• Korean Journal of Plant Taxonomy
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• v.43 no.3
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• pp.165-167
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• 2013

Five taxa of the genus Ajuga L. (Lamiaceae) were known previously in Korea which were mainly distributed in lowland and lower montane areas at 50-1000 m elevation. We report an unrecorded taxon of the genus Ajuga in Korea, namely Ajuga nipponensis Makino. This taxon was discovered at Is. Nok, Boryeong-si, in Chungcheongnam Province. A. nipponensis is found to be distributed along roadsides near villages of the island. A. nipponensis was distinguishable from other Ajuga in Korea by following combination of characters: Stems erect or procumbent, arranged in a dense cluster, corolla whitish-pale pink, 10-12 mm long. This taxon was named 'Bun-hong-kkot-jo-gae-na-mul' in Korean based on color of the corolla. The key to the genus Ajuga in Korea is also provided.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.12 no.2
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• pp.87-99
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• 1992

The types of dam-break have been classified as instantaneous and gradual failure. Equations for estimating the peak outflow have been derived respectively as a metric unit. New dimensionless routing curves have been deveoloped based on the distance parameter which has been used in SMPDBK and hydro-geometric characteristics of dams and reservoirs in Korea. These suggested curves can be used for any case of the flow of supercritical or subcritical. The computed peak flowrate shows the trend of decreasing dependence on the Froude numbers as it increases. These curves are applied to Hyogi dam. and the results have good agreements with the data observed in the peak discharges, peak elevations and flood travel time. The simplified dam-break model in this study would contribute effectively to forecast the dam-break flood in this country with minimum informations in a short time.

• Korean Journal of Environmental Biology
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• v.25 no.3
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• pp.249-259
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• 2007

This study was carried out the analysis of forest vegetation structure using the phytosociological methods by Braun-Blanquet from April to November in 2006. The results were summarized as follows. The forest vegetation was classified into 23 communities and 3 forest ecosystem types such as slope forest type, valley forest type and artificial forest type. By the actual vegetation map, Quercus mongolica forest was widely distributed in the area and Pinus densiflora forest and Quercus variabilis forest in the southern parts of the slope and valley forest mainly in valley area, respectively. The importance value in the Q. mongolica forest and artificial forest was absolutely high for the species dominated in tree layer. The typical valley species of Lindera erythrocarpa and Styrax japonica were abundantly occupied in the all layers. Species diversity indices of Alnus hirsta forest was the lowest as 0.2191, and that of valley forest was about 0.9, the highest among the all forest types.

• Journal of Korea Water Resources Association
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• v.38 no.5 s.154
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• pp.345-354
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• 2005

Time Domain Reflectometry (TDR) with multiplex system has been installed to configure the spatial and temporal characteristics of soil moisture at the Bumreunsa hillslope of Sulmachun Watershed. An intensive surveying was performed to build a refined digital elevation model (DEM) and flow determination algorithms with inverse surveying have been applied to establish an efficient soil moisture monitoring system. Soil moisture data were collected through intensive monitoring during 380 hrs in November of 2003. Soil moisture data shows corresponding variation characteristics of soil moisture on the upper, middle and lower parts of the hillslope which were classified from terrain analysis. Measured soil moisture data have been discussed on the context of physical process of hydrological modeling.

• Journal of Korean Society of Forest Science
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• v.18 no.1
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• pp.13-16
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• 1973

The article was carried out to study the relationships between the causes of barelands and topographic factors such as altitudes, slopes and bearings. Using the forest utility demarcation maps of 1 : 50,000 in scale and the aerial photographs drawn and taken by the Forest Resources Institute, Seoul, the areas of each bareland and the topographic factors were calculated from the maps and photographs and the critical causes of barelands were analyzed based on the various topographic factors. The results obtained were as follows: 1. There were some positive relation between area of barelands and slopes, and between area of barelands and altitudes. 2. However. there were no significant difference between number of barelands and altitudes, between number of barelands and slopes, between number of barelands and bearings, and between area of barelands and bearings.

