舰船高噪声环境下的语音编解码系统的实现

在研究语音编解码技术现状和发展趋势的基础上,针对舰船高噪声背景下语音信号的特点,利用DSP开发研制了一种语音编解码系统。详细阐述了系统的组成及工作原理,并采用自适应干扰抵消和G.729E相结合的方法,实现了低码率高语音质量的语音压缩与解压缩。     

MVB通信网卡的研制与开发

在分析MVB通信协议特点的基础上,依据MVB网卡的设计需求,详细介绍了通信网卡的硬件结构、器件组成和接口实现,在系统软件设计中,根据MVB过程数据、消息数据和监控数据的不同特点,介绍了MVB通讯控制器的链路层接口函数.     

关于JB/T5983—92多楔带传动设计包角系数K_α和楔合系数K_γ的讨论

本文讨论了K_α和K_T的计算公式与相互关系。指出了JB/T5983—92中K_c数据的问题。同时提供了K_α和K_T的实用公式及计算用表。     

803E掘进机刀盘振动问题浅探

 大伙房引水隧道工程TBM2标采用德国Wirth公司型号为803E的掘进机。掘进过程中刀盘振动问题较为严重，导致联接螺栓超常松动和联接部件裂纹，影响了施工进度和设备的完好率。从该机主机受力结构的动刚度以及刀盘结构形式方面浅探该机刀盘振动问题，并与Robbins公司掘进机的主体结构进行比较，试图提出选型和设计方面的建议。     

SS7E型电力机车平稳性问题的原因分析及改善

主要对SS7E型电力机车的油压减振器与轴箱拉杆对机车的影响进行分析与研究，并对其进行跟踪性试验，提出了对机车平稳性能改进的方案，并在机车上运用，获得了较好的效果。     

RS编码器的FPGA设计和实现

RS码是一种线性分组循环码，具有极强的随机错误和突发错误纠正能力。基于有限域乘法算法，设计了一种RS（128，124）编码器，同时给出了编码器的仿真结果，并进行了FPGA硬件仿真验证。     

动态变形模量E_(vd)标准的应用与展望

系统介绍国外高速铁路路基压实标准和检测手段的发展历程 ,阐明动态变形模量Evd 标准已成为高速铁路路基压实标准的发展趋势 ,论证高速铁路路基工程质量控制标准采用Evd 的必要性及可行性。     

一种雷达窄带数字接收机设计及关键技术研究

雷达接收机领域的数字化技术在日趋发展,如何借助数字化的软硬件技术设计出易实现、灵活,并功能稳定、性能良好的数字接收机成为工程设计的重点。文章研究了一种被动雷达系统窄带数字接收机,阐述了该接收机的总体设计思想、系统组成和工作流程,对设计中的关键技术和实现方法进行了深入的研究,具有结构简便、系统先进的特点,有较好的工程实用价值。     

主机遥控系统转速控制故障探析

对某船主机遥控系统转速控制故障的机理进行了简述,并对故障形成的原因进行了分析和探讨,还从管理的角度提出了一些建议。     

Surface chlorophyll in the Black Sea over 1978–1986 derived from satellite and in situ data

Absolute values of chlorophyll a concentration and its spatial and seasonal variations in the Black Sea were assessed by using satellite CZCS and in situ data. Since the satellite CZCS had operated for the 1978–1986 period, CZCS data was used for assessing the past state of the Black Sea just before the onset of drastic changes observed in late 1980s. The approach used for the calculation of the absolute values of chlorophyll a concentration from CZCS data was based on the direct comparison of in situ chlorophyll a data and those of CZCS and by applying the algorithm developed for the transformation of CZCS data into chlorophyll a values. CZCS Level 2 data related with pigment concentration having a spatial resolution of 1 km at nadir were used. The daily Level 3 files were derived by binning Level 2 values into 4-km grid cells and the monthly and seasonal Level 3 files were created by averaging the daily Level 3 files over the corresponding period. In situ chlorophyll a data were obtained by spectrophotometric and fluorometric methods in 15 scientific cruises over the 1978–1986 period. Total number of ship-measured data used for the comparison with those CZCS values was 590.Chlorophyll a concentration (Chl) was derived from CZCS values (C) with regression equations Chl=kC; the coefficient of transformation k was calculated from six different data sets by taking into account distinctions between subregions and seasons. The reasons for difference in the k values have been analyzed.Statistical comparison of the chlorophyll a values measured in situ and those derived from CZCS data was based on log-transformed data and gave the following results: regression SLOPE=0.842, regression INTERCEPT=−0.081, coefficient of determination (R²)=0.806, root–mean–square ERROR=0.195. The mean monthly chlorophyll a distributions derived from CZCS data over 1978–1986 have been constructed and the mean seasonal chlorophyll a values in different regions have been calculated and analyzed. The significant difference in chlorophyll concentration between the western shelf regions and the open part of the Black Sea has been demonstrated, especially in warm season. At almost all seasons, the highest chlorophyll concentration is observed in the western interior shelf region which is under strong influence of Danube. The summer mean chlorophyll concentration in this region is 18 times higher than that in the open parts and about nine times higher than in the eastern shelf region. The greatest seasonal variations are observed in the open part of the Black Sea: chlorophyll concentration in cold season is four to six times higher than in summer and three to five times higher than in April and October. To the contrary, in the western interior shelf regions, the concentration is higher in May–October (about twice than that in November–March). Seasonal variations in the western outer shelf regions are smoothed out as compared with both the western interior shelf and the open regions.