• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2020년도 학술발표회
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• pp.190-190
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• 2020

한국에서 겨울철에 주로 발생하는 자연재해는 대설이다. 마우나리조트 사고나 동해안 폭설 피해 등 직·간접적인 대설피해가 증가함에 따라 대설피해에 대한 관심이 증가하는 추세이다. 본 연구에서는 우리나라 230개 시군구를 대상으로 기후변화에 따른 대설피해에 대한 취약성 분석을 실시하였다. 대설 취약성 분석을 위해 RCP 기후변화 시나리오를 이용하였고, PSR(Pressure-State-Response) 구조를 적용하여 압력, 상태, 대응지수로 대설피해에 영향을 줄 수 있는 요인들을 분류하였으며 엔트로피 이론을 이용하여 각 인자의 가중치를 계산하였다. 그 결과 각 지역의 대설피해 취약성 순위를 도출해낼 수 있었고 도출해낸 취약성 순위를 바탕으로 향후 대설피해에 대한 대응마련을 실시할 경우 우선순위를 판단하는데 도움이 될 것으로 기대한다.

• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 1999년도 추계학술대회 논문집
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• pp.107-110
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• 1999

The ultrasonic spray method was employed to make (Y,Gd)BO$_3$:Eu Phosphor, and its optical properties under 147nm VUV and 254 nm UV excitations were characterized and then compared with that produced by the solid-state reaction. The mixed solution of acetate hydrates of Y, Gd, Eu and boric acid diluted in water or methanol was used as the precursor fur the spray. It was found that (Y,Gd)BO$_3$:Eu phosphor made by this ultrasonic spray had a spherical shape and fine particle size of 1${\mu}{\textrm}{m}$. The crystalline structure for the as-sprayed phosphor was amorphous, but it converted into the same polycrystalline phase of solid state reaction after post heat treatment at 110$0^{\circ}C$ for 2hr. The emitting intensity under VUV and UV excitations for the spray-formed (Y,Gd)BO$_3$:Eu phosphor, however, was inferior to the later one. The excitation spectra were also studied and compared under VUV and UV excitations to explain the change of emitting intensity with Gd substitution in (Y$_{1-x}$ Gd$_{x}$)BO$_3$:Eu Phosphors made by spray and solid state reaction.on.

• 한국광물학회지
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• 제13권3호
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• pp.115-120
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• 2000

황철석의 산화에 의한 토양 및 지표수의 산성화는 심각한 환경문제를 야기하여 왔다. 특이산 성토의 이차광물과 화학적 특징은 풍화과정을 반영하고 있다. 택지 및 골프장 조성과정에서 지표에 노출된 11.8% 황철석을 함유한 열수변질 안산암의 풍화에 따른 광물학적 변화를 X-선 회절, 전자현미경 (SEM, TEM), 배수의 화학분석을 통하여 연구하였다 수용성 염, ferrihydrite, jarosite가 풍화과정의 이차 광물로서 관찰되었다. 전자현미경하에서, ferrihydrite는 미세입자들의 입단, jarosite는 판상, 수용성 염은 기둥모양을 나타내었다. 안산암 내에 존재하는 황철석은 입자의 크기가 증가할수록 정육면체 형태/육각기둥 형태의 비가 증가하였다. 배수는 강산성 (pH 3.5) 이었으며 ferrihydrite, jarosite와 화학적 평형을 이루고 있었다.

• 대한본초학회지
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• 제35권1호
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• pp.27-33
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• 2020

Objectives : In previous studies, I presented various effects of Seosiokyongsan (SSOOS) cp soap on facial skin. However, in the case of skin clinical trials, various factors such as lifestyle, alcohol, tobacco, and stress could not be excluded. The purpose of this study was to investigate the effect of face wash using SSOOS cp soap on the skin without environmental factors. Methods : The same water and towel were used at the same place in order to examine the skin change state immediately before and after washing face with SSOOS cp soap. The skin test was performed before washing the face and after 10 minutes washing the face to compare the changes. As a control group, the case of washing with water without using cleanser and the case of washing with S-K cleanser, which is a popular commercial product, were set. Three cases were compared and analyzed. Results : In the case of water washing, the decrease in moisture was similar to that of the S-K cleanser and the amount of oil and pores decreased, but it was weaker than that of the S-K cleanser. The SSOOS cp soap showed a decrease in oil, pores, and pigments, but it was not significant, the moisture showed a significant decrease, but it was mild compared to S-K cleanser and water wash. Conclusion : In the case of SSOOS cp soap, the stimulation caused by facial cleansing was the least, showing a gentle change.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2005년도 춘계 학술발표회 논문집
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• pp.1140-1147
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• 2005

