• Proceedings of the Korean Fiber Society Conference
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• 2001.10a
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• pp.167-170
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• 2001

실의 겉보기 물성 (apparent properties)은 실의 품질을 결정하는 중요한 요인중의 하나이다. 특히, 직물 또는 편성물과 같은 평면 섬유물의 경우, 실의 겉보기 굵기 변동은 섬유물의 표면 평활도, 색상, 등 감성적 제품 품질을 결정하게 된다. 이에 따라 실의 겉보기 성질이 섬유제품의 품질에 차지하는 비중이 점차 커지게 되었다 본 연구에서는 광속 밀도가 높고 회절이 적은 레이저 비임을 이용하여 실의 겉보기 굵기를 측정하여 방적사의 겉보기 굵기가 가지는 변동 특성을 해석하고, 측정 조건이 실의 굵기 측정 결과에 미치는 영향을 소개하고자 한다. (중략)

• Korean Journal of Materials Research
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• v.7 no.12
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• pp.1033-1040
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• 1997

Si가 첨가된 ZNR의 겉보기 유전상구, 겉보기 비유전손율, 유전비저항의 주파수 특성을 여러 측정온도에서 조사하였다. 모든 ZNR에 대하여 유전분산현상 및 유전흡수현상이 뚜렷이 나타났으며, 비슷한 경향의 유전성질을 나타냈다. SiO$_{2}$첨가량이 증가함에 따라 겉보기 유전상수, 피이크 겉보기 비유전손율은 감소하였으며, 유전비저항은 증가하였다. 온도상승시 겉보기 유전상수, 피이크 겉보기 비유전손율은 증가하였으며, 흡수 피이크 주파수는 고주파측으로 이동하였다. SiO$_{2}$첨가량이 증가함에 따라 ZNR은 Cole-Cole원호에서 0.68-0.72범위 내에서 증가하는 $\beta$값을 가지며, 완화시간의 분포가 좁아지는 유전특성을 나타냈다.

• Geophysics and Geophysical Exploration
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• v.24 no.4
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• pp.139-148
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• 2021

Negative apparent chargeability data in time-domain induced polarization (IP) survey are very often considered as noise and rejected before the inversion stage. Negative IP data can, however, occur naturally as a consequence of the distribution of chargeable zones in the ground. In some cases, the negative apparent chargeability values may account for most of the data measured. Negative IP data are caused by the geometry of chargeable zones and electrode positions. Negative apparent chargeability data appear most frequently when a dipole-dipole array is used. In this study, the effect of negative apparent chargeability data on inversion results is analyzed through the numerical 2D time-domain IP modeling and nonlinear inversion. The results demonstrate clearly that negative apparent chargeability data have to be included in the inversion as they contain important information on the distribution of subsurface chargeability.

• Journal of IKEEE
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• v.23 no.1
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• pp.318-321
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• 2019

The apparent soil resistivity is used for estimating multilayer soil parameters, such as, layer's depth and soil resistivity. The apparent soil resistivity can be measured, and also can be calculated if soil parameters are given, becacuse the apparent soil resistivity is a function of these parameters. Therefore, any optimization algorithms can be used to find these parameters which make the calculated apparent soil resistivity close to the measured one. The equation for calculating the apparent soil resistivity is complicated and time consumed, because it is composed of an infinite integral which includes a zero order Bessel's function of the first kind. In this paper, a fast algorithm for calculating the apparent soil resistivity of horizontal multilayer earth structure has been presented using complex image method.

• Tunnel and Underground Space
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• v.30 no.6
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• pp.551-558
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• 2020

This note presents the calculation of nominal area for rock core specimen under direct shear testing condition. The initial nominal area was assumed as ellipsoid, and the equations for calculating the nominal area are derived. The normalized shear displacement and normalized nominal area have an identical relationship regardless of the ellipsoid shape. New testing constants and the generalized method were suggested to calculate the decrease of the nominal area. The method was applied to calculate the direct shear testing data and the changes of result were discussed.

• Journal of the Korean Geosynthetics Society
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• v.19 no.4
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• pp.33-40
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• 2020

It is now common to find the wastes buried in the past during the excavation process of soil for large scale housing and land development. Without proper treatment of the wastes environmentally, the excavation process is no longer able to proceed, and an action plan should be provided to treat the wastes with environmental and economic viability. In the study, the relationship between the apparent density of the wastes and the volume conversion factor, which is the basis in the estimation of waste treatment cost was investigated. From 10 sampling points of a landfill site, wastes were sampled, analyzed for physical characteristics, and the apparent density of mixed and sorted waste was assessed. Applying the empirical formula, and the formula we suggested here, the volume conversion factors were compared with that measured directly in the field using dump truck and excavator. Obviously there was a close relationship among the volume conversion factors resulting from the empirical formula, the formula we suggested and that measured in the field.

