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S0, S1, S2, S4, S6, S6′, S7, and SR are major seismic reflection boundaries.
We conducted two experiments, one to reveal the penetration depth and resolution of the GPR antenna and to reconstruct the 3D architecture of fluvial deposits created in a flume, and the other to examine the characteristics of reflection boundaries.
The proposed sensor utilizes curved-edge diffraction (CED), which uses the effect of the cylindrical surface curvature on the diffraction phenomenon in the transition regions adjacent to shadow, transmission, and reflection boundaries.
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The boundary conditions are shearing periodic in x and reflective in z (see Bai and Stone 2010b concerning the adequacy of the reflection boundary condition).
Both specular and diffuse reflection boundary conditions are implemented.
It involves the application of a partial reflection boundary condition for this sidewall.
This paper is concerned with the Boltzmann equation with specular reflection boundary condition.
The yellow horizon is a discontinuous/continuous reflection boundary, which can be traced throughout the whole Beppu Bay.
First, we interpret the discontinuous/continuous reflection boundary as the unconformity between the Sekinan Group and the Oita Group.
We discuss three new implementation versions of diffuse reflection boundary conditions in a thermal lattice Boltzmann model.
High-order specular reflection boundary conditions enable high-fidelity treatment of plasma distribution functions at the axis and at wall boundaries.
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