精密补偿器水准仪磁致误差及其测试方法

分析了精密补偿器水准仪磁致误差的成因，介绍了研制的一套磁致误差检测设备以及完整的检测方法。通过大量的检测数据与数理统计，表明４测回的标准差为０．００８″。该设备已为全国一等水准网复测，地震形变测量和精密工程测量等检测磁致误差１００多台次。     

国家地震局推出第一部精密水准仪检定规程

我国地震系统拥有大批DS_(05)、DSZ_(05)级精密水准仪。为了保证这些高精度仪器作业时处于正常状态,保证仪器观测值准确可靠,在国家尚未制定精密水准仪检定规程的情况下,国家地震局科技监测司率先于’90无锡计量工作座谈会上提出了制定我国第一部DS_(05)、DSZ_(05)级精密水准仪检定规程的计划,并确定由国家地震局地震研究所负责编写,国家地震局第一、二地形变监测中心参加编写工作。检定规程立足于用室内检定方法取代室外检定方法,因此编写难度较大。经过编写人员近一年的艰苦努力,提出了完整的检定项目、合理的技术指标、标准的计量     

数字水准仪应用于区域精密水准测量的有关问题研究

基于试验和实践,讨论了数字水准仪的特性和误差来源及其对观测结果的影响。在此基础上阐述了该仪器应用于区域精密水准测量中应予关注的各种问题和提高精度的措施。指出：应制定有关该仪器的测量规范。     

DQG综合监控仪在上海通过技术鉴定

DQG综合监控仪是由地震所一室(牵头),陕西乾县地震台和西北光学仪器厂共同研制的。它是一种可广泛应用于水平摆倾斜仪及其它光记录观测仪器作:(1) 交、直流自动转换,(2) 光源灯和时号灯光亮度调节,(3) 光源灯及其备用灯转换与故障报警,(4)时号灯及其备用转换与故障报警和(5)推动钟(滚筒)停走故障监控报警等五功能之辅助设备。     

丰满台水管仪观测资料质量评定及综合分析

通过对丰满台近几年水管仪的漂移量、连续率、一致性、数据精度等指标的检验,评定水管仪的性能和观测质量。结果显示,水管仪各项指标均在规范要求的范围之内。同时确认了影响仪器观测精度的原因是降雨、大风、气候变化、调修仪器、标定等的干扰。     

基于非对称传感器的地震预警与烈度速报综合用烈度仪

对典型的地震预警与烈度速报方法进行分析,提出了基于非对称传感器的地震预警与烈度速报综合用烈度仪,其由非对称结构的三分量传感器和基于ARM嵌入式系统的专用数据采集器组成。经过测试,该地震烈度仪的专用数据采集器具有大于107 dB的动态范围;其非对称三分量传感器结构中,所选的单分量B类传感器的加速度误差小于0.8%,动态范围大于105 dB,而所选的三分量C类传感器的加速度误差小于5%,动态范围大于61 dB。该地震烈度仪的各项指标均满足地震预警与烈度速报综合应用的各项技术要求,且功耗低、成本低,适合于高密度布设。     

Romberg算法和Matlab的综合应用精确计算精密光学器材的体积

实际工程应用中,对复杂形体实现高精度高效率的体积运算比较困难,通过在完成国内某大型光学产品公司的报价系统的过程中,综合运用Romberg计算方法和Matlab软件工具,找到了一种用三重积分来计算较复杂形体体积的方法.     

Simulation test apparatus for marine corrosion

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类的集成测试级别研究

为了减少类测试中集成测试的桩模块的数量，分析了类之间的依赖关系，提出确定类的静态测试级别和动态测试级别的算法。     

Model test of the influence of cyclic water level fluctuations on a landslide

Many landslides in reservoir areas continuously deform under cyclic water level fluctuations due to reservoir operations. In this paper,a landslide model, developed for a typical colluvial landslide in the Three Gorges Reservoir area, is used to study the effect of cyclic water level fluctuations on the landslide. Five cyclic water level fluctuations were implemented in the test, and the fluctuation rate in the last two fluctuations doubled over the first three fluctuations. The pore water pressure and lateral landslide profiles were obtained during the test. A measurement of the landslide soil loss was proposed to quantitatively evaluate the influence of water level fluctuations. The test results show that the first water level rising is most negative to the landslide among the five cycles. The fourth drawdown with a higher drawdown rate caused further large landslide deformation. An increase of the water level drawdown rