天津水泥工业设计研究院有限公司 以技术创新、装备研发为依托 走“科技型”工程总承包之路

水泥工业是我国国民经济的支柱产业之一,天津水泥工业设计研究院有限公司（以下简称＂天津水泥院＂）是我国水泥工程勘察设计咨询业的主要成员之一。天津水泥院创建于1953年,是新中国成立后最早建立的大型工业设计院之一,2000年国务院勘察设计企业改制后,天津水泥院进入中央企业工委,曾是国资委直接管理的10家设计院之一,2005年伴随企业重组的步伐,天津水泥院进入中央企业——中国中材集团公司。     

发挥技术装备优势实施"走出去"战略(摘要)

天津水泥工业设计研究院（以下简称“天津院”）成立于1953年，是我国最早成立的水泥工业设计院。上世纪70年代末、80年代初，国家先后从天津院抽调部分员工与有关科研院所合并，组建了南京水泥工业设计研究院（以F简称“南京院”）和成都建材工业设计院（以下简称“成都院”）。至此，我国便有了以天津院为代表的_三家水泥设计院（以下简称“水泥行业院”）。[第一段]     

天津水泥工业设计院

值此世界建筑师大会召开之际,天津水泥工业设计院全体员工向大会表示热烈的祝贺！ 国家建材局天津水泥工业设计研究院(TCDRI)成立于1953年,是我国最早建立的主要设计院之一,是全国建材行业实力雄厚的甲级设计院。联合国援建的“中国水泥发展中心”就设在院内。1992年被国家经贸部授予对外经营权。1993年建设部首次在全国评选“勘察设计单位综合实力百强”,我院榜上有名,而且是建材行业唯一一家     

扬企业创新风帆 乘“一带一路”东风走出去

<正>天津水泥工业设计研究院有限公司(以下简称"天津水泥院")成立于1953年,是大型国家骨干工业设计院之一。66年来,伴随中国水泥工业由小变大、由弱变强,从勇担新型干法水泥技术的开发重任,到"一带一路"展现大国央企风范,再到新时代开启数字化、智能化、服务化的新征程,如今的天津水泥院已经发展成为一家国际化工程公司。进入21世纪,国际水泥工程总承包市场增长迅速,这为在技术、装备方面有一定比较     

中机工程总院二级单位产权制度改革的实践

中机国际工程咨询设计总院始建于1951年，前身是机械工业部第七设计研究院，原隶属于机械工业部，是我国勘察设计单位综合实力百强之一。五十多年来，我院为我国的社会主义建设，尤其是为输变电设备行业的电器电材工业的创立和发展，做出了应有贡献。2000年按照国务院“国办发[2000]7l号”文件精神，我院由事业单位改制为科技型企业，是国务院国有资产监督管理委员会管理的大型科研设计单位。     

天津水泥工业设计研究院简介

天津水泥工业设计研究院(TCDRI)成立于1953年,是我国最早建立的主要设计院之一,也是中国第一家水泥专业设计院。现为全国建材行业中实力雄厚的甲级设计院。1992年被国家经贸部授予“直接对外经营权”,1993年、1997年两次被评为“中国勘察设计单位综合实力百强”。1995年被国务院发展研究中心认定为“全国首家设计新型干法水泥生产线的设计研究院”,并收入《中华之最》荣誉大典。1996年在建材设计院中,首家通过了ISO9000质量体系认证。 联合国工发组织援建的“中国水泥发展中心”就设在院内。     

自强不息 开拓前进

一、天津水泥院国外工程开展的回顾 我院建于53年,主要从事水泥工厂的勘测设计工作,在文革以前。我院代表国家先后向卢旺达、阿尔巴尼亚、柬埔寨提供了三个水泥工厂的技术和设备的援助——即所谓的经援项目。81年我院合院于天津,并定名为天津水泥工业设计研究院,考虑到今后水泥市场的格局和国内市场的发展情况,院领导决心开始拓展国际市场,利用我国改革开放的机会,我院引进了一些国外先进的水泥技术,并加强与外国水泥工程公司和商社的联     

发挥技术装备优势实施“走出去”战略(摘要)

天津水泥工业设计研究院(以下简称"天津院")成立于1953年,是我国最早成立的水泥工业设计院。上世纪70年代末、80年代初,国家先后     

以先进的技术装备 实现水泥工业的节能减排

天津水泥工业设计研究院（以下简称天津院）在中国水泥工业发展的不同阶段都发挥了技术引领作用。近几年天津院已经完成从传统单一的设计院到集科研开发、工程设计与技术服务、机电设备制造与成套供货、工程总承包、备品备件物流为一体的大型科技集团的转变。装备产业在天津院四大业务平台中起支撑作用,现可提供20多种水泥生产专业装备的研发、制造、营销及技术服务,其范围包括水泥生产全过程的专业主机设备,包括原料破碎、均化、生料粉磨、生料均化、熟料烧成、水泥粉磨、水泥储存及发运、煤粉制备以及矿渣粉磨等水泥生产过程中的各种主机,还有与各系统相配套的环保设备,以及相关的电控设备。简要介绍了天津院开发设计的主要水泥技术装备。     

热烈庆祝云南化工设计院有限公司成立五周年

云南化工设计院有限公司是云南省化工设计院整体改制设立的工程有限公司。公司始建于1974年．隶属云南煤化工集团有限公司。是知识密集、人才集中、为国家和社会提供智力服务和技术支持的科技型企业．云南省综合性甲级骨干勘察设计单位。     

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.     

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.     

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″.     

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。      

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。     

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.     

Paleomagnetic implications on the evolution of the tethys belt from the atlantic ocean to the pamirs since the triassic

We first re-examined the apparent polar wander curves for stable Eurasia and Africa since the Triassic. These curves were then combined together with curves of North and South America according to the kinematics of the Atlantic ocean and a synthetic polar wander curve was given. Then, most of the paleomagnetic results from the Tethys mobile belt, from the Atlantic to the Pamirs, were analysed.Several groups of plates, microplates and blocks can be seen. First, relatively stable regions like Maghreb and Sicily, which have not moved much. Then we have a group formed by Iberia, Sardinia, Italy and, to a lesser extent, Corsica and the Western and Central Alps. For these blocks, movements are anticlockwise rotations chiefly driven by the anticlockwise rotation of Africa, but they are sometimes stronger.To the east, a major change takes place. The north of the Aegean Sea and the Ionian zone are clockwise rotated and these rotations are recent: Oligocene-Miocene for the first part, Pliocene to the present for the second part.A major problem arises in Turkey, Caucasus and Iran. Paleomagnetic results indicate a position far to the south of Eurasia, and, at the same time, geological evidence is in favour of a position close to Eurasia. We discuss these discrepancies.