固定式海洋平台利用TLD的减震研究

本文研究固定式海洋平台利用调谐液体阻尼器（ＴｕｎｅｄＬｉｑｕｉｄＤａｍｐｅｒ，简称ＴＬＤ）减小地震反应的方法。首先探讨了调谐频率比、激磁频率比对减震效果的影响，在此基础上建立了ＴＬＤ——平台系统的力学模型和运动方程，通过数值计算验证了该方法的有效性     

CG 2A型垂线观测仪固定式的使用

介绍CG-2A型垂线观测仪固定式的使用情况,并与便携带式进行了比较。     

胜利滩浅海油田开发新型固定平台技术

该项目主要针对胜利滩浅海油田开发建设和工程难题,研制了适应胜利滩浅海油田开发的新型固定采修一体化平台及其模块化扩展。主要技术内容包括:通过平台扩展总体     

固定式钻孔倾斜仪在滑坡示范监测中的应用

固定式钻孔倾斜仪具有灵敏度高、精度高的特点,并可以实现数据的自动连续采集,是测定滑坡体沿滑带产生的变形方向、变形量、变形速率,判断滑体深部变形状态的行之有效的监测仪器之一。本文通过对EL固定式钻孔倾斜仪的介绍,分析了其优缺点,并结合在巫山县向家沟滑坡实时监测中的应用,说明该仪器在滑坡示范监测中的能发挥较好的作用。     

基于重点抽样法的固定式平台结构风险评价研究

在建立海上油气设施的风险分析系统时,对由台风引发的极端海况造成的结构失效进行风险评估是1个十分重要的问题。为了建立实用可靠的风险评价方法,本文使用基于重点抽样法的随机模拟技术,对渤海海域CB12-C井组平台结构进行了全概率法失效概率计算,并在此基础上进行了平台结构的风险评价。该方法是1种适用于固定式海洋平台的定量风险评价方法,充分考虑了平台结构风险分析过程中各种不确定性的影响,极大提高了定量风险评价结果的可靠性。     

全站仪对中器检定方法研究

针对现有文献提出的对中器检定方法无法高效准确地完成固定式对中器的检定,提出通过增加辅助基座、竖轴转接器,实现待检对中器的快速准确检定.首先将辅助基座安置在三脚架或者全站仪检定台上,在辅助基座上安置竖轴转接器,再将待检对中器安置在竖轴转接器上,用辅助基座的脚螺旋对准天花板或者地面标志点,旋转待检对中器180°,如果待检对中器十字丝的像偏离标志点,则用待检对中器调整螺丝至其偏移量的一半,用辅助基座的脚螺旋调整其剩余的一半,重复这个过程即可完成固定式对中器的快速精确检定.这种方法可以满足测绘生产中快速检定固定式对中器检定的实际需求.     

Viva固定式基站在“百里风区”的应用

一、背景概述兰新铁路第二双线是一条新的铁路大动脉,它将贯穿我国西北地区的甘肃、青海、新疆3省区。兰新铁路第二双线自兰州西站引出,经青海西宁,甘肃张掖、酒泉、嘉峪关,新疆哈密、吐鲁番,引入乌鲁     

固定式海洋平台极限强度试验研究

根据墨西哥湾某海域一典型固定式海洋平台为原型,按照几何相似准则和刚度相似准则设计并制作海洋平台试验模型,开展极限强度模型试验研究,观察并记录其破坏过程。并采用非线性有限元方法(ANSYS)对试验模型进行极限强度数值计算,将计算结果与试验结果对比,结果表明计算结果与试验结果吻合较好,验证非线性有限元方法的有效性。     

Analysis of Stationary-Wave Nonstationarity in the Northern Hemisphere 500-hPa Height Field

In this paper, the concept of stationary-wave nonstationarity is presented and elucidated in the framework of the Lorenz circulation decomposition. This concept indicates the relative magnitude of the zonal nonuniform abnormity to the intensity of stationary waves on the monthly mean scale. Based on the Lorenz circulation decomposition, the nonstationarity degree Ius(Ilus) of the global (local) stationary waves is defined, and then used to analyze the stationary-wave nonstationarity at 30° 60°N, where the intensity of stationary waves at 500 hPa in the Northern Hemisphere, as is well known, is very high. The following findings are obtained: (1) There exist seasonal southward and northward movements in the position of the nonstationarity zones of the global stationary waves. The steady stationary waves occur in midlatitudes (35°-55°N) in winter and in the subtropical region (south of 35°N) in summer, associated with the major troughs over East Asia and North America and the weak European trough in winter, and with the relatively steady subtropical high system in summer. A high value center of Ius is at 35°N in spring and 50°N in summer, which might be caused by the seasonal variation of stationary-wave intensity, particularly in association with the interannual variability of trough ridge positions of stationary waves on the monthly mean maps. (2) There exists obvious asymmetry in Ilus, with the steady zones always located in the areas controlled by strong troughs/ridges and the unsteady ones in the areas where the stationary-wave intensity is low. The Ilus in the subtropics (south of 35°N) is larger in winter than in summer, and vice versa in the midlatitude region (north of 35°N). The summertime distribution of Ilus on the whole shows a rather complicated structure. However, North Europe is the most unsteady area for local stationary waves, as represented by high values of Ilus in both summer and winter, while over the North American continent (about 120°E-60°W), the °Ilus is slightly less than 1 in summer, indicating that the stationary waves in this region are more steady than those over other mid and high latitude regions. (3) From North China to Northwest Pacific, there is a high value zone of Ilus in summer, with its center (45°N, 130°E) located in the east of Heilongjiang Province. This influences the summer climate of northern China, including Northeast, North, and Northwest China. It is obvious that the nonstationarity is an intrinsic attribute of stationary waves, and can be regarded as being of the same importance as the intensity and energy-spectrum structure of stationary waves in the studies of the general circulation system.