热液成矿系统中一维反应扩散过程的混沌边缘

用耦合单峰映象格子模型描述了一维热液成矿系统的反应扩散过程 ,在a×ε =[0 ,2 ]× [0 ,1 ]参数空间内模拟计算了模型的静态斑图熵、斑图动力学熵和最大李雅普洛夫指数等动力系统刻画量 ,结合系统的空间振幅变化图、时空行为发展图和空间功率谱特征 ,对热液成矿过程的动力学行为进行了研究 ,结果表明成矿发生在混沌边缘 ,并且指出了参数空间中的混沌边缘域     

地震应急卫星通信网路由异常分析

地震应急卫星通信网一直存在路由异常的问题,时常造成卫星站点通信不畅。通过对网络拓扑结构进行分析,总结造成路由异常的原因。通过列举实例,提出以通过设置静态路由的方式,来解决目前网络中存在的路由异常问题。     

土地利用配置的混沌蚁群优化算法研究

土地利用优化配置是促进土地可持续发展的重要举措,然而现有研究缺乏有效求解土地利用优化配置模型的新型混合式智能优化算法。本文结合蚁群算法和混沌模型,形成混沌蚁群优化（Chaos Ant Colony Optimization,CACO）算法,并以广州市增城区为研究区,对土地利用现状进行优化配置;然后在数量结构、目标函数值、空间布局等方面将优化结果与土地现状及标准蚁群算法优化结果进行对比分析。结果表明：① CACO算法能在满足多种约束条件下,有效解决多目标土地利用优化配置问题;② 与标准蚁群算法相比,CACO算法能增加土地利用的经济效益7.18亿元、生态效益0.33亿元、社会效益1.13%,同时降低地类转换成本1.15%;③ CACO算法能使土地利用现状空间分布多样性和均匀性的下降控制在1.30%以内,同时缩减地块数量8.86%,并使平均斑块大小增加9.77%,从而提升土地集约利用水平,更合理地配置各现状地类的空间分布,为研究区土地利用的科学规划与决策提供支持。     

利用地震属性技术研究岩溶裂隙发育带

利用地震属性技术,从三维地震数据体中提取对岩溶裂隙发育带相关的二维分形参数,预测岩溶裂隙发育带、奥灰顶部岩层的富水性以及有关的水文地质条件,为高产高效矿井地质保障系统提供依据。通过许厂煤矿430采区实际资料的检验,预测的地质效果良好。     

湖南郴州柿竹园超大型钨多金属矿床的成矿复杂性研究

用非线性科学和复杂性理论对湖南郴州柿竹园超大型钨多金属矿床的成矿复杂性进行系统、深入的研究 ,以成矿作用与时空结构是一切矿产资源的本质与核心的自然哲学理念为根本立足点 ,从一种新的视角 ,就矿床的动力学属性、矿床的物质成分与结构、矿床的地质学场和成矿系统的演化四大相互联系的范畴 ,对矿产资源进行再认识 ,提出了矿床的新定义 ,并较深刻地揭示了矿床的动力学属性、成矿物质高度多样化和复杂性及其超常规模集成、矿田成矿分带的内部结构、矿床地质学场的时空分形结构、成矿系统时间演化的长期性和成矿过程的多期多阶段性以及成矿作用的发生和矿床形成的分形生长机制等方面的复杂性与动力学本质。项目成果将矿床学的研究提高到非线性科学和复杂性理论的层次 ,提供了如何应用这种理论和方法对矿床的成矿复杂性进行研究的实例 ,也是第一作者所提出的关于成矿系统复杂性的新成矿理论与方法论“成矿动力系统在混沌边缘分形生长”的具体化及其进一步深化。沿着这一研究方向的不断开拓将可使传统矿床学向精确科学跨越。     

