• Title/Summary/Keyword: 포화-불포화 흐름

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Acidogenesis of Lipids-Containing Wastewater in Anaerobic Sequencing Batch Reactor (혐기성 연속 회분식 반응조를 이용한 지질 함유 폐수의 산발효 특성)

  • Kim, Sang-Hyoun;Shin, Hang-Sik
    • Journal of Korean Society of Environmental Engineers
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    • v.31 no.12
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    • pp.1075-1080
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    • 2009
  • The partial lipid degradation with the saturation of double-bond at the acidogenesis stage is known to help subsequent methanogenesis during anaerobic digestion. Acidogenic reactions in an anaerobic sequencing batch reactor (ASBR) and a continuously stirred tank reactor (CSTR) were carried out to compare their performances. A mixture of two unsaturated (oleate and linoleate) and two saturated (palmitate and stearate) long-chain fatty acids (LCFAs) was used as a model substrate. Biomass retention in the ASBR contributed to the enhanced performance at hydraulic retention time (HRT) below 15 hr. Biomass retention in the ASBR contributed to the enhanced performance compared to CSTR even at shorter HRT. ASBR would be a proper reactor configuration for the acidogenesis of lipid-containing wastewater.

The water cycle analysis of Kyeongancheon-watershed by using GSSHA (GSSHA 모형을 이용한 경안천 유역의 물순환 해석)

  • Jang Cheol Hee;Kim Hyeon Jun;Noh Seong Jin;Kim Chul Gyum
    • Proceedings of the Korea Water Resources Association Conference
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    • 2005.05b
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    • pp.75-79
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    • 2005
  • GSSHA(Gridded Surface Subsurface Hydrologic Analysis) 모형은 미 공병단 연구개발센터(USACE ERDC; US Army Corps of Engineers Engineering Research and Development Center)체서 개발된 물리적인 개념의 공간 분포형(PBSD; Physically Based Spatially Distributed) 수문모형으로, CASC2D 모형(Ogden 와 Julien, 2002; Downer 등, 2002)을 개선, 확장한 모형이다. GSSHA 모형의 실행에는 Brigham Young 대학의 컴퓨터그래픽공학연구실에 의해 개발된 미 국방성 WMS(Watershed Modeling System) 인터페이스를 사용하며, 이를 통해 많은 입력과 출력조건을 가지는 분포형 모형의 복잡한 모의 과정을 효과적으로 처리할 수 있다. 본 연구에서는 GSSHA 모형을 이용하여 경안천 유역의 물순환 양상을 분석하였다. GSSHA 모형은 유역을 균일한 유한 차분 격자로 나누어 각각의 격자를 기본 단위로 모의한다. 모형의 주요 모의 모듈은 강우 분포, 융설, 차단, 침투, 증발산, 지표면 저류, 2차원 표면류 추적, 1차원 하도 추적, 불포화 층 모의, 2차원 포화 지하 대수층 흐름, 지표면 유사 침식, 하천 유사 추적 등이 포함된다.

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Modeling saturated-unsaturated moisture flow in soils (포화층및 불포화층에 대한 토양수분흐름의 모델링)

  • 정상옥
    • Proceedings of the Korea Water Resources Association Conference
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    • 1988.07a
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    • pp.85-92
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    • 1988
  • A model for the transient one-dimensional moisture movement in the saturated-unsaturated zone using a finite difference method is developed. Hysteresis in the soil water retention is incorporated. The model considers layered geologic formations. Monte Carlo simulation, together with the nearest neighbor model is used. Outputs of the model include pressure head, water content, and the water table elevation. Two Monte Carlo simulations of 100 realizations each are made for a 12-day simulation period with different input values. The simulation results show that the S.D. of the outputs increases with an increase in the input, the S.D. of the log K$$. The model is applied to predict a long term water table fluctuation, and the predicted water table agress well with the observed one.

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Estimation of Seepage Rate through Core Zone of Rockfill Dam (중심코어형 사력댐의 코어죤 침투량 예측기법)

  • Lee, Jong-Wook;Lim, Heui-Dae
    • Journal of the Korean Geotechnical Society
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    • v.26 no.4
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    • pp.47-58
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    • 2010
  • Seepage rate through the core zone of rockfill dam, estimated from graphical technique and the equation by Sakamoto (1998), is different from the real condition because of neglecting unsaturated flow. With existing method to estimate total seepage rate, it is difficult to understand the tendency of total seepage rate changes by reservoir water level change. Steady state seepage rate and the factors affecting the time needed to attain to changes of reservoir water level and saturated hydraulic conductivity and unsaturated hydraulic properties of core material are analysed thorough the 2-D steady and unsteady state seepage analyses of Soyanggang dam. Numerical results revealed that the seepage rate can be expressed by the linear equation form and the value of unsaturated soil parameter n is the most important factor affecting the seepage rate and the time needed to attain steady state. The estimation method presented in this study can be used by the designer and the personnel of dam safety for convenient estimation of seepage rate and quantitative analysis of measured seepage rate without 2-D and 3-D numerical analyses.

