排序方式: 共有44条查询结果,搜索用时 31 毫秒
31.
研究空气弹簧键合图建模方法,建立空气弹簧的功率键合图模型,使用20-sim软件进行动态仿真,得到系统压力和位移的动态响应曲线,研究不同负载和节流孔直径对空气弹簧性能的影响规律;通过建立系统的Simulink模型,进行对比仿真分析,验证空气弹簧键合图模型的正确性与仿真结果的可靠性.研究工作为空气弹簧的动力学建模及仿真提供... 相似文献
32.
33.
34.
本文介绍TADSP—TS20XS数据传输的几种方式,即以CPU内核写或者DMA方式通过链路口或者外总线的方式进行数据传送。论述了其在分布式信号处理中的应用,并说明了传输标准对于多DSP互连的重要性,以利于系统的升级和维护。 相似文献
35.
Objective To investigate the dynamic expression of the 20S proteasome in peripheral blood mononuclear cells (PBMCs) of type 2 diabetic patients without vascular complications. Methods PBMCs were prepared from 30 type 2 diabetic patients and 30 nondiabetic controls. The general indexes including weight, height and blood pressure were recorded. Fasting plasma glucose, fasting plasma insulin and glycosylated hemoglobin were measured. The protein level of the 20S proteasome was measured by Western blotting. The mRNA expression levels of the 20S proteasome β1, β2 and β5 subunits were detected by real-time PCR. Results Compared with that in the nondiabetic controls, the protein level of the 20S proteasome was significantly increased in the diabetic patients and was positively associated with glycosylated hemoglobin. Conclusion Type 2 diabetic patients without vascular complications have an increased 20S proteasome expression, the significance of which needs to be explored by further study. 相似文献
36.
37.
研究了Fe-25Cr-20Ni合金中层状碳化物M23C6的形态、晶体学特征、析出动力学及氮对层状M23C6的析出作用。结果表明,层状M23C6呈板条状,与基体奥氏体(A)的位向关系是{001}M23C6〃{001}A,〈001〉M23C6〃〈001〉A。它的析出量受基体中碳的溶解度控制,氮能提高基体的溶解度,促进层状M23C6的析出。 相似文献
38.
本文介绍了基于DS18820的温度实时采集与显示系统的设计与实现。设计中选取单片机AT89S52作为系统控制中心,数字温度传感器DS18820作为单片机外部信号源,精度较好的液晶显示模块1602显示温度。在软件方面利用C语言编程控制单片机,完成对DS18B20与AT89S52的控制,最终实现温度的实时采集与显示。 相似文献
39.
40.
The dense overflow across the Denmark Strait is investigated with hydrographic and hydro-chemical data and the water mass composition of the Denmark Strait Overflow Water (DSOW) is determined by multivariate analysis. Hydrographical properties, the transient tracers CFC-11 and CFC-12, oxygen and nutrients are utilized for the water mass definitions. Distribution and characteristics of water masses north of Denmark Strait are described, the important water masses at the sill and the variability on weekly time-scales are discussed, and the entrainment and mixing of water into the overflow plume in the northern Irminger Basin is calculated. The analysis indicates that water masses both from the Nordic Seas and the Arctic Ocean are important for the formation of DSOW. It is found that water masses transported with the East Greenland Current make up about 75% of the overflow at the sill. The overflow at, and shortly south of, the sill is inhomogeneous with a low-salinity component dominated by Polar Intermediate Water. The high-salinity component of the overflow is mainly of Arctic origin. The water mass composition, and the short-term variability for 7 repeats of sections close to the sill are described, and these illustrate that the overflow is in fact a composite of a number of water masses with different formation and transport histories. This indicate that the overflow is a robust feature, but that it responds to variations in the circulation or atmospheric forcing that influences the formation of intermediate and deep water masses within the Arctic Mediterranean and the North Atlantic. At a section about 400 km south of the sill the overflow is well mixed and modified by entrainment of, mainly, Iceland–Scotland Overflow Water and Labrador Sea Water, together constituting 30% of the overflow plume. The entrainment of Middle Irminger Water dominates shortly downstream of the sill, before the overflow plume reaches too deep but the entrainment seems to be intermittent in time. 相似文献