香港青马大桥在交通荷载作用下的疲劳评估

在全桥三维有限元模型基础上 ,进行了车载响应分析 ,得到全桥的动力响应 ,并与实测结果进行了分析对比 ;对疲劳危险部位建立局部有限元模型 ,并进行了局部应力分析。在结构健康安全监测系统实测数据基础上 ,得到应变循环标准块 ,用基于热点应力疲劳评估方法对危险部位进行了疲劳寿命评估。     

地震灾害生命损失的时空强分布特征分析

本文简要地分析了全球和我国地震灾害造成人员死亡的历史资料状况，认为在公元１５００年之前可能漏记大量的地震灾害生命损失事件。对近一二百年的资料分析表明，地震灾害生命损失的时间和空间分布显示出不均匀的性质，它不仅与地震活动水平有关，还强烈地依赖于人口密度和建筑物的抗震性能；在历史的地震灾害事件中，人员死亡度与其累加频度之间满足ｌｏｇ∑＝Ａ－ＢＥ的统计关系，表明死亡人数较多的事件，发生次数较少。     

Field test of an intelligent stiffener for bridges at the I-35 Walnut Creek bridge

The addition of controllable hardware to structures to mitigate vibration that results from dynamic loads is an emerging area of technological development. The paper describes the results of a research project that was conducted to test a relatively new approach to structural control: an adjustable semi-active hydraulic actuation system that was attached to an in service interstate bridge. The system, which is powered by a 12-volt automative battery, has been tested over a 2- year period. Data indicates that the system reduces truck induced peak stresses by over 50 per cent, and calculations, per NCHRP 299, indicate that the safe life of the structure is increased by approximately 50 yr. The installed cost of the system represents less than 10 per cent of the cost to replace the bridge. Copyright © 1999 John Wiley & Sons, Ltd.     

洞庭湖湿地植物生活型与生态型

研究植物生活型和生态型可以深刻解析植物群落结构和其环境的关系,对研究植物群落的发生、发展以及演替规律都具有重要意义.通过对洞庭湖湿地植物群落物种生活型及生态型进行调查研究,结果表明:洞庭湖湿地植物主要生长型为草本植物,其次为藤本植物,木本类植物缺乏;生活型主要为一年生植物,其次为地下芽和地面芽植物,高位芽和地上芽植物最少.在不同典型群落中,高位芽和地上芽植物在不同群落中所占比重随着高程的递增而增加,且相同生活型在不同群落中所占的比重也随高程的递增而增加.植物生态型构成中,水分生态型以湿生植物为主,土壤pH值生态型以中性土植物最多,光照强度生态型以阳性植物为主,淤积生态型以非淤积植物最多.洞庭湖湿地不同高程典型植物群落生态型组成为:阳性、旱生、中生、碱性,中性、非淤积型植物主要分布于高、中程区,淤积植物主要分布于低程区;阴性、耐阴性、酸性、碱性、非淤积型植物随高程的递增而递增.在洞庭湖湿地,能同时适应洪水和泥沙淤积胁迫的生长型和生活型所占比例较高.水分是决定不同植物生态型分布的关键因子,在湿地高程区分布的物种更多,植物生态型更丰富.     

矿山钻探应急救援中生命通道的钻井技术以山东栖霞笏山金矿事故救援1号孔为例

矿山事故发生后,首先救人。如果井筒或巷道遭到破坏,救援人员要想到达井下事故现场,必须清理井筒、巷道,如清理所需时间长,危险性高,则必须果断采取地面钻井救人的方法。先钻小眼井,贯通巷道,保障被困矿工生命,包括送风、送给养、送药品、通讯等,称为生命通道;然后,钻进大眼井,实施地面钻井垂直救援,称为救生通道。以栖霞笏山金矿救援1号孔为例,介绍生命通道的钻井工艺技术。     

