• KOMUNHWA
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• no.58
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• pp.3-24
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• 2001

The origin of raw materials of Angdeok-ni earthenwares was reasonably interpreted by the combination of data derived from mineralogical and REE analyses. Geoscientific analysis, including microscope observation, X -ray diffractometry analysis and rare ear

• Proceedings of the Korea Water Resources Association Conference
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• 2023.05a
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• pp.135-135
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• 2023

우리나라의 전 국토면적 중 약 63% 이상이 산지로 이루어져 있으며 이는 OECD국가 중 4위에 해당할 정도로 매우 높은 비율이다. 광활한 산지 면적의 효율적 이용을 위해 사면개발, 태양광 시설, 관광자원으로써의 활용 등이 이루어져 토양침식에 매우 취약해졌으며, 하천으로의 토사유입량이 증가하고 있다. 따라서 하천으로 유입된 유사량의 조사가 매우 중요하며, 유사량 중 입경이 큰 소류사량을 추정하기 위한 조사 장비 중 간접적 방법인 하이드로폰에 관한 국내·외 연구가 활발히 진행되고 있다. 본 연구에서는 기존 소류사량 추정 방법 중 추정식을 활용한 방법의 추정량이 많아질수록 정확도가 낮아지는 문제를 개선하기 위한 노력으로 인공신경망의 한 종류인 Convolutional Neural Networks(CNN)를 소류사량의 계측에 적용하기 위한 연구를 시도하였으며, 그 결과와 실제 소류사량의 정확도를 비교 및 분석하였다. 실험데이터를 획득하기 위하여 실내수로를 구축하였으며, Labview를 이용하여 소류사량에 대한 충돌음 이미지데이터를 취득한 후 학습을 진행한 결과, 검증데이터에 대한 정확도는 60%이상의 값으로 나타났다. 향후 추가적인 데이터 확보를 통해 정확도 향상을 위한 연구를 진행하고자 한다.

• Proceedings of the Korea Water Resources Association Conference
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• 2020.06a
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• pp.39-39
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• 2020

Low-flow 하천에서의 최저수위를 나타내는 지표이다. 일반적으로 유황곡선의 갈수량(Q355)를 대표적으로 사용한다. Low-flow는 물 공급 관리 및 계획, 관개용수, 생태계등 다양한 분야에 영향을 미친다. 이러한 Low-flow를 산정하기 위해서는 충분한 기간의 유량자료가 필요하다. 하지만 국토의 70%가 산지지형으로 구성되어 있는 우리나라의 경우 국가하천과 1급하천을 제외한 산지유역은 수위관측소가 부재하거나 결측으로 인해 자료가 충분하지 않아 Low-flow분석에 한계가 있다. 이에 과거에는 미계측지역의 갈수량을 예측하기 위해서 다중회귀분석, ARIMA 모형 등 다양한 기법을 사용하였지만, 최근들어 머신러닝 모형의 수요가 증가하고 있다. 이에 본 연구에서는 새로운 패러다임에 맞는 머신러닝 기법인 DNN기법을 사용하고자 한다. DNN기법은 ANN기법의 단점인 학습과정에서 최적 매개변수값을 찾기 어렵고, 학습시간이 느린 단점을 보완한 방법이다. 따라서 본연구에서는 머신러닝 기법인 DNN기법을 통해 미계측지역에 적용 가능한 지역화 Low-flow indices를 산정하고자 한다. 먼저, Low-flow에 영향을 미치는 인자들을 수집하고 인자들간의 상관분석, 다중공선성 분석을 통해 통계적으로 유의한 변수를 선정하여, 머신러닝 모형에 입력자료를 구축하였다. 또한 기존의 갈수량 예측기법인 다중회귀분석 결과와 비교하여 머신러닝 기법의 효용성을 검토하였다.

