苏南块体的深部构造及其油气前景

苏南块体中地壳存在一低速层,Vp约为5.8～6.0km/s,它与地下高导层相对应,电阻率仅4～20Ω·m,是中地壳塑性层的反映;苏南块体属于太平洋型块体,是有利的油气分布区块;它处在地球化学急变带上,壳幔相互作用比较强烈,故该区的油气受深部因素的影响或控制比较明显,是有利的深部无机成因油气分布区。中地壳低速高导层(蛇纹石化橄榄岩)构成油气“发生器”;上地幔则是“原料库”;沉积盆地是“存储器”。当地幔流体中H2缺失或不足时便没有烃生成,只能形成CO2或以CO2为主的气藏。黄桥CO2气藏已被公认是幔源无机成因气体,实质上是由在中地壳进行的不完整费-托合成反应所致。镇江—常州—无锡—苏州—昆山一带为油气富集带,具有深部成因油气的良好远景。     

MATHEMATICAL MODEL OF SLUDGE SEDIMENTATION

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Directional interpolation of multicomponent data

A method for interpolation of multicomponent streamer data based on using the local directionality structure is presented. The derivative components are used to estimate a vector field that locally describes the direction with the least variability. Given this vector field, the interpolation can be phrased in terms of the solution of a partial differential equation that describes how energy is transported between regions of missing data. The approach can be efficiently implemented using readily available routines for computer graphics. The method is robust to noise in the measurements and particularly towards high levels of low‐frequent noise that is present in the derivative components of the multicomponent streamer data.     

基于地缘影响力模型的大国地缘政治博弈——以钓鱼岛问题背景下的中美博弈为例

大国地缘政治博弈事关国家安全,影响世界格局。通过对地理要素的综合考量构建了地缘影响力模型,并基于博弈论建立了钓鱼岛问题大国地缘政治博弈树,对中美博弈过程进行了分析。最后针对钓鱼岛问题4种博弈走势提出了战略应对参考建议。研究结果表明：①在中国大陆主导时,各国保持合作将共赢,一旦动武,若美俄地缘战略决策指数不高,形势对中国大陆不利。②当美国地缘战略决策指数较小,俄罗斯较大时,是解决钓鱼岛问题的战略良机。③中国台湾是中国解决钓鱼岛问题的重要影响因素,要灵活把握与处理。④ 在4种战略博弈形势下,均存在中美战略博弈的纳什均衡,但美国、日本和中国台湾有一定概率铤而走险,要保持警惕并做好战略应对。⑤ 博弈分析结果较为客观的反映了钓鱼岛问题的多种战略走向,并与当前相关大国关于钓鱼岛问题的战略基本吻合,印证了地缘影响力模型对地理要素量化的可行性以及大国地缘政治博弈分析方法的合理性。     

四川泸州地区测震台网地震监测能力研究

为加强川南泸州区域的地震监测能力,新建15个流动测震台站,与泸州和荣昌2个固定台站形成泸州台网.根据《地震震级的规定GB 17740-2017》,计算了泸州台网的震级监测能力,并通过实际地震事件的统计分析,验证了震级监测能力计算结果的准确性和合理性.基于D值理论,计算了泸州台网在研究区域的震中定位误差和震源深度定位误差...     

灰色系统理论在建筑物变形分析中的应用

介绍了灰色系统理论的原理以及计算过程,并应用其对建筑物的变形进行定量分析与变形预报,取得较好的效果。     

Rigid‐plastic seismic design of reinforced concrete structures

In this paper a new seismic design procedure for Reinforced Concrete (R/C) structures is proposed—the Rigid‐Plastic Seismic Design (RPSD) method. This is a design procedure based on Non‐Linear Time‐ History Analysis (NLTHA) for systems expected to perform in the non‐linear range during a lifetime earthquake event. The theoretical background is the Theory of Plasticity (Rigid‐Plastic Structures). Firstly, a collapse mechanism is chosen and the corresponding stress field is made safe outside the regions where plastic behaviour takes place. It is shown that this allows the determination of the required structural strength with respect to a pre‐defined performance parameter using a rigid‐plastic response spectrum, which is characteristic of the ground motion alone. The maximum strength demand at any point is solely dependent on the intensity of the ground motion, which facilitates the task of distributing required strength throughout the structure. Any artificial considerations intended to adjust results according to empirical observations are avoided, which, from a conceptual point of view, is considered to be an advantage over other simplified design procedures for seismic design. The procedure is formulated using a step‐by‐step format followed by a design example of a 4‐storey‐R/C‐plane‐frame. Results are compared with refined NLTHA and found to be extremely encouraging. Copyright © 2006 John Wiley & Sons, Ltd.     

邓小平语言中的礼貌现象

《邓小平文选》是领导者语言的范例，存在大量的礼貌现象．体现着礼貌的思想。它们的运用可以给交际对方留面子，从而使交际活动更好地进行下去。以Brown和Levinson的面子保全论为理论基础，运用Leeoh的礼貌原则及六个次准则分析了《邓小平文选》领导语言中的各种礼貌的语言现象，其实现途径以及它的内在语用机制。这说明礼貌理论对文本交际活动也具有很强的阐释力。     

Equation of a Barotropic Fluid on a Rotating Spherical Surface and its Inertial Manifold

The inertial manifold is a positive invariant set which exponentially attracts all the trajectories of a dissipative dynamic system. It was introduced for the purpose of studying the asymptotic behaviour of such systems. The initial infinitely dimensional dynamic system, generated by a partial differential evolution equation, can be projected on to it, in order to obtain the final system of ordinary differential equations (inertial equations). These equations then simulate the initial object. Although the inertial manifold is an object relatively simpler than the attractor (a very complicated set of non-integer dimension may be an attractor) it is more difficult to prove its existence than that of the attractor. The equation of a barotropic fluid on a rotating spherical surface is one of the examples of dissipative dynamic systems with an inertial manifold. This kindles the hope that also the equations of the dynamics of the real atmosphere will have an inertial manifold. The reduction of the sample system to this Lipschitz manifold of finite dimension thus justifies us in analysing the behaviour of the atmosphere on non-linear models of finite dimensions and few parameters, in a finite system of ordinary differential equations.     

地震时间序列多重分形计算精度估计

目前计算地震时间分形的方法很多,但具体各种计算方法的误差（或精度）是多少,还没有一个定量的结果。本文针对这一问题,利用Ｃａｎｔｏｒ多分形集理论模型数值模拟来估算其精度（误差）,进而解决了限、离散、点集的多重分形维数谱的计算精度（误差）估计问题。通过一维（时间）理论模型数值模拟得出如下结论：（１）存在尺度问题、样本容量问题、基准点选取问题、不同计算方法差异等;（２）固定质量（ＭＡＳ）法和最小生成树（