• Steel and Composite Structures
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• 제49권5호
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• pp.503-516
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• 2023

In the current examination, a trigonometric shear deformation theory is hired to govern natural frequencies of a functionally graded porous microplate which is covered by two nanocomposite layers. The properties of the structure are varied based on the specified patterns. Utilizing the modified form of couple stress theory for taking the scale effect into account in conjunction with Hamilton's principle, the motion equations are obtained. Then, they are solved via Fourier series functions as an analytical approach. After confirming the results' accuracy, various parameters' effect on the results is investigated. Designing and manufacturing more efficient structures, especially those that are subjected to multi-physical loads can be accounted as findings of this work.

• 한국추진공학회지
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• 제5권4호
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• pp.1-11
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• 2001

다공성 카본 페놀릭 복합재의 재료상수를 실험데이터로부터 결정하기 위하여 시간의존 이론과 유한요소법을 적용하였다. 이 이론은 Biot 의 상수와 투과율 사이의 관계를 다공성의 함수로 사용하여 기존의 Lee, Salamon, Sullivan[1］의 논문을 수정하였다. 수정된 유한요소 프로그램과 재료의 모델링은 (1) 다공성 재료 이론에 더 충실하고 (2) 새롭게 발견된 해석적 단순함을 포함하고 (3) 재료의 성질을 더욱 정확하게 기술하였다. 실험 데이터에 대한 적용과 비교는 어떻게 재료의 파라미터들이 재료의 응답 즉 온도에 따르는 압력의 크기와 최대치의 위치 지배되는지 명백하게 나타낸다. 특별히 응답이 투과율에 매우 민감하게 나타났다.

• Geomechanics and Engineering
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• 제23권4호
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• pp.327-338
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• 2020

The role of precise prediction of subsurface fluids and discrimination among them cannot be ignored in reservoir characterization and petroleum prospecting. A suitable rock physics model should be build for the extraction of valuable information form seismic data. The main intent of current work is to present a rock physics model to analyze the characteristics of seismic wave propagating through a cracked porous rock saturated by a three phase fluid. Furthermore, the influence on wave characteristics due to variation in saturation of water, oil and gas were also analyzed for oil and water as wet cases. With this approach the objective to explore wave attenuation and dispersion due to wave induce fluid flow (WIFF) at seismic and sub-seismic frequencies can be precisely achieved. We accomplished our proposed approach by using BISQ equations and by applying appropriate boundary conditions to incorporate heterogeneity due to saturation of three immiscible fluids forming a layered system. To authenticate the proposed methodology, we compared our results with White's mesoscopic theory and with the results obtained by using Biot's poroelastic relations. The outcomes reveals that, at low frequencies seismic wave characteristics are in good agreement with White's mesoscopic theory, however a slight increase in attenuation at seismic frequencies is because of the squirt flow. Moreover, our work crop up as a practical tool for the development of rock physical theories with the intention to identify and estimate properties of different fluids from seismic data.