最小二乘解存在的充分必要条件

本文提出了当观测值的权矩阵为正定或半正定的前提下，其最小二乘解存在的充分必要条件为并以间接平差为例验证了该结论的正确性。     

a-Si:H的光电导衰退与微结构的关系

目前,主要流行的两类微观机制模型——“负有效相关能模型”和“断键模型”——都表明a-Si:H的光诱导变化与其微观结构有关.本文研究了不同制备工艺条件对a-Si:H微结构的影响,和样品的光电导衰退依赖于微结构的关系.最后,从S—W效应的微观机制作了简短讨论.     

非晶硅太阳电池在反偏压下的光照特性

研究了温度循环和在反偏压下强光照对非晶硅太阳电池性能的影响。电池在90℃,4.5V反偏压下,经550mW/cm~2 的卤钨灯光照后,短路电流增加.光致衰降减小,长波响应改善.用内电场的变化进行了解释.     

变频调速中的电压测量技术

以ＭＣＳ８０９８单片机为核心，提出一种新的测量技术，在硬件上采用同步采样技术，在软件上实现准同步算法，并且采取了预先存准同步采样权系数和正，余弦值在ＥＥＰＲＯＭ２８６４中的方法，提高其实时性，利用傅立叶变换，得到频域的各次谐波结果，准确地在线测量了变频调整速的谐波，并给出了实验结果。     

Dating formation of natural gas pools using fluid inclusion data from reservoirs

A method has been suggested which is based on the homogenization temperatures and other data of fluid inclusions from a reservoir rock, with the combination of burial and geothermal history of the hosted rock, to date the gas reservoir formation. On the basis of this, a case study of the Carboniferous-Permiangas pools in the Ordos Basin has been conducted. The results have shown that the reservoir sandstones of the gas pool were filled by gases during 125-150 Ma, earlier in the southern area and later in the northern area, which is consistentwith the basin's geological and geochemical background under which the gas pools formed.     

Research and Development of Nuclear Heating Reactors in China

ＲｅｓｅａｒｃｈａｎｄＤｅｖｅｌｏｐｍｅｎｔｏｆＮｕｃｌｅａｒＨｅａｔｉｎｇＲｅａｃｔｏｒｓｉｎＣｈｉｎａＷａｎｇＤａｚｈｏｎｇ（王大中）；ＺｈｅｎｇＷｅｎｘｉａｎｇ（郑文祥）；ＬｉｎＪｉａｇｕｉ（林家桂）；ＭａＣｈａｎｇｗｅｎ（马昌文）；ＤｏｎｇＤ...     

劳斯(Routh)稳定性判据判定范围再划分

对劳斯稳定性判据判定范围进行了再划分,明确地判定出某线性定常系统属于渐近稳定,还是临界稳定,或是发散不稳定。并以具有代表性的一些例题,说明如何判定一个线性定常系统的稳定性的类别,推证出特征方程所有对称于坐标原点互为相反数根的一般表达式。     

An investigation of water-gas interface migration of the upper Paleozoic gas pool of the Ordos Basin using reservoir fluid inclusion information

There is a particular characteristic in the formation of the Upper Paleozoic gas pool in the Ordos Basin that is its water-gas interface migrated regional during geological history. However, there has been lack of detailed research on this problem and also no similar report on other basins. In this paper, the formation time of the fluid inclusions formed in the water-gas transition zone of the gas pool was deduced using their trapping temperatures and combining of the burial with geothermal history of the basin. On the basis of this, the isochrone of water-gas interface migration for the gas pool was mapped. The result shows that the gas pool began to form around the Yanan Area at about I65Ma, and then developed and enlarged toward the north direction. The gas pool finally formed at about 129 Ma. Since the basin uplifted from the late Cretaceous and gas supply decreased, the water-gas interface of the gas pool migrated back to the present position.     

Conformal minimal two-spheres with constant Gauss curvature inU(3)

A complete classification of all conformal minimal 2-sphere with constant Gauss curvature is given inU(3).