• Proceedings of the Korea Water Resources Association Conference
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• 2021.06a
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• pp.231-231
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• 2021

하천 및 하천시설물 관리 등을 위해서는 유역에서 하천으로 유출되는 유사량 파악이 필요하다. 현재 유사량측정은 하천에서 여러 개(3~7개)의 측선에서 부유사채취기를 이용하여 측정하여 농도를 분석하여 유사량을 산정하게 된다. 본 연구는 유량측정 기법 중 최근 자동유량측정기술에 활용하는 지표유속법(index velocity method)을 부유사량 측정에 적용하고 검토하였다. 지표법(index method) 적용 방법은 여러 개의 측선에서 측정된 부유사농도와 평균농도와의 관계를 분석하고, 평균농도와 가장 상관성이 높은 측선의 부유사농도를 지표 부유사농도로 설정하여 지표부유사 농도와 평균부유사농도와의 관계식을 개발하여 부유사량 산정에 활용하였다. 대상하천은 주천강에 위치한 영월군(주천교) 지점을 선정하였으며, 2020년 주요 홍수사상에서 27개의 부유사 측정성과를 확보하였다. 부유사 측정을 위하여 5개의 측선에서 부유사를 측정하였고, 부유사농도 규모는 2.20~373.20mg/ℓ이다. 평균부유사농도와 가장 상관성(상관계수 0.9988)이 높은 4번 측선의 부유사농도를 지표부유사농도로 설정하고 평균부유사농도와 지표부유사농도의 관계식을 개발하였다. 그 결과 지표관계식의 결정계수(R²)는 0.9977로 매우 높게 산정되었으며, 실측 평균부유사농도와 계산 평균부유사농도의 편차율은 평균 26.71%(0.60~103.26%)로 분석되었다. 편차율은 상대적으로 부유사농도가 낮은 성과에서 높았으며, 부유사농도가 10mg/ℓ 이상에서는 편차율이 14.81%로 1/2 가까이 줄어들었다. 즉 유량이 적은 경우 흐름 및 부유사가 하천의 일부구간으로 불규칙하게 편중되거나 흐름 전체적으로 확산되지 않아 편차율이 높게 산정되는 것으로 판단된다. 이러한 결과를 볼 때 홍수시 부유사농도의 지표법을 이용한 부유사량 산정이 가능 할 것으로 판단된다.

• Korean Journal of Mineralogy and Petrology
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• v.33 no.3
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• pp.215-232
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• 2020

The study area of Nokjeonri in Yeongwol belongs to the Taebaeksan Mineralized District. Ca and Mg skarn and related ore mineralization are developed in the Pungchon formation along the contact with the Imog granite. Ca skarn hosted in limestone mostly comprises garnet and pyroxene. Mg skarn developed in dolomite includes olivine and serpentine. Magnetite-hematite and pyrrhotite(±scheelite)-pyritegalena-sphalerite were mineralized during early and late stage, respectively. Garnet compositions are dominated by andradite series in proximal area and grossular series in distal area. Pyroxene compositions correspond to diopside series in majority. These compositional changes indicate that the fluids varied from oxidizing condition to reducing condition due to increased reaction with carbonated wall rocks as the fluids moved from the granite to a distal place. Fe₂O₃ and MgO concentrations of magnetite are higher in Mg skarn than those in Ca skarn, while FeO shows opposite trend. The Zn/Fe ratio of sphalerite increases with distance from the Imog granite. The δ³⁴S values of sulfide minerals are similar to those of the Imog granite, indicating magmatic origin in ore sulfur. Mineralization was established in the order of skarn, oxide and sulfide minerals with decreasing temperature and oxygen fugacity and increasing sulfur fugacity.