• Proceedings of the Plant Resources Society of Korea Conference
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• 2018.04a
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• pp.35-35
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• 2018

터리풀속(Filipendula)은 장미과(Rosaceae), 장미아과(Rosoideae)에 속하는 다년생 초본이며, 북반구 온대지역의 산지지역에 서식하며 15-20여 종이 보고되어 있고, 이 중 10여종이 한국, 중국, 일본, 타이완 등의 동아시아 지역에 분포한다. 본 연구의 목적은 DNA 염기서열 자료를 이용하여 터리풀속(Filipendula)내 종들간의 계통관계를 규명하기 위하여 본 연구를 수행하였다. 이를 위해서 11종 29개체의 터리풀속(Filipendula)샘플과 외군인 산딸기나무속(Rubus)에 속하는 3종 5개체의 샘플을 이용하였다. 추가로 Genbank에서 3속 10종 18개의 염기서열을 다운받아 비교분석에 이용하였다. 계통연구를 위하여 엽록체에 존재하는 atpF-atpH, psbK-psbI, psbA-trnH, matK, rbcL, 5개 마커와 핵에 존재하는 ITS, 총 6개 마커의 염기서열을 생산하였다. 총 52개의 샘플에 대하여 엽록체유전체 5개 마커지역은 염기서열 길이가 3,485bp였고 핵 ITS지역은 631bp였으며, 이들을 합한 염기서열 길이는 4,116bp였다. 계통분석결과, 터리풀속(Filipendula)은 단계통군을 이루었다. F. occidentalis와 F. vulgaris가 기저분류군을 이루었고 이들은 각각의 아속에 해당한다. 그리고 나머지 종들은 모두 하나의 단계통군을 이루었다. 위의 결과들은 1961년 시미즈가 본 속을 Hypogyna아속, Filipendula아속, Ulmaria아속으로 나눈 분류시스템과 일치한다. 나아가 분자계통수에서 Ulmaria아속은 크게 4개의 subclade로 구분되었다. 먼저 subclade I에는 F. vestita, F. kiraishiensis, F. tsuguwoi, F. multijiuga, F. purpurea 등 5개 종으로 구성되었다. Subclade II는 F. ulmaria 한 종으로만 구성되었다. Subclade III에는 F. glaberrima, F. koreana, F. formosa, F.camtschatica 로 구성되었으며 subclade III에는 한국에 서식하는 3종이 포함되었다. Subclade IV에는 F. rubra, F. angustiloba, F. palmata, F. intermedia 4종으로 구성되었다. 이번연구에서는 Ulmaria아속내에 4개의 subclade가 존재함이 처음으로 확인되었다.

• Journal of the Korean Crystal Growth and Crystal Technology
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• v.16 no.1
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• pp.25-31
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• 2006

Many amethysts of different origins such as South America, Aftrica, and Asia were compared. According to ICP-AES analysis, the colorizing elements were Fe, Cr, Cu, and Co. Amethysts from South America showed higher concentrations of the elements. UV- VIS analysis showed that both natural and synthetic amethysts were characterized by the higher absorption at 350 nm and 550 nm wavelength. The natural amethysts had lower permeability than that of the synthetic amethysts. According to FT-IR analysis, the synthetic amethysts were distinguished from the natural amethysts in that they had a typical absorption band of $3543cm^{-1}$. The amethyst from South America showed strong absorption bands of $3584cm^{-1}\;and\;3435cm^{-1}$, and African amethyst had absorption bands of $3299cm^{-1}\;and\;3196cm^{-1}$. $3381cm^{-1}$ absorption band was shown strongly for Asian origins.

• Geotechnical Engineering
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• v.11 no.4
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• pp.111-124
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• 1995

On development of mountaneous or hilly area, stability of cut slope should be provided to prevent undesirable landslides. When piles are used as a countermeasure to stabilize existing landslide, stabilities for both piles and slope should be simultaneously satisfied to obtain the whole stability of the slope reinforced by piles. In order to confirm the effect of stabilizing piles on slope stabilization, it is necessary to investigate the behavior of the slope, in which the piles are installed. In this paper, first, the countermeasures used commonly to control unstable slope in Korea were summerized systematically. Nezt, the behavior of piles and slope soil was investigated by instrumentation installed into a cut slope for an apartment stabilized by a row of piles. Instrumentation could present sufficient effect of piles on slope stabilization Construction works in front of the row of piles affected the displacement of piles and slope. The construction works were divided into four stages, i.e. initial cutting stage of slope, excavation stages for retaining wall and parking space, and construction of retaining wall. As the result of research, the applicability of the proposed design method could be confirmed sufficiently.

