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Traditional hardening laws cannot accurately model these phenomena.
A linear time-frequency representation of acoustic data is unable to model these phenomena.
A better understanding of the mechanisms of alteration resumption, linked to the precipitation of zeolite, is necessary to model these phenomena.
Since the drifted particles interact with these waves many times, it is possible to consider these interactions as stochastic processes, and we can model these phenomena as radial diffusion.
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Usually equations modeling these phenomena depend on several parameters.
However, there are some hindrances in modeling these phenomena.
Matsumura (2005) has also modeled these phenomena as occurring simultaneously under redistribution of the tectonic stress, resulting in a net quiescence.
In ecological modelling, these phenomena generally occur on large scales and are generally difficult to simulate efficiently because of the number of entities.
A theoretical model describing these phenomena was applied and a reasonable agreement with experiments was achieved.
The simplest model of these phenomena is known as the DLVO (Deryaguin-Landau-Verwey-Overbeek) theory [23].
The model ascribes these phenomena to changes in the catalytically active membrane surface area and in the accessible membrane pore volume, which are brought upon by the deposition of phosphorous-containing by-products of the DMMP's thermocatalytic decomposition reaction.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com