苏北溱潼凹陷非线性动力学特征浅析

混沌动力学研究提出的方法，可以从观测数据角度重建系统的演变规则。本文在扼要介绍非线性数学模型反演理论的基础上，采用时序资料重建复杂系统动力学特征的方法，求得苏北溱潼凹陷演化的非线性动力学方程，并对系统Ｌｙａｐｕｎｏｖ指数、熵及Ｌｙａｐｕｎｏｖ维数的变化特征和溱潼凹陷演化过程的混沌特征进行了研究和初步分析，为分析盆地演化特征提供了方法。系统信息维的变化特征，反映了滤潼地区断陷阶段活动剧烈、凹陷阶段活     

Localized folding of viscoelastic layers

Naturally occurring fold systems are typically irregular. Although such systems may sometimes be approximated by a periodic geometry, in reality they are commonly aperiodic. Ord (1994) has proposed that naturally occurring fold systems may display spatial chaos in their geometry. Previous work has indicated that linear theories for the formation of fold systems, such as those developed by Biot (1965), result in strictly periodic geometries. In this paper the development of spatially chaotic geometries is explored for a thin compressed elastic layer embedded in a viscoelastic medium which shows elastic softening. In particular, it is shown that spatially localized forms of buckling can develop and the evolution of these systems in the time domain is presented. A nonlinear partial differential equation, fourth order in a spatial variable and first order in time, is found to govern the evolution. A related nonlinear fourth-order ordinary differential equation governs an initial elastic phase of folding. The latter equation belongs to a class with spatially chaotic solutions. The paper reviews the implications of localization in the geological framework, and draws some tentative conclusions about the development of spatial chaos. Crudely arrived-at, yet plausible, evolutionary time plots under the constraint of constant applied end displacement are presented. Emphasis throughout is on phenomenology, rather than underlying mathematics or numerics.     

Chaos and secondary resonances in the mimas–tethys system

We have investigated the role of the 200yr period discovered by Vienne and Duriez (1992) on the tidal evolution of the Mimas–Tethys system through the 2:4 ii present resonance. Three terms are found to generate this period. We present a perturbedpendulum model in which these terms bring about a perturbation to the ideal ii resonance pendulum, which is in a direct ratio to the eccentricity e of Tethys. Although e is now very small, it is shown that this quantity could have been much greater in the past. We also show, thanks to this model, that these terms may have brought about a stochastic layer of noticeable width at the time of capture in the ii resonance, with the consequence that the possible values of the inclination i of Mimas before capture range from 0.4° to 0.6° (these uncertainties arise from the present uncertainties on e). The role of each one of the three terms is examined in the appearance of chaos. A capture into the 1/1 secondary resonance (between the libration period of the primary ii resonance and the period of about 200yr) is found possible. It means that the system could have experienced several captures in the primary resonance, instead of a single one, and that i could have been, with this assumption, much lower than 0.4°. A probability of capture into this secondary resonance as a function of the eccentricity of Tethys on encounter is derived, using Malhotra's method (Malhotra, 1990). Allan's values of i = 0.42° and e 0 (Allan, 1969) are therefore called into question, and taking e 0 is shown to be absolutely necessary if we want to understand the phenomena at work in the Mimas–Tethys system.     

B-ZCNN的混沌边缘和局部活性域

将由Zhabotinski反应扩散方程对应的非线性细胞网络方程称为B ZCNN ,应用局部活性理论中关于两个状态变量的反应扩散CNNs的结果 ,讨论计算了B ZCNN的局部活性域和混沌边缘域 ,因此确定了该系统可能出现的复杂性动力学行为的系统参数的范围。取处在混沌边缘域内系统参数点进行模拟 ,得到了嵌套式目标斑图等时空有序结构。最后指出局部活性是成矿发生的必要条件 ,研究成矿发生应该从成矿系统参数域的局部活性研究入手。     

长江日流量混沌变化特性研究——Ⅱ相空间嵌入维数的确定

为了以新途径探索长江水量变化规律并在此基础上做出预测,全面而系统地研究了宜昌站日流量混沌变化特性并建立了新预测模型.重点论述相空间嵌入维数的确定.嵌入维数是混沌分析的一个重要参数.给出了饱和关联维数法、伪最邻近点法和真实矢量场法3种嵌入维数的确定方法.它们各有优缺点.研究结果表明,最优嵌入维数的确定必须进行综合分析并考虑最优嵌入窗宽.