The objective of this study was to identify the effect of the degree of saturation on the resilient modulus of cohesive soils as subgrade. Six representative cohesive soils representing A-4, A-6, and A-7-6 soil types collected from road construction sites across Ohio, were tested in the laboratory to determine their basic engineering properties. Resilient modulus tests were conducted on unsaturated cohesive soils at optimum moisture content, and samples compacted to optimum conditions but allowed to fully saturate. The subgrade compacted at optimum moisture content may be fully saturated due to seasonal change. Laboratory tests on fully saturated cohesive soils showed that the resilient modulus of saturated soils decreased to less than half that of soil specimens tested at optimum moisture content. The reduction of resilient modulus would possibly be caused by the buildup of pore water pressure. In resilient modulus testing performed in this study on saturated samples, pore water pressure increases were observed. Pore water pressure and residual pore water pressure gradually increased with an increase in deviator stress.

• 한국정보통신학회논문지
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• 제16권3호
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• pp.626-634
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• 2012

양식 환경의 과학적이고 체계적인 관리와 양식어민을 위해 실시간 수질 및 급이 정보 이외에도 자료의 종합적인 판단과 변화 이력을 확인하고 관리할 수 있는 시스템이 필요하다. 따라서 본 연구에서는 양식장의 수질, 급이의 현재 상태를 제시하고 이력 정보를 기반으로 시뮬레이션 가능하며 상태 변화를 단계 별로 확인 가능한 시스템을 비주얼 C++를 이용하여 구현하였다. 또한 수질, 급이 상태 정보를 수산지식을 기반으로 종합적으로 분석할 수 있고 제시할 수 있는 엔트로피 모델을 제안하였다. 이는 추후 질병 및 다양한 연구 결과를 반영한 고차원의 양식 환경 모델을 생성할 수 있는 토대가 될 수 있다.

• 한국수자원학회논문집
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• 제50권12호
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• pp.837-847
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• 2017

본 연구에서는 소양강댐 유역의 수문기상인자들의 시공간적 변동성을 명확히 파악하기 위하여 지표해석모형을 구축하였다. 지표해석 모형으로는 Variable Infiltration Capacity (VIC) 모형을 사용하였으며, 모형의 공간 해상도는 10 km, 시간 해상도는 1일로 정하였다. 2007~2010년 기간의 일유량자료를 바탕으로 Isolated Particle Swarm Optimization 알고리즘을 사용하여 모형의 7개 매개변수를 보정하였고, 2011~2014년 기간의 일유량자료를 사용하여 모형을 검증하였다. 보정된 모형은 보정기간과 검증기간 모두에 대하여 0.90의 Nash-Sutcliffe Coefficient값과 0.95의 상관계수를 보였다. 소양강댐유역에 대하여 산출된 인자들은 여름철에 강우가 집중되어있는 우리나라의 계절적인 특성과 기온변화로 인한 장 단파 복사량의 변화와, 지표면 온도의 변화, 이로 인해 피복층에서의 증발과 식생 증산의 변화가 고려되어 총 증발산이 변화하는 경향이 잘 반영된 것으로 나타났다. 산출된 수문인자를 검증하기 위하여 지상관측토양수분자료와 비교하였다. 겨울철을 제외한 4~11월의 비교결과 두 자료의 추세선의 기울기는 1.087로 나타났고, 상관계수는 0.723의 값을 나타냈다. 이러한 본 연구의 결과는 지표해석모형이 우리나라 주요 댐 유역의 수문기상인자의 시공간적인 변화를 정확히 파악하는데 활용될 수 있으며, 나아가서는 더욱 정밀하고 효율적인 수자원계획을 수립하는 데에도 활용될 수 있다는 점을 시사한다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2022년도 학술발표회
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• pp.211-211
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• 2022

The marketization reform from the open-door policy in 1978 was not only booming export-oriented industries with foreign investment but also expanding the role of private actors in the Chinese water sector. Private Sector Participation (PSP) has become an important element in developing urban infrastructure by providing better services with advanced facilities. The rapid development of PSP-driven urban water infrastructure in China has a positive impacted on Chinese economic development, particularly in coastal areas. PPPs in some coastal areas have successfully spread out over China since China applied the first Build-Operate-Transfer (BOT) mode in the water sector in the early 1990s. The market-oriented water and wastewater, Public-Private Partnership (PPP) mechanism in the initial period of China has been transformed into a state-dominated PPP mechanism. The development pattern of the water and wastewater PPPs in China has been divided in four stages: the first period from 1984 to 2002, the second period from 2003 to 2008, the third period from 2009 to 2014, and the last period after 2015. The study aims to investigate the successful process of water and wastewater PPPs in local areas through five socioeconomic elements: export-oriented economic strategy, urbanization, cheap land policy, infrastructure investment, and water issues and climate change. In addition, the study focuses on analyzing the extent to which the Chinese government re-asserted its control over the PPP mechanism by classifying five elements in three different development Phases from early 2000 to 2020. The Jiangsu Province in the estern coastal area has actively invited PPP projects in the water and wastewater sectors. The successful introduction and rapid growth of PPPs in the urban water infrastructure has made the province an attractive area for a foreign investor.

