Figure - PMC

Skip to main content

An official website of the United States government

Here's how you know

Here's how you know

Official websites use .gov
A .gov website belongs to an official government organization in the United States.

Secure .gov websites use HTTPS
A lock ( ) or https:// means you've safely connected to the .gov website. Share sensitive information only on official, secure websites.

View full-text article in PMC

. 2015 Aug 3;5:12764. doi: 10.1038/srep12764

Search in PMC
Search in PubMed
View in NLM Catalog
Add to search

Copyright © 2015, Macmillan Publishers Limited

This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

PMC Copyright notice

The TE transmission (top) and reflection (bottom) coefficients (Eq. 1) are plotted as a function of k_x for a LMNZ layer (solid lines) and an isotropic layer with μ_x = μ_z (dashed lines). At frequencies away from the ω = ω₀ point, transmission is high (gray curve). When , transmission is significantly reduced (and reflection enhanced), with larger attenuation for larger Q values. The LMNZ layer reflects almost as well as the isotropic layer. The layer thickness here is assumed to be λ/250, and the shaded region corresponds to k_x > k₀, where the angle of incidence is imaginary.

Inline graphic — The TE transmission (top) and reflection (bottom) coefficients (Eq. 1) are plotted as a function of k_x for a LMNZ layer (solid lines) and an isotropic layer with μ_x = μ_z (dashed lines). At frequencies away from the ω = ω₀ point, transmission is high (gray curve). When , transmission is significantly reduced (and reflection enhanced), with larger attenuation for larger Q values. The LMNZ layer reflects almost as well as the isotropic layer. The layer thickness here is assumed to be λ/250, and the shaded region corresponds to k_x > k₀, where the angle of incidence is imaginary.