• Journal of Plant Biology
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• v.34 no.1
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• pp.77-90
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• 1991

Fresh fungi were obtained during collection trips to Ullung Island in October, 1989, and August, 1990. Among them, some corticioid fungi were identified. Ten fungi were confirmed new to Korea and are recorded here with descriptions. They are Athelia epiphylla, Grandinia alutaria, G. gran.utosa, G. stenospora. Cylindrobasidium evolvens. Hyphoderma rlldula, H setigerum, Hypochnicium eichleri, Trechispora Illbo-ochracea, and T. farinllcea.nllcea.

• Proceedings of the Korea Water Resources Association Conference
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• 2017.05a
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• pp.92-92
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• 2017

본 연구에서는 수치모델을 이용하여 대하천서 발생되는 조류의 공간적 농도 분포를 예측하였고, 현장실험을 통해 모델을 검증하였다. 국내하천은 다수의 지류가 본류로 유입됨에 따라 오염물질의 생산과 공급이 지속적으로 발생하고, 하천의 유로연장과 하폭에 비해 수심이 낮은 지형학적 특성을 지닌다. 따라서 지류 유입 이후 발생되는 조류의 거동 특성을 분석하기 위해 수심 적분된 2차원 이송-확산 모델을 사용하였다. 광합성 성장을 이루는 조류의 성장속도 계산을 위해 영양염류, 수온, 일사량과 수심 등을 변수로 하는 성장속도 함수들을 위의 모델과 결합하였다. 본 연구의 대상구간은 낙동강과 금호강 합류부를 포함한 강정고령보 하류 약 9.2 km 구간으로 모델 검증을 위한 현장실험을 수행하였다. 2차원 이송-확산 모델의 입력 값인 유속 및 수심을 계산하는 수리동역학 모델 검증을 위해 미국 Sontek사의 M9을 이용하여 낙동강과 금호강 각각 32개, 12개 측선에 대하여 수리량을 측정하였다. 수리량 측정결과, 금호강과 낙동강의 평균 유량은 각각 $240m^3/s$, $60m^3/s$로 측정되었고 측정된 유량을 모델의 상류단 경계조건으로 사용하여 측정 유속 및 수심과 유사한 결과를 모델로부터 취득할 수 있었다. 조류 농도 측정을 위해 독일 bbe사의 AlgaeTorch 10을 사용하였으며, 수리량 측정과 동일한 측선서 총 조류 세포수(cells/ml)를 측정하였다. 농도 측정결과, 하류로 내려감에 따라 조류의 농도가 증가하는 경향이 나타났고 금호강 합류 후 최대농도는 측정구간 최하류 우안서 4,460 cells/ml로 나타났다. 주 흐름이 발생하는 하천 중앙부에 비해 유속이 느린 하안서 상대적으로 높은 농도가 측정되었으며, 이와 같은 경향은 하류로 내려감에 따라 강하게 나타났다. 측정된 조류 농도를 이용한 2차원 이송-확산 모델 검증결과, 합류부 최상류 측선서 MAPE = 10.5 %의 최대오차가 발생하였고 최하류 측선서 MAPE = 6.7 %의 최소오차가 발생하였다. 인과 질소와 같은 영양염류의 농도가 높고 횡 방향 수온 분포가 균일한 대상구간의 특성상 영양염류 함수와 수온 함수로부터 계산된 성장속도 가중치 범위는 각각 0.8~1.0, 0.91~1.09로 공간적 변동성이 크게 나타나지 않은 반면, 수심을 변수로 하는 일사량 함수의 성장속도 가중치 범위는 0.05~1.00으로 상대적으로 매우 높은 공간적 변동성이 나타났다. 수심이 4 m 이하인 하천 양안서 0.8 이상의 가중치가 나타났으며, 수심이 7 m 이상인 하천 중앙서 0.4 이하의 가중치가 나타났다. 본 연구의 수치모의 결과, 수리동역학 모델로부터 계산된 수심이 모델 결과 값에 큰 영향을 미치는 것으로 판단된다.

