Wide Field-of-View Free-space Optical Receiver based on Surface Plasmon Polaritons

来源 :中国通信 | 被引量 : 0次 | 上传用户:liusheng123321
下载到本地 , 更方便阅读
声明 : 本文档内容版权归属内容提供方 , 如果您对本文有版权争议 , 可与客服联系进行内容授权或下架
论文部分内容阅读
Wide field-of-view(FOV)free-space receivers are promising for optical wireless communications,which can reduce the requirements on aiming and tracking.However,the FOV is limited by some tradeoffs of the receiver’s components employing conventional optical devices.In this paper,we proposed a wide FOV optical receiver based on the extraordinary optical transmission mechanism of surface plasmons on a dielectricmetal interface.The proposed receiver has a flat response over a relative wide range of incidence angles.Moreover,the received optical energy density has been enhanced greatly compared to the incidence.Related mechanisms as well as the optimization method are investigated.Potential applications are also discussed. Wide field-of-view (FOV) free-space receivers are promising for optical wireless communications, which can reduce the requirements on aiming and tracking. Ultimately, the FOV is limited by some tradeoffs of the receiver’s systems employing conventional optical devices. This paper, we proposed a wide FOV optical receiver based on the extraordinary optical transmission mechanism of surface plasmons on a dielectric metal interface. proposed proposed receiver has a flat response over a relative wide range of incidence angles. Moreover, the received optical energy density has been enhanced greatly compared to the incidence. Related mechanisms as well as the optimization method are investigated. Potential applications are also discussed.
其他文献
锆石SHRIMP U-Pb年龄的测定结果表明:王坪石正长花岗岩的侵位年龄为(163+1.3)Ma.SiO2在73~76%之间,显示出超酸性、SiO2过饱和的特征,ALK(Na2O++K2O)为7.83~9.41wt%.Al2O3在12.48~1
会议
柳江盆地位于燕山东段,完整地出露了从前寒武纪到中生界的华北地台盖层沉积地层,被喻为地质学的“袖珍教科书”.柳江盆地的地层序列总体上呈中间新,两侧老的特点,东侧岩层向
会议
郯庐断裂带是中国东部一条十分重要的断裂带,对中国东部乃至亚洲大地构造演化有重要影响(Xu et al,1987;Okay A I et al,1992).中段-北段海陆过渡部分研究程度相对较低.作为
大别-苏鲁造山带作为世界上出露面积最大超高压变质带,其俯冲和折返受到国内外地质学者的广泛关注.大量的岩石学成果(Wang et al.,1989;Okay,1993;Ye et al.,2000)表明造山带
会议
华北克拉通区古生代时期和新生代岩石圈之间存在着巨大的厚度差异这一点是目前人们普遍接受的重要事实.地质、地球物理和地球化学研究提供了充分的证据,并对于晚中生代以来发
会议
中国东部断裂体系的研究中,由于盆地的广泛发育,地表揭示较差,对断裂系统的研究存在很多局限.最明显的是很多学者把中国东部的断裂构造及其相关地质作用简单归结为新华夏体系
江西井冈山地区位于华南加里东造山带中段,北以江山—萍乡断裂带与江南新元古代造山带相望,南以政和—大埔断裂带与东南沿海晚中生代花岗质火山—侵入杂岩带相接.区内存在三
会议
一、蟠桃优良品种1.早露蟠桃北京农林科学院以撒花红×早香玉杂交选育而成。果实扁平型,果顶凹入,缝合线浅;平均单果重68克,最大果重95克;果皮底色乳黄,果面10%覆盖红晕;茸毛
中国东部晚中生代高原存在与否是一个有争议的课题.张旗等(2008)从岩石学角度认为高原存留时间大致从175~113 Ma,主要发育在165~125 Ma.汪洋(2006)则认为燕山地区的高原地貌出
会议
武夷山地区加里东构造和岩浆岩均很发育,是研究加里东运动的理想地带.加里东运动不仅使震旦系至下古生界地层发生褶皱,与泥盆系底部形成区域性地层角度不整合,同时使基底变质
会议