important information on early neurotoxic effects in generally. Therefore, we need to concerns about eye health in workers.

• Journal of the Korean Society of Marine Environment & Safety
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• v.26 no.5
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• pp.466-473
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• 2020

A marine air drone is a new device that can be used to respond to and prevent marine casualties. Determining the districts where marine air drones can be deployed helps the government decision makers identify efficient policy. The aim of this study is to develop a model using the fuzzy-analytic hierarchy process (F-AHP) and additive ratio assessment (ARAS) method to evaluate appropriate districts for deploying marine air drones. To verify the applicability of the proposed model, a case study was performed with respect to the Korea coast guard (KCG) districts. Since the deployed marine air drones are characterized by a high degree of overlap between the evaluation attributes. the F-AHP is used to determine the weights of identified criteria. The results of this study, show that missing people from the shore was the most important criterion for deployment of the drone. For ranking the local districts of the KCG, the ARAS is applied in the case study with the single goal of 50% reduction in marine casualties. Consequently, the highest priority district was identified as Mokpo, followed by Incheon, Seogwipo, Taean, Wando, Yeosu, Pohang, Tongyeong, Gunsan, Bolyeong, Jeju, Buan, Donghae, Sokcho, Ulsan, Uljin, Busan, Changwon, and Pyeongtaeg.