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Here we demonstrate a new, process-based 1D layered model that captures the dynamic shifts in water potential gradients of 3D RSA under different soil moisture conditions: the RSA stencil.
For example, the original 7-layer OSI model is better replaced by the layered model that is more widely used today.
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Zalesak et al. (1982) have developed a three-layer model that consists of the magnetic equatorial plane and the conjugate E regions connected by the magnetic field lines.
To make a scale transition from the atomistic to the continuum scale, we propose a surface layer model that is informed by atomistic simulations.
Here, we used a single-layer model that was based on the assumption that all concentrations of electrons are located in an infinitely thin spherical shell at 350 km height; locations of the fluctuations are related to ionosphere piercing points.
In order to simulate the experimental data and estimate relevant physical parameters of the SCL material, we introduce a general mathematical multi-layer model that takes into account diffusion within each layer as well as the effects of both partition and barriers between layers.
Based on experimental data using suspended fibroblasts, we create two structural models: a thick shell actin cortex model that describes cell deformation for a localized stress distribution on these cells and a three-layered model that considers the entire cytoskeleton when a broad stress distribution is applied.
Soil ECa variation with depth was represented by both two- and three-layer models that were visualized and parameterized with the use of penetrometer ECa data.
To define the microstructural evolution of collagen gels under PC, this study applied a two-layer micromechanical model that was previously developed to measure hydraulic permeability (k) under SC.
For ease of diagnosis from a model, an approximate version of the universal expression is explored and illustrated for a forced/dissipative equatorial basin mode simulated by a single-layer oceanic model that includes both mid-latitude RWs and equatorial waves.
AERMOD is a widely used boundary layer pollution model that involves release of a source plume of tracers (e.g. SO2 or ash), which are then tracked as they are carried by wind and interact with topography (Cimorelli et al, 2005).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com