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In a sedimentary environment, layered models with abrupt boundaries between the different soil units represent the soil profile accurately.
After a comparison between the estimated RFs and the observed teleseismic waveforms, we constructed simple two-dimensional layered models with anisotropic media to explain the estimated RFs at the N.WTRF and N.WATH stations.
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The main reason for this discrepancy results from the use of a simplified 2D layered model with the blood vessel represented as a layer of blood.
The 1000 °С annealed films are described in the framework of the two-layer models with the sharp boundary between the layers.
Coating design has been based mainly on discrete layer models with abruptly changing properties at interface perfectly bonded to a substrate.
As it will be seen below, when presenting the results of the simulation, we used single-layer and two-layer models with the following types of layers: Isotropic uniform transparent layer (IUTL) with n, h.
A simple numerical solution method, which can easily be extended to more components, is illustrated for the popular chemical-engineering film, penetration, and boundary-layer models with a particular example of evaporation of acetone and methanol through air.
Second, a seven-layer model with low competence contrast is modelled under direct tension parallel to the layering and bending conditions with the focus on investigating through-going fracture formation across layer interfaces.
A double-layer model with sharp interfaces was established for the fitting of the ellipsometry parameters.
Fig. 5 Measured and calculated reflectance spectra using FDTD with the anionic layer model, with and without absorption.
Such interface condition was modeled using the linear spring layer model with a continuous traction but a displacement jump.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com