• Proceedings of the Korea Water Resources Association Conference
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• 2012.05a
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• pp.274-274
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• 2012

증발산량 관측은 오랜 기간 연구되어 왔으며, 미기상 관측 시스템의 최적화와 상호 공동비교 실험 및 자료 처리의 일관성을 유지를 위해 한국에는 KoFlux라고 하는 플럭스 네트워크가 2002년 1월에 구축되었다. 이를 시작으로 미기상 관측에 대한 관심이 많은 연구자들이 관측망 구축에 힘쓰고 있으며, 에디공분산 방법을 이용해 증발산량을 산정하고 있다. 에디 공분산 방법은 다른 방법에 비해 연직농도 차이가 적은 산림 위에서의 플럭스 값을 측정 할 수 있으며, 측정 시 식물 환경에 방해를 주지 않는 등의 장점이 있다. 하지만 자료 처리와 품질관리에 있어 연구자의 주관성에 의해 상당 부분 불확실성을 초래한다. 또한 다른 관측지점과의 일관적인 비교를 위해 좌표보정을 수행하며, 일반적으로 바람이 평평한 지역 위로 분다는 가정 하에 이루어진다. 좌표보정은 일반적으로 Planar Fit Rotation방법을 사용하며, 평판 분할은 지형에 따라 12개까지 분할하여 분석한다. 하지만 덕유산 플럭스관측 타워지점처럼 산지 특성이 뚜렷하고 1 m/s이하의 풍속 데이터의 빈도가 큰 경우 평판 분할 수의 제한이 발생한다. 이러한 문제를 해결하기 위해 좌표보정계수산정 방법에 따라 등간격의 평판분할 방법(Scenario A), 주풍향을 고려한 평판분할 방법(Scenario B)과 빈도에 의한 평판분할방법(Scenario C)으로 수행하였다. 또한 각 Scenario는 풍속의 제한 조건에 따라 CASE A(0.5 m/s 이상), CASE B(1.0 m/s이상)로 구분하여 분석하였다. 본 연구를 통해 제안 한 자료처리 절차는 첫째, 바람자료의 빈도 분석을 통한 지역특성 파악 둘째, 풍속제한 조건 설정 셋째, 바람과 수증기의 공분산 계산으로 요약된다. 덕유산 플럭스관측 타워지점의 경우 풍속 제한을 1.0 m/s이상에서 0.5 m/s이상으로 하향 조정하였으며, 평판 분할 방법은 Scenario C의 평판 수 12개를 채택하였다.

• Journal of Korean Society of Forest Science
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• v.22 no.1
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• pp.63-65
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• 1974

In this study, it is aimed to elucidate the relationship between the distribution of barren land in mountainous area and the geological and topographical characteristics of barren land in south Korea. To do this, the Land Use Classification Maps for mountainous areas (scale:1/50,000), compiled by the Roseources Survey Office of Mountainous and Forest Areas, Geological Maps of Korea (scale: 1/50,000), and Map of Geology of Korea (scale: 1,000,000), compiled by the construction Research Institute of Korea were used. The following conclusions have been obtained from this study. 1) Areas of strata that are most liable to dilapidation are found in such order of the broadest to broad as region of granite, granite-gneiss, and the specific stratum called the Kyongsang Stratum (named after the provinces) of the northern and southern Kyongsang Provinces comprising sandstones, gravelstones, crumblestones, and other stones similar to these species. These rocky hills occupy vast areas in size, so to speak, they are estimated to cover roughly 57% of the total barren and naked areas in the country. 2) The average size in area of barren and nated land, as one piece of land, 32 hectares of granite region, 15 hectares of granite-gneiss region and little less than 13 hectares of Kyongsang strata region were calculated.