步进电机升降速的离散控制

介绍了步进电机升降速的计算方法，用离散法对步进电机升降速的过程进行了处理，并用C语言编程实现了单片机对步进电机升降速的离散控制。     

公路交通流车速-流量实用关系模型

针对常用的公路交通流车速-流量关系模型不能进行交通流超饱和状态下交通分析的不足，本文首先应用大量的交通观测数据建立了各级公路车速-流量关系理论模型，通过对公路高峰小时超饱和状态下交通流消散过程的机理分析，研究了各级公路在不同交通负荷条件下的车速-流量关系通用模型的结构，并通过与大量观测数据的拟合，建立了各级公路在任何交通负荷条件下的车速-流量关系通用模型的函数表达式，提出了各级公路在不同设计车速下的实用模型参数．该模型成功地解决了高峰小时超饱和状态下的交通流速度预测问题，为公路网络规划类、终济分析类项目的开展提供了理论基础．     

利用单片机实现直流他激电机的无触点无级调速系统

以比例式零压法为基础 ,提出了直流他激电机的无触点无级调速控制方案和对低压电机用场效应管替代晶闸管的办法 .利用单片机直接控制晶闸管 ,解决了触点寿命问题 .通过单片机的计数口检测电机轴脉冲轮的脉冲信号可实现电机的速度控制和位置控制 .检测和控制都避开了 A/D和 D/A转换 ,具有一定的实用价值 .     

旋转变换理论及其在平面度误差评定中的应用

将旋转变换理论应用于平面度误差评定中，通过实例证明了其可行性。     

论FDI对西部制度变迁的影响及对策

本文首先对我国西部地区利用FDI的现状进行了描述 ,然后运用回归分析的方法分析了FDI和制度变迁的关系 ,指出FDI是影响区域制度变迁的重要因素 ,FDI在区域分布上的不均衡严重制约着西部地区制度变迁的进程。西部地区应该加快体制改革的步伐 ,改善投资环境 ,吸引FDI ,进而通过FDI带动西部地区制度变迁的进程 ,最终形成FDI和制度变迁相互推动、相互促进的良性循环。     

Holocene lake deposits of Bosten Lake, southern Xinjiang, China

A 9.25-m-long sediment core from Bosten Lake,Xinjiang, provides detailed information about changes in the water budget and biological acticity over the last 8400 cal-endar years. The chronology is constructed from six AMS radiocarbon dates on the terrestrial plant remains. Based onanalyses of TOC, CO3, detrital compounds and biogenic SiO2,lake level fluctuations and periods of remarkably-negative water budget appeared at 8.4-8.2 cal ka, 7.38-7.25 cal ka,5.7-5.5 cal ka, 3.7-3.4 cal ka and 3.3-2.9 cal ka, respec-tively. As they are in-phase with low lake levels at Sumxl Co and Bangong Co in western Tibet Plateau and with paleo-lakes in Inner Mongolia, a climate-induced change to some-what drier and warmer conditions is inferred. A further drop in lake level after 1320 AD of about 200 yr duration may heattributed to a negative water balance prior to the main phase of the Little Ice Age. Deep and stable lake phases of 1500 yr and 1800 yr duration at 7.2-5.7 cal ka and 5.5-3.7cal ka coincide with maximum moisture during the Holocene Megathermai in China. The long term trend towards aridity since about 4.3 cal ka can dearly be recognised. The reduced water budget of Bosten Lake from 640-1200 AD may be attributed to local effects.     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.     

改变水分子簇的结构及诱发的生物效应研究

概述了水分子簇理论研究的基本状况,以及改变水分子团簇结构的4种方法,包括外加磁场、外加电场、激光辐射以及直接加热法;最后简要介绍了改变水分子团簇结构所诱发的生物效应.     

并联电压负反馈输入、输出电阻的讨论

电路中引入负反馈,使输入、输出电阻均发生变化,并且输入、输出电阻对放大电路有很大的影响.从并联电压负反馈的角度,对输入电阻和输出电阻给出了下列4种方法的定量讨论.     

水平轴变转速风力机气动参数辨识

文章对变转速水平轴风力机气动参数辨识的问题进行了研究 .风轮的功率曲线为风力机气动性能的整体体现 ,直接影响系统的经济性与控制性能 .通常情况下 ,功率曲线与桨距角和叶尖速比有关 ,可以看成是它们的非线性函数 ,一般由气动性能计算得到 .本文首先利用辨识算法 ,在风轮功率曲线的函数形式假设已知的前提下 ,利用测量的输入输出数据 ,辨识出功率曲线函数的参数 .最后 ,利用辨识出的曲线参数 ,预估系统风轮转速 ,并与测量的转速对比 ,以验证辨识模型的准确性 .