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KONG Qiao-ling MA Jie State Key Laboratory of Ocean Engineering Shanghai Jiaotong University Shanghai China 《船舶与海洋工程学报》2007,6(4)
The phase change characteristic of the power source of an underwater glider propelled by the ocean's thermal energy is the key factor in glider attitude control. A numerical model has been established based on the enthalpy method to analyze the phase change heat transfer process under convective boundary conditions. Phase change is not an isothermal process,but one that occurs at a range of temperature. The total melting time of the material is very sensitive to the surrounding temperature. When the temperature of the surroundings decreases 8 degrees,the total melting time increases 1.8 times. But variations in surrounding temperature have little effect on the initial temperature of phase change,and the slope of the temperature time history curve remains the same. However,the temperature at which phase change is completed decreases significantly. Our research shows that the phase change process is also affected by container size,boundary conditions,and the power source's cross sectional area. Materials stored in 3 cylindrical containers with a diameter of 38mm needed the shortest phase change time. Our conclusions should be helpful in effective design of underwater glider power systems. 相似文献
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针对我国远洋渔船装备落后、操纵性差、机舱环境恶劣、电站管理水平低、劳动强度大以及渔船机舱自动化水平低等问题,介绍里海远洋渔船无人机舱系统的设计与组成。通过采用主机遥控系统、电站功率管理系统、机舱监测报警系统以及网络通信等技术,将自动化、电气化、信息化和智能化控制技术等船舶前沿科技应用于实船,构建一个满足法国船级社(BV)机舱自动化最高等级AUT-UMS要求的无人机舱系统,以提高远洋渔船的操控性、安全性和可靠性,提升供电系统自动化管理水平,改善作业人员工作环境。对该自动化系统的效果和特点进行分析,结果可为我国远洋渔船自动化系统的研究提供策略和思路。 相似文献
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高云超 《铁路通信信号工程技术》2021,(1):76-79
青岛地铁11号线采用的是国内自主研发的自动列车监控系统(ATS),ATS系统作为一个综合信息监控系统的实现平台,以通信前置机作为通信枢纽,与时钟系统、乘客信息系统、广播系统、综合监控系统、无线系统等实现接口.现结合现场实际运行数据,采用UltraEdit文本编辑工具对通信前置机的日志进行检索、分析,通过系统后台的日志分... 相似文献
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以一工作水深为375 m的转塔式浮式生产存储系统(FPSO)为例,研究了复杂系泊系统静力特性计算方法.基本思路是,首先计算出每种类型锚泊线的水平张力TH-水平跨距X曲线,以离散点的形式给出;然后依次给出上端系缆点水平移动距离,相应的计算每根锚泊线新的水平跨距,再根据这些新的水平跨距在对应的TH-X曲线中插值求出此时的每根锚泊线水平张力,将其向X轴正方向投影,合成后即得上端系缆点移动后的系泊系统X方向水平恢复力.对垂直方向的恢复力计算方法与此类似.计算结果与Dynfloat软件结果吻合得很好.此方法简单直观,容易理解,且耗时较少,比较适用于复杂系泊系统静力特性计算. 相似文献
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John H. Simpson J.A. Mattias Green Tom P. Rippeth Thomas R. Osborn W. Alex M. Nimmo-Smith 《Journal of Marine Systems》2009,77(4):428
We report on an intensive campaign in the summer of 2006 to observe turbulent energy dissipation in the vicinity of a tidal mixing front which separates well mixed and seasonally stratified regimes in the western Irish Sea. The rate of turbulent dissipation ε was observed on a section across the front by a combination of vertical profiles with the FLY dissipation profiler and horizontal profiles by shear sensors mounted on an AUV (Autosub). Mean flow conditions and stratification were obtained from a bed mounted ADCP and a vertical chain of thermistors on a mooring. During an Autosub mission of 60 h, the vehicle, moving at a speed of ~ 1.2 m s− 1, completed 10 useable frontal crossings between end points which were allowed to move with the mean flow. The results were combined with parallel measurements of the vertical profile of ε which were made using FLY for periods of up to 13 h at positions along the Autosub track. The two data sets, which show a satisfactory degree of consistency, were combined to elucidate the space–time variation of dissipation in the frontal zone. Using harmonic analysis, the spatial structure of dissipation was separated from the strong time dependent signal at the M4 tidal frequency to yield a picture of the cross-frontal distribution of energy dissipation. A complementary picture of the frontal velocity field was obtained from a moored ADCP and estimates of the mean velocity derived from the thermal wind using the observed density distribution. which indicated the presence of a strong (0.2 m s− 1) jet-like flow in the high gradient region of the front. Under neap tidal conditions, mean dissipation varied across the section by 3 orders of magnitude exceeding 10− 2 W m− 3 near the seabed in the mixed regime and decreasing to 10− 5 W m− 3. in the strongly stratified interior regime. The spatial pattern of dissipation is consistent in general form with the predictions of models of tidal mixing and does not reflect any strong influence by the frontal jet. 相似文献