• 베이커리
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• no.4 s.333
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• pp.120-121
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• 1996

• 한국보건간호학회:학술대회논문집
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• 1997.12a
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• pp.22-32
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• 1997

• 대학교육
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• s.47
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• pp.88-93
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• 1990

• Korean Architects
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• s.474
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• pp.78-83
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• 2008

• Proceedings of the Korea Water Resources Association Conference
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• 2022.05a
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• pp.195-195
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• 2022

도림천의 최상류인 관악산 유역에 서울대학교 관악캠퍼스가 건설되었다. 이로 인해 물순환은 기존의 자연 상태에서 점점 변해 왔는데, 이는 하류 도림천의 홍수 및 수질 오염의 피해를 증가시켰다. 도시화된 서울대학교 관악캠퍼스의 물순환 회복은 하류 홍수피해 방지와 지속 가능한 친환경 캠퍼스를 위해 중요하나, 이에 관한 연구는 미흡한 실정이다. 따라서 본 연구에서는 SWMM(Storm Wastewater Management Model)을 활용하여 캠퍼스 내 물순환 현황을 시간과 공간에 대해 정량적으로 파악하고, 물순환 회복을 위해 지속 가능한 효율적인 시스템을 구현하고자 한다. 먼저 유역 현황 조사와 함께 SWMM 구축에 필요한 수문·기상학적 변수와 물리적 매개변수를 확립하였다. 수문·기상학적 변수로는 기상관측장비 ATMOS-41의 설치와 기상청 자료로부터 수집하였으며, 물리적 매개변수는 환경부의 자료를 활용하였다. 그 후, 서울대-도림천 배수분구에 대해 SWMM을 적용하여 월별로 유출량, 침투량, 그리고 증발산량을 모의하였다. 시간에 따른 물순환 분석의 경우 강수량 자료와 불투수율의 변화 정도에 따라 월별 물수지 비율을 파악하고, 공간에 따른 물순환 분석의 경우 동일한 기간에 대해 분할한 16개의 소유역 별 유출량과 유역의 평균 유출량을 비교하여 분석하였다. 대상 유역의 월별 물수지 비율을 모의하는데 효율성을 높이고자 배수 구역 및 관망을 세밀하게 나눈 경우와 그렇지 않은 경우에 대해 분석하였다. 그 결과, 시간에 따른 연평균 물수지 비율의 차이는 2020년 모의 결과와 최근 5년 평균(2015~2019년) 모의 결과 비교 시 각 물수지 항목별로 0.47~2.34%의 차이를 보였다. 공간적으로는 16개 소유역 중 저류시설을 포함한 9개 소유역의 표면 유출량이 유역의 평균 유출량보다 많게 모의 되었다. 또한, 유역을 구성할 때보다 관망을 구성할 때 높은 정확성이 요구됨을 알 수 있었다. 본 연구는 ATMOS-41을 통한 지속적인 수문·기상학적 요소의 모니터링과 SWMM 모델 구축을 통해 앞으로도 변경사항을 추가함으로써 친환경 캠퍼스로의 전환에 이바지할 것으로 기대한다.

• Analytical Science and Technology
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• v.23 no.3
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• pp.269-277
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• 2010

Air samples were collected and analyzed to investigate regional level of PAHs and its emission sources. The average concentrations of PAHs in the suburban (Gwanak) and in the urban (Seodaemun) area were $16.52\;ng/m^3$ and $59.1\;ng/m^3$, respectively. Phenanthrene, fluoranthene, pyrene, and fluorene were predominant PAHs species, as their sum contributed to 55.6% and 60.8% of the total PAHs, respectively. The possible major source of PAHs was suspect to be the combustion of diesel fueled vehicles in both areas, particularly for Seodaemun.

• Journal of the Korea Academia-Industrial cooperation Society
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• v.10 no.11
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• pp.3506-3513
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• 2009

This study is to analyze the ripple effects of Jeju International Wind Ensemble Festival on Jeju regional economy and to explain the influence of the festival on Jeju regional society and culture. This study analyzed the economic ripple effects of the tourism industry with the Jeju inter-industry relation table. To explain the influence on Jeju regional society and culture, this study examined society-integrating part, policy-advertising part, culture-developing part, and industry-developing part.

