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In 1988, the Russian physicist Mikhail (Michel) I. Dyakonov has theoretically predicted a new class of surface electromagnetic waves, now called Dyakonov surface waves (DSWs). Unlike other types of acoustic and electromagnetic surface waves, the DSW’s existence is due to the difference in symmetry of materials forming the interface. He considered the interface between an isotropic transmitting medium and an anisotropic uniaxial crystal, and showed that under certain conditions waves localized at the interface should exist. Later, similar waves were predicted to exist at the interface between two identical uniaxial crystals with different orientations. The previously known electromagnetic surface waves, surface plasmons and surface plasmon polaritons, exist under the condition that the permittivity of one of the materials forming the interface is negative, while the other one is positive (for example, this is the case for the air/metal interface below the plasma frequency). In contrast, the DSW can propagate when both materials are transparent; hence they are virtually lossless, which is their most fascinating property. In recent years, the significance and potential of the DSW have attracted the attention of many researchers: a change of the constitutive properties of one or both of the two partnering materials – due to, say, infiltration by any chemical or biological agent – could measurably change the characteristics of the wave. Consequently, numerous potential applications are envisaged, including devices for integrated optics, chemical and biological surface sensing, etc.〔 〕 However, it is not easy to satisfy the necessary conditions for the DSW, and because of this the first proof-of-principle experimental observation of DSW was reported only 20 years after the original prediction. A large number of theoretical work appeared dealing with various aspects of this phenomenon, see the detailed review. In particular, DSW propagation at magnetic interfaces, in left-handed materials, in electro-optical, and chiral materials was studied. Resonant transmission due to DSW in structures using prisms was predicted, and combination and interaction between DSW and surface plasmons (Dyakonov plasmons) was studied. == Physical properties of Dyakonov surface waves == The simplest configuration considered in Ref. 1 consists of an interface between an isotropic material with permittivity ε and a uniaxial crystal with permittivities εo and εe for the ordinary and the extraordinary waves respectively. The crystal ''C'' axis is parallel to the interface. For this configuration, the DSW can propagate along the interface within certain angular intervals with respect to the ''C'' axis, provided that the condition of εe > ε > εo is satisfied. Thus DSW are supported by interfaces with positive birefringent crystals only (εe > εo). The angular interval is defined by the parameter η =εe/εo − 1. The angular intervals for the DSW phase and group velocities (Δθph and Δθgr) are different. The phase velocity interval is proportional to η^2 and even for the most strongly birefringent natural crystals is very narrow Δθph ≃ 1° (Rutile) and Δθph ≃4° (Calomel). However the physically more important group velocity interval is substantially larger (proportional to η). Calculations give Δθgr ≃ 7° for Rutile, and Δθgr ≃ 20° for Calomel. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Dyakonov surface waves」の詳細全文を読む スポンサード リンク
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