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Hydraulic-Thermal-Mechanical Properties and Radionuclide Release-Retarding Capacity of Kyungju Bentonite (경주 벤토나이트의 수리-열-역학적 특성 및 핵종 유출 저지능)

  • Jae-Owan Lee;Won-Jin Cho;Pil-Soo Hahn
    • Journal of Nuclear Fuel Cycle and Waste Technology(JNFCWT)
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    • v.2 no.2
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    • pp.87-96
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    • 2004
  • Studies were conducted to select the candidate buffer material for a high-level waste (HLW) repository in Korea. This paper presents the hydraulic properties, the swelling properties, the thermal properties, and the mechanical properties as well as the radionuclide release-retarding capacity of Kyungju bentonite as part of those studies. Experimental results showed that the hydraulic conductivities of the compacted bentonite were very low and less than $10^{-11}$m/s. The values decreased with increasing the dry density of the compacted bentonite. The swelling pressures were in the range of 0.66 MPa to 14.4 ㎫ and they increased with increasing the dry density. The thermal conductivities were in the range of 0.80 ㎉/m $h^{\circ}C$ to 1.52 ㎉/m $h^{\circ}C$. The unconfined compressive strength, Young's modulus and Poison's ratio showed the range of 0.55 ㎫ to 8.83 ㎫, 59 ㎫ to 1275 ㎫, and 0.05 to 0.20, respectively, when the dry densities of the compacted bentonite were 1.4 Ms/㎥ to 1.8 Mg/㎥. The diffusion coefficients in the compacted bentonite were measured under an oxidizing condition. The values were $1.7{\times}10^{-10}$m^2$/s to 3.4{\times}10^{-10}$m^2$/s for electrically neutral tritium (H-3), 8.6{\times}10^{-14}$m^2$/s to 1.3{\times}10^{-12}$m^2$/s for cations (Cs, Sr, Ni), 1.2{\times}10^{-11}$m^2$/s to 9.5{\times}10^{-11}$m^2$/s for anions (I, Tc), and 3.0{\times}10^{-14} $m^2$/s to 1.8{\times}10^{-13}$m^2$/s $for actinides (U, Am), when tile dry densities were in the range of 1.2 Mg/㎥ to 1.8 Mg/㎥. The obtained results will be used in assessing the barrier properties of Kyungju bentonite as a buffer material of a repository in Korea.n Korea.

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Morphological Characteristics of Four Species in the Genus Skeletonema in Coastal Waters of South Korea

  • Jung, Seung-Won;Yun, Suk-Min;Lee, Sang-Deuk;Kim, Young-Ok;Lee, Jin-Hwan
    • ALGAE
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    • v.24 no.4
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    • pp.195-203
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    • 2009
  • Most Skeletonema species have been identified under the name of S. costatum. To assess the morphological species diversity in the genus Skeletonema, we surveyed the nine localities in the coastal waters of South Korea. The light microscopy (LM) and scanning electron microscopy (SEM) observations in this study showed that ultrastructural features of genus Skeletonema discriminated among four species: S. dohrnii Sarno & Kooistra, S. marinoi Sarno & Zingone, S. subsalsum (Cleve) Bethge, and S. tropicum Cleve. In S. dohrnii, cell diameters were 3-6 ${\mu}m$ and the pervalvar axes were 13-19 ${\mu}m$. One or two partial chloroplasts were visible in a cell. Cells of S. marinoi were 4-10 ${\mu}m$ and the pervalvar axes were 8-18 ${\mu}m$. Each cell contained one chloroplast. Cells of S. subsalsum which contained 1-2 chloroplasts were 8-13 ${\mu}m$ and the pervalvar axes were 11-20 ${\mu}m$. Cells of S. tropicum were 10-18 ${\mu}m$ and the pervalvar axes were 4-9 ${\mu}m$. 2-4 chloroplasts were seen in each cell. Tip width of fultoportula in S. dohrnii and S. marioni was flared and flat, but that in S. subsalsum and S. tropicum was narrow. Morphological groups among them, S. dohrnii and S. marinoi were the most widely distributed in all seasons, while S. tropicum was only occurred in a summer season.