• Korean Journal of Environment and Ecology
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• v.27 no.3
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• pp.344-356
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• 2013

This study is a continuation of the 22 year consecutive study (1972~1993) to monitor community dynamics of forest in Mt. Kwanak. This study was intended to provide basic data for urban forest management in the future by analyzing actual changes in vegetation structure of forest in Mt. Kwanak caused by urban environmental changes. For the past 39 years (1972~2010), average temperature increased by approximate between 1.1 and $1.7^{\circ}C$ and soil acidification (pH $5.40{\rightarrow}4.50$) and contents of $K^+$ ($0.67{\rightarrow}0.25$) and $Ca^{{+}{+}}$ ($3.20{\rightarrow}0.87$) apparently tended to decrease. According to analysis importance percentage and DBH class of community types classified based on DCA, the succession stopped at Quercus mongolica for 39 years. In addition, the succession was expected to be held at Q. mongolica or to shift from Pinus densiflora to Q. mongolica and from Q. acutissima to Q. serrata. Size of trees growing in forest of Mt. Kwanak increased but the number of species and population of trees showed a downward trend for the 39 years and Styrax japonica and Sorbus alnifolia, which are indicator species, increased their dominance continuously. Decrease in contents of $K^+$, $Ca^{{+}{+}}$, and $Mg^{{+}{+}}$ and soil acidification for the past 39 years was found to affect degradation of vegetation structure in Mt. Kwanak.

• Korean Journal of Construction Engineering and Management
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• v.14 no.4
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• pp.55-64
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• 2013

As GHG target management is introduced in Korea, designated establishment takes responsibilities to reduce more than 30% of expected GHG emission until 2020. Although decreasing GHG has been requested to universities which consume great amount of energy, there are difficulties to apply high cost countermeasures. Therefore, this research suggest a low cost, easily-applicable energy saving method, and derive potential GHG reduction amount in the case of SNU, Kwan-ak campus. First of all, 11 rooms of different use were chosen as the samples, and energy consumption in each room was measured. Standard models for each room were built through researching on the electric devices in each room. Moreover, energy consumption was computed for each devices through analyzing the pattern of electricity consumption. 32 GHG reduction technology and action program were chosen, and they were applied to the standard models for individual rooms. Through multiplying energy reduction rate of each program to energy consumption of each electric device, maximum energy reduction of each electric device is derived. Through that, Maximum GHG reduction for individual rooms and each month and the total GHG reduction capacity of Kwan-ak campus were computed. It was found out that approximately $5,311tCO_2$-eq can be reduced, when reduction technology and action program suggested by this research are applied. It appeared 24.48% of requested reduction amount to SNU can be reduced, till 2016.

• The Journal of the Petrological Society of Korea
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• v.4 no.1
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• pp.31-48
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• 1995

The Jurassic Kwanaksan stock, so far known to be composed of biotite granite only, has the mineral assemblage of quartz+K-feldspar+plagioclase+biotite${\pm}$gernet. The lithology of the stock is classified as alkali feldspar granite by their mode and plagioclase compositions (An<5). Subsolvus feldspars, rather early crystallization of biotite, and shallow emplacement depth estimated from Q-Ab-Or diagram suggest hydrous nature of the magma, which contrasts with anhydrous A-type like geochemistry described below. Major and trace element compositions of the Kwanaksan stock are distinct from those of the adjacent Seoul batholith, suggesting a genetic difference between the two, The Kwanaksan stock shows geochemical characteristics similar to A-type granite in contrast to most other Mesozoic granites in Korea, in that it has high $SiO_2$(73~78wt%), $Na_2O+K_2O$, Ga(27~47 ppm). Nb(22~40 ppm), Y(48~95 ppm), Fe/Mg and Ga/Al, and low CaO(<0.51 wt%). Ba (8~75 ppm) and Sr(2~23 ppm). However, it has lower Zr and LREE and higher Rb(384~796 ppm) than typical A-type granite. LREE-depleted rare earth element pattern with strong negative Eu anomaly of previous studies is reinterpreted as representing source magma characteristics. The residual material during partial melting is not compatible with pyroxenes, amphibole or garnet, while significant amount of plagioclase is required. Similarity of geochemistry of the Kwanaksan stock to A-type granite suggests the origin of the stock has a chose relationship with that of A-type granite. These observations lead us to propose that the Kwanaksan stock was formed by partial melting of felsic source rock.