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     

广东沿海台风灾害链现象与防治途径的设想

通过对登陆广东沿海地区的台风活动特征进行分析，初步探讨了台风灾害链的主要成因和一般规律，广东省每年7－9月是台风及其引发的灾害链最易肆虐的时期。而全年都须提高。根据历史上典型台风灾害特点，对台风造成的狂风、暴雨和风暴潮灾害，及其衍生的次一级灾害链的主要环节和类型进行了初步划分。广东沿海人口密集，经济发达，因而台风灾害的损失也非常巨大。为此，迫切需要进一步加强台风及其灾害链的预测、预警网络建设，健全和完善防灾设施，强化综合减灾信息管理和预防对策的研究，建立现代化的减灾信息系统。     

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     

米邦塔食用仙人掌组培快繁的研究

用米邦塔食用仙人掌半成熟的茎片作外植体，经表面消毒和初代培养后建立了无菌材料。以“MS＋5.0mg/L KT 0.5-1.0mg/L BA 0.25-1.0mg/L NAA”作为增殖培养基可以获得理想的增殖效果，每块带有2－3个小芽的继代材料在该培养基上经50－60d培养可产生约20个丛生芽。在组培条件下，米邦塔食用仙人掌的茎呈圆柱形，而非自然条件下的掌状。根系的形成对外源激素和基本培养基种类等条件要求不严，即使在KT浓度高达10.0mg／L的增殖培养基上，丛芽的基部仍可形成较发达的根系.但比较理想的生根壮苗培养基为B5＋2.0-5.0mg/L NAA 0-0.5mg/L KT。组培小苗移栽到罩有塑料薄膜和遮阳网站的沙床上，成活率高达92．5％以上。移栽后11d时始见植株顶部增粗变扁；第64d时株高平均为9．98cm。掌片宽度平均为1．49cm，掌片长度为5．29cm。     

基于DMC204的数控系统开发与应用

提出了在Windows操作系统平台上实现实时多任务处理的CNC系统控制体系结构，并依据这一结构方案，具体实现了一个具有开放性、模块化特征的简易CNC应用软件，该数控软件在经改造后的CK6140H普通车床上应用结果表明，车床的运行精度和效率大为提高。     

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.     

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.     

Coesite eclogite facies metamorphic tectonite: Evidence for ultrahigh pressure deformation

An ultrahigh pressure ductile shear mélange crops out on the beach of Yangkou Bay near Qingdao City. The mélange is composed of weakly deformed blocks in a highly ductilly flow mylonites. Ultrahigh pressure metamorphic (UHPM) tectonite includes strongly deformed eclogite and mylonitized eclogite. Coesite occurs in the tectonite as both interstitial mineral and inclusions in garnet and omphacite, indicating that the deformation took place in the stability field of coesite (800—850℃, >30 GPa) in the upper mantle. Coesite is rounded or short prismatic grains with undulatory extinction, and often fractured, suggesting brittle deformation. Garnet is also characterized by brittle fractures and sometimes necked and slightly elongated. Omphacite is elongated, with long axis preferred orientation. Undulatory extinction, subgrains and dynamically recrystallized grains suggest plastic flow of omphacite. Ultrahigh pressure metamorphic tectonite was probably formed in the ductile shear zone during the early stage of exhumation of the ultrahigh pressure metamorphic rocks. Its kinematic indicators point to the transport direction of the UHPM slab during the early stage of exhumation.