• Journal of Korea Water Resources Association
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• v.53 no.8
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• pp.627-636
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• 2020

Debris flow disasters primarily occur in mountainous terrains far from cities. As such, they have been underestimated to cause relatively less damage compared with other natural disasters. However, owing to urbanization, several residential areas and major facilities have been built in mountainous regions, and the frequency of debris flow disasters is steadily increasing owing to the increase in rainfall with environmental and climate changes. Thus, the risk of debris flow is on the rise. However, only a few studies have explored the characteristics of flooding and reduction measures for debris flow in areas designated as steep slopes. In this regard, it is necessary to conduct research on securing independent disaster prevention technology, suitable for the environment in South Korea and reflective of the topographical characteristics thereof, and update and improve disaster prevention information. Accordingly, this study aimed to calculate the amount of debris flow, depending on disaster prevention performance targets for regions designated as steep slopes in South Korea, and develop an independent model to not only evaluate the impact of debris flow but also identify debris barriers that are optimal for mitigating damage. To validate the reliability of the two-dimensional debris flow model developed for the evaluation of debris barriers, the model's performance was compared with that of the hydraulic model. Furthermore, a 2-D debris model was constructed in consideration of the regional characteristics around the steep slopes to analyze the flow characteristics of the debris that directly reaches the damaged area. The flow characteristics of the debris delivered downstream were further analyzed, depending on the specifications (height) and installation locations of the debris barriers employed to reduce the damage. The experimental results showed that the reliability of the developed model is satisfactory; further, this study confirmed significant performance degradation of debris barriers in areas where the barriers were installed at a slope of 20° or more, which is the slope at which debris flows occur.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.4 no.1
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• pp.10-17
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• 1999

The purpose of this study is to investigate the baroclinic response of the upper-layer of two-layered fluid when the lower-layer motion is driven by pumping an external fluid into the lower-layer or by pumping out the lower-layer fluid. Recent observations of the barotropic nature of deep water movements in the East Sea (fakematsu et al., 1994; KORDI, 1997) may suggest a possibility of interaction between the upper and lower layer via interface tilting. For homogeneous fluid, steady and axisymmetric source or sink causes axisymmetric geostrophic flow, and the lower-layer motion in two-layered fluid was similar to homogeneous flow. But as Rossby number (${\varepsilon}$) or internal Froude number ($f_2$) increases, the lower-layer motion was affected by the interface tilting. The interface tilting calculated based on the observed azimuthal velocities of upper- and lower-layers becomes greater as $f_2$ increases. In other words, the increase of the $f_2$ changes the barotropic system to baroclinic system.

• Journal of Korean Society for Geospatial Information Science
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• v.24 no.3
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• pp.59-66
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• 2016

The 2011 debris flow in Mt. Umyeonsan in Seoul, South Korea caused significant damages to the surrounding urban area, unlike other similar incidents reported to have occurred in the past in the country's mountainous regions. Accordingly, landslides and debris flows cause damage in various surroundings, regardless of mountainous area and urban area, at a great speed and with enormous impact. Hence, many researchers attempted to forecast the extent of impact of debris flows to help minimize the damage. The most fundamental part in forecasting the impact extent of debris flow is to understand the debris flow behavior and sedimentation mechanism in complex three-dimensional topography. To understand sedimentation mechanism, in particular, it is necessary to calculate the amount of energy and erosion according to debris flow behavior. The previously developed debris flow models, however, are limited in their ability to calculate the erosion amount of debris flow. This study calculated the extent of damage caused by a massive debris flow that occurred in 2011 in Seoul's urban area adjacent to Mt. Umyeonsan by using DEM, created from aerial photography and airborne LiDAR data, for both before and after the damage; and developed and compared a debris flow behavioral analysis model that can assess the amount of erosion based on energy theory. In addition, simulations using the existing debris flow model (RWM, Debris 2D) and a comprehensive comparison of debris flow-stricken areas were performed in the same study area.

• ICROS
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• v.10 no.4
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• pp.35-42
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• 2004

일반적으로 21세기에는 로봇이 기존의 인간이 가지고 있던 작업영역을 대처 할 거라고 말해지고 있으며 가까운 미래에 재난 현장, 인명구조, 지뢰제거, 정찰과 같은 위험작업 영역에 대해서 먼저 기존 인력을 대처할 수 있는 이러한 로봇의 필요성이 두각 되고 있다. 그러나 이러한 위험 작업 현장에서 운영이 가능한 로봇이 만들어지기 위해서는 일차적으로 일반적인 위험작업 지역인 계단과 같은 비 평탄 지형에 대한 이동 성능을 보장할 수 있는 로봇 이동 기술의 개발이 필요하다 일반적으로 이동형 로봇은 Wheel Type, Track Type 그리고 Walking Type으로 구분이 된다. 하지만 비평탄 지역에서 Wheel Type은 Track Type에 비해서 상대적인 주행성능이 떨어진다고 일반적으로 말해지고 있으며 또한 Walking Type은 제어방식이 복잡하고 제어부의 크기가 커서 앞의 두 방식에 비해 절대적으로 이동속도가 느리다는 단점을 가지고 있다. (중략)

