• 대한토목학회논문집
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• 제32권3C호
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• pp.113-120
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• 2012

진주 잔류토 사면의 실제 붕괴사례에 대한 해석을 수행하였다. 강우시 침투로 인하여 불포화층에서 유효응력과 전단 강도가 감소하여 안전율이 저하된다. 본 연구에서는 함수특성곡선을 이용하여 흡수응력에 기반한 유효응력을 산정하였다. 대상 현장에서 채취한 시료로부터 함수특성곡선, 투수계수, 전단강도와 관련한 불포화 물성들을 획득하였다. 실제 강우에 대한 불포화층의 침투해석을 수행하고 사면 지층의 간극수압 분포를 구할 수 있었다. 유한요소 응력장에서 탄성 해석으로 지층내 전응력을 계산하고 활동면에 작용하는 전단응력의 분포를 계산하였다. 활동면에 작용하는 흡수응력 및 유효응력을 산정하여 전단강도를 평가할 수 있었다. 이로부터 강우에 따른 안전율을 계산하였으며, 실제 강우에 의하여 사면이 활동이 일어나는 것을 모의할 수 있었다. 또한 활동면에서 흡수응력이 증가하고 유효응력이 감소하는 동시에 전단강도가 감소하는 것을 추적할 수 있었다.

• 수산해양기술연구
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• 제52권4호
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• pp.281-289
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• 2016

Spinyhead sculpin Dasycottus setiger, a species of cold water fish, is distributed along the eastern coastal waters of Korea. A series of fishing experiments was carried out in the waters near Uljin from June, 2002 to November, 2004, using the experimental monofilament gill nets of different mesh sizes (82.2, 89.4, 104.8, and 120.2 mm) to describe the selectivity of the gill net for the fish. The SELECT (Share Each Length's Catch Total) analysis with maximum likelihood method was applied to fit the different functional models (normal, lognormal, and bi-normal models) for selection curves to the catch data. The bi-normal model with the fixed relative fishing intensity was selected as the best-fit selection curve by AIC (Akaike's Information Criterion) comparison. For the best-fit selection curve, the optimum relative length (the ratio of fish total length to mesh size) with the maximum efficiency and the selection range ($R_{50%,large}-R_{50%,small}$) of 50% retention were obtained as 2.363 and 0.851, respectively. The ratios of body girth to mesh perimeter at 100% retention where the selection curve of each mesh size represented the optimum total length were calculated as the range of 0.86 ~ 0.87.

• 한국물환경학회지
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• 제25권1호
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• pp.159-166
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• 2009

This study has been attempted to generate electricity, while simultaneously treating artificial organic wastewater using both batch and continuous microbial fuel cells (MFCs). In the batch MFC, current-voltage curve showed an onset potential of -0.69 V vs. Ag/AgCl. The potential range between this potential and 0 potential displayed an available voltage for an automatic production of electric energy and glucose, which was oxidized and treated at the same time. The 486 mg/L glucose solution showed the maximum power of $30mW/m^2$ and the maximum current density of $75mA/m^2$ shown in the power curve. As a result, discharging of the cell containing COD 423 mg/L at the constant current density of $60mA/m^2$ showed a continuous electricity generation for about 22 hours that dropped rapidly due to dissipating of organic material. Total electric energy production was 18.0 Wh. While discharging, the pH change was low and dropped from pH 6.53 to 6.20 then increased to 6.47, then stabilized at this charge. The COD treatment efficiency was found to be 72%. In the continuous MFC, COD removal tends to increase as the hydraulic retention time is increased. At one day of hydraulic retention time as the maximum value reaches the COD removal efficiency, power production rate and power production rate per COD removal that were obtained were 68.8%, $14mW/m^2$, and $20.8mW/m^2/g$ CODrm, respectively. In the continuous MFC, the power production rate per COD removal increases as the hydraulic retention time is increased and decreases as the organic loading rate is increased. At the values lower than an organic loading rate of $1kgCOD/m^3/d$, the values higher than about $18.1mW/m^2/g$ CODrm could be obtained.

• 대한원격탐사학회지
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• 제30권5호
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• pp.587-596
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• 2014

토양수분의 시공간적 변동성은 유역의 수문학적인 반응과 지표 대기간의 상호작용에서 중요한 관심사로 특히, 강우유출 예측 시 유역의 강우사상에서 사전 토양수분 상태 즉, 선행습윤조건(antecedent wetness conditions, AWC)이 고려되어야 한다. 본 연구에서는 선행습윤조건을 알아보기 위한 지표로 토양 습윤지수(SWI), 5일 선행강우지수($API_5$), 위성토양수분($SM_{rs}$), 5일 지점토양수분($SM_{g5}$)을 선정하여 한반도 4개 지점에 대한 선행수분조건을 파악하였다. 토양수분 자료는 AMSR-E로 관측된 자료를 활용하였으며, 이에 따라 각 지역별로 2011년의 강우사상을 선택하여 Soil Conservation Service-Curve Number (SCS-CN)법과 강우량을 활용하여 직접유출고와 최대잠재보유량을 산정하였다. 이를 토양의 습윤상태를 나타내는 4개 지표와의 관계를 살펴본 결과 최대잠재보유량과 SWI가 평균 -0.73의 높은 상관계수를 보였다. 또한 토양수분의 시간적 변동성을 나타내는 time length를 산정한 결과 지역 별로 상이하게 나타났으며 이는 연구지역 및 토양 특성을 반영한 것으로 판단된다. 추후 관측된 토양수분이 지표의 습윤상태를 예측하는데 정량적인 정보를 제공할 수 있으므로 이에 대한 지속적인 모니터링 및 분석이 필요할 것으로 사료된다.

