中小设计企业 数智化转型势在必行 ——福建博宇建筑设计有限公司数智化转型的实践与思考

近年来,随着国家一系列政策的出台,设计行业从增量市场向存量市场转换,市场竞争愈发激烈.市场容量不断缩减、资源不断向头部企业集中,中小设计企业在同质化竞争的环境下利润率逐年降低.在信息化时代,广大中小设计企业应该为客户提供什么样的产品和服务,如何更好地转型发展,成为摆在广大中小设计企业面前的严峻课题,需要我们认真思考.     

产品创新 服务为先

正建皓科技的专注服务2002年10月,佛山市建皓科技发展有限公司(以下简称"建皓科技")正式成立,公司的宗旨是面向全国设计企业,提供先进的信息化建设解决方案。2009年,随着业务的不断发展,建皓科技总部迁入广州天河软件园(广州建皓信息技术有限公司)。几年来,公司获得了各类奖项,也积累了各行业设计院信息管理系统的开发经验,熟悉了各行业设计院的管理流程及客户需求。在此基础上不断升级、改进与完善了建皓设计院综合信息管理系统,务求实现"实用的才是管用的"这一服务理念。自建皓科技创办以来,着重从以下三个方面来实现建皓综合信息管理系统的改进与完善,为客户提供满意的产品。一是准确理解客户需求,通过对设计企业的广     

符合独特品位的杰作

对这栋房子的设计者来说,挑战之处在于要设计出符合这对夫妇的独特品位的房子;设计作品不只是一个简单符合房主的要求,而是要综合考虑各种风格要求.     

应对变局,谋求发展

<正>在近期召开的全国勘察设计同业协会秘书长工作会议上,"变局"成为与会者关注的热词之一。随着中国社会经济进入转型期,国家层面政令频出,行业发展模式改变,企业普遍面临着客户需求、竞争格局、服务价值体现等方面深层次的变化,这都将为工程勘察设计行业带来颠覆性的影响。如何正确认识并应对诸多变局,已成为工程勘察设计企业实现持续发展面临的巨大考验。     

设计企业未来路在何方——谈设计企业产品和服务关系的演变

<正>设计行业仍有未来，但不是所有的设计企业都有未来。基于过去既定的生产、生活方式已经不在，企业无论是经营逻辑还是产品逻辑，都需要作出调整。设计行业有未来，是因为设计有它的核心价值；部分设计企业没有未来，是因为没有办法帮助客户实现价值，没有提供有价值的产品和服务。     

浅论设计企业的内部质量控制

针对当前设计企业在设计前期服务、方案设计、施工图设计、设计后期服务等四个环节出现的质量问题进行了分析总结,提出了设计企业要提高设计质量,就要对这四个环节实施质量控制的措施。     

坚守在客户身边的彩虹——记客户服务中心成立半周年

北京理正是勘察设计行业中唯一一家能提供全面信息化技术服务的大型软件企业,十几年来始终致力于为设计企业提供全方位服务,CAD辅助设计软件、设计院管理信息系统、协同设计软件这三大系列六十多种软件产品几乎覆盖了设计院信息化建设需求的方方面面.     

大力推进工程总承包 加快勘察设计企业转型升级

正面对产能过剩、固定资产投资结构调整的压力,勘察设计市场竞争越来越激烈。不少设计企业利润下滑,有的企业甚至处于亏损状态。部分行业和领域投资严重下滑,由于专业限制,设计市场必然会出现僧多粥少的现象,导致恶性压价竞争。这是在市场经济环境下产能过剩的反应,但对勘察设计行业来说是结构性过剩问题,是专业技术、从业领域、服务范围不能全面满足工程建设需求的问题。对于设计企业来说,充分发挥专业技术优势,以项目为核心为业主提供全过程技术和管理服务是今后努力的方向。     

项目负责人的人文素养

设计者应当研究不同业主的企业文化。不仅要关心自己专业知识的完善,还需要提高自身的人文素养。尤其是对于设计单位的项目负责人而言,更为重要。     

中国电子院眼中的知识管理

<正>当前社会已经进入移动互联网时代,同时也从传统经济时代转变为知识经济时代,知识管理能力已成为企业的核心管理能力之一。在当前的互联网形势下,如何进行知识管理是每个勘察设计企业面临的难题之一。勘察设计企业是以项目模式为客户提供服务的人力资源密集型组织,项目的执行需要大量知识的运用,反过来知识的产生、利用、创新又源于项目,因此,该类企业的知识管理活动应围绕项目的实施展开。作为一家具有66年历史的勘察设计企业,中国电子工程设计院有限公司(以下简称"中国电子院")深切体会到互联网对知识管理出发点和落脚点的改变,笔者结合多年来在勘察设计企业知识管理方面的实践,阐述在互联网环境下中国电子院对知识管理的认识。     

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。     

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.     

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.