科技交流中心刚性屋面索穹顶结构施工

无锡新区科技交流中心G区部分屋盖采用刚性圆形屋面空间索穹顶结构,该结构体系由上弦脊索、下弦斜索、环索、压杆、外环受压环及内环刚性拉力环构成,为肋环型索穹顶结构体系。索穹顶结构平面为圆形,屋面覆盖材料采用铝板和玻璃结合的刚性屋面,刚性屋面与下部索穹顶结构体系结合,是目前国内第一个空间索穹顶结构实例。施工方法可供类似工程参考。     

标志索升降器简介

水文站的测速、取沙,一般采用固定垂线法,因此在河宽不大的测站,都可用固定标志索来定位。该方法的特点是简单易行,缺点是当水位变化后,因标志索重锤高度固死,造成中、低水位挂锤悬空过高,从而使定位不准。我们在标志索上加了一套升降器,用     

柔索桩护坡技术

柔索桩是一种新型的护坡桩。在基坑外围将钢筋、铜棒或钢管等柔索材料按网格状平面布置，竖向植入土体内，周围灌浆或灌砂与土体紧密结合，桩端进入基坑底面标高下一定深度或计算的滑裂面下的稳固土体内，桩顶用混凝土梁或锚板将成排的桩群联成整体。这种上下紧箍的钢筋、铜棒或钢管等柔索材料与周围土体形成一个良好的三维高强复合土体。     

水文缆道循环索的应急修架

介绍了一种水文缆道循环索的应急修架方法.     

基于Strand7平台的索膜结构找形分析及API程序实现

索膜结构为柔性的张拉结构体系,必须通过施加预应力和调整结构曲面曲率使之处于稳定的初始平衡状态,本文采用非线性有限元找形方法,以大型通用有限元软件Strand7为平台,用其二次开发程序Strand 7API编制了相应的程序,对两个典型的索膜结构实例和一个大型索膜结构工程进行了找形验证。分析结果发现该找形方法适合各类索膜结构的找形分析,可以快速有效地得到索膜结构的初始平衡形态。     

水文缆道循环索托架简介

水文缆道循环索托架简介游立潜，李庆金（黄委会山东水文水资源局）１前言水文缆道在６０至７０年代，大多架设在中小河流上，跨度一般在１００～２００ｍ，最大也只有３００ｍ。在大江大河上推广应用受到限制，主要因为跨度一大，由循环系统引起的测深、测距误差较大，且...     

城基于Strand7平台的索膜结构找形分析及API程序实现

索膜结构为柔性的张拉结构体系,必须通过施加预应力和调整结构曲面曲率使之处于稳定的初始平衡状态,本文采用非线性有限元找形方法,以大型通用有限元软件Strand7为平台,用其二次开发程序Strand7API编制了相应的程序,对两个典型的索膜结构实例和一个大型索膜结构工程进行了找形验证.分析结果发现该找形方法适合各类索膜结构的找形分析,可以快速有效地得到索膜结构的初始平衡形态.     

柔索桩护坡技术

柔索桩是一种新型的护坡桩。在基坑外围将钢筋、铜棒或钢管等柔索材料按网格状平面布置,竖向植入土体内,周围灌浆或灌砂与土体紧密结合,桩端进入基坑底面标高下一定深度或计算的滑裂面下的稳固土体内,桩预用混凝土梁或锚板将成排的桩群联成整体。这种上下紧箍的钢筋、铜棒或钢管等柔索材料与周围土体形成一个良好的三维高强复合土体。     

锚杆(索)作用力学特性分析及让压试验

在对锚杆(索)作用机理及其对岩体作用力学效应分析的基础上,研究了锚杆(索)受力及变形特性,探讨了在锚杆支护中使用碟形托盘及其组合体进行让压支护的可行性,使支护体在高应力大变形或瞬间冲击荷载下,在确保锚杆承载力不受影响前提下有一定变形,通过释放部分应力来实现减少或避免锚杆破断,有效地提高锚杆的支护效果。      

裂隙岩体加索支护模型及其工程应用

根据预应力锚索与裂隙岩体的联合作用机理，在深入研究了裂隙岩体的损伤断裂变形特性以及锚索的空问锚固效应后，建立了一种加索支护模型模拟锚索对裂隙岩体的加固效果。将建立的力学模型用于指导一岩体边坡工程的支护设计与施工,取得了显著效果。     

