The dynamics of a unidirectional nonlinear delayed-coupling chaos system is investigated. Based on the local Hopf bifurcation at the zero equilibrium, we prove the global existence of periodic solutions using a global...The dynamics of a unidirectional nonlinear delayed-coupling chaos system is investigated. Based on the local Hopf bifurcation at the zero equilibrium, we prove the global existence of periodic solutions using a global Hopf bifurcation result due to Wu and a Bendixson’s criterion for higher dimensional ordinary differential equations due to Li & Muldowney.展开更多
文摘The dynamics of a unidirectional nonlinear delayed-coupling chaos system is investigated. Based on the local Hopf bifurcation at the zero equilibrium, we prove the global existence of periodic solutions using a global Hopf bifurcation result due to Wu and a Bendixson’s criterion for higher dimensional ordinary differential equations due to Li & Muldowney.
文摘为研究西部寒旱区盐渍土传热传质行为,首先,在无压补给条件下进行非饱和硫酸盐渍土的单向冻结试验;其次,考虑结晶潜热、结晶阻抗及结晶消耗等因素,建立非饱和硫酸盐渍土水-热-盐三场耦合模型;最后,采用COMSOL Multi-physics对耦合模型进行数值模拟,将模拟结果与试验数据进行对比分析.研究结果表明:盐渍土内温度随冻结时长呈三阶段发展,逐步形成上冷下暖的温度梯度;在温度梯度和基质吸力双重驱动下,水、盐向冻结锋位置迁移,冻结锋位置水、盐含量出现峰值,峰值含水率、含盐量相较初始值分别增加2.16%和0.28%;冻结锋沿冻结温度线移动,形成冻结锋面;土柱最大冻结深度约为15.5 cm.
基金the National Natural Science Foundation of China(10662002),the Natural Science Foundation of Guangxi Zhuang Autonomous Region(Grant No.640003)and the Innovation Project of Guangxi Graduate Education(Grant No.2006105930702M15)