激光吸收铒掺杂上转换材料的光谱特性实验分析

采用湿化学法制备了铒掺杂氧化钇上转换纳米粉体材料.研究了不同掺杂浓度、掺杂元素种类对材料显微结构、物相组成和光谱特性的影响.结果表明,通过控制掺杂元素的种类、掺杂浓度可以实现对光谱性能（包括光谱反射系数和上转换光谱）的调控.实验表明,该材料对106 μm激光具有较好的吸收性能. 关键词： 铒掺杂氧化钇纳米粉体 上转换材料 激光与红外复合隐身 光谱反射系数     

回旋行波放大器输出端反射对注-波互作用的影响

基于回旋行波放大器的非线性自洽理论,研究渐变输出端反射对回旋行波放大器注-波互作用的影响.数值模拟结果表明,对于Ka波段TE₀₁模基波工作回旋行波放大器,渐变输出端渐变角的变化以及互作用长度的改变将导致不同的反射系数幅度和相位,从而影响注-波互作用过程,改变功率演化过程.在输出饱和功率不变的情况下,合理选择输出渐变角,可能可以减小注-波互作用长度,展宽互作用频带. 关键词： 回旋行波放大器 注-波互作用 反射系数     

各向同性晶体栅阵反射系数的二维理论分析

声表面波器件是一个有限弹性体而不是半无限体,依据有限弹性体中的声表面波传输理论,分析声表面波器件周期栅阵对声表面的反射.假定晶体是各向同性的,结合声表面波在周期栅中传播特性的变分原理,用有限弹性体中二维理论的振动位移推导力学负载效应引起的反射系数,求解短路栅阵质量负载的反射系数.通过数值计算得到了玻璃基片不同长度下铝指条的反射系数.发现当基片长度与声波波长之比是奇数倍时,反射系数为正,但绝对值较小;当基片长度与声波波长之比是偶数倍时,反射系数为负,但绝对值较大.这说明要得到较大的反射系数,基片长度应当是声波波长的偶数倍.     

关于一维量子散射中一些问题的简单说明

简单讨论了一维量子散射的各种处理手段,对于一维量子散射中的一些问题和误区给予说明与澄清.     

修正算子γB00的物理含义及精度分析

多次透射公式是一种用于无限介质波动数值模拟中的局部人工边界条件,飘移失稳是多次透射公式在时步积分数值模拟实现中出现的一种失稳现象,可通过在多次透射公式算子中加上修正算子γB00的简便处理方法消除.本文依据球面波传播原理和介质阻尼效应解释了修正算子γB00的物理含义,并在两种极限情形(理想暂态情形和理想稳态情形)下对加修...     

基于大掠射角海底反射特性的深海地声参数反演

海底声学参数的获取对于海洋声学研究有着重要意义.通过推导分层吸收介质下的海底反射系数,理论分析了大掠射角条件下吸收系数对海底反射系数的影响.海底反射系数随频率振荡过程中,将其等于海水-沉积层界面反射系数模时所对应的频点定义为1/4振荡周期频率.在该频率下,沉积层吸收系数与基底地声参数的耦合程度小于其他频点.本文基于大掠射角下的海底反射特性,提出一种深海地声参数分步反演方法.首先,利用相关法提取得到海底反射系数的干涉周期,利用干涉周期反演了沉积层声速和厚度.声速的反演结果结合Hamilton经验公式反演密度.第二步,通过结合基底声速的穷举边界,给出沉积层吸收系数的假设值,利用1/4振荡周期频率下的海底反射系数对基底声速进行一维反演.最后利用半波层频率下的海底反射系数对沉积层吸收系数进行一维反演.大掠射角海底反射特性结合分步反演,实现了基底声速和沉积层吸收系数一定程度的解耦合.实验结果表明,在大掠射角测量条件下,该方法反演的地声参数可有效应用在一定范围内的传播损失预报.     

环氧树脂-玻璃微珠多孔复合材料的水声性能

为提高薄板吸声材料的吸声性能,用改性环氧树脂和空心玻璃微珠等原料合成了25mm厚环氧树脂-玻璃微珠多孔复合材料,在脉冲声管中测试了合成材料试样的声压反射系数和吸声系数,研究了合成工艺参数对其水下声学性能的影响.测试结果表明:环氧树脂-玻璃微珠多孔复合材料是一种良好的水下吸声材料,其吸声性能受到空心玻璃微珠的种类及其含量和固化剂种类等参数的影响.制备了填充多种空心玻璃微珠低频吸声性能良好的环氧树脂-玻璃微珠声学材料.合理地设计实验工艺参数,可以得到水下声学性能更佳的环氧树脂-玻璃微珠多孔复合材料.     

Prediction and Elimination of Multiples Based on Energy Flux Conservation Theorem and Prediction Operator Equation

The received wave field including primaries and all of the multiples can be associated with the reflection coefficients which are only primaries by a prediction operator and two equations： the energy flux conservation equation and the prediction operator equation that is developed from the Levinson recursion and can be easily solved by Li group method under a two-dimensional condition. Given reflection coefficients, the prediction operator can be obtained by solving the prediction operator equation. By the energy flux conservation equation, the reciprocal of the prediction operator times the conjugate of it, the wave field can be predicted, in which both of the surface multiples and the internal multiples are involved. On the other hand, if the wave field is given, based on the energy flux conservation equation solved by the 2D spectral factorization, a fully automated data-driven algorithm is developed to remove the surface multiples as well as the internal multiples.     

用路径积分方法研究势垒散射

本文利用量子力学路径积分的基本思想,严格导出单重势垒与双重势垒的反射系数和透射系数的解析表达式,为研究多重势垒量子阱结构的散射提供一种新的理论方法.     

A Broadband Geoacoustic Inversion Scheme

A geoacoustic inversion scheme, which combines several inversion methods together to invert for the bottomparameters, has been proposed based on the fact that the bottom acoustic parameters have different sensitivitiesto the different physical parameters of acoustic field. Firstly, the characteristic impedance of the bottom is invertedby measuring the vertical bottom reflective coefficients. Secondly, the derived bottom characteristic impedance isused as a constrained condition in another inversion procedure, which is very sensitive to the bottom sound speedbut less sensitive to the attenuation, to inverse the bottom sound speed and bottom density. Lastly, the bottomattenuation can be estimated from methods such as transmission loss data, the vertical correlation of propagationdata, and the normal mode attenuation. To obtain the characteristic impedance of the bottom accurately, vacuumglass spheres (VGS) are used as broadband sound sources, and a special mechanism is designed to trigger theVGS imploded at the preset depth. The inversion scheme has been successfully used for a set of sea experimentaldata. It shows that the inverted bottom parameters could distinguish the atlas marked bottom type quite well.The excellent comparison of the numerical results with the experimental data shows the validity of the invertedparameters.