智能微型小车的迷宫搜索控制策略

本文分析平面型迷宫的道路特征及其识别方法 ,讨论智能微型小车的几种迷宫搜索方法并给出一种搜索控制策略的程序框图 ,在应用中出现的问题及最终所得到的结果 .     

数字图书馆--图书馆发展的新阶段

文章从数字图书馆的产生，定义，特点等方面入手，论述了数字图书馆是图书馆发展的一个新阶段，并就数字图书馆的建设提出了建议。     

张力减径机孔型设计系统

主要研究开发了钢管张力减径机减径过程的传统孔型、圆孔型、椭圆孔型的设计系统 ,研究了有关孔型设计过程的优化问题 ,成功地为钢管生产厂家提供一套张力减径机孔型自动设计系统 ,有效地提高了工作效率和设计的可靠性     

钻柱纵向自由振动研究

提出了钻柱纵向自由振动的离散力学模型 ,根据Lagrange方程推导建立了相应的数学模型和特征值的计算式 ,并用实际算例进行了计算 .计算结果表明 ,按离散模型确定的固有振动圆频率比按连续等直杆模型确定的固有振动圆频率略小 .考虑到实际钻柱系统的非等直性 ,可以认为离散模型的精度将高于连续等直杆模型的精度     

线阵CCD图像减影技术实现抛射物体轨迹实时检测

为对抛射物体的运动进行分析 ,克服使用高速录像并逐帧分析像片图像的方法需要较长的后期分析时间 ,不便于对结果进行自动快速分析的缺点 ,论文基于抛射物体的运动学规律 ,通过在抛射曲线上的两个固定点的高度和跨越时间的检测 ,获得了抛射物的初始角度和初始速度。对高度和时间的检测 ,采用了线阵电荷耦合器件 (CCD)为图像传感器进行摄像并采用图像减影的方法识别抛射物体。在对系统进行静态标定的基础上 ,在抛射架上进行了抛射实验检测。用该文提供的方法和用录像检测方法对不同条件下的初始发射角和初速度进行检测 ,二者数据符合得很好     

Loess in the Tian Shan and its implications for the development of the Gurbantunggut Desert and drying of northern Xinjiang

Eolian loess is widely distributed on the various geomorphic surfaces between 700–2400 m a.s.l. on the northern slope of the Tian Shan. It is formed in a synchronous manner with dust transported from the Gurbantunggut Desert in the Junggar Basin. The thickest section of loess was found in the Shawan and Shihezi regions. Paleomagnetic and climatic proxy analyses of over 71 m of a loess-paleosol sequence on the highest terrace of the Qingshui He (River) in the Shawan show that the paleomagnetic Bruhues/Matuyama (B/M) boundary lies at the bottom of paleosol S8, at a depth of 69.5 m, and the bottom of the sequence was estimated to be ∼0.8 Ma. This implies that the extremely dry climatic conditions in the Junggar Basin and the initial Gurbantunggut Desert were present at least by 0.8 Ma. High-resolution grain size series demonstrate that this area and desert expansion experienced two dramatic periods of desert expansions that occurred at ∼0.65 Ma and 0.5 Ma, respectively; and the subsequent continuous enhancement led to the environment presently observed. This tremendous environmental effect, caused by large-scale expansion of the desert and arid region of inner Asia, might be an important driving force for the global temperature drop that occurred in the mid-Pleistocene.     

PGE patterns of ores of Dajing Cu-polymetallic deposit in Linxi County,Inner Mongolia: Indicator to source of metallogenic elements

By comparing PGE patterns of sulfide ores with that of basic-ultrabasic dikes occurring in the Dajing Cu-polymetallic deposit, we discover that there are similar positive slopes between the basic-ultrabasic dikes and the black ores composed mainly of sphalerite and galena, reflecting affinity of their source. The PGE patterns of the yellow ores composed basically of chalcopyrite, arsenopyrite and pyrite are actually different. One is close to the pattern of the mantle lherzolite, and others resemble the pattern of the basic rocks. However, the concentrations of Ru are higher in the yellow ores, reflecting that sulfur attains or approaches saturation in their parent magma. The PGE characteristics of ores and dikes show that the magmas derived from the deep of crust and the metallogenic elements were supplied mainly by growth material of the crust. In addition, the mantle-derived magma also offered some elements.     

Palaeolake and palaeoenvironment between 42 and 18 kaBP in tengger desert, NW China

Comprehensive field investigations and laboratory analyses show that palaeolakes, including fresh- mesohaline water Megalake Tengger and other semi-con- nected, isolated water bodies, during late Pleistocene covered an area of more than 20000 km², which is more than half of the Tengger Desert in NW China. Stratigraphic correlation and chronological evidence indicate that before ca. 42000 aBP the area was more arid. The palaeolakes started to develop around 40000 uncal. ¹⁴C aBP but until 37000 ¹⁴C aBP their scope was limited. High water levels established from 35000 ¹⁴C aBP lasted until 22000 ¹⁴CaBP. Lake levels regressed between 22000 and 20000 ¹⁴C aBP but transgressed from 20000 to 18600 ¹⁴C aBP. Subsequently, water level declined further and the Megalake Tengger finally desiccated at around 18000 ¹⁴C aBP. Megalake Tengger possessed a fresh-mesohaline water property, implying that the regional precipitation increased significantly. During the period of Megalake Tengger, the climate was warmer-humid than present. The annual rainfall was 250 to 350 mm more than that of today and the temperature was 1.5 to 3.0℃ higher.