二○一九第三届中国工程勘察设计行业创新发展高峰论坛致辞

<正>尊敬的宋春华副部长,各位领导、各位来宾、各位代表:大家上午好!今天,中国勘察设计协会所属的《中国勘察设计》杂志社联合中国武汉工程设计产业联盟共同举办的第三届中国工程勘察设计行业创新发展高峰论坛如期召开了!看到会场上高朋满座,热情飞扬,心情十分激动。这表明大家对论坛主题价值的认同和期盼。在此,我谨代表中国勘察设计协会对宋春华副部长     

河南省勘察设计协会召开第六届第四次理事（扩大）会议

2009年7月10日,河南省勘察设计协会第六届第四次理事会议在郑州召开。河南省副省长张大卫、河南省发展和改革委员会主任张维宁、中国勘察设计协会理事长吴奕良、中国勘察设计协会常务副秘书长王子牛、河南省勘察设计协会常务副理事长林效森及河南省各勘察设计单位负责人等参加了此次会议。     

王素卿司长在北京勘察设计协会第六次会员大会上的讲话

各位领导、各位代表：大家好!非常高兴能参加北京勘察设计协会第六次会员大会,在此,我代表住房和城乡建设部建筑市场监管司向大会的召开表示热烈的祝贺!向北京市的勘察设计企业和广大的勘察设计工作者致以诚挚的问候和良好的祝愿!     

在中国勘察设计协会第五届会员代表大会和全国优秀工程勘察设计奖颁奖大会上的讲话

（2010年7月6日）各位代表,同志们,大家上午好：今天,中国勘察设计协会第五届会员代表大会和2008年度全国优秀工程勘察设计奖颁奖大会同时在这里隆重举行,刚才对获得全国优秀工程勘察设计奖金奖的单位进行了颁奖,中国勘察设计协会也选举产生了新一届理事会,会议开得很成功。在此,我谨代表住房和城乡建设部向新一届理事会的成立表示祝贺!向获奖单位和个人以及全国工程勘察设计工作者致以亲切的慰问和良好的祝愿!下面,我谈几点意见。     

同心协力创新机制共同推动工程咨询设计行业健康发展

各位领导、各位专家、各位来宾:中国工程咨询协会、中国勘察设计协会、中国国际工程咨询协会联合举办的"全国工程咨询设计行业发展高峰论坛",是贯     

奋斗七秩 峥嵘岁月创辉煌 砥砺前行 创新发展续华章——在全国勘察设计同业协会共庆新中国成立70周年大会暨中国勘察设计协会六届二次会员代表大会上的报告

正各位领导,各位代表,同志们:今天,全国勘察设计同业协会的领导以及协会会员单位的代表们在广州隆重集会,召开全国勘察设计同业协会共庆新中国成立70周年大会暨中国勘察设计协会六届二次会员代表大会。首先,我代表中国勘察设计协会对大家出席会议表示热烈的欢迎!对广东省住建厅、广州市住建局的大力支持,对以     

以改革创新促稳求进 为行业发展积极贡献——在中国勘察设计协会五届四次常务理事会议暨全国勘察设计同业协会秘书长工作会议上的讲话

正各位常务理事、各位同业协会秘书长、各位代表:今天,中国勘察设计协会在成都召开五届四次常务理事会和同业协会秘书长工作会议,四川省勘察设计协会为了这次会议做了认真的准备和配合,保证了会议如期的举办。刚才,四川省住房城乡建设厅于桂副厅长、四川省协会赵振元理事长作了致辞;住房城乡建设部人事司郭鹏伟副司长、工程质量安全监管司苗喜梅处长作了讲话,对中国勘察设计协会的工作给予了充分肯     

第三届全国勘察设计行业工程项目管理大会在京召开

正本刊讯6月22日—23日,以"创新管理、提升能力、防范风险、提高效率"为主题的第三届全国勘察设计行业工程项目管理大会在京召开。中国勘察设计协会理事长施设出席大会并致辞;住房和城乡建设部建筑市场监管司二级巡视员江华出席大会并讲话;中国石油和化工勘察设计协会理事长、中国勘察设计协会副理事长兼中国勘察设计协会建设项目管理和工程总承包分会会长荣世立出席大会并作主题演讲;中国勘察设计协会原副理事长、中国勘察设计协会建设项目管理和工程总承包分会名誉会长袁纽等出席大会。大会分别由中国勘察设计协会副理事长王树平,     