Analysis of suppling instream flow in Imgo reservior under RCP 8.5 (RCP 8.5 시나리오에 의한 임고 저수지의 하천유지유량 공급량 분석)

  • Lee, Jae Nam;Noh, Jae Kyoung
    • Proceedings of the Korea Water Resources Association Conference
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    • 2015.05a
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    • pp.632-632
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    • 2015
  • 기후변화로 정상적인 물 순환 체계가 변화되면서, 건천화로 하천의 정상정인 기능이 어렵게 될 것이다. 농업용 저수지의 둑 높이기 사업으로 수자원의 저류공간이 증가되었고, 확보된 수자원을 기후변화에 대응해 하천유지유량으로 활용 할 수 있게 되었다. 본 연구에서는 기후변화 시나리오 RCP 8.5를 기반으로 임고 저수지의 둑 높이기 사업 전과 후의 공급 가능한 하천유지유량을 평가하였다. 하천유지유량의 공급은 일별 일정량을 공급하도록 하여 이수안전도 90%를 만족하도록 설정하였고, 상시공급과 갈수시 공급으로 구분하여 분석한 결과는 다음과 같다. 첫째, 둑 높이기 사업 전에 하천유지유량의 공급 없이 용수공급 능력을 분석한 결과, 2025s기간, 2055s기간, 2085s기간의 이수안전도는 각각 100%, 93.3%, 96.7%로 분석되어 농업용수의 공급 능력은 충분한 것으로 분석되었다. 둘째, 미래 2025s기간, 2055s기간, 2085s기간에 대하여 둑 높이기 사업 전, 농업용수 공급과 함께 하천유지유량을 상시 공급하였을 경우에는 각각 일별로 3.7천$m^3$, 1천$m^3$, 1.2천$m^3$ 공급 가능하였고, 갈수시만 공급 하였을 경우에는 각각 일별로 7천$m^3$, 2.2천$m^3$, 3.5천$m^3$ 공급 가능한 것으로 분석되었다. 셋째, 미래 2025s기간, 2055s기간, 2085s기간에 대하여 둑 높이기 사업 후, 농업용수 공급과 함께 하천유지유량을 상시 공급하였을 경우에는 각각 일별로 10.5천$m^3$, 4.5천$m^3$, 7천$m^3$ 공급 가능하였고, 갈수시만 공급 하였을 경우에는 각각 일별로 16.6천$m^3$, 7천$m^3$, 12.2천$m^3$ 공급 가능한 것으로 분석되었다. 결론하여 농업용수 공급능력이 충분한 임고 저수지는 둑높이기 사업 후 확보된 수자원을 하천 유지유량으로 공급하면, 증고사업 전보다 상시공급일 경우에 2.8-5.8배, 갈수시 공급일 경우에 2.4-3.4배 많은 양을 공급 할 수 있는 것으로 나타났다.

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Simulating Inflow to Busa Estuary Reservoir Considered Outflows from Boryeong Dam (보령호 방류량을 고려한 부사호 유입량 모의)

  • Noh, Jae-Kyoung;Lee, Jae-Nam
    • Proceedings of the Korea Water Resources Association Conference
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    • 2012.05a
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    • pp.368-368
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    • 2012
  • 부사호는 당초 유역면적이 $288km^2$로 이 중에서 상류 유역에 건설된 보령댐 유역면적 $163.6km^2$(57%)가 제외됨에 따라 부사호로 유입량이 급격히 줄어들어 약간의 가뭄에도 수질악화가 반복되고 있다. 부사호의 합리적인 용수 수급 관리를 위해 정확한 부사호 유입량의 추정은 절실하다. 부사호 유입량은 보령호 방류량과 부사호 지류 유역 유입량으로 구성되며, 보령호 방류량은 소수력 발전용수, 관개용수, 하천유지용수, 홍수조절 방류량, 월류량으로 구성된다. 부사호 지류 유역으로부터 자연유량에서 하천에서 취수한 공업용수를 공급하고, 웅천읍의 생활용수 $1,164m^3$/일로부터 회귀수가 유입되고, 보령댐 수혜답 1039.5 ha에 관개용수를 공급하고 회귀수가 유입되고, 부사호에서 양수하여 공급한 부사 유역 수혜답 1,141 ha의 회귀수가 유입되고, 6개 저수지 수혜답 396.5 ha의 회귀수가 유입되는 등 지류 유입량의 구성은 매우 복잡하다. 하천에서 취수하여 공급하는 공업용수는 서해화력 5천 $m^3$/일, 보령화력 15천 $m^3$/일로 구성된다. ONE (One parameter New Exponential) 모형을 근간으로 유입량 모형을 구성하였고, 보령댐 자료로 매개변수를 결정하여, 1966~2011년의 부사호 일 유입량을 모의한 결과를 요약하면 다음과 같다. 첫째, 유역면적 $124.4km^2$인 부사호의 지류 유입량과 보령댐 방류량을 고려한 부사호 유입량 자료로부터 유황을 분석한 결과는 연평균하여 풍수량은 2.1 mm/d, $3.083m^3/s$, 평수량은 0.89mm/d, $1.280m^3/s$, 저수량은 0.48 mm/d, $0.695m^3/s$, 갈수량은 0.30 mm/d, $0.428m^3/s$였으며, 연 유입량은 127.23백만 $m^3$에 이르렀다. 둘째, 유역면적 $288km^2$인 보령호 유역의 포함한 부사호의 자연 유입량 자료로부터 즉 보령댐이 없는 경우 유황을 분석한 결과는 연평균하여 풍수량은 1.4 mm/d, $4.599m^3/s$, 평수량은 0.51 mm/d, $1.689m^3/s$, 저수량은 0.20 mm/d, $0.664m^3/s$, 갈수량은 0.06 mm/d, $0.204m^3/s$, 연 유입량은 197.00백만 $m^3$에 이르렀다. 셋째, 보령호가 있는 경우와 없는 경우 유황을 비교하면 있는 경우에서 부사호의 유입량은 고수위의 유량은 감소하고, 저수위의 유량은 증가하는 전형적 상류에 위치한 댐의 저류효과 영향을 여실히 나타내고 있었다. 넷째, 한국하천 유황곡선식에 의한 유역면적 $288km^2$인 부사호 유입량의 풍수량은 1.29 mm/d, $4.292m^3/s$, 평수량은 0.59 mm/d, $1.964m^3/s$, 저수량은 0.33 mm/d, $1.093m^3/s$, 갈수량은 0.13mm/d, $0.424m^3$이르렀다. 결론하면, 보령댐이 있는 경우 연 유입량은 70백만 $m^3$ 감소하였으나, 평갈수기 유입량은 증가하였다.