• Korean Journal of Agricultural and Forest Meteorology
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• v.12 no.4
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• pp.307-316
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• 2010

Complex terrain refers to irregular surface properties of the earth that influence gradients in climate, lateral transfer of materials, landscape distribution in soils properties, habitat selection of organisms, and via human preferences, the patterning in development of land use. Complex terrain of mountainous areas represents ca. 20% of the Earth's terrestrial surface; and such regions provide fresh water to at least half of humankind. Most major river systems originate in such terrain, and their resources are often associated with socio-economic competition and political disputes. The goals of the TERRECO-IRTG focus on building a bridge between ecosystem understanding in complex terrain and spatial assessments of ecosystem performance with respect to derived ecosystem services. More specifically, a coordinated assessment framework will be developed from landscape to regional scale applications to quantify trade-offs and will be applied to determine how shifts in climate and land use in complex terrain influence naturally derived ecosystem services. Within the scope of TERRECO, the abiotic and biotic studies of water yield and quality, production and biodiversity, soil processing of materials and trace gas emissions in complex terrain are merged. There is a need to quantitatively understand 1) the ecosystem services derived in regions of complex terrain, 2) the process regulation occurred to maintain those services, and 3) the sensitivities defining thresholds critical in stability of these systems. The TERRECO-IRTG is dedicated to joint study of ecosystems in complex terrain from landscape to regional scales. Our objectives are to reveal the spatial patterns in driving variables of essential ecosystem processes involved in ecosystem services of complex terrain region and hence, to evaluate the resulting ecosystem services, and further to provide new tools for understanding and managing such areas.

• Korean Journal of Environment and Ecology
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• v.21 no.1
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• pp.22-29
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• 2007

Investigation of carabid beetles as on ecological indicator species for wetland characterization and monitoring was conducted in three types of wetlands such as emergent wetland, forested wetland, and estuary, During the investigation period, twenty-eight species belonging to twenty-two genera and three families(Carabidae, Harpalidae, Brachinidae) were identified. The diversity of carabid beetles at riverine wetland such as Woopo (H'=1.18) and Hwapo-neup (H'=1.08) were higher than in the forested wetland (H'=1.03) and estuarine (H'=0.91). Species compositions in each wetland were significantly different(${\chi}^2=1716.8$, P<0.01). Riverine wetlands differed significantly from the forested wetland. Indicator species for the wetland chose with indicator species analysis were reacted sensitively on the parameter such as soil composition, moisture of soil, and environmental change. Thus, it was consequently suggested that these indicator species may be applied for wetland characterization and monitoring of the wetland ecosystem.

• Journal of Korea Water Resources Association
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• v.41 no.6
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• pp.565-574
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• 2008

Fire-enhanced soil hydrophobicity often increases runoff and erosion in the mountain hillslope following severe wildfires. Estimation techniques for WEPP's parameters were studied in burnt mountain slopes. In burnt mountain slopes, the model over-predicted runoff in the small runoff and under-predicted runoff in the great runoff, and in the lower sediment runoff it had a tendency to over-predict soil loss. The effective hydraulic conductivity was most sensitive in the WEPP's runoff and its sediment runoff was mainly effected by the effective hydraulic conductivity, initial saturation, rill erodibility, and interrill erodibility. To improve the applicability of the WEPP, the adjustment coefficient of effective hydraulic conductivity was defined for runoff and the adjustment coefficient of rill erodibility and interrill erodibility was presented for sediment runoff. The adjustment coefficient of effective hydraulic conductivity in wildfire mountain slopes increased with maximum rainfall intensity of single storm and the vegetation height index. The adjustment coefficients of rill erodibility depended on soil components of size distribution curve and total rainfall depths in single storm. The adjustment coefficients of interrill erodibility decreased with increases of maximum rainfall intensity and vegetation height index. These results may be used in the application of WEPP model for wildfire mountain slopes.

• Journal of the Korean Society of Hazard Mitigation
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• v.9 no.6
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• pp.119-124
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• 2009

In this study, the characteristics of estimating methodology for RUSLE factors such as soil erodibility factor, slope length-steepness factor, and cover management factor were reviewed and then the relative error according to each methodology was analyzed. RUSLE was applied to experimental watershed for 42 storm events and their results were compared with measured sediment yield to examine the applicability of RUSLE. As a result, this paper found that it should be necessary to consider vegetation effect for forest application of RUSLE as cover management was the most sensitive factor. Also, soil erodbility factor was calculated from data of soil series by National Academy of Agricultural Science caused sediment yield to be overestimated because there were big differences between the soil series and on-site soil texture. The 22.7% of maximum relative error was shown according to selecting the rain energy equation. In addition, it will be necessary to verify the RUSLE factors with more data in order to improve their accuracy.