• 방사성폐기물학회지
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• 제17권3호
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• pp.329-338
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• 2019

불포화 벤토나이트 완충재의 수분흡입력은 공학적방벽의 수리-역학적 성능평가 및 설계에 있어 매우 중요한 입력인자이다. 본 연구에서는 문헌에 보고된 불포화 다공성매질의 수분흡입력 측정기술과 구성모델을 분석하고, 고준위폐기물처분장의 벤토나이트 완충재에 적합한 수분흡입력 측정기술과 구성모델을 제안하였다. 문헌 분석결과, 벤토나이트 완충재의 수분흡입력은 일반토질보다 훨씬 높은 값을 가지며, 매트릭수분흡입력과 삼투흡입력을 포함하는 총수분흡입력을 측정하여 사용하였다. 벤토나이트 완충재의 수분흡입력 측정에는 상대습도센서를 이용한 측정방법(RH-Cell, RH-Cell/Sensor)이 적합하였으며, 핵종 붕괴열에 의한 온도변화와 측정 소요시간을 고려했을 때에는 RH-Cell/Sensor 방법이 더 선호되었다. 벤토나이트 완충재의 수분보유모델은 실험을 통해 여러 가지 모델이 제안되었지만, 불포화 완충재의 수리-역학적 성능평가 구성모델로는 대부분 van Genuchten모델이 사용되었다. 벤토나이트 완충재의 수분특성곡선은 벤토나이트의 종류, 건조밀도, 온도, 염도, 측정 시 시료상태와 이력과정에 따라 서로 다른 경향을 보였다. 수분보유모델의 선정 및 모델인자 결정에는 신뢰도 향상을 위해 이러한 인자들의 영향이 고려되어야 한다.

• 한국농공학회논문집
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• 제47권3호
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• pp.59-68
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• 2005

The rainfall-runoff potential of Jangseong reservoir watershed was studied based on SCS (Soil Conservation Service, which is now the NRCS, Natural Resources Conservation Service, USDA) runoff curve number (CN) technique. Precipitation and reservoir operation data had been collected. The rainfall-runoff pairs from the watershed for ten years was estimated using reservoir water balance analysis using reservoir operation records. The maximum retention, S, for each storm event from rainfall-runoff pair was estimated for selected storm events. The estimated S values were arranged in descending order, then its probability distribution was determined as log-normal distribution, and associated CNs were found about probability levels of Pr=0.1, 0.5, and 0.9, respectively. A subwatershed that has the similar portions of land use categories to the whole watershed of Jangseong reservoir was selected and hydrologic monitoring was conducted. CNs for subwatershed were determined using observed data. CNs determined from observed rainfall-runoff data and reservoir water balance analysis were compared to the suggested CNs by the method of SCS-NEH4. The $CN_{II}$ measured and estimated from water balance analysis in this study were 78.0 and 78.1, respectively. However, the $CN_{II}$, which was determined based on hydrologic soil group, land use, was 67.2 indicating that actual runoff potential of Jangseong reservoir watershed is higher than that evaluated by SCS-NEH4 method. The results showed that watershed runoff potential for large scale agricultural reservoirs needs to be examined for efficient management of water resources and flood prevention.

• 한국농공학회논문집
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• 제48권5호
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• pp.83-93
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• 2006

In unsaturated porous media, the air-water interface (AWI) plays an important role in removing of biocolloids such as bacteria, viruses, and protozoan (oo)cysts. In this study, four models related to calculation of specific AWI area are analyzed to determine the appropriate model, and the selected models are verified using the previously reported experimental data. The results indicate that the modified model from Niemet et al. (2002) is the most appropriate tool for calculating the specific AWI area using the van Genuchten (1980) parameters obtained from the water retention curve. Hence, it is expected that this model could be used to quantitatively determine the attachment of biocolloids to AWI in the transport modeling of biocolloids in unsaturated porous media.