• Resources Recycling
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• v.26 no.6
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• pp.102-107
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• 2017

To estimate the bulk density applying the composition rate for recyclable residential waste, the composition rates by volume and weight basis, the bulk densities of the separated and commingled wastes were investigated four times respectively for recyclable waste of 1,800 kg transported to waste recovery facility. The bulk densities for separated wastes were $379.0kg/m^3$ of glass bottles that is highest and metals, residues, others, cans, plastics in order. The composition rates for each separated waste were changed widely depending on either volume basis or weight basis. The composition rate by weight basis as 40.6% of the glass bottles, 32.6% of the plastics were changed to 60.2% of the plastics and 8.9% of the glass bottles in that by volume basis. The bulk density of the commingled wastes applying the composition rate by volume basis showed the similar value to the measured density than by weight basis. So it was estimated that the composition rate by volume basis was appropriate for determining the bulk density of the commingled recyclable wastes.

• Tunnel and Underground Space
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• v.33 no.3
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• pp.150-168
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• 2023

The anisotropic behavior of rocks is primarily attributed to the directional arrangement of rock-forming minerals and the distribution characteristics of microcracks. Notably, sedimentary and metamorphic rocks often exhibit distinct transverse isotropy in terms of their strength and deformation characteristics. Consequently, it is crucial to gain accurate insights into the deformation and failure characteristics of transversely isotropic rocks during rock mechanics design processes. The deformation of such rocks is described by five independent elastic constants, which are determined through laboratory testing. In this study, the characteristics of the directional variation of apparent elastic constants in transversely isotropic rocks were investigated using experimental data reported in the literature. To achieve this, the constitutive equation proposed by Mehrabadi & Cowin was introduced to calculate the apparent elastic constants more efficiently and systematically in a rotated Cartesian coordinate system. Four transversely isotropic rock types from the literature were selected, and the influence of changes in the orientation of the weak plane on the variations of the apparent elastic modulus, apparent shear modulus, and apparent Poisson's ratio was analyzed. Based on the investigation, a new constraint on the elastic constants has been proposed. If the proposed constraint is satisfied, the directional variation of the apparent elastic constants in transversely isotropic rocks aligns with intuitive predictions of their tendencies.

• Journal of the KSME
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• v.32 no.6
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• pp.514-523
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• 1992

스트레인 게이지를 이용하여 변형측정을 할 때 온도변화의 영향으로 나타나는 겉보기 변형도와 게이지 상수의 변화에 대하여 설명하였고 실제 측정시 정확한 측정값을 얻기위한 온도보상 방 법에 대하여 기술하였다. 온도변화에 의한 겉보기 변형도의 값은 기계적 하중에 의한 변형도에 비하여 무시할 수 없는 큰 값을 나타내기 때문에 적절한 보상에 의하여 정확한 측정값을 얻어 내야 한다. 항공우주산업, 원자력산업 등의 분야에서 널리 응용되는 극저온 환경에서 겉보기 변 형도와 게이지 상수의 측정결과를 제시하였다. 극저온에서는 자체 온도보상된 스트레인 게이지라 할지라도 대단히 큰 온도영향을 받기 때문에 본시험에서 제시한 바와 같이 측정결과를 온도보 상하여 처리해야만 의미있는 결과를 얻을 수 있다. 본 시험에서 4차식으로 구해진 겉보기 변형 도에 대한 특성곡선과 게이지 상수에 대한 시험결과는 극저온에서 변형을 측정할 때 직접적으로 보상하여 사용될 수 있다.

• Journal of the Korean Society of Earth Science Education
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• v.13 no.1
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• pp.29-39
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• 2020

In this study, to find out the learning effects and difficulties of role play activities to learn the earth's rotation and the sun's apparent motion, the degree of concept understanding through role play activities, difficulties arising from activities collected by interview, and eye movement during activities are analyzed. 22 fifth graders participated in this study and collected and analyzed experimental behaviors, post-interviews, and eye movement data during the role play of the students. The study found that students could explain the rotation and direction of the Earth through role play activities, but it was difficult to explain the apparent motion of the sun. Since it is difficult to perceive the sun's apparent motion through role play activities, the learning effect of the earth rotation role play activity is low.