The impact environment of the Hadean Earth

Impact bombardment in the first billion years of solar system history determined in large part the initial physical and chemical states of the inner planets and their potential to host biospheres. The range of physical states and thermal consequences of the impact epoch, however, are not well quantified. Here, we assess these effects on the young Earth's crust as well as the likelihood that a record of such effects could be preserved in the oldest terrestrial minerals and rocks. We place special emphasis on modeling the thermal effects of the late heavy bombardment (LHB) – a putative spike in the number of impacts at about 3.9 Gyr ago – using several different numerical modeling and analytical techniques. A comprehensive array of impact-produced heat sources was evaluated which includes shock heating, impact melt generation, uplift, and ejecta heating. Results indicate that ∼1.5–2.5 vol.% of the upper 20 km of Earth's crust was melted in the LHB, with only ∼0.3–1.5 vol.% in a molten state at any given time. The model predicts that approximately 5–10% of the planet's surface area was covered by >1 km deep impact melt sheets. A global average of ∼600–800 m of ejecta and ∼800–1000 m of condensed rock vapor is predicted to have been deposited in the LHB, with most of the condensed rock vapor produced by the largest (>100-km) projectiles. To explore for a record of such catastrophic events, we created two- and three-dimensional models of post-impact cooling of ejecta and craters, coupled to diffusion models of radiogenic Pb*-loss in zircons. We used this to estimate what the cumulative effects of putative LHB-induced age resetting would be of Hadean zircons on a global scale. Zircons entrained in ejecta are projected to have the following average global distribution after the end of the LHB: ∼59% with no impact-induced Pb*-loss, ∼26% with partial Pb*-loss and ∼15% with complete Pb*-loss or destruction of the grain. In addition to the relatively high erodibility of ejecta, our results show that if discordant ca. 3.9 Gyr old zones in the Jack Hills zircons are a signature of the LHB, they were most likely sourced from impact ejecta.     

现代海底热水活动的系统性研究及其科学意义

现代海底热水活动是当前地球系统科学研究的一个重要组成部分,它是研究海底地质作用体系中的一个关键环节。海底的构造作用、岩浆活动等因素制约了热水循环的发育和活动规律,而热水活动又直接或间接地产生了一些地质效应,如海底的热水喷流成岩成矿效应,此外它还与海底的热能输导与转化、海洋化学组分特征、海洋生命和生命起源等现象有着密切的成因联系。开展现代海底热水活动的系统性研究,应注重将热水循环的内部动力学机制和热水活动所引发的外部环境效应相结合,为此我们把它初步展开为：热水循环的空间组构研究、热量输导作用研究、热水流体的化学成分研究、热水活动与极端生命的关系研究以及热水活动的生命周期研究等5个方面,分别解析其内部特征以及引发的环境效应。最后初步探讨了开展海底热水活动的系统性研究的科学意义。     

Seismic Performance of RC Frames Designed to Eurocode 8 or to the Greek Codes 2000

For the first time after the finalisation of the European Norm for seismic design of buildings (Eurocode 8 – EC8),the performance of RC buildings designed with this code is evaluated through systematic nonlinear analyses. Regular 4-, 8- or 12-storey RC frames are designed for a PGA of 0.2 or 0.4 g and to one of the three alternative ductility classes in EC8. As the Eurocodes are meant to replace soon existing national codes, design and performance is also compared to that of similar frames designed with the 2000 Greek national codes. The performance of alternative designs under the life-safety (475 years) and the damage limitation (95 years) earthquakes is evaluated through nonlinear seismic response analyses. The large difference in material quantities and detailing of the alternative designs does not translate into large differences in performance. Design for either Ductility Class High (H) or Medium (M) of EC8 is much more cost-effective than design for Ductility Class Low (L), even in moderate seismicity. It is also much more cost-effective than design to the 2000 Greek national codes.     

Impact de la vie benthique sur la genèse de nodules calcaires dans les black shales

The study of calcareous nodules from four organic-rich black shale series allows us to suggest a prominent part for benthic organisms in creating heterogeneities in the sediment, thus favouring microbially mediated early diagenesis based on organic matter consumption. To cite this article: J.-G. Bréhéret et al., C. R. Geoscience 336 (2004).     

海带属褐藻生物学研究成就与进展

以海带(Laminaria ja ponica Aresch)为重点，综述了海带属褐藻生物学研究成就，介绍了海带属褐藻遗传育种技术、育苗技术和分子生物学研究进展。海带属褐藻生物学研究基础好，种质资源丰富，经济、生态价值高，是进行大型海藻遗传学和基因组学研究的理想材料。