混合指数更新模型下平均折现惩罚函数

本文讨论了以混合指数分布为点间间距的更新风险模型下平均折现惩罚函数, 在简单条件下, 利用Dickson and Hipp (2001)中引入的变换方法, 得到了平均折现惩罚函数的Laplace变换的精确表达式.     

Banach空间中极大单调算子的一个邻近点算法

设E是Banach空间,T∶E→2E*是极大单调算子,T-10≠ф.令x0∈E,yn=(J λnT)-1xn en,xn 1=J-1(αnJxn (1-αn)Jyn),n0,λn>0,αn∈[0,1],文章研究了{xn}收敛性.     

离散型半参数广义线性纵向数据模型的方差成分检验

在回归分析中, 随机误差是否存在方差非齐性是大家十分关心的问题, 本文根据Laplace展开原理针对随机效应的影响研究了基于纵向数据的离散型半参数广义线性模型的方差成分检验,得到了Score检验统计量, 最后通过一个实例和计算机模拟验证了本文所提出的方法的有效性.     

Minimax Theorems Involving Two Functions and Strictly Monotone Transformations of Their Values

Two two-function minimax theorems are proved.The concavity-convexity conditions of the twofunctions involve strictly monotone transformations and mixing of the values of the two functions,and aredescribed by the inequalities as upward and weakly downward conditions.     

向量变分不等式的严格可行性问题

本篇文章首先定义了向量变分不等式的严格可行点概念,其次在假设了映射是强(D)-伪单调的情况下,证明了向量变分不等式解集非空有界与其严格可行点存在的等价性问题,推广了在数量变分不等式上得到的相应结果．     

单调和Fuzzy单调变分不等式的补偿方法

在实自反Banach空间,用补偿方法研究单调和Fuzzy单调广义非线性变分不等式,得到了几个解的存在性定理.改进和推广了Browder,Pascali-Sburlan,Zhang等人的各种结果.     

拟单调问题的讨论

This paper gives the necessary condition and one sufficient condition of the quasi-monotonic function, and proves that the linear fractional function is quasi-monotone.     

求解大规模带边界约束二次规划问题的单调投影梯度法

受投影BB(PBB)方法的启发, 提出并分析了求解大规模带边界约束的二次规划问题的单调投影梯度方法. 通过数值实例和数值分析证明,对于此类方法,直接采用负梯度方向计算步长往往会导致糟糕的数值计算效果, 为此提出了利用投影梯度来计算单调步长的思想.大量的数值实验表明所给出的新方法通常要好于PBB方法.     

Cntinuity of Some Classes of Functions Related to Degenerate Parabolic Equations and Its Applications

We study some classes of functions satisfying the assumptions similar to but weaker than those for the classical B2 function classes used in the research of quasi-linear parabolic equations as well as the ones used in the research of degenerate parabolic equations including porous medium equationsl.Comsequently,we prove that a function in such a class is continuous.As an application,we obtain the estimate for the continuous modulus of the solutions of a few degenerate parabolic equations in divergence form,including the anisotropic porous equations.