基于改进遗传算法的非线性半刚接钢框架优化

运用小生境技术的改进遗传算法对半刚接多层钢框架进行优化设计,提高了算法的收敛性,可直接从H型钢表或热轧型钢表中选取截面,并且从用钢量角度分析了二阶效应对半刚接钢框架的影响.实际算例表明半刚性连接会使二阶效应的影响增大,用钢量也随之增加.     

带有随机时滞的非线性网络控制系统的镇定

考虑了一类非线性离散系统的网络控制问题.通过齐次马尔可夫链描述采样器-控制器和控制器-执行器的时延,将网络控制系统建模为带跳非线性系统.利用Lyapunov方法和线性矩阵不等式技巧,得到了系统随机稳定的充分条件,并给出了镇定控制器的设计方法.数值例子的仿真结果验证了所得方法的有效性.     

对流扩散方程基于三次周期样条插值紧致特征差分法

对一维对流扩散方程给出了一个在空闯方向计算精度比较高的紧致特征差分格式，该差分格式中的插值部分运用了三次周期样条插值，同时给出了L2模的误差估计式．数值算例表明格式在很大程度上消除了插值误差对计算格式的影响，具有比较好的计算效果．     

具有实际地形的溃堤水流数值模拟

为了减小因溃堤洪水而造成的人员生命和财产损失,建立了能够模拟具有实际地形的溃堤水流的数学模型。该模型基于非结构网格的有限体积法,采用HLL格式的近似R iem ann解计算界面通量,并利用TVD-MU SCL格式和H ancock格式将计算精度升高到二阶。对底坡源项采用分解法处理,对摩阻项采用了半隐式离散的方法来增加计算的稳定性。通过溃坝算例和混合流算例,验证了该方法的稳定性、和谐性和健全性。该模型已应用于哈尔滨市松北区溃堤水流的模拟。结果表明,该模型能较好地模拟具有实际地形的溃堤水流运动。     

一类快速非线性预测控制的分析与改进

针对仿射非线性系统,分析了一类快速预测控制算法稳态误差的来源,给出了误差的解析表达式.通过反馈校正消除稳态误差,提高了算法对模型失配的鲁棒性.对水箱液位控制系统的仿真和实验研究,结果验证了分析和改进的有效性.     

弱条件下二阶椭圆问题求解的数值积分格式与收敛性分析

给出了一种带有数值积分方案的求解二阶椭圆问题的有限元计算格式.与精确方法相比,仍保持收敛性和收敛价,并在较弱条件下给出了收敛性分析.数值算例说明算法可行,并且与理论分析结果一致.     

锚支巷道沿空延迟冒落采空区风流规律研究

锚杆锚索支护的回采巷道采后不及时冒落,形成特殊的沿空漏风边界的采空区流场.运用有限元数值模拟方法,结合铁法小青矿S2-705工作面现场实际,从理论上描绘了采空区漏风流动规律的改变特征,给出风流强度分布图解.研究认为,不冒落形成的沿空漏风边界是工作面向采空区的漏入、漏回的主流边界,漏风强度最高;贴近工作面边界的冒落非压实带存在平行渗流.这种流势导致了在下游回风侧的沿空巷道内形成瓦斯集聚,并提出了预先拆锚杆卸顶或局部通风机抽排放两种解决途径.图5,参5.     

BBM方程的精确解

利用齐次平衡法和一个辅助的常微分方程,研究了BBM方程的椭圆函数解,其中包括了Jacobi正弦函数解、余弦函数解、第三类Jacobi椭圆函数解及其组合形式解.这种方法可应用于其他的非线性演化方程的求解.     

Nonlinear interactions between gravity waves and background winds

Using the nonlinear propagating gravity waves (GW) model in the two-dimensional compressible atmosphere and the linear GW theory, the process of GW propagation in different background winds, e.g. the direction of the background wind is opposite to (dead wind) or the same as (tail wind) the direction of the horizontal phase velocity of GW, is studied. The results show that the dead wind prolongs the vertical wavelength and accelerates GW propagation. Therefore, GW propagates up to a higher height becomes instable in a short time and eventually induces an inverse jet flow. Then, the vertical wavelength is becoming short due to the nonlinear interactions between GW and the inverse jet flow. The vertical wavelength and group velocity decrease after GW propagates into the tail wind. The initial instable time is delayed. Although most of GW is trapped in the instable region, some of GW propagates above the instable region. Compared with GW propagation in the tail wind, the nonlinear interactions between GW and the dead wind are also strong. In contrast, the linear GW theory predicts that GW can propagate freely in the dead wind. The vertical wavelength simulated by the nonlinear numerical model is different from that predicted by the linear theory greatly after GW propagates into the dead wind.     

Wavelet Numerical Solutions for Weakly Singular Fredholm Integral Equations of the Second Kind

Daubechies interval wavelet is used to solve numerically weakly singular Fredholm integral equations of the second kind. Utilizing the orthogonality of the wavelet basis,the integral equation is reduced into a linear system of equations. The vanishing moments of the wavelet make the wavelet coefficient matrices sparse,while the continuity of the derivative functions of basis overcomes naturally the singular problem of the integral solution. The uniform convergence of the approximate solution by the wavelet method is proved and the error bound is given. Finally,numerical example is presented to show the application of the wavelet method.