板几何中一类具周期边界条件迁移算子的谱分析

分析了板几何中一类与时间有关的具周期边界条件的线性迁移方程一些谱的性质，证明了：这类迁移算子的谱在区域中仅由有限个具有限代数重数的离散本征值组成，并证明了该迁移算子的占优本征值的存在性等结果。     

一阶拟线性椭圆型复方程的广义DC型边值问题

研究了一般的一阶拟线性椭圆型复方程的边界条件中含有斜微商的广义Carleman型边值问题。采用直接将广义DC型问题化为奇异积分方程的方法析出特征部分，然后通过对特征方程的研究得到了广义DC问题的可解条件和计算指标。     

无穷直线上的双解析函数的Riemann边值问题

研究双解析函数在无穷直线上的Riemann边值问题，并给出了该问题的可解性定理。     

陕西省人均粮食与人均耕地变化研究

对陕西省人均粮食及人均耕地变化进行了时空差异分析,结果表明:(1)近50余年的绝大多数年份为人均粮食占有量的递增期,且不同时段的增幅不同;粮食增长率大于人口增长率的时期,对应人均粮食的增长时期;(2)1978—1998年绝大多数地、市人均粮食递增,且地域差异明显;(3)近50多年来全省耕地面积总体逐年递减,近10年来减少之势加剧;同期人口数量的持续增长,造成人均耕地面积急剧减少.相关回归分析显示:各地、市人均粮食绝对增量与其相对增量之间呈正相关,人均粮食增加量占粮食增量的份额整体偏低;提高粮食生产水平及控制人口是增加全省人均粮食占有量的重要途径.     

双解析函数的Riemann边值逆问题

给出双解析函数的一类Riemann边值逆问题正则型与非正则型情况的提法。基于双解析函数的正则型Riemann边值问题，讨论了双解析函数Riemann边值逆问题正则型情况的可解性，得到了该边值逆问题的可解性结论：当问题的指标κ≥0时，该边值逆问题具有2κ 1个线性无关解；当指标κ＜0时，该边值逆问题只有零解，即双解析函数的正则型Riemann边值逆问题的一般解具有2κ 1个自由度。     

B-样条曲面的G1连续性

得到了关于两个双三次内部重结点B-样条曲面片G1连续的充分必要条件和在公共边界线上控制向量的本征条件,这些条件直接由两个B-样条曲面的控制向量表示.利用本文所给的条件,得到了具有局部性质且是真正G1光滑的曲面模型.     

对开发性移民的法律解释

开发性移民方针的提出是我国水库移民理论的一次重大创新，开发性移民是对补偿性移民的发展．从法律角度来看，开发性移民的实质是遵循市场经济的基本规律，运用法制手段，以移民补偿和库区开发为基础，对国家、集体、个人利益关系的一种平衡和协调，以实现库区经济社会的可持续发展．     

辽河盆地东部凹陷北部地区Es1+2/Es3不整合面与油气运聚的关系

根据 2 2 4口井的实际资料 ,结合地层沉积特征和地震剖面解释结果对辽河盆地东部凹陷北部地区Es1+ 2 /Es3 不整合面的上、下地层的接触关系及岩性组合特征进行了平面规划及分类 ,探讨了该不整合面与油气运聚的关系。研究结果表明 ,不整合面在油气运聚过程中所起的作用主要是由不整合面上、下地层的接触关系及岩性配置所决定。研究区凹陷北部茨 5 9井—茨 80井、龙 12井—龙 2 4井等区域为寻找不整合面之下遮挡油气藏的有利地区 ,茨 6 7—茨 6 15区域是该不整合面之上油气聚集的有利区     

Compact difference approximation with consistent boundary condition

For simulating multi-scale complex flow fields it should be noted that all the physical quantities we are interested in must be simulated well. With limitation of the computer resources it is preferred to use high order accurate difference schemes. Because of their high accuracy and small stencil of grid points computational fluid dynamics (CFD) workers pay more attention to compact schemes recently. For simulating the complex flow fields the treatment of boundary conditions at the far field boundary points and near far field boundary points is very important. According to authors' experience and published results some aspects of boundary condition treatment for far field boundary are presented, and the emphasis is on treatment of boundary conditions for the upwind compact schemes. The consistent treatment of boundary conditions at the near boundary points is also discussed. At the end of the paper are given some numerical examples. The computed results with presented method are satisfactory.     

Contributions of different land cover types in Otindag Sandy Land and Bashang area of Hebei Province to the material source of sand stormy weather in Beijing

Different land cover types in Otindag Sandy Land and Bashang area of Hebei Province are linked to a material source of sand stormy weather in Beijing based on results of field vegetation and soil survey and laboratory works. Results of grain size analysis show that dust release potential in per unit area of moving sandy land is small,while lowland meadow and meadow steppe in stony hills have high potential of releasing dusts in per unit area during sand stormy weather occurrence. Further considering the effects of vegetation, it is inferred that the moving sandy land served as a material source of past dust storm and the possibility of dust release in per unit area is low in current time.Typical steppe in stony hills is undergoing desertification and its dust release possibility in per unit area is high. Farmland has strong potential of release dusts when they are ploughed in spring, but a large amount of therophytes grow and thus prevent dusts from release when cultivation was terminated.Potentials of dust release in per unit area in fixed sand dunes,stony mountain meadow steppe and low land meadow are lowdue to high cover of perennials. Sand dune reactivation and desiccation of lakes and lowlands under estimated future climatic change will make them serve as a future material source of sand stormy weather.