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The choice of μs'500nm scales the strength of scattering.
Seismogram envelopes have been used to estimate the strength of scattering and absorption in the Earth.
Synthesizing realistic seismogram envelopes is needed to model observed envelopes and to invert for the strength of scattering and absorption in the Earth.
This consistency strongly suggests that the peak energy ratios represent the strength of scattering in the structure, although the results at 4 8 Hz show some differences in the spatial distributions: for example, a large scattering loss in west Japan from Chugoku to central Japan.
The second mechanism is related to the effect of the strength of scattering on ϵ.
In other words, the water content of the tissue has been used as an internal standard to allow specification of the strength of scattering, μs'500nm.
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The simulator can also take into account various compositions of the seabed in terms of scattering strengths.
The μs'500nm is allowed to vary so as to scale the strength of this scattering to match the scattering of a particular skin site, but the initial choice is 43 cm−1.
At relatively low temperatures, the electron-phonon interaction is achieved mainly via phonon emission scattering channels, and the strength of the scattering increases with temperature.
It has been shown that the strength of ultrasonic scattering is proportional to the fourth power of frequency and sixth power of scatterer size [ 31].
The choice of the laser wavelength plays a significant role on both the strength of light scattering and absorption (dispersion).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com