• The Journal of Korea Institute of Information, Electronics, and Communication Technology
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• v.7 no.4
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• pp.178-187
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• 2014

The purpose of this study is to study the coexistent development of the touristic and education cultures of temples. For the study, an investigation on the actual conditions of temples in Youngwol and a set of interviews were conducted from 13th June to 7th November in 2014. The analysis was conducted through the field observations and the interviews with building owners based on the criteria and SPSSWIN 18.0 program was used for statistical processes. The results of analysis are as follows. First, the temples are found to be the extremely valuable local cultural assets with the cultural values and historical backgrounds. Second, the major temple buildings show that they have the unique and distinct characteristics that cannot be found from other general temples, so it is necessary for developing the unique local tourism resources from them. Third, since the study shows that there is a lack of tourism and educational culture resources, so a relevant plan thereof is urgently required. The implication of this study is that there is an urgent necessity for the succession and the modern reinterpretation regarding the cultures of traditional temples, based on which a shift of viewpoint to the digital tourism, which covers both the traditional temple cultures and the modern cultures, could arise.

• The Journal of Korea Institute of Information, Electronics, and Communication Technology
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• v.7 no.4
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• pp.168-177
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• 2014

The purpose of this study is to analyze the activation plan with the traditional houses for the local tourism and culture welfare system. For the study, an investigation on the actual conditions of Youngwol-gun and a set of interviews were conducted from 13th June to 7thNovember in 2014. The analysis was conducted through the field observations and the interviews with building owners based on the criteria and SPSSWIN 18.0 program was used for statistical processes. The results of analysis are as follows. First, in order to understand the strengths and weaknesses of the local tourism and culture welfare system and to find its regional identity, the traditional houses need to be taken as a means of representing the local traditions and cultures. Second, a unique experiencecenter of traditional lifestyle and culture is necessary. Third, various local events on the tourism resources and traditional housings, development of various programs and promotion of local images are required for reinterpreting and reviewing the values of traditional houses. The implication of this study is that it provides the valuable information for enhancing the development and income of the local region and attracting tourists much more than now, since the succession and reinterpretation of the traditional housing cultures can harmonize the past, current and the future.

• Korean Journal of Soil Science and Fertilizer
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• v.22 no.4
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• pp.265-270
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• 1989

Soil properties for the limestone-derived soil were examined to relate soil formation to stratigraphy of parent materials and hillslope positions in Bangjeol Ri, Yeongweol Eup, Gangweon Do. Pyeongchang, Anmi, Yulgog and Mungyeong series were described for topographic positions such as shoulder position, footslope, terrace and local bottom associated with toposequence where the landscape consisted of gently rolling hillslopes and nearly level plains. 1. Pyeongchang, Anmi, Yulgog and Mungyeong series had the standard hue of the 2.5YR, 5YR, 10YR and 2.5Y, respectively. Thus, color sequence of soil could be related to hillslope positions on the landscape. 2. With ascending slope toward summit, the clay content increased while silt content decreased 3. Silt/Clay ratios ranged from 0.27 to 3.76 and it was increased with descending to bottom. It, also, appeared that maturity of soil was higher at summit position than at bottom. 4. Soils developed in limestone were neutral in soil reaction and very low in available $P_2O_5$. OM, available $SiO_2$, CEC, and active Fe in soils seemed to be increased with ascending to summit position.

• Economic and Environmental Geology
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• v.54 no.4
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• pp.457-464
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• 2021

The objectives of this study were to analyze of soil chemical characteristics of abandoned coal mine forest rehabilitation areas in Gangwon-do. The study sites were 8 areas and the investigations were performed 11 times according to elapsed time. Soil characteristics were soil pH, TOC, Total-N, C/N ratio, and Av. P₂O₅. Soil pH and Av. P₂O₅ were decreased according to elapsed time after forest rehabilitation, while TOC, Total-N, and C/N ratio increased. TOC and Total-N arrived at quality requirements of covering soil for forest rehabilitation in abandoned coal mine area passed 10 years after forest rehabilitation, while soil pH became lower than that. Therefore, it needs long-term monitoring of soil chemical characteristics after the forest rehabilitation and to establish post management.