Experimental Study on the Hysteresis of Suction Stress in Unsaturated Sand (불포화 모래의 흡입응력 이력현상에 대한 실험적 연구)

  • Song, Young-Suk;Choi, Jin-Su;Kim, Gyo-Won
    • The Journal of Engineering Geology
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    • v.22 no.2
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    • pp.145-155
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    • 2012
  • The matric suction and volumetric water content of Jumunin standard sand with a relative density of 60% were measured using an Automated Soil-Water Characteristic Curve (SWCC) apparatus during both drying and wetting processes. The test time for the drying process was longer than that for the wetting process, because the flow of water is likely to be protected by air trapped in voids within the soils during the drying process. Based on the matric suction and volumetric water content, the SWCC was estimated using the model proposed by van Genuchten (1980). For the drying process, the unsaturated fitting parameters ${\alpha}$, n, and m were 0.399, 8.586, and 0.884, respectively; for the wetting process, the values were 0.548, 5.625, and 8.220, respectively. The hysteresis phenomenon occurred in the SWCCs, which means the SWCC of the drying process is not matched with the SWCC of the wetting process. Using these unsaturated parameters, we estimated the Suction Stress Characteristic Curve (SSCC), based on the relationship between suction stress and the effective degree of saturation. The suction stress showed a rapid decrease when the matric suction exceeds the Air Entry Value (AEV). Therefore, the effective stress of unsaturated soils is different from that of saturated soils when the matric suction exceeds the AEV. The suction stress of the drying process exceeds that of the wetting process for a given effective degree of saturation. The hysteresis phenomenon was also recognized in SSCCs. The hysteresis phenomenon of SSCCs arises from that of SWCCs, which is induced by the ink bottle effect and the contact angle effect. In the case of a sandy slope, the suction stress is positive and acts to enhance the slope stability as the water infiltrates the ground, but is negative when the suction stress exceeds the AEV. The results obtained for the wetting process should be applied in analyses of slope stability, because the process of water infiltration into ground is similar to the wetting process.

Experimental Study on the Effect of Degree of Saturation on the Electrical Conductivity of Soils (포화도에 따른 흙의 전기전도도 변화에 대한 실험적 연구)

  • Ko, Hyojung;Choo, Hyunwook
    • Journal of the Korean Geotechnical Society
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    • v.39 no.8
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    • pp.29-39
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    • 2023
  • The degree of saturation determines the connectivity of void space and the particle surface. Thus, it greatly affects the electrical conductivity of soils. This study aimed to analyze the electrical conductivities of coarse grains with a high relevance of pore water conduction and fine grains with a high relevance of surface conduction based on the degree of saturation. It also aimed to express the electrical conductivity of unsaturated soils as a combination of surface and pore water conductions using the modified Archie's equation. Samples were prepared in a plastic cell equipped with four electrodes, and the electrical conductivity was measured based on the porosity at various degrees of saturation (40%~100%). The results demonstrate that Archie's equation can be used to express the electrical conductivity of coarse grains, with a saturation exponent of ~1.93 regardless of the pore water conductivity. However, the saturation exponent of fine grains varied considerably with pore water concentration. This variation can be attributed to the relative magnitude of surface conduction with respect to the electrical conductivity of soils at different pore water concentrations. Thus, the degree of saturation has varying effects on pore water conduction and surface conduction. Therefore, different saturation exponents must be used for pore water conduction and surface conduction to predict the electrical conductivity of unsaturated soils using the modified Archie's equation.

Comparison between the Spatially Integrated Model and the Spatially Distributed Model in the Nonpoint Source Contaminants of Groundwater (지하수 분산오염원에 대한 공간적분모형과 공간분포모형의 비교)

  • Lee, Do-Hun;Lee, Eun-Tae;Jeong, Sang-Man
    • Journal of Korea Water Resources Association
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    • v.31 no.2
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    • pp.177-187
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    • 1998
  • The spatially integrated model (SIM) which can evaluate temporal variation of groundwater quality is proposed in the stream-aquifer setting entered by nonpoint source contaminants. And the developed SIM included unsaturated soil zone and was tested against the spatially distributed model (SDM) of the coupled advection-dispersion and Richards equations for the various hydrologic and aquifer simulating conditions. The result of the comparison showed that the average concentration responses of saturated aquifer and groundwater outflow between the SIM and the SDM was in good agreement, except for the case of the large dispersivity ratio and thick aquifer system. And it is shown that for the cases of the large dispersivity ratio and thick aquifer system the performance of the nonlinear SIM is better than that of the linear SIM for evaluating the average concentration of groundwater outflow response.