• Ocean and Polar Research
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• 제38권3호
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• pp.195-207
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• 2016

Because the high latitude region in the North Pacific is characterized by high primary production in the surface water enriched with nutrients, it is important to understand the variation of surface water productivity and associated nutrient variability in terms of global carbon cycle. Surface water productivity change or its related nutrient utilization rate during the Northern Hemisphere Glaciation (NHG; ca. 2.73 Ma) has been reported, but little is known about such circumstances under gradual climate cooling since the NHG. Bulk nitrogen isotope (${\delta}^{15}N_{bulk}$) of sedimentary organic matter has been used for the reconstruction of nutrient utilization rate in the surface water. However, sedimentary organic matter experiences diagenesis incessantly during sinking through the water column and after burial within the sediments. Thus, in this study we examine the degree of nitrate utilization rate during the early Pleistocene (2.4-1.25 Ma) since the NHG, using the diatom-bound nitrogen isotope (${\delta}^{15}N_{db}$), which is known to be little influenced by diagenesis, from Site U1343 in the Bering slope area. ${\delta}^{15}N_{db}$ values range from ~0.5 to 5.5‰, which is lower than ${\delta}^{15}N_{bulk}$ values, but they vary with larger amplitude. Variation patterns between ${\delta}^{15}N_{db}$ values and biogenic opal concentration are generally consistent, which indicates that the nitrate utilization rate is closely related to opal productivity change in the surface water. A positive correlation between opal productivity and nitrate utilization rate was observed, which is different from the other high latitude regions in the North Pacific. The main reason for this contrasting relationship is that the primary production in the surface water at Site U1343 is influenced mostly by the degree of sea ice formation. Still, although concerns about diagenetic alteration have been avoided by using ${\delta}^{15}N_{db}$, the effects of the preservation state of biogenic opal and the species-dependent isotopic fractionation on ${\delta}^{15}N_{db}$ should be assessed in the future studies.

• Journal of Ecology and Environment
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• 제47권2호
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• pp.49-62
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• 2023

Background: Over the past three decades, gradual eustatic sea-level rise has been considered a primary exogenous factor in the increased frequency of flooding and biological changes in several salt marshes. Under this paradigm, the potential importance of short-term events, such as ocean storminess, in coastal hydrology and ecology is underrepresented in the literature. In this study, a simulation was developed to evaluate the influence of wind waves driven by atmospheric oscillations on sedimentary and vegetation dynamics at the Skallingen salt marsh in southwestern Denmark. The model was built based on long-term data of mean sea level, sediment accretion, and plant species composition collected at the Skallingen salt marsh from 1933-2006. In the model, the submergence frequency (number yr^-1) was estimated as a combined function of wind-driven high water level (HWL) events (> 80 cm Danish Ordnance Datum) affected by the North Atlantic Oscillation (NAO) and changes in surface elevation (cm yr^-1). Vegetation dynamics were represented as transitions between successional stages controlled by flooding effects. Two types of simulations were performed: (1) baseline modeling, which assumed no effect of wind-driven sea-level change, and (2) experimental modeling, which considered both normal tidal activity and wind-driven sea-level change. Results: Experimental modeling successfully represented the patterns of vegetation change observed in the field. It realistically simulated a retarded or retrogressive successional state dominated by early- to mid-successional species, despite a continuous increase in surface elevation at Skallingen. This situation is believed to be caused by an increase in extreme HWL events that cannot occur without meteorological ocean storms. In contrast, baseline modeling showed progressive succession towards the predominance of late-successional species, which was not the then-current state in the marsh. Conclusions: These findings support the hypothesis that variations in the NAO index toward its positive phase have increased storminess and wind tides on the North Sea surface (especially since the 1980s). This led to an increased frequency and duration of submergence and delayed ecological succession. Researchers should therefore employ a multitemporal perspective, recognizing the importance of short-term sea-level changes nested within long-term gradual trends.