• 한국수자원학회논문집
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• 제57권5호
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• pp.347-357
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• 2024

많은 연구에서 비점착성 부유사의 입경분포를 평균입경와 표준편차를 이용해 묘사한다. 그러나 부유사는 크기가 다른 많은 입자의 혼합물로 구성되어 있다. 난류조건에서 부유사의 이동은 크기와 밀도로부터 계산된 침강속도에 영향을 받는다. 따라서 비점착성 부유사의 이동을 이해하려면 입경 분포를 보다 정량적으로 고려하는 것이 중요하다. 본 연구의 목적은 난류조건에서 부유사의 입경분포를 모의할 수 있는 간편한 모형화 방법을 제시하는 것이다. 점착성 유사와 비점착성 유사의 차이에 대한 이해를 바탕으로, 점착성 부유사를 위한 추계학적 응집 모형을 비점착성 유사의 입경분포 모의에 적합하도록 수정하였다. 본 연구에서 제안하는 간편법의 적용성을 살펴보기 위해 선행연구의 실험자료에 적용하여 모의 결과와 비교하였다. 수치 모의의 결과를 통해 본 연구에서 제안한 모형이 실험값에서 나타나는 주요한 특성을 모사할 수 있다는 점을 확인하였다. 이를 바탕으로 유사 이동 모형을 사용하여 부유사 입경분포를 모의하는 접근 방식이 부유사 입경분포의 중요한 특성을 이해하기에 효과적이라는 결론을 얻었다.

• 한국농공학회논문집
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• 제53권6호
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• pp.43-50
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• 2011

The fractal method has recently been applied to a model for determining soil grain size distribution. The objective of this study is to review the applicability of the fractal method for a analysis of submarine sedimentary environments by comparing fractal constants with grain size statistical analysis for the soil samples of Pohang (PH) and Namhae (NH). The y-interception of log (grain size)-log (passing) equation was also used because grain size distribution couldn't be expressed with fractal dimension only. The result of comparison between fractal constants (dimension, y-interception) and grain size statistical indices, the fractal dimension was directly proportional to the mean and the sorting. And the y-interception showed high correlation with the mean. The fractal dimension and y-interception didn't show significant correlation with the skewness and the kurtosis. Thus regression equations between fractal constants and two statistical indices (mean, sorting) were derived. All classifications of the mean and the sorting could be determined using the regression equation based on the fractal dimension and y-interception. Therefore, fractal constants could be used as an alternative index representing the sedimentary environments instead of the mean and sorting.

• 한국소성가공학회:학술대회논문집
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• 한국소성가공학회 1995년도 제2회 단조심포지엄 단조기술의 진보
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• pp.100-123
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• 1995

The relationship between plastic deformation and crystal grain change in warm forging processes of SM100 carbon steel is studied. If the carbon steel is deformed in warm forging temperature (about recrystallization range), the crystal grain and cementite of the internal part are changed, so material properties are changed. Some experimental values, such as the elliptic degree of cementite, the grain size of cementitie and ferrite grain size, are investigated. When the plastic deformation proceeds, the elliptic degree of cementite becomes large, the grain size of cementite particle is small, and the size of ferrite grain appears fine by recrystallization. The elliptic degree of cementite has a considerable effect on formability. The distribution of effective strain in the forging is calculated by the rigid visco-plastic FEM analysis. The effective strain distribution obtained from the FEM simulation is compared with the experimental result. At effective strain 0.3 dynamic recovery and dynamic recrystallization begin, over 2.5 the organization of material has better quality that is suitable for the following cold forming.

• 한국세라믹학회지
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• 제36권8호
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• pp.782-790
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• 1999

The compressibility sinterability sintering behaviour and thermal stability of AlOOH added UO2 pellt and PVA-Al(III) complex added UO2 pellet were investigated respectively. Compared with characteristics of AlOOH added UO2 pellet the green density and the sintered density of PVA-Al(III) complex added UO2 pellet were lowered but the grain size and the pore size of that were more increased in accordance with higher compacting pressure. The AlOOH added UO2 pellet had the grain size of about 14${\mu}{\textrm}{m}$ with monomodal pore size distribution while the PVA-Al(III) complex added UO2 pellet had the grain size of about 42 ${\mu}{\textrm}{m}$ with bimodal pore size distribution. The PVA-A(III) complex added UO2 pellet had a similiar open porosity to the AlOOH added UO2 pellet and a lower resintered density change than the AlOOH added UO2 pellet.

• 대한금속재료학회지
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• 제48권9호
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• pp.847-855
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• 2010

The grain size of a cross-section of $8{\mu}m$-thick copper film was determined by electron backscatter diffraction analysis. Grain size distribution histogram showed the presence of a large fraction of small-sized grains, and the mean grain size was significantly affected by handling of them. A cut-off grain size, below which all grains are ignored as noise and eliminated for the calculation of the mean value, should be three or four times as large as the step size. Due to the presence of small grains, the linear intercept method derived larger mean grain size, which depends less sensitively on the cut-off grain size than the equivalent circle diameter method.