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Analysis of Levee Infiltration in Flood-time (홍수시 제방의 침투 해석에 대한 연구)

  • Lee, Nam-Joo;Yu, Kwon-Kyu;Lee, Sang-Ho
    • Proceedings of the Korea Water Resources Association Conference
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    • 2010.05a
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    • pp.1878-1882
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    • 2010
  • 이 연구는 제방의 침투 수리모형 실험의 자료를 이용해 안전도 평가 지표 선정을 위한 자료 제공하고 향후 수행할 침투 수치모의에 필요한 보정 및 검증 자료를 확보할 목적으로 수행하였다. 제방 축조 현장에서 구한 제체재료를 사용하여 실험실에 제방축소모형을 $14.5m{\times}0.6m{\times}1.6 m$의 수조 내부에 제작하였다. 제방 사면의 경사는 1:2, 제방 저면의 길이는 4.60 m, 제방 상부의 길이는 2.40 m, 제체의 높이는 0.55 m로 제작하였다. 모형제방은 제방축조 방법과 유사하게 다짐을 하기위해 흙을 쌓으면서 0.20 m 높이 마다 다짐을 실시하였다. 다짐방법은 고무망치를 이용한 층다짐을 하였다. 들밀도실험에 의한 제방모형의 건조단위중량과 다짐도는 각각 1.71g/cm3, 93%로 측정되었다. 홍수위 증가에 따른 비정상 상태의 침투수위 측정을 수행하였다. 수리모형실험은 약 8일 동안 수행하였다. 침윤선의 수두와 위압계별 수두는 상류쪽(제외지 사면)부터 증가하기 시작하며 하류쪽(제내지 사면)로 확장됨을 알 수 있으며, 실험 초기에는 상류쪽의 수두가 급격히 상승하지만, 점차 상승속도가 둔화되는 등의 일반적인 경향이 나타나고 있음을 확인할 수 있다. 실험시작 18시간 경과 후부터 제외지 사면 하단부에서 유출이 발생하였으며, 21시간 경과 후부터는 상류부의 수두가 안정되는 현상이 나타났다. 측정된 침투수위의 변화 양상은 향후 수치모형을 이용한 침투해석의 검보정 자료로 활용할 계획이다.

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Evaluation of Soil-Water Characteristic Curve for Domestic Bentonite Buffer (국내 벤토나이트 완충재의 함수특성곡선 평가)

  • Yoon, Seok;Jeon, Jun-Seo;Lee, Changsoo;Cho, Won-Jin;Lee, Seung-Rae;Kim, Geon-Young
    • Journal of Nuclear Fuel Cycle and Waste Technology(JNFCWT)
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    • v.17 no.1
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    • pp.29-36
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    • 2019
  • High-level radioactive waste (HLW) such as spent fuel is inevitably produced when nuclear power plants are operated. A geological repository has been considered as one of the most adequate options for the disposal of HLW, and it will be constructed in host rock at a depth of 500~1,000 meters below ground level with the concept of an engineered barrier system (EBS) and a natural barrier system. The compacted bentonite buffer is one of the most important components of the EBS. As the compacted bentonite buffer is located between disposal canisters with spent fuel and the host rock, it can restrain the release of radionuclides and protect canisters from the inflow of groundwater. Because of inflow of groundwater into the compacted bentonite buffer, it is essential to investigate soil-water characteristic curves (SWCC) of the compacted bentonite buffer in order to evaluate the entire safety performance of the EBS. Therefore, this paper conducted laboratory experiments to analyze the SWCC for a Korean Ca-type compacted bentonite buffer considering dry density, confined or unconfined condition, and drying or wetting path. There was no significant difference of SWCC considering dry density under unconfined condition. Furthermore, it was found that there was higher water suction in unconfined condition that in confined condition, and higher water suction during drying path than during wetting path.

Simulation for application of pumping-and-treatment system to the recovery of non-aqueous phase liquids (NAPLs) at and below the water table (토양의 포화지대에 분포하는 고밀도비수상액체(DNAPL)와 저밀도비수상액체(LNAPL)의 펌핑 제거공정에 대한 모사)

  • 김주형;이종협
    • Journal of Korea Soil Environment Society
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    • v.2 no.1
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    • pp.51-61
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    • 1997
  • The objective of this study is to evaluate the feasibility of Pumping-and-Treatment system (PTS) for remediation of the saturated zones contaminated with NAPLs. A simulation is carried out for the removal of DNAPLs (denser-than-water non-aqueous phase liquids) and LNAPLS (lighter-than-water non-aqueous phase liquids) distributing at and below the water table. In the study, LNAPL and DNAPL are assumed to be n-hexane and 1,1-dichloroacetone, respectively. The model system studied consists of four heterogeneous soil layers with different permeabilities. Groundwater flows through the bottom layer and a pumping well is located under the initial water table. The time-driven deformation of the water table and removal efficiency of contaminants are estimated after vacuum application to the inlet of the well. In the calculation, FVM (Finite Volumetric Method) with SIMPLEC algorithm is applied. Results show that removal efficiencies of both DNAPL and LNAPL are negligible for the first 5 days after the PTS operation. However, when the cone-shape water table is formed around the inlet of the pumping well, the rapid removal rate is obtained since NAPLs migrate rapidly through the curvature of the water table. The removal efficiency of DNAPL is estimated to be higher than that of LNAPL due to the gravity. The results also show that the fluctuation or cone-shaped depression of the water table enhances the removal efficiency of NAPLs in saturated zones. The simulation results could provide a basis of the PTS design for the removal of NAPLs in saturated zones.

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