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An Algorithm for S-to-M Mapping in CMAC (CMAC의 S-to-M 변환을 위한 알고리즘)

  • Gwon, Seong-Gyu
    • Transactions of the Korean Society of Mechanical Engineers A
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    • v.20 no.10
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    • pp.3135-3141
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    • 1996
  • In order to develop an efficient algorithm for S-to-M mapping in CMCA, characteristics of CMCA mappings is studied and conceptual mapping procedure is physically described. Then, careful observations on the mapping procedure and experience reveal a simple algorithm of the S-to-M mapping. The algorithm is described and compared with other procedures for S-to-M mapping. It is found very efficient in terms of computational operations and processing time.

Measurement of the Movement Speed and Density of People on a Building Corridor (건물 복도에서의 밀도와 이동속도 측정)

  • Kim, Woon Hyung;Lee, Gyu Hong;Kim, Jong Hoon
    • Fire Science and Engineering
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    • v.31 no.1
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    • pp.36-41
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    • 2017
  • In this study, the experimental measurements from a one-way moving experiment showed that the average movement speed was 0.55 m/s with an average crowd density of $2.36P/m^2$ in a corridor. The cCalculation result of the correlations between the crowd density and movement speed from the SFPE Handbook showed an average of 0.53 m/s. The difference between the calculation and experiment was 0.02 m/s. A comparison of each data set showed that the maximum difference was 0.38 m/s. Some experimental results showed that the crowd density increased with increasing movement speed and the average data from the entire experiment time was used for the analysis. When the short time interval for frame by frame analysis for video files was conducted, the experimental data was expected to be more reliable.

Structural Analysis of Multipurpose Fishway in Chuksan River (척산천의 다기능 어도의 구조 해석)

  • Lee, Young Jae;Lee, Jung Shin;Kim, Mun Gi;Park, Sung Sik;Jang, Hyeong Kyu
    • Journal of The Korean Society of Agricultural Engineers
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    • v.59 no.1
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    • pp.97-107
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    • 2017
  • In this study, the validity and applicability of the multipurpose fishway which has been constructed for the upstream migration of fish at Chuksan river in Uljin is assessed and analyzed by a commercial software. The upper slab types of fishway in this investigation are reinforced concrete slab (S1 type) and reinforced concrete slab with steel plate (S2 type). The three different sizes of subway passage ($0.8m{\times}0.1m$, $0.8m{\times}0.2m$, $0.8 m{\times}0.3m$) and velocities (0.6 m/s, 1.2 m/s, 1.8 m/s) of Chuksan fishway was investigated and compared for the Chuksan in government design code. The analysis showed that the maximum stress and bending moment of S1 type decreased 1~21 % and 12~27 % compared to the Chuksan in government design code, respectively. Also, the maximum stress of and bending moment of S2 type decreased 11~32 % and 27~39 %. From the numerical analysis, it was found that the S2 type was greatly effective and the subway passage size of $0.8m{\times}0.2m$ was most safe. This result can be utilized to be the basic data for design of the Multipurpose fishway.

