Observation of Dyakonov Surface Waves
Observation of Dyakonov Surface Waves
复制标题
DOI:
10.1103/physrevlett.102.043903
复制
发表时间:
2009-06
期刊:
影响因子:
--
通讯作者:
O. Takayama;L. Crasovan;D. Artigas;L. Torner
中科院分区:
文献类型:
--
作者:
O. Takayama;L. Crasovan;D. Artigas;L. Torner
A special type of surface wave was predicted by M. I. Dyakonov in 1988 [1]. Such waves exist under special conditions at the interface of transparent anisotropic materials, and hens they are lossless. This surface waves require at least one of the two media to be an anisotropic medium, either biaxial or positive uniaxial, and various configurations have been investigated [2]. In the case of the interface of a biaxial anisotropic medium with refractive indices nx, ny and nz, and an isotropic medium with refractive indices nc, surface waves form only when the refractive indices fulfill the condition n1 ≫ nc ≫ n2 ≫ n3, (1) where n1 = max (nx ; ny ; nz), n3 = min (nx ; ny ; nz) and, n2 is in between n1 and n3[3]. For a positive uniaxial medium, the condition becomes ne ≫ nc ≫ no, where no and ne are the ordinary and extraordinary refractive indices, respectively. When such a condition is fulfilled, hybrid surface waves containing both ordinary and extraordinary field components propagate within a narrow angular band, Δθ, with respect to the crystal optical axis. The allowed propagation angles are referred to as the angular existence domain.