• Journal of Korean Society of Transportation
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• v.16 no.3
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• pp.15-24
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• 1998

도로망 전체구간의 소통 장애와 안전을 저해하는 요소 중의 하나로 터널구간을 들 수 있다. 특히 산악과 구릉지형이 많은 우리 나라의 도로설계에서 터널에 관한 교통특성이 중시되어야하지만 이에 대한 국내외의 기준이 명확히 정립되어 있지 못하다. 이러한 과제를 해결하기 위한 기초적인 시도로 본 논문에서는 영상처리기법에 의하여 양방 2차로와 4차로 의 도로에 포함된 터널부에 대하여 기본적인 교통특성을 조사·분석하였다. 양방 2차로에서 는 용량이 1,500대/시로 기본구간에 비하여 약 6%의 감소를 보이며, 4차로의 경우는 용량 이 2,000대/시로 기본구간에 비하여 10%의 감소를 보였다. 한편 교통밀도와 속도와의 관계 에 있어서는 양방 2차로의 경우 Underwood Edie의 모형이 그리고, 양방 4차로의 경우 Underwood의 모형이 비교적 설명력이 높은 것으로 나타났다.

• 한국해양학회지
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• v.21 no.4
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• pp.236-244
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• 1986

This study was carried out for appreciable information on the proper habitats and feeding modes of some dominant polychaetes in the continental shelf of the East Sea during April, 1985. Among 95 polychaete species, we select ed 9 dominant species in terms of their occurring frequency, abundance and population density. These are Terebellides stroemi, Chaetozone setosa, Magelona japonica, Ampharete arctica, Aglaophamus sinensis, Nothria holobranchiata, Lumbrineris japonica, Myriochele gracilis, Notoproctus pacificus. Major food item s of these species are centric diatoms and detritus. The feeding modes of the the m are mainly surtace or subsurface deposit feeding, though two specters, M.holobranchiata and L. japonica, could be assumed to be potential carnivores. To a certain degree, most deposit feeders in the coarse sediments showed selectivity in feeding and tube building. The feeding mode, gut content and the tube structure, and the distribution pattern of dominant polychaetes correspond well with the habitat tharacters, e.g.the bottom topography, the source of food and the sediment composition.

• Korean Journal of Environment and Ecology
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• v.32 no.2
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• pp.147-153
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• 2018

There are few available studies for insect diversity in relation to coastal dune despite the unique landscape features and high conservation value. Therefore, this study compared ground beetle assemblages inhabiting between windbreak forests and sand dunes in the Taeanhaean National Park. It investigated five windbreak forests and three coastal dunes using pitfall traps from middle of June to middle of October in 2014. A total of 2,335 ground beetles belonging to 30 species of 15 genera were collected. Synuchus arcuarticollis (158 individuals) and Dolichus halensis halensis (153 individuals) were dominant of 25 specifies collected from sand dunes while Synuchus arcuarticollis (1,630 individuals), Synuchus nitidus (130 individuals), and Synuchus cycloderus (42 individuals) were dominant of 14 species collected from windbreak forests. The similarity of ground beetles compositions in sand dunes and windbreak forests was significantly low at 27.4%. The results of this study showed that sand dune geographical features found in the Taeanhaean National Park had different insect assemblages from windbreak forests. It will be the useful information for conservation of insects in the future.

• Economic and Environmental Geology
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• v.29 no.3
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• pp.381-393
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• 1996

Cretaceous volcanics and volcaniclastic sediments are abundantly distributed in the Haenam area located at the tip of the southwestern part of the Yongdong-Kwangju depression zone. The Cretaceous strata correlated with the Yuchon Group of the Kyongsang Supergroup are divided into three formations: Hwawon Formation, Uhangri Formation and Haenam Formation in ascending order. The stratovolcanic Hwawon Formation is mainly composed of andesite and andesitic pyroclastics. The Uhangri Formation is the lacustrine sedimentary deposit. The Haenam Formation is composed of Hwangsan tuff, Haenam tuff, Yongdang tuff, Seoho tuff, and also Acidic lava, both being formed by a cogenetic acidic volcanism. The topographic circular structure of the Cretaceous strata was controlled by the doming of Jurassic Sani granite. Cretaceous volcanism in the study area is characterized by the two stages of intermediate volcanic activity in Cenomanian to Albian, and acidic volcanic activity in Campanian to Coniacian.