在中国勘察设计协会理事长和全国勘察设计同业协会秘书长工作会议上的讲话

尊敬的吴奕良理事长,住房和城乡建设部的各位领导,来自全国各地工程勘察设计行业的各位领导、同志们：非常高兴能参加中国勘察设计协会理事长和全国勘察设计同业协会秘书长工作会议。首先,我谨代表江苏省建设厅对会议的召开表示热烈的祝贺和对各位来苏州指导工作表示热烈的欢迎!为了便于大家了解苏州,指导我省勘察设计行业的工作,借此机会我把江苏省城乡建设工作尤其是勘察设计工作的有关情况作一简要介绍,     

吴奕良理事长在开幕式上的讲话

各位领导,各位来宾,各位代表: 在党的十六大胜利召开的喜庆日子里,由中国勘察设计协会和中国工程咨询协会共同组织召开的“建设项目管理和工程总承包经验交流暨表彰大会”,现在正式开会。首先,让我代表中国勘察设计协会和中国工程咨询协会,向参加本次大会的领导、来宾、代表以及新闻界的朋友们表示热烈的欢迎。     

南秦岭下地壳组成及岩石圈的拆离俯冲作用

根据新提供的Pb同位素组成及岩石地球化学研究成果，本文进一步证实了位于北秦岭北界的明港地区发育的早中生代安山玄武质火山角砾岩岩筒所携带的下地壳捕虏体属于南秦岭。所恢复的南秦岭下地壳剖面自下而上为：底侵成因的变辉长岩-基性麻粒岩(其中含有榴辉岩及辉石岩的透镜体)-酸性麻粒岩。秦岭造山带总体的岩石因模型为：南秦岭(扬子块体)向北拆离俯冲，北秦岭地壳向华北仰冲，华北岩石因呈楔状插入秦岭造山带，拆离面约在中、下地壳之间。南秦岭俯冲岩片延伸的范围在平面上有可能达到400km。     

青藏高原综合观测研究站的回顾与展望

中国科学院青藏高原综合观测研究站从１９８８年建站到１９９８年以来,在各个方面均取得了长足的发展,横向生产性项目的开展和完成不仅解决了部队和地方的实际问题,而且缓和了观测研究站在运行过程中所面临的经费严重不足的问题,同时也为我所冻土专业研究人员提供了在生产中实践的机会,在基础理论研究方面,承担了国家攀登计划项目,国家基金项目,中国科学院重点项目和中国科学院冰冻圈专项项目等的研究工作,在多年冻土变化,     

Principles of spatial organization and evolution of the biosphere and the noosphere

In his last lifetime essay, “A Few Words about the Noosphere”, Academician V.I. Vernadsky (1944) wrote that all living organisms on the planet, including man, are integral to the biosphere of the Earth, its material and energy structure and cannot be physically independent of it even for a minute. However, the substrate that generates all living beings and is no less tightly bound to the biosphere has always been characterized by a significant geochemical heterogeneity, traced both in the vertical and in the lateral structure of all geospheres.

The present work is devoted to three most important aspects of modern geochemistry and biogeochemistry:

• — evolution of the ecological and geochemical state of the environment under conditions of a virgin (anthropogenically untouched) biosphere;
• — structural features of the geochemical organization of the modern noosphere;
• — specificity of the interaction of living matter with the environment under increasing anthropogenic load.