• 한국지하수토양환경학회지:지하수토양환경
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• 제26권1호
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• pp.1-7
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• 2021

Air-water interfacial area is of great importance for the analysis of contaminant mass transfer processes occurring in the soil systems. Capillary bundle model has been proposed to estimate the specific air-water interfacial areas in unsaturated soils. In this study, the measured air-water interfacial areas of a soil (loam) using the gaseous interfacial tracer technique were compared to those from capillary bundle model. The measured values converged to the specific solid surface area (7.6×104 ㎠/㎤) of the soil. However, the simulated air-water interfacial areas based on the capillary bundle model deviated significantly from those measured. The simulated values were substantially over-estimated at low end of the water content range, whereas the model under-estimated the air-water interfacial area for the most of the water content range. This under-estimation is considered to be caused by the nature of the capillary bundle model that replaces the soil pores with a bundle of glass capillaries and thus no surface roughness at the inner surface of the capillaries is taken into account for the estimation of the air-water interfacial area with the capillary bundle model. Subsequently, appropriate correction is necessary for the capillary bundle model to estimate the air-water interfacial area in soils. Since the soil-moisture release curve data is the basis of the capillary bundle model, the model can be of use due to its simplicity, while the gaseous tracer technique requires complicated experimental equipment followed by moment analysis of the breakthrough curves. The size distribution profile of the pores filled with gas estimated by the water retention curve was found to be similar to that of particle size at different size range. The shifted distribution of gas-filled pores toward smaller size side compared to the particle size distribution was also found.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2023년도 학술발표회
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• pp.32-32
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• 2023

Incidences of urban flood and extreme heat waves (due to the urban heat island effect) are expected to increase in New Zealand under future climate change (IPCC 2022; MfE 2020). Increasingly, the mitigation of such events will depend on the resilience of a range Nature-Based Solutions (NBS) used in Sustainable Urban Drainage Schemes (SUDS), or Water Sensitive Urban Design (WSUD) (Jamei and Tapper 2019; Johnson et al 2021). Understanding the impact of changing precipitation and temperature regimes due climate change is therefore critical to the long-term resilience of such urban infrastructure and design. Cuthbert et al (2022) have assessed the trade-offs between the water retention and cooling benefits of different urban greening methods (such as WSUD) relative to global location and climate. Using the Budyko water-energy balance framework (Budyko 1974), they demonstrated that the potential for water infiltration and storage (thus flood mitigation) was greater where potential evaporation is high relative to precipitation. Similarly, they found that the potential for mitigation of drought conditions was greater in cooler environments. Subsequently, Jaramillo et al. (2022) have illustrated the locations worldwide that will deviate from their current Budyko curve characteristic under climate change scenarios, as the relationship between actual evapotranspiration (AET) and potential evapotranspiration (PET) changes relative to precipitation. Using the above approach we assess the impact of future climate change on the urban water-energy balance in three contrasting New Zealand cities (Auckland, Wellington, Christchurch and Invercargill). The variation in Budyko curve characteristics is then used to describe expected changes in water storage and cooling potential in each urban area as a result of climate change. The implications of the results are then considered with respect to existing WSUD guidelines according to both the current and future climate in each location. It was concluded that calculation of Budyko curve deviation due to climate change could be calculated for any location and land-use type combination in New Zealand and could therefore be used to advance the general understanding of climate change impacts. Moreover, the approach could be used to better define the concept of urban infrastructure resilience and contribute to a better understanding of Budyko curve dynamics under climate change (questions raised by Berghuijs et al 2020)). Whilst this knowledge will assist in implementation of national climate change adaptation (MfE, 2022; UNEP, 2022) and improve climate resilience in urban areas in New Zealand, the approach could be repeated for any global location for which present and future mean precipitation and temperature conditions are known.

• 한국수자원학회논문집
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• 제47권1호
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• pp.83-93
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• 2014

기후변화 및 도시화 등의 요인으로 인하여 증가하는 불확실성에 대처하기 위하여 건설되는 홍수저류지 형태의 치수시설물이 기존의 치수시설물과 연계되어 치수능력을 극대화 할 수 있는 설계기준과 절차의 제시를 위하여 본 연구가 수행되었다. 본류의 홍수위 증가량에 대비할 수 있는 저류지용량결정, 저류지용량이 주어져 있을 경우의 본류의 홍수위 저감효과산정 등에 적용할 수 있는 다양한 시나리오 하에서의 분석을 위한 절차를 제시하였다. 기존 설계홍수량 산정절차에 근거한 IDQ (Intensity-Duration-Quantity) 분석을 이용하여 임의지속시간에서의 설계홍수수문곡선 산정기법을 제시하였고 그 활용사례를 제시하였다. IDQ 분석을 통해 산정한 강우량을 기반으로 등가첨두 수문곡선을 산정할 수 있으며, 기존 수문곡선과 동일한 지속시간 하에서 하천의 수위가 높아질 수 있는 저빈도 수문곡선과, 기존 수문곡선과 동일한 첨두홍수량을 지니지만 강우지속기간의 증가로 인해 유출체적이 증가하는 수문곡선, 기존 수문곡선에 비해 하천의 수위 및 수문곡선의 부피 모두 증가하는 수문곡선 등 다양한 형태의 수문곡선에 대한 시나리오해석을 가능하게 한다.