• Proceedings of the Korea Water Resources Association Conference
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• 2021.06a
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• pp.229-229
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• 2021

최근 이상기상으로 국지성 집중호우가 빈번하게 발생함에 따라 토사유출에 의해 피해가 증가하고 있다. 급경사 사면을 갖는 교란산지와 개발지의 경사면은 토양침식 위험에 노출되어 있다. 특히 지표유출수의 집중흐름에 의한 세류발달은 세류간침식에 비해 많은 토양침식과 토사유출을 발생시킨다. 이러한 급경사 사면에서의 세류발달에 대한 수리학적 메터니즘과 한계조건을 파악하고자 강우와 유입수 모의를 통한 토양침식 실험을 수행하였다. 강우와 유입수의 상호작용에 의한 세류발달의 특성과 토사유출량 증가를 파악하고자, 강우량의 증가와 유입수 유무에 따른 실험이 이루어졌다. 강우강도의 범위는 100~140mm/hr이고, 유입수는 170ml/s 이였다. 유입수량은 합리식으로 계산하였으며, 토양상자 상단에서 균등분사식으로 유입되었다. 세류발달의 수리학적 특성치를 취득하기 파악하기 위해, 염료주입 지표수 거동에 대한 동영상을 판독하였다. 세류발달은 유입수가 없는 경우 3분 이내 그리고 유입수가 있는 경우 30초 이내에 발생하였다. 토양상자내의 평균 유속범위는 7.83~29.27 cm/s 이였다. 실험에서 발달된 세류는 15분경과 후부터 평형상태를 유지하였다. 경사실험조건별로 세류 차수분석을 위해 각 세류의 최대길이, 폭, 넓이를 측정한 결과 세류의 차수는 강우만 있는 경우 1~2차로 발달하였으며, 유입수가 있을 때는 2~3차로 발달하였다. 지표유출이 증가하면서 세류발달의 개수는 줄었지만 규모는 더 크게 나타났다. 세류가 발달하는 시점의 한계유속은 10~20cm/s 범위인 것으로 파악되었다. 지표유출이 증가하면서 세류의 발달도 더 심화되지만, 동일한 강우에 일정시간동안 노출되면서 세류는 평형상태가 되어 더 이상 침식이 활발하게 진행되지는 않았다. 유입수가 있는 조건에서 수량은 약 2배가 증가하였지만, 토사유출량은 세류확장에 의해 약 4배가 증가하는 것으로 나타났다.

• Journal of Korean Society of Forest Science
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• v.86 no.2
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• pp.119-127
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• 1997

Japanese red pines growing along the Taebaek mountains have been called "Kangsong" and considered to be superior in growth and wood quality. An attempt was made to determine whether their boundaries for planting may be expanded by testing their early growth at eight experimental plantations of the Republic of Korea. Seeds were collected from the six different natural populations including Uljin in Kyongbuk province. For the provenance test, they were planted in eight different regions including Taean in the spring of 1987. Experimental planting was a randomized complete block design with 3 replications. Height growth was measured at the ages of 2, 4, and 6 after planting, and the diameter at root collar at the age of 6 after planting. Significant variation in height growth was observed among the plantations. The height growth measured at the age of 6 after planting showed a positive correlation with the latitude of the test plantation, and the contents of phosphate, potassium and calcium in the soil. A negative correlation, however, was observed between the longitude of the test plantation and height growth. Ponghwa provenance appeared to be the best among the provenances in that the trees from the area grew 16% better in volume growth than the average of all the trees tested in the study, while the worst one was Kyongju from which trees grew 11% less than the average.

• Journal of the Korean Geographical Society
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• v.49 no.2
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• pp.221-244
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• 2014

We suggested several implications by examining geochemical properties of sediments in Simjeok, Jangdo, and Hwaeomneup mountain wetlands which are natural preservation areas. Geochemical properties of wetland sediments show that all wetlands were included in the type of fens, but their distribution patterns were different from one another. We classified three sub-groups of sediments using the two step cluster analysis on the ratio of exchangeable cations. Wetland sediments can be grouped into Ca-dominated, Mg-dominated, and K-dominated types. Simjeok wetland have Ca-dominated sediments, while the sediments of Jangdo wetland indicate the Mg-dominated and Ca-dominated characteristics. Hwaeomneup wetland is composed of K-dominated sediment mainly. Different properties in the ratio are affected by various environmental factors such as geological, pedological, and vegetational settings. Because these geochemical properties will be affected by climate change and human impacts, these will be environmental indicator in mountain wetlands and be used in wetland management. This scheme can be used for classification of mountain wetlands. Therefore, we should work on geochemical properties of wetland sediments and classification schemes based on geochemical properties not only to widen understanding in geomorphic system or ecosystem of mountain wetlands but to conserve mountain wetlands properly.