加热弹性圆板的大振幅自由振动

基于ｖｏｎＫáｒｍáｎ理论和Ｈａｍｉｌｔｏｎ原理，导出了均匀加热弹性圆板用中面位移表示的大振幅自由振动动力学控制方程．并在调和振动模态假设下，采用Ｋａｎ－ｔｏｒｏｖｉｃｈ平均方法将所得混合初－边值问题转化为相应的非线性常微分方程两点边值问题，采用打靶法和解析延拓法，分别获得了不可移简支和夹紧加热圆板非线性振动的调和振动响应，绘出了不同加热温度下的幅－频特征曲线．得出：升温使圆板的固有频率降低，从而实现改变板的温度对其固有频率的控制     

LAPLACE—STIELTJES变换所定义的解析函数的下级

对于Ｌａｐｌａｃｅ－Ｓｔｉｅｌｔｊｅｓ变换所定义的整函数或在半平面内解析的函数，分别定义了下级，适当引进序列０≤λｎ↑＋∞，建立该变换的最大模与“最大项”之间的关系，并由这些关系推导了两类下级的充分必要条件。     

测地坐标计算椭球面上凸多边形面积的算法

推导出用三顶点的测地坐标计算地球椭球面上三角形面积的公式．公式表明，主项的表示式与按平面坐标求面积的计算式完全一致，而附加项的表示式亦有规律可循．因此，该公式的适用范围可由椭球面三角形推广至椭球面上任意凸多边形．与高斯平面上计算的面积相比，由于不受投影变形的影响，因而更接近于实际面积．这就为至今较难实施的椭球面的面积计算开拓了一个新的途径，有利于做出更客观的GIS空间量度与分析．实际数据的验算充分证实了该算法的正确性和有效性．     

钢的过冷奥氏体连续转变（CCT）曲线的解析化

用数值分析法预报奥氏体变形后相变产物的类型和形态的首要问题是对CCT曲线进行解析化处理。通过曲线拟合获得在半对数坐标下的CCT曲线的解析式,利用同类钢种中的有限条相邻碳当量的CCT曲线做出的解析关系,采用插值法获得在研究范围内的特定初始条件下的任意碳当量所对应的CCT曲线。     

解析函数的一种简单求法

文章利用解析函数的Cauchy-Riemanne条件,给出了调和函数作为解析函数的实部或虚部时解析函数的一种简单求法.     

抽油井分层测压技术及其应用

尕斯库勒油田位于青海省柴达木盆地西部南区的尕斯断陷亚区红柳泉跃进一号断鼻带上的一个三级构造,位于狮子沟——油砂山大逆断层下盘,石油地质储量7200多万吨,目前,尕斯库勒油田已步入中后期开发阶段,由于开采的各小层间和层内地质特征的差异(如各小层地层压力、渗透率、孔隙度等物性的不同),在油田注水开发后,地下水线推进速度相差很大,致使油井见水时间、含水率及各分层的出力状况相差悬殊,严重时甚至非主力层出力甚微或根本不出力,多层合采时的产量远远低于分层开采时的产量之和,从而制约了油井生产寿命,严重影响了油田的长期稳产。因此…     

解析北京奥运食品安全"方程式"

北京奥运蔬菜准备在哪儿种？都有什么品种？普通市民何时能在市场上买到能量棒、蛋白棒和减重棒？怎样才能保证北京奥运会期间所消费的各种食品的安全……[编者按]     

SHRIMP zircon U-Pb dating for volcanic rocks of the Dasi Formation in southeast Hubei Province, middle-lower reaches of the Yangtze River and its implications

The Jinniu Basin in southeast Hubei,located at the westernmost part of middle-lower val-ley of the Yangtze River,is one of the important vol-canic basins in East China. Volcanic rocks in the Jin-niu Basin are distributed mainly in the Majiashan Formation,the Lingxiang Formation and the Dasi Formation,consisting of rhyolite,basalt and basaltic andesite,(trachy)-basalt and basaltic trachy-andesite and (trachy)-andesite and (trachy)-dacite and rhyolite respectively,in which the Dasi volcanism is volumet-rically dominant and widespread. The Dasi volcanic rocks were selected for SHRIMP zircon U-Pb dating to confirm the timing of volcanism. The results indi-cate that there exist a large amount of magmatic zir-cons characterized by high U and Th contents in the volcanic rocks. The concordia ages for 13 points are 128 ± 1Ma (MSWD = 3.0). On account of the shape of zircons and Th/U ratios,this age is considered to represent the crystallization time of the Dasi volcan-ism. The volcanic rocks in the Dasi,Majiashan and Lingxiang Formations share similar trace elementand REE partition patterns as well as Sr-Nd isotopic compositions. In combination with the regional geol-ogy,it is proposed that the southeast Hubei volcanic rocks were formed mainly during the Early Creta-ceous,just like other volcanic basins in middle-lower Yangtze valley. A lithospheric extension is also sug-gested for tectonic regime in this region in the Cre-taceous Period.     

Growth ages of ferromanganese crusts from the western and central Pacific： Comparison between nannofossil analysis and ^10Be dating

Based on results of nannofossil analysis and 10Be dating in ferromanganese crusts M1-1 and A1-1 (no nannofossils were found in it),from the western and central Pacific respectively,it is found that the crust growth ages from nannofossil biostrati-graphy agree well with those based on 10Be isotope analysis. Both crusts have three growth layers,and the oldest layer was deposited in Miocene at about 12.80 Ma. The maximum,minimum,and average growth rates of crust A1-1 (from the central Pacific) are 8.11,1.92 and 3.47 mm/Ma,and those of crust M1-1 (from the western Pacific) are 2.93,0.47,and 0.94 mm/Ma.     

Bloch类空间之间的加权复合算子的有界性(英文)

设H为复Hilbert空间,B(H)为H上算子范数不大于1的有界线性算子集,E=E*为B(H)中的两两可换子集.作者用E和E上的解析算子函数分别取代了复单位圆盘和复单位圆盘上的解析函数,在算子Bloch型空间上定义并讨论了加权复合算子的有界性,得到了Bα到Bβ的加权复合算子有界的充分必要条件