非线性退缩抛物型方程组初边值问题的可解性

应用上、下解方法证明非线性退缩抛物组初边值问题当1相似文献   

独立数≤5的3-边连通简单图的上可嵌入性

结合边连通度，本文探讨了3-边连通简单网的独立数与上可嵌人性的关系，我们得到了下列结果：设G是一个3-边连通简单图，α（G）是G的独立数，若α／（G）≤5，则G是上可嵌入的，同时我们又得到了两个在3-边连通意义下最小的非上可嵌入图例．     

离散大系统解的有界性与周期解的存在性

本文分别利用向量Ｌｙａｐｕｎｏｖ函数方法和标量Ｌｙａｐｕｎｏｖ函数方法，给出了判定离散大系统解的有界性与周期解的存在性的充分条件，并讨论了一类具有非线性时变周期离散大系统的平稳振荡存在性问题．     

有交易费用的衍生物定价模型

该文对考虑交易费费用的衍生物定价方程进行了研究，证明了在一定条件下其可化为线性偏微分方程求解，并得出了具体的定价公式。     

CONSTRUCTIVE KISSING NUMBERS IN HIGH-DIMENSIONAL SPACES

In the present paper, we focus on constructive spherical codes. By employing algebraic geometry codes, we give an explicit construction of spherical code sequences. By making use of the idea involved in the proof of the Gilbert-Varshamov bound in coding theory, we construct a spherical code sequence in exponential time which meets the best-known asymptotic bound by Shamsiev and Wyner.     

矿井瓦斯来源分析

从矿井瓦斯的来源、瓦斯的运移及运移参数,表明上邻近层是回采面瓦斯的主要来源,指出瓦斯抽放是治理瓦斯的治本措施。     

关于点变差函数的某些性质

设ｆ（ｘ）为定义于区间Ⅰ（有限或无限）上的有限实函数。任给实数δ＞０，ｘ∈０，∈Ｉ，Ｖ＾Ｘ＋δＸ－δ（ｆ）表示ｆ（ｘ）在［ｘ－δ，ｘ＋δ］上之全变差。     

压水堆控制棒导向筒结构改进对落棒的影响

为改善横向水力载荷对控制棒导向筒的作用，对靠近上腔室出口管嘴附近的控制棒导向筒（对称的４组：０２－２６，０３－２５，１１－２９，１２－２８）加设了保护套．在秦山核电站压水堆上腔室１４的可视化模拟体中，以水为介质进行了实验研究，把结果与未加设保护套的实验结果作了分析比较，得到了对靠近上腔室出口管嘴附近的控制棒导向筒加设保护套有助于改善流场对控制棒导向筒的水力载荷作用和确保控制棒能按指令在导向筒中自由升降和快速下插的结论．     

基于水光电力系统时序生产模拟模型的水光优化配比研究

基于考虑系统负荷、新能源发电出力等时序变化特性的时序生产模拟法,建立了水光电力系统时序生产模拟模型;从系统结构性、经济性、灵活性与可靠性方面综合确定最佳水光容量配比,并通过金沙江上游川藏段水光系统验证了模型的合理性。金沙江上游川藏段光伏电站与水电站出力具有较好的年内、日内互补特性;对于2030年水平年,考虑枯期水电留存,913.6万kW水电配套400万kW光伏的方案综合性能更优,其新增非水可再生电量约60亿kW·h。     

Critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau

Scientific evidence for the upper limit of farmland is proposed. Shallow gully erosion is one of erosion types distributed extensively on sloping farmland in the hilly regions of the Loess Plateau. Field observation and aerial photos interpretation, as well as laboratory experiments show that the shallow gully erosion occurring on the steeper farmland in the hilly regions of the Loess Plateau is an important factor leading to intensive erosion on slope, because of its extensive distribution and intensive runoff collection. The data on the formation, development and distribution of shallow gullies on sloping farmland indicate that critical slope gradient for shallow gully initiation ranges from 15 to 20 degrees with an average of 18.2 degrees. Therefore, it is suggested that critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau should be kept within the critical slope gradient for shallow gully initiation to prevent shallow gully formation in order to control soil loss more effectively. But as the first step, the cultivation on the slopes with slope larger than 25 degrees where the maximum erosion occurs should be strictly forbidden.