耗能型防落梁装置铝蜂窝缓冲器轴向吸能特性研究

耗能型防落梁装置是由普通拉索式防落梁装置改进而来的,其主要吸能部件为吸能控制管,由扩径管和铝蜂窝缓冲器组成。为了给铝蜂窝缓冲器的设计与优化提供可靠的理论依据,建立了铝蜂窝轴向压缩简化模型,对其轴向压缩应力进行了分析、推导并采用有限元模拟和借鉴相关文献试验数据进行了验证,同时分析了加载速率对铝蜂窝材料吸能特性的影响。此外分析了铝蜂窝芯铝箔厚度和蜂窝边长对其吸能特性的影响,并通过桥梁工程实例来分析和评价铝蜂窝缓冲器在吸能控制管中的吸能作用。研究结果表明:铝蜂窝轴向压缩简化模型精度较高,理论计算值相对于有限元计算值的偏差平均值为4.53%,相对于文献试验值的偏差平均值为6.47%;随着加载速率的提高,铝蜂窝材料的单位体积吸能值、初始峰值应力和屈服平均应力均有所提高;在铝蜂窝芯铝箔厚度或蜂窝边长一定的情况下,两者之比β值越大,铝蜂窝缓冲器吸能性能越好;配置了铝蜂窝缓冲器的吸能控制管,其总吸能值平均增大率为18.56%,最大增大率为29.51%,吸能性能提升最大可达近30%,在消耗地震能量方面将发挥显著的作用。     

岩土工程新材料“EMC”测试与研究

我们对ＥＭＣ进行了物理力学性质测试,测试表明ＥＭＣ能有效提高处理材料的抗压强度、抗剪强度、密实度、承载力及抗机械蚀能力。使用ＥＭＣ与使用常规传统稳定剂比较有较高的经济效益。ＥＭＣ属新型环保产品,对环境无害。     

Some Aspects Regarding the Tectonic Setting of High– and Low-sulfidation Epithermal Gold Deposits of Chile

Abstract: In Chile the principal gold deposits of the low- and high-sulfidation types occur in the middle Creataceous-early Eocene Precordillera and in the middle to late Miocene Andean Cordillera, respectively. In both areas their related magma-tism migrates south-east with time. This feature suggests that the metallogenic integrity is greatly affected by a change in the tectonic regime from a transpressive oblique subduction to a weakly-compressive normal subduction. Moreover, certain differences in the geologic setting, such as the structure of host rocks are recognized between the two types of Chilean epither-mal gold deposits. This data provide us not only with genetic implications regarding epithermal gold deposits, but also an important guide for gold exploration in the Chilean Cordillera.     

反复荷载作用下锈蚀钢筋混凝土压弯构件恢复力性能的试验研究

采用外加电流对混凝土压弯构件中的钢筋进行了快速锈蚀试验,通过钢筋锈蚀混土压弯构件在水平反复荷载作用下的试验研究,探讨了钢筋锈蚀程度对混凝土压弯构件的承载力,刚度,延性,耗能能力等的影响,给出了锈蚀构件的滞回曲线和骨架曲线。     

石灰改性膨胀土工程性质的试验研究

通过对济南、淄博地区膨胀土的室内物理力学性质、石灰改性的系列试验分析,确定了膨胀土的等级、改性后土的胀缩性、强度与剂量的关系及掺入石灰的最佳配比。     

辽东湾东岸海冰抗压强度特征分析

本文利用辽东湾东岸鲅鱼圈、营口和长兴岛三地实测海冰抗压强度资料,分析了海冰破坏应力与破坏时间的关系,应变率和冰温对海冰抗压强度的影响,以及海冰生成环境对海冰抗压强度的影响。综合分析表明,三地破坏应力随破坏时间变化的整体趋势一致,应变率对三地海冰抗压强度有显著的影响,三地海冰抗压强度随温度降低总体有增大的趋势,冰龄、盐度、含沙量的差异是造成辽东湾东岸海冰抗压强度不同的主要原因。     

关于软土状态确定标准的讨论

软土状态是软土勘探、设计和施工中常用评价内容或依据。由于状态确定依据差异, 使结果颇多出入。     

水泥土搅拌桩无损检测方法探讨——水泥土弹性波波速与强度关系的试验研究

通过室内不同龄期水泥土弹性波速度和抗压强度的对比试验,探讨两者关系。试验数据的数理统计分析,证明水泥土弹性波速度和抗压强度间存在着非线性指数关系。并提出了关系式。为低应变动测方法在水泥土搅拌桩无损检测中的实际应用条件提供了参考。     

Effect of Sample Disturbance on Unconfined Compression Strength of Natural Marine Clays

1 .IntroductionCoastalstructuresoftenencountersettlementandstabilityproblemsofsoftmarinefoundation (Liuetal.,1 999;Zhouetal.,2 0 0 0 ;Liuetal.,2 0 0 3) .Manyresearchershaveillustratedthatnaturalmarineclaysaregenerallysubjectedtotheeffectsofsoilstructureduringtheirdepositionalandpost depositionalprocesses (Zhangetal.,1 995;Hongetal.,2 0 0 3a ;2 0 0 3b) .Thesoilstructureofnat uralmarineclaysiseasilydamagedduringsamplingandhandlingbecausenaturalmarineclaysgeneral lyhavehighwatercontentandlowsti…     

Compressive tectonism along the eastern margin of Malaita Island (Solomon Islands)

New bathymetric and geophysical data were collected in the region east of the island of Malaita during the SOPACMAPS II cruise of the French research vessel L'ATALANTE. This region, part of the Malaita Anticlinorium was interpreted as a piece of oceanic crust from the Ontong Java Plateau obducted over the old Solomon Islands arc during collision between the Pacific and Australian plates. It has been generally accepted that convergent motion between the Australia and Pacific plates since the Late Miocene was absorbed exclusively along the San Cristobal trench, southwest of the Solomon Islands Arc.Bathymetry, imagery, and geophysical data (magnetism, gravity, seismic) acquired during the SOPACMAPS II survey allow us to classify the successive parallel ridges mapped within the region as being recent volcanic, oceanic crust, or deformed sedimentary ridges.Seismic profiling provides evidence of successive compressive events along the Malaita margin caused by the relative motion between the Solomon Islands and the Pacific plate. The main phase of convergence probably occurred during Oligocene-early Miocene time, but some relative motion between the two domains are still being absorbed along the East Malaita boundary. The existence of active faulting in the sedimentary cover throughout the region and the present-day deformation of the outer sedimentary ridge is a good illustration of this phenomenon.