• Korean Journal of Plant Resources
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• v.13 no.2
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• pp.104-110
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• 2000

To analyse the genetic relationship and intraspecific variations among the Eleutherococcus senticosus population, the polymerase chain reaction(PCR) was performed total genomic DNAs of 10 E. senticosus collections by random 10 primers. The genetic diversity and genetic distance among 10 collections of Eleutherococcus spp. were used to describe the dendrogram showing phylogenic relationship. Ten collections were classfied into two group(group I, II) at the similarity coefficient value of 0.50. Group I included E. senticosus of Bukhado(Japanese), youngwal(Korea), E. seoulense, and E. chiisanesis while group II included several internal and Russia collection. The range of polymorphism was from 66.7 to 90.9% in 87 amplified DNA fragments. The similarity value of all collections ranged from 0.41 to 0.92. The average of genetic distance was 0.61.

• The Journal of the Korea Contents Association
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• v.17 no.4
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• pp.1-11
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• 2017

Interest in all kinds of renewable energies has been highly increased while the micro-small-hydro power(MSHP) development has shown relatively slowly growth because of the negative public recognition about dam site development. It is, however, announced that the micro-SHP shows higher energy conversion efficiency compared to other renewable energies and does not emit any carbon dioxide. Thus, it is concerned about the development and application of micro-SHP as an alternative energy. In this study, the application for Android was exploited with Eclipse to visualize readily the potential realizable amount of hydropower by micro-SHP. With this application, we can select the region from the map, obtain the design discharge of the selected site was calculated with HEC-HMS, presented by U.S. Army of Corp. and perform the simply economic analysis in sequence. Yeongwol in Gangwon-do Province, Korea was chosen as the target area since historically abundant precipitation was found and it is possible to obtain fundamental data from WAMIS. Results from this study could be expanded the whole region of Korea. Also, the initial investment cost would be reduced if the location for micro-SHP would be determined properly, because this application can help us easily select and examine the potential micro-SHP sites without on-the-spot visit.

• Journal of Korean Society of Forest Science
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• v.95 no.1
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• pp.55-59
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• 2006

The objectives of this study, an analysis of the morphological characteristics among six provenances of a rare Rhododendron micranthum could be used for the conservation of gene resources and could provide information on superior trees selection. The following results were obtained. Approximately Mt.worak region showed larger values at petal character. On the other hand, Bonghwa region showed smaller values at petal character. Yeonha-ri region showed larger values at leaf character. On the other hand, Bonghwa region showed smaller values at leaf character. The results of principal component analysis (PCA) for morphological characteristics showed that the first for principal components(PC's) explained 41.6% of the total variation. From th third PC explained 81.5% of the total variation. The first PC was correlated with those characteristics that were mainly related to the Petal length (PL), Leaf length (LL) width (LW), Stigma length (SL). The second PC was correlated with the Petiole length (PTW), Anther length (AL). The third PC was correlated with the Flower pedicel length (FPL), Filament length (FL). Therefore, these characteristics was important to analysis of the variation for morphological characteristics among provenances of Rhododendron micranthum. Cluster analysis using single linkage method based on morphological characteristics showed that six provenances of Rhododendron micranthum could be clustered into three groups. Group I is Jicdong-ri, Group II is Mt.worak and Yeonha-ri, and Group III is Taeback, Bonghwa, and Samcheok. These results corresponded well with that of principal component analysis.

• Journal of the Mineralogical Society of Korea
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• v.2 no.2
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• pp.73-80
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• 1989

The sedimentary siderite rock or siderostone has been firstly found from the upper part of the Cambrian Myobong Slate in the Sangdong Tungsten Mine area. It occurs as layers between slate and calc-silicate rock (originally siliceous ankerite rock and ferroan dolostone) or within calc-silicate rock. Some parts of the siderostone bed, however, are considerably skarnized to iron-rich skarns, leaving only small-scaled relics. Siderostone consists mainly of siderite and quartz with minor amount of bertioerine and fluorite or apatite and is commonly microcrystalling granular in texture. Stratification is well developed in some siderstone. The siderostone and its skarnized rocks occasionally contain scheelite grains. Siderite also occurs in sandstone and slate. Mineralogy and textures of the siderostone suggest that it might be formed in the shallow marine basin where enough organic matter was present to maintain a low Eh and iron was supplied, and that siderite might be formed largely by diagenesis from iron-rich berthierine mud.