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61.
关于地震丛集特征、成因及临界状态的讨论   总被引:10,自引:1,他引:9  
罗灼礼  孟国杰 《地震》2002,22(3):2-14
给出了研究地震临界丛集现象的最新方法,即时间变异诊断方法。讨论了不同类型的地震丛集活动特征和成因,结合中国大陆及邻区M≥ 8. 0大震序列和华北地区自1966年以来M≥6. 0地震序列,研究了丛集状态的自相似性及临界时间分支现象。对发震系统的内部时间给出了定义,并研究了地震丛集的非线性时间结构特征。研究认为: ① 事件的发生意味着系统现存的能量一次跳跃式的释放和状态的一次转换。只有当系统以某种足够随机方式动作时,系统状态才会转换,事件才会发生;② 涨落是系统状态的探测器,在临界状态时系统出现很大的涨落,时间变异系数W= 1。临界丛集是由系统内在随机性决定的,事件发生时间是随机地出现的,未来可能出现不止一次的W= 1的临界点;③ 相继发生的事件(M≥ M0) 可以反映系统的演化过程和特征,丛集是系统演化过程中的有序性和无序性的综合反映;④ 事件丛集和丛集的事件具有自相似性和分形结构,也具有耗散系统的自组织和映射特点;⑤ 根据时间变异系数,系统内部时间(年龄),时间间隔与所经历时间非线性关系式以及映射和迭代方法可以用来预测未来地震趋势和未来M≥ M0 地震发生的可能时间点。  相似文献   
62.
GPS水汽反演技术在四川地区的应用研究   总被引:1,自引:0,他引:1  
根据四川网络GPS站点附近的气压、温度计算了天顶静力学延迟量,经过综合分析,得到了最适于四川地区的天顶静力学延迟模型。建立了适于四川地区的加权平均温度计算公式,并说明了此公式的有效性。使用了全球气压和温度模型(GPT)代替实测气象数据进行水汽反演,将GPT可降水量与实测气象可降水量、探空数据可降水量以及实际降水量进行比较分析,得出了一些有益结论。  相似文献   
63.
Batch kinetic studies were carried out for the removal of safranin from aqueous solution using a biomatrix prepared from rice husk. The adsorption kinetic data were modeled using the pseudo‐first‐order and pseudo‐second‐order kinetic equations. The linear and non‐linear forms of these two widely used kinetic models were compared in this study. In order to determine the best‐fitting equation, the coefficient of determination (r2), the sum of the squares of the errors (SSE), sum of the absolute errors (SAE), average relative error (ARE), hybrid fractional error function (HYBRID), Marquardt's percent standard deviation (MPSD), and the Chi‐squared test (χ2) were used as error analysis methods. Results showed that the non‐linear forms of pseudo‐first‐order and pseudo‐second‐order models were more suitable than the linear forms for fitting the experimental data. Non‐linear method is thus more appropriate for estimating the kinetic parameters and should primarily be used to describe adsorption kinetics.  相似文献   
64.
介绍了对信号与强噪声干扰所进行的非线性变换,以实现对噪声干扰的抑制,可获得高质量的有用信号  相似文献   
65.
Stress affects chemical processes on all scales in the Earth but the magnitude of its effect is debated. Here, I give a new synthesis of the theory that describes the effects of stress on chemistry, elaborating upon work in Materials Science which is built from fundamental thermodynamic laws, and show its significance in Earth Science. There are separate but compatible relationships describing what happens (1) at interfaces and (2) within grains. (1) The main chemical effects of stress in the Earth are due to variations in normal stress along grain interfaces and between interfaces with different orientations. For reactions involving diffusion these variations give effects on mineral stability broadly equivalent to pressure changes of (molar volume)/(molar volume change during reaction) × (stress variation). The volume ratio is generally large and so the effects of normal stress variations are always important since all stressed rocks have interfaces supporting different normal stresses. There is no global chemical equilibrium in a stressed system, so reaction kinetics contribute to ongoing evolution until stresses relax: this evolution can include deformation by diffusion creep and pressure solution, possibly with new mineral growth. These effects are relevant for predicting the conditions for reactions involving fluids, such as serpentinite formation and breakdown (relevant for the Earth's volatile cycles) and for other reactions such as ringwoodite breakdown (relevant for understanding the 660 km mantle discontinuity). (2) Within stressed solid solution grains it is not possible to define chemical potentials of all chemical components since one has to be specified as “immobile.” The chemical potential of a “mobile” component such as an exchange vector can be defined. It depends on the “partial molar strain,” a second rank tensor defining the variation in unit cell geometry with composition. In cubic crystals the partial molar strain is isotropic and the chemical potential of a mobile component depends on mean stress. In other crystal systems the partial molar strain is anisotropic and the chemical potential depends on a “weighted” mean stress; orientation as well as magnitude of stress has an influence. I propose “chemical palaeopiezometry”—the possibility of measuring past stress levels via chemistry. Examples show that stress variations in hundreds of MPa to GPa are required to produce 2% variations in composition but high stresses and/or precise chemical analyses will allow this proposal to be tested. High stresses around inclusions and dislocations could be targeted. So, the weighted mean stress inside grains has an effect which is relatively minor although potentially valuable in explaining chemical variations; the normal stress at interfaces plays the main role in chemical processes and its effects are of significant magnitude.  相似文献   
66.
Estimating elastic parameters from prestack seismic data remains a subject of interest for the exploration and development of hydrocarbon reservoirs. In geophysical inverse problems, data and models are in general non‐linearly related. Linearized inversion methods often have the disadvantage of strong dependence on the initial model. When the initial model is far from the global minimum, inversion iteration is likely to converge to the local minimum. This problem can be avoided by using global optimization methods. In this paper, we implemented and tested a prestack seismic inversion scheme based on a quantum‐behaved particle swarm optimization (QPSO) algorithm aided by an edge‐preserving smoothing ( EPS) operator. We applied the algorithm to estimate elastic parameters from prestack seismic data. Its performance on both synthetic data and real seismic data indicates that QPSO optimization with the EPS operator yields an accurate solution.  相似文献   
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69.
地基GPS遥感大气水汽总量中的"静力延迟"和"湿延迟"   总被引:9,自引:2,他引:7  
李成才  毛节泰 《大气科学》2004,28(5):795-800
介绍了静力延迟和湿延迟概念的由来,推导了由对流层延迟计算水汽总量的一般公式;与李延兴等提出的新模型进行了对比,对其相应的观点提出讨论意见.认为国际上通用的AN模型比较严密地求解了对流层大气水汽总量,不存在与"真值"相比偏小的问题.  相似文献   
70.
陈家炜  张海滨 《海洋通报》2017,36(6):601-610
随着海洋深度的增加,压力逐渐升高而温度逐渐降低。因此,应对压力和温度变化的能力直接影响着海洋动物的垂直分布模式。本文综述了近年来国际上关于压力及温度对海洋动物生理影响的研究进展,概述了3种常用的研究方法,包括直接比较不同深度近缘海洋动物的差异、使用加压装置培养海洋动物、在常压及原位温度下培养深海动物;然后归纳了压力及温度对海洋动物生理的影响,包括有机渗透调节物质浓度及蛋白质序列、胚胎及幼体发育速率和畸变率、行为模式及代谢速率、基因表达水平;最后讨论了海洋动物适应高压环境的生理机制,压力对海洋动物垂直分布的限制能力,以及浅海动物和深海动物的起源关系。  相似文献   
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