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The reflection (R) could be collected and detected.
In Figure 4, the transmission (t) and reflection(r) phases are demonstrated.
Reflection (R) spectra were obtained using a Shimadzu UV-3600 spectrophotometer (Kyoto, Japan).
First of all, the simulated reflection (R) and EQE spectra were compared with the experimental results.
Firstly, we used the Shimadzu UV-3600 spectoophotomeasureo measure the transmission (T) and reflection (R) spectra of the samples.
And then their optical constants are obtained by fitting their reflection (R) and transmission (T) spectra in the wavelength range of 300 2500 nm using SCOUT software.
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Reflections (R).
Four different simulation configurations are investigated and compared, where the number of allowed reflections (R), transmissions (T), and diffractions (D) are varied.
For a given path, radio wave may undergo p reflections (R) and/or q diffractions (D) before arriving at the receiver.
Briefly, using the laboratory spectra and sample thicknesses (L), we calculated absorption coefficients (A) for forsterite, MgO, and fused silica via Eq. (1), accounting for specular back reflections (R) in the samples.
The primary loss mechanisms are expected to be Fresnel reflections (R), mode coupling, radiation, and loss due to reflection towards the source.
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