• 한국해안·해양공학회논문집
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• 제35권6호
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• pp.164-172
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• 2023

백사장 모래의 입도분포는 해빈의 침식과 퇴적을 파악하는 데 중요한 정보를 제공한다. 모래의 입도분포 분석에 보편적으로 사용되는 체가름시험은 분석 시간이 길고 개별 입자의 형상과 색에 대한 정보를 얻을 수 없다는 한계점이 있다. 본 연구에서는 체가름시험법 보다 측정 과정이 간편하고 효율적인 스마트폰 디지털 이미지를 이용한 입도분포 분석 방법을 제안하였다. 이미지 분석 과정 중 이미지 기울기(Image Gradient) 계산을 통한 입자 경계 추출로 해상도가 상대적으로 낮은 스마트폰 디지털 이미지의 배경으로부터 입자를 효과적으로 검출하였다. 경상북도 4곳의 해수욕장에서 채취한 시료를 이용해 본 연구에서 제안한 경계 추출 이미지 분석법과 경계를 추출하지 않는 분석법을 각각 체가름시험 결과와 비교 검증하였을 때, 본 연구에서 제안한 방식은 D₅₀에서 평균 8.21%의 평균 오차율을 보여 경계를 추출하지 않는 분석법 보다 65% 낮은 오차를 보였다. 따라서 스마트폰 디지털 이미지를 이용한 입도분포 분석은 간편하고 효율적이며 체가름시험에 준하는 정확성을 가짐을 확인하였다.

• 한국지반공학회논문집
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• 제29권7호
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• pp.47-55
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• 2013

조립재료의 요소시험에서 장비에 허용되는 조립재료의 입자크기가 실제 현장에서 사용되는 입자크기에 비해 작은 경우가 종종 발생하기 때문에, 이러한 경우에는 시험에 사용되는 재료의 최대입경을 시험장치의 가용 크기까지 축소시켜 시험을 수행하게 된다. 본 연구에서는 이처럼 최대입경 크기를 축소시켜 입도를 조정했을 때, 저변형률에서의 탄성계수에 미치는 영향을 평가하기 위해 대형반복삼축압축시험을 수행하였다. 본 연구 대상재료의 시험 결과, 입도 조정된 시편들은 원입도 시편의 탄성계수를 과소평가하는 경향이 있었으며, 그 차이는 저변형률에서 더 크게 발생되었다.

• 한국세라믹학회지
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• 제32권6호
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• pp.653-658
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• 1995

Directional effect of applied pressure during sintering on the microstructure and fracture toughness of the heat-treated silicon nitride ceramics has been investigated. The specimens with a composition of 92Si3N4-8Y2O3(in wt%) were sintered at 172$0^{\circ}C$ by a hot press (HP ) and a hot isostatic press (HIP) and heat-treated for grain growth at 1800~20$0^{\circ}C$. The fracture toughness of the HP samples increased with the grain size while the fracture toughness of the HIP treated samples remained the same even though the grain growth occurred. This discrepancy was explained by a bimodal grain size distribution and large aspect ratio of the HPed samples and a monomodal grain size distributjion and samll aspect ratio of the HIP treated samples.

• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 2002년도 하계학술대회 논문집
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• pp.466-469
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• 2002

In the sintering of YIG, abnormal grain growth phenomena was observed. This abnormal grain growth is related to the sintering temperature in this experiment. In the sintering below 145$0^{\circ}C$., the sintered body showed narrow size distribution. However, in the sintering at 145$0^{\circ}C$, a few grains grew rapidly with respect to other grains, and bimodal size distribution was appeared. Liquid phase was not observed far from the abnormally grown large grains, but only near the large grains. This means that the abnormal grain growth was caused by the nonuniform distribution of liquid phase which promote the grains growth. This nonuniform distribution of liquid phase was thought to be due to the nonuniform mixing of the starting materials. This abnormal grain growth was suppressed by enhance the compositional uniformity by multiple calcination.

• 한국지형학회지
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• 제27권3호
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• pp.13-24
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• 2020

This study analyzed the characteristics of the grain size distribution of the sediments obtained from the flooding in Ibang-myeon, Changnyeong-gun, which was caused by the collapse of a embarkment on the Nakdong River on August 9, 2020. As a results, it was found that the mean grain size decreases and the sorting becomes poorer as the distance from the embarkment collapse point increases. This is attributed to the fact that the transport energy of the river decreases when flooding occurs, ensuring that coarse-grained sediments are deposited first. Further, as the transport energy further reduces and becomes dispersed, the sorting for the fine-grained sediments becomes poor. Considering the characteristics of spatial distribution, sediments along the farm road showed the properties of floodplain deposits that transport to natural levee and back swamp due to river flooding. On the other hand, sediments along the irrigation ditch exhibited the properties of the deposits that are carried by the flow backward of ditch from the river after the collapse of the embarkment. The results of this study are significant because characteristics of flood sediments were elucidated for major rivers where flooding rarely occurs due to the recently built artificial structures. In addition, by applying the grain size distribution characteristics of present river flood sediments, it will be able to contribute to clarifying the sedimentary environments of the paleo river flood deposits.