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非制冷红外焦平面阵列(UFPA)不可避免地存在无效像元, 这对UFPA的成像效果造成了极坏的影响。为解决这一问题, 在分析并总结各种非制冷红外焦平面无效像元识别算法优缺点的基础上, 提出一种新的无效像元识别与实时补偿方法。根据像元响应特性, 采用循环迭代法以搜索最优的无效像元判别阈值, 并据此标识出无效像元的位置。在硬件实现阶段, 对于M×N的UFPA器件, 在任意采样时刻, 利用移位寄存器保存当前采样点之前的M个响应值, 使其输出可实时更新为与采样点同列的上一个数据; 同时, 利用一般的寄存器实时保存与采样点同行的前一个数据, 采用同帧行列间内插法实现无效像元的实时补偿。该算法有效地解决了无效像元识别阈值选取困难及不易实时补偿的问题。针对320×240的UFPA器件, 该算法在基于FPGA的红外图像处理系统上得以实时实现, 成功地消除了无效像元对UFPA成像效果的影响。 相似文献
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Q-mode factor analysis was applied to 99 surface samples from the South China Sea to define four planktonic foraminiferal assemblages: tropical-subtropical assemblage, high-salinity assemblage, transitional assemblage and dissolution resistant assemblage. The tropical-subtropical assemblage is a dominant assemblage. The variation of the planktonic foraminifera of this assemblage reflects the changes of tropical surface water from the west Pacific to South China Sea. These four assemblages reveal that different planktonic foraminiferal assemblages are controlled by different factors in the South China Sea, such as tropical-subtropical assemblage controlled by sea surface temperature (SST), high-sallnity assemblage mainly by salinity besides SST, transitional assemblage by SST and dissolution resistant assemblage by water depth. 相似文献
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以柔性材料聚对苯二甲酸乙二酯(PET)为基底,在自行溅射的方阻为50 Ω/□的氧化铟锡(ITO)导电薄膜上制备了结构为PET/ITO/NPB/Alq3/Mg:Ag和PET/ITO/NPB/Alq3:DCJTB/Mg:Ag的绿色和红色器件,其最高亮度分别为18 cd/m2和170 cd/m2.利用原子力显微镜(AFM)表征了柔性ITO和有机薄膜的形态,结果表明,影响柔性电致发光器件性能的主要因素是ITO薄膜与PET基板的附着性问题,从而导致柔性基片在湿法刻蚀和清洗中ITO薄膜的剥离.另外,通过使用致密的氮化硅(Si3N4)绝缘层取代常规蚀刻的方法,制备了高性能的4×2阵列的柔性有机电致发光器件. 相似文献
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基于现场可编程门阵列的高性能红外热成像系统 总被引:1,自引:0,他引:1
探讨了红外成像系统实时信号处理算法、硬件结构等关键技术.提出了一种新的自适应两点非均匀性校正(ATPC)算法,该算法以快门为目标场景来实时更新校正参数,能有效克服红外焦平面阵列(IRFPA)响应随时间漂移导致的两点非均匀性校正算法失效问题.采用查找表结构来实现平台直方图均衡(PE)算法,并对PE算法进行了优化,降低了运算量和存储空间需求.硬件系统采用两片同步动态随机存储器(SDRAM)的乒乓缓存结构,在单片现场可编程门阵列(FPGA)上实现了IRFPA的ATPC和PE算法的并行操作.实验结果表明,对320×240的IRFPA,在50 MHz系统时钟下,帧频为60 Hz时系统工作良好,处理后的红外图像质量有了明显改善,系统结构简单便于小型化,能够满足实时动态检测及追踪需求. 相似文献
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Based on grain size types of the sediments, combined with characteristics of organism, mineral and chemical composition of the sediments, and a comprehensive analysis from the viewpoint of the origin of sediments, sediments in the region studied are classified into four sedimentary types, namely, terrigenous detritus (including five zones of sediments), biogenic-terrigcnous (including three zones of sediments), authigenous-terrigenous (containing some authigenic scdimentary minerals) and volcanic-terrigenous (containing certain volcanic detritus) types. Characteristics of all these types, their relationships and spatial distributions are also discussed. 相似文献
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