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用自由口模式实现S7-200系列PLC与IPC的通讯 被引量:1
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作者 安军强 许建敏 +1 位作者 盖军旗 高观望 《河北工业科技》 CAS 2004年第1期7-9,13,共4页
介绍了如何用自由口模式实现西门子公司的S7 200系列PLC与上位机的通讯,给出了一种简单的用户自定义协议,着重介绍了上,下位机之间具体通讯过程的实现,并给出了部分程序和流程图。该方案具有硬件简单、使用灵活的特点,对中小型控制系统... 介绍了如何用自由口模式实现西门子公司的S7 200系列PLC与上位机的通讯,给出了一种简单的用户自定义协议,着重介绍了上,下位机之间具体通讯过程的实现,并给出了部分程序和流程图。该方案具有硬件简单、使用灵活的特点,对中小型控制系统实现通讯有一定的参考价值。 展开更多
关键词 PLC IPC 自由口模式 控制系统 通讯协议 水厂 送水机
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Applications of GSTARS Computer Models for Solving River and Reservoir Sedimentation Problems 被引量:2
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作者 YANG Chih Ted 《Transactions of Tianjin University》 EI CAS 2008年第4期235-247,共13页
GSTARS (Generalized Sediment Transport model for Alluvial River Simulation) is a series of computer models developed by the U.S. Bureau of Reclamation while the author was employed by that agency. The stream tube conc... GSTARS (Generalized Sediment Transport model for Alluvial River Simulation) is a series of computer models developed by the U.S. Bureau of Reclamation while the author was employed by that agency. The stream tube concept is used in all GSTARS models which allow us to solve one-dimensional equations for each stream tube independently and obtain semi-two-dimensional variation of the hydraulic conditions along and across stream tubes for rivers and reservoirs. Sedi-ment transport, scour, and deposition processes are simulated along each stream tube independently to give us a semi-three-dimensional variation of the bed geometry. Most sediment transport computer models assume that channel width is given and cannot change during the simulation process. GSTARS models apply the theory of minimum stream power to the determination of optimum channel width and channel geometry. The concepts of channel side stability, and active, inactive, and armoring layers are used in all GSTARS models for realistic long-term simulation and prediction of the scour and deposition processes in rivers and reservoirs.GSTARS models have been applied in many countries for solving a wide range of river and reservoir sedimentation problems. Case studies will be used to illustrate the applications of GSTARS computer models. 展开更多
关键词 computer model RESERVOIR RIVER sediment transport
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IMPACT OF ENSO ON THE PRECIPITATION OVER CHINA IN WINTER HALF-YEARS 被引量:5
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作者 李天然 张人禾 温敏 《Journal of Tropical Meteorology》 SCIE 2015年第2期161-170,共10页
In this paper, the impact of ENSO on the precipitation over China in the winter half-year is investigated diagnostically. The results show that positive precipitation anomalies with statistical significance appear ove... In this paper, the impact of ENSO on the precipitation over China in the winter half-year is investigated diagnostically. The results show that positive precipitation anomalies with statistical significance appear over southern China in El Nio episodes, which are caused by the enhanced warm and humid southwesterlies along the East Asian coast in the lower troposphere. The enhanced southwesterlies transport more water vapor to southern China, and the convergence of water vapor over southern China increases the precipitable water and specific humidity. In La Nia episodes,although atmospheric elements change reversely, they are not statistically significant as those in El Nio periods. The possible physical mechanism of the different impact of ENSO cycle on the precipitation over southern China is investigated by analyzing the intraseasonal oscillations(ISOs) in El Nio and La Nia winter half-years, respectively. By comparing the characteristics of ISOs in El Nio and La Nia, a physical mechanism is proposed to explain the different responses of the precipitation over China to ENSO in the winter half-year. In El Nio episodes, over western North Pacific(WNP) and South China Sea(SCS) the ISOs are inactive and exert little effect on water vapor transport and convergence, inducing positive precipitation anomalies with statistical significance over southern China in El Nio episodes. In La Nia episodes, however, the ISOs are active, which weaken the interannual variation signals of ENSO over WNP and southern China and lead to the insignificance of the interannual signals related to ENSO. Therefore, the different responses of precipitation over China to ENSO in the winter half-year are possibly caused by the difference of intraseasonal oscillations over WNP and SCS between El Nio and La Nia. 展开更多
关键词 precipitation over China ENSO intraseasonal oscillation winter half-year
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