Unity of the national and the international in the socio-cultural development of the peoples of the USSR

International unity is becoming ever stronger in this country owing to an increasing similarity in the development of the cultural environment. This comprises the provision of all the country's republics with a sufficient number of schools, theatres, and other institutions and cultural information media in accordance with the needs of the population. An important part is played by the rise in ‘the general educational level, as well as the level of professional qualifications and skills. Among all the Soviet nations and nationalities, this rise being more rapid among formerly backward peoples. Prominent among the factors of internationalization is the progressive development of the nationalities’ cultural resources, while professional culture is being increasingly brought within the reach of the masses.The implementation of the nationalities policy promotes the all-round development of all Soviet nations and nationalities, their drawing together, the upsurge of the individual capabilities of every Soviet citizen.     

Deviation of the major axis of the inertia ellipsoid of the Moon from the direction toward the Earth

It is known from observations that the center of mass of the Moon does not coincide with the geometric center of its figure, and the line connecting these two centers is not aligned with the direction toward the center of the Earth, instead deviating toward the Southeast. This stationary deviation of the axis of the inertia ellipsoid of the Moon to the South of the direction toward the Earth is analyzed. A system of five linear differential equations describing the physical libration of the Moon in latitude is considered, and these equations are derived using a new vector method taking into account perturbations from the Earth and partly from the Sun. The characteristic equation of this system is obtained, and all five oscillation frequencies are found. Special attention is paid to the fifth (zero) frequency, for which the solution of the latitude libration equations are stationary and represents a previously unknown additional motion of the rotational axis of theMoon in a cone with a small opening angle. In contrast to the astronomical precession of the Earth, the rotation of the angular-velocity vector is in the positive direction (counter-clockwise), with the period T ₃ = 27.32 days. On this basis, this phenomenon has been named “quasi-precession.” This quasi-precession leads to a stationary inclination of the major axis of the inertia ellipsoid of theMoon to the South (for an observer on Earth), making it possible to explain one component of the observed deviation of the center of mass of the Moon from the direction toward the Earth. The opening angle of the quasiprecession cone is approximately 0.834″.     

Global repeating events in the history of the Earth and the motion of the Sun in the Galaxy

Chronological analyses of correlations between certain global repeating events (mass extinctions of marine organisms, meteorite impacts, and flashes in the frequency of geomagnetic reversals) during the Phanerozoic Eon and the motion of the solar system in the Galaxy are presented for five rotationally symmetrical models for the regular Galactic gravitational field. Thirteen of sixteen mass-extinction events can be described by a repetition interval of 183±3 million years. This is in agreement with the anomalistic period (interval between two subsequent passages of the Sun through the apocenter of its Galactic orbit) in the model of Allen and Martos. The positions of the minima and maxima in Gaussian functions approximating the frequency distribution for geomagnetic reversals also agree with the times of passage of the Sun through the apocenter and pericenter, respectively, of its Galactic orbit in this model. The maximum in the distribution of the deviations of the dates of mass extinctions from the nearest dates of impacts of large, crater-forming bodies is close to zero, providing evidence that many such events are correlated. As a rule, extinctions follow impact events. The impacts of large bodies have occurred most often when the solar system passes through the Galactic plane, while mass extinctions occur more often at some distance from the Galactic plane (about 40 pc). As a rule, intervals of increases in the frequency of geomagnetic reversals coincide with dates of impacts of large bodies. At the same time, these intervals do not show a clear correlation with the dates of mass extinctions. The intensity of mass extinctions, like the energy released by impacts, is consistently higher in periods when the Sun is moving from the apocenter toward the pericenter of its orbit, than when it is moving from the pericenter toward the apocenter. Thus, there is evidence for a variety of relationships between repeating global events in the Phanerozoic and the motion of the Sun in the Galaxy. Long-period variations in the frequency of geomagnetic reversals are correlated with the orbital motion of the Sun, and increases in the frequency of geomagnetic reversals are correlated with impacts. Mass extinctions are correlated with the impacts of large bodies, whose motions may have been perturbed by clouds of interstellar material concentrated toward the Galactic plane and by the shock front associated with the Perseus spiral arm, through which the solar system passes. The velocity of the Sun relative to the spiral pattern is estimated.     