On the basis of theoretical concepts of biogeochemistry and geochemical ecology, formulated in the works of V.I. Vernadsky, A.P. Vinogradov, A.E. Fersman, B.B. Polynov, A.I. Perel’man, M.A. Glazovskaya, V.V. Kovalsky, E. Odum, B. Commoner, E.I. Kolchinskii and others, the author puts forward a hypothesis that there exist two qualitatively different stages in the evolution of the biosphere.The first stage is recognized as the period of natural evolution of the biosphere during which it evolves successively into a more complex and more biogeochemically specialized object. In the course of the geological time, this constantly results, on the one hand, in an increase in species diversity and the perfection of individual species, and, on the other hand, to directed improvement and a greater differentiation of the geochemical conditions of the environment. At this stage, the evolution of all systems of the biosphere that were controlled by the mechanisms of self-organization and self-regulation resulted in the establishment of a dynamic equilibrium, which was responsible for the cycling of all essential chemical elements and therefore providing ecologically optimal geochemical conditions in all ecological niches and for all species and biocenoses inhabiting the biosphere at any given moment.The beginning of the second stage is related to the appearance of reason and qualitative changes in the biosphere caused by the goal-directed activity of the human mind, as an entirely new geological force that appeared to be able not only to disrupt the functioning of natural mechanisms of self-regulation and selforganization, but also to transform the environment in the intersts of a single biological species, Homo sapiens. A direct consequence of this change was the uncontrolled transformation of the natural environment, during which the primary structure (geochemical background) created in the course of billions of years was eventually superimposed by a qualitatively new layer of anthropogenically-derived chemical elements and compounds, thus building an interference pattern of a new geochemical field with which practically all modern living organisms are now forced to interact.An outstanding feature of the new evolutionary stage of the natural environment, called by Vernadsky the noosphere, is that biogeochemical changes at this stage proceed at a rate which exceeds that required for the living matter to adapt to these changes. The result is the disruption of the existing parameters of the biological cycle, leading to the emergence of a significant number of endemic diseases of geochemical nature.The proposed approach was used to prove the anthropogenic genesis of existing geochemical endemic diseases and explain the mechanisms of their appearance. In addition, this approach allowed us to develop a new methodology for mapping zones of ecological and geochemical risk and noticeably simplify the procedure of monitoring distribution and prevention of all diseases of geochemical nature.     

铀钍的地球化学及对地壳演化和生物进化的影响

本文论述了在含挥发份和贫挥发份条件下Ｕ、Ｔｈ的迁移行为及其对地球和行星演化的影响,并阐述了造成地球独特地质演化历史的原因。提出了Ｕ、Ｔｈ在地球中的迁移模式以及该模式对地壳形成、演化的控制作用和对生物发展演化的可能影响。     

Wavelets and the Generalization of the Variogram

The experimental variogram computed in the usual way by the method of moments and the Haar wavelet transform are similar in that they filter data and yield informative summaries that may be interpreted. The variogram filters out constant values; wavelets can filter variation at several spatial scales and thereby provide a richer repertoire for analysis and demand no assumptions other than that of finite variance. This paper compares the two functions, identifying that part of the Haar wavelet transform that gives it its advantages. It goes on to show that the generalized variogram of order k=1, 2, and 3 filters linear, quadratic, and cubic polynomials from the data, respectively, which correspond with more complex wavelets in Daubechies's family. The additional filter coefficients of the latter can reveal features of the data that are not evident in its usual form. Three examples in which data recorded at regular intervals on transects are analyzed illustrate the extended form of the variogram. The apparent periodicity of gilgais in Australia seems to be accentuated as filter coefficients are added, but otherwise the analysis provides no new insight. Analysis of hyerpsectral data with a strong linear trend showed that the wavelet-based variograms filtered it out. Adding filter coefficients in the analysis of the topsoil across the Jurassic scarplands of England changed the upper bound of the variogram; it then resembled the within-class variogram computed by the method of moments. To elucidate these results, we simulated several series of data to represent a random process with values fluctuating about a mean, data with long-range linear trend, data with local trend, and data with stepped transitions. The results suggest that the wavelet variogram can filter out the effects of long-range trend, but not local trend, and of transitions from one class to another, as across boundaries.     

A geodynamic model of the evolution of the Arctic basin and adjacent territories in the Mesozoic and Cenozoic and the outer limit of the Russian Continental Shelf

The tectonic evolution of the Arctic Region in the Mesozoic and Cenozoic is considered with allowance for the Paleozoic stage of evolution of the ancient Arctida continent. A new geodynamic model of the evolution of the Arctic is based on the idea of the development of upper mantle convection beneath the continent caused by subduction of the Pacific lithosphere under the Eurasian and North American lithospheric plates. The structure of the Amerasia and Eurasia basins of the Arctic is shown to have formed progressively due to destruction of the ancient Arctida continent, a retained fragment of which comprises the structural units of the central segment of the Arctic Ocean, including the Lomonosov Ridge, the Alpha-Mendeleev Rise, and the Podvodnikov and Makarov basins. The proposed model is considered to be a scientific substantiation of the updated Russian territorial claim to the UN Commission on the determination of the Limits of the Continental Shelf in the Arctic Region.     

Palaeoecology and the origin of the coconut

While botanists, archaeologists, historians and linguists have contributed to the debate on the origin of the coconut pollen analysts have been silent. This article attempts to integrate the results of recent palaeoecological research with findings from the other disciplines.