双锥冲头反挤杯形件的主应力解

推导了双锥冲头的主应力解,分析了主应力解轴间应力表达式中各项的物理意义。并且与平直冲头的主应力解作了比较,指出平直冲头的主应力解是双锥冲头主应力解的特例。根据挤压力的计算值与实测值的比较,说明用本文推导的双锥冲头主应力解的结果计算反挤杯形件的挤压力可满足一般工程需要。     

UHF机械调谐器调谐电容片形的程序设计

采用传输线理论可以计算机械式UHF调谐器对应不同频率点的调谐电容量。在进行满足直线频率关系的调谐电容片形设计时,应当求出调谐电容量C_Τ与旋转角θ的显式函数关系。但对于分布参数的电路,这有一定的困难。本文采用数值计算方法完成了具有良好直线频率跟踪特性的调谐电容片形的设计,并由计算机自动绘出了片形。     

地幔柱的发生机制研究——以Ferrar为例

利用三维数值模拟方法,根据地幔对流控制方程,以180 Ma喷发的Ferrar大火成岩省(LIP)为例,在模型中引入Pangea超大陆、大型横波低速带(LLSVPs)和Pangea超大陆边缘的俯冲带,模拟地幔对流过程,研究其对应地幔热柱从地球内部热边界层(例如核幔边界)的生成过程,并讨论导致该地幔柱产生的相关因素.结果表...     

Opening and evolution of the South China Sea constrained by studies on volcanic rocks: Preliminary results and a research design

The South China Sea (SCS) is characterized by abundant seamounts, which provide important information about the evolution of the SCS and related deep processes. Cenozoic volcanism in the SCS and its surroundings comprises three stages relative to the spreading of the SCS:prespreading (>32 Ma), syn-spreading (32-16 Ma), and post-spreading (<16 Ma). The pre-spreading magmatism predominantly occurs on the northern margin of the SCS and in South China coastal areas and shows a bi-modal affinity. The syn-spreading magmatic activity was very limited on the periphery of the SCS, but may be concentrated in the SCS. However, seafloor samples of this stage are not available yet because of overlying thick sedimentary deposits. Post-spreading magmatism is widespread in the central and southwest sub-basins of the SCS, Hainan Island, Leizhou Peninsula, Thailand, and Vietnam. These are mainly alkali basalts with subordinate tholeiites, and display OIB-type geochemical characteristics. The Dupal isotope anomaly and presence of high-magnesian olivine phenocrysts suggests their possible derivation from the Hainan mantle plume. The temporal and spatial distribution of Cenozoic volcanism in the SCS and its surroundings may be accounted for either by plate stress re-organization before and after SCS spreading, or by ridge suction of plume flow during opening of the SCS. If the latter is the case, the volcanic rocks within the SCS basin may not be typical mid-ocean ridge basalts (MORB). It remains puz-zling, however, that the transition between the South China continental margin and the SCS basin does not have features typical of a volcanic rifted margin. Clearly, the relationship between mantle plume and SCS opening needs further evaluation. A better un-derstanding of the link between deep processes and opening of the SCS not only requires enhanced studies on igneous petrogene-sis, but also is heavily dependent on systematic sampling of seafloor rocks.     

石膏模-混凝土组合空腹楼盖用磷石膏力学特性研究

对石膏模-混凝土组合楼盖用磷石膏的抗压强度与含水率的关系、抗压强度取值、弹性模量取值、石膏与混凝土之间两类抗剪连接件受力性能进行了试验研究。研究结果表明,磷石膏的抗压强度随含水率的减小而增大,且随着含水率的降低,磷石膏的强度增加幅值越来越大,大致呈对数函数关系;磷石膏具有较好的抗压性能,其抗压强度较高,抗压强度可取4.8MPa,且受力过程中有明显的弹性阶段,根据曲线,其弹性模量取值约550MPa;对混凝土与石膏间的两类剪力连接件进行推出试验,结果表明两类连接件具有相同的抗剪强度,而B类连接件比A类连接件连接效果优越,试验数据比较稳定,最终以石膏破坏而导致构件破坏,连接件较为可靠。     

利用SS前驱波研究纳斯卡–南美俯冲带周边上地幔间断面起伏及其动力学意义

利用USArray的远震记录资料, 对1万多条地震记录的SS前驱波进行共反射点叠加分析(叠加范围是半径为5°的球冠), 得到纳斯卡板块南部及南美板块西部(120°W—60°W, 30°S—5°N)上地幔间断面的起伏形态。由于数据很好地覆盖了研究区域, 叠加范围更小, 因此比以往的结果具有更高的空间分辨率。在Galapagos, Easter和 San Felix这3个热点下方观测到的间断面起伏形态符合地幔深部存在高温异常的假设。还观测到: 在东太平洋洋隆南段下方, 410 km间断面深度增加; 在俯冲带下方, 410 km和 660 km间断面深度增加。     

插肩袖的结构设计

分析了插肩袖的结构形式,得出了合体插肩袖型的结构设计方法．为裁好插肩袖提供了理论基础依据．     

华南地壳演化过程及其构造格架

华南大陆基底由两大块体联合组成：即古扬子块和武夷块。古扬子块基底岩石主要为太古宙灰色片麻岩,古、中元古代科马提绿岩,新元古代蛇绿岩绿岩组成。而武夷块由角闪岩、变粒岩、浅粒岩等组成。地壳生长由西北向东南,由老到新具有由原始未分异地幔向超镁铁质→偏硅铝质→碱质前进演化。在华南大陆形成过程中,主要构造事件为两次碰撞、三次裂解的主体构造格局。大陆生长和构造动力机制均受地幔柱迁移所控制。燕山期以后,华南形成的构造格局为：扬子—特提斯构造域及太平洋构造域。     

滚动轴承力与变形关系试验装置设计

提出了一种测量滚动轴承力与变形关系的试验装置的设计方案,完成了试验原理的拟定、测量方案的设计和结构设计等工作。该装置可用于验证滚动轴承力与变形之间关系的计算公式的正确性,为下一步试验装置的制作和试验测量提供了前提条件。