摩擦桩基桩土间极限摩阻力取值问题探讨

通过对广珠东线高速公路横沥大桥的试桩及土体的工程地质条件分析,总结出影响摩擦桩基桩土间极限摩阻力取值的一般问题以及解决问题的方法和措施。     

从榴辉岩与围岩的关系论苏鲁榴辉岩的形成与折返

位于华北和扬子两板块碰撞带中的苏鲁榴辉岩形成的温压条件不但是超高压，而且是高温。榴辉岩的PTt轨迹表明其为陆-陆磁撞俯冲带的产物。榴辉岩的区域性围岩花岗质片麻岩为新元古代同碰撞期花岗岩，榴辉岩及其他直接围岩皆呈包体存在于其中，并见新元古代花岗岩呈脉状侵入榴辉岩包体中。区域性围岩新元古代花岗岩的锆石中发现有柯石英、绿辉石等包裹体，表明新元古代花岗岩的组成物质也经受过超高压变质作用，且榴辉岩与围岩新元古代花岗岩的锆石U-Pb体系同位素年龄基本相同。但新元古代花岗岩所记录的变质作用和变形作用期次（或阶段）却少于榴辉岩。椐上述可得如下推断：超高压榴辉岩与新元古代花岗岩岩浆是同时在碰撞带底部（俯冲板块前部）形成的；榴辉岩的第一折返阶段是由新元古代花岗岩岩浆携带上升的，其第二折返阶段是和新元古代花岗岩一起由逆冲及区域性隆起而上升，遭受剥蚀。     

某高速公路下伏煤矿采空区稳定性分析

在论述某高速公路下伏砦脖煤矿采空区地质、采矿和工程地质特征的基础上, 进行了稳定性数值模拟分析, 定性与定量地分析与评价了该煤矿采空区的地表变形特征及稳定性。研究结果表明: 该煤矿采空区的变形尚未完成, 对拟建的高速公路将产生很大的危害, 必须采取相应的工程治理措施。      

The Importance of the Precipitation and the Susceptibility of the Slopes for the Triggering of Landslides Along the Roads

In order to characterise the influence of the heavyrains on the observed landslides during the 1996–1997hydrological cycle, rainfall records for the last 100years are analysed from 104 stations in easternAndalusia. Regarding the amounts of rain recordedbetween October 1996 and March 1997 in the 104stations studied, 31 presented new all-time records;15 presented values that were 80–100% of thepre-1995 record; 49 stations, 80–50%; and 9stations, < 50%. A map has been devised of thesusceptibility of the materials through which thesouth-eastern Andalusian road network crosses,together with an inventory of the damage caused byinstability phenomena on banks and cuttings of theroad network during the winter of 1996–1997. Therelationships between the rainfall during the studyperiod, the damage caused to the road network and thesusceptibility of the materials affected are analysed.The results indicate that there is a clearcorrespondence between the rainfall recorded and thesusceptibility of the materials with the inventorieddamage. It is concluded that the widespread seriousdamage caused in early 1997 to the roads andsurrounding areas in the Alpujarra region and thecoast of the Province of Granada was mainly caused bythe extraordinarily heavy rains. However, considerablyless damage was observed where the susceptibility ofthe terrain is low, thus highlighting the extremeusefulness of terrain-susceptibility maps for riskprevention and territorial planning.     

On the consistency of proposed models for the Pyrenees with the structure of the eastern parts of the belt

The structure of the eastern Pyrenees consists mainly of south-directed thrusts involving basement and cover rocks. An antiformal stack developed by the piling up of basement thrust sheets which outcrop in the Axial zone. These structures account for a thin-skinned thrust model rather than a vertical fault model in which the Axial zone would be essentially autochthonous, and the North-Pyrenean fault the axial plane of a fan thrust system. New data from the Eastern Pyrenees and the thin-skinned model suggest that(1) the structure east of the Pedraforca nappe is similar to that of the Central Pyrenees; (2) the cover rocks of the South-Pyrenean units and of the Axial zone-after restoration—built up a northwards-thickening prism consistent with the existence of a unique Pyrenean sedimentary basin during Mesozoic time; (3) the Axial zone is only a complex antiformal stack developed as a part of South-Pyrenean system related to the Paleogene thrusting-tectonics. The Axial zone palaeogeographic area had no special meaning during Mesozoic time.