Analysis on the Effects of the Heat Loss Coefficient on the Operation Time of Sprinkler in Compartment Fire (구획 화재에서 스프링클러 열 손실계수 변화에 따른 작동 시간 분석)

  • You, Woo Jun
    • Fire Science and Engineering
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    • v.32 no.5
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    • pp.34-39
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    • 2018
  • In this study, the experiment conditions for the variation of heat release rate in compartment space were constructed to analyze the effects of fire spread and the operation time of sprinkler in accordance with the heat loss of the sprinkler's heat element. The compartment composed of fire board (width = 0.3 m, height = 0.5 m, length = 3.0 m), are manufactured to measure the temperature distributions in the inner space, the mass loss rate and heat release rate during the experiment of N-heptane pool fire test. Also, the operation time of sprinkler is analyzed with the installation of sprinkler and C-factor using Fire Dynamics Simulator Ver.6 under the experiment conditions. The results show that the operation time of sprinkler, which has RTI $100(m{\cdot}s)^{0.5}$ operating temperature $70^{\circ}C$, is 30 s~60 s for C-factor = 0 and 1, 62 s~92 s for C-factor = 3, and 120 s over for C-factor = 5, respectively.

Security Analysis on GFN with Secret S-box (비밀 S-box를 사용한 GFN에 대한 안전성 분석)

  • Lee, Yongseong;Kang, HyungChul;Hong, Deukjo;Sung, Jaechul;Hong, Seokhie
    • Journal of the Korea Institute of Information Security & Cryptology
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    • v.27 no.3
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    • pp.467-476
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    • 2017
  • In this paper, we analyze Generalized Feistel Network(GFN) Type I, Type II, Type III that round function use SP update function, secret S-box and $k{\times}k$ MDS matirx. In this case an attacker has no advantage about S-box. For each type of GFN, we analyze and restore secret S-box in 9, 6, 6 round using the basis of integral cryptanalysis with chosen plaintext attack. Also we restore secret S-box in 16 round of GFN Type I with chosen ciphertext attack. In conclusion, we need $2^{2m}$ data complexity and ${\frac{2^{3m}}{32k}},{\frac{2^{3m}}{24k}},{\frac{2^{3m}}{36k}}$ time complexity to restore m bit secret S-box in GFN Type I, Type II, Type III.

Geophysical Study on the Ultramafic Rocks of Chungnam Province, Korea: Characteristics of Seismic Velocity (충남지역 초염기성 암체의 지구물리학적 연구: 탄성파 속도 특성)

  • Suh, Man-Cheol;Woo, Young-Kyun;Song, Suck-Hwan;Tianyao, Hao
    • Journal of the Korean earth science society
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    • v.21 no.3
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    • pp.349-358
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    • 2000
  • Compressional and shear wave velocities (Vp and Vs) and densities have been measured for serpentinite, amphibolite, amphibole and biotite schist, and gneiss from western part of Chungnam Province at room temperature. Ranges of the density are 2.6${\sim}$2.86g/cm$^3$ for serpentinite, 2.25${\sim}$2.81g/cm$^3$ for talc, and 2.74${\sim}$3.07g/cm$^3$ for metamorphic rocks. Of these rocks, talc shows wider ranges than serpentinite and amphibolites due to its metamorphic process from serpentinite. Values of Vp and Vs are 5719${\sim}$6062m/s and 2898${\sim}$3351m/s for serpentinites, 4019${\sim}$5478m/s and 2241/${\sim}$2976m/s for talc, 5375${\sim}$6372m/s and 3042${\sim}$3625m/s for amphibolite, 5290${\sim}$5499m/s and 2968${\sim}$3137m/s for schist, and 4788m/s and 2804m/s for gneiss, respectively. Velocity of P wave increases 1.47 times faster than S wave with increase of density. The results of seismic velocity measurement show anisotropy, higher velocity across than along the schistocity of rocks, especially in metamorphic rocks. This fact indicates that there were regional metamorphism related with tectonic forces. Values of seismic velocity increase with increasing pressure from 20 MPa to 70 MPa, especially in metamorphic rocks. Overall recalculated Vp and Vs values suggest that the serpentinite indicates for upper mantle in the respects of seismic characteristics, in spite of high degree of serpentinization. In addition, those of the amphibolite do for low crust, and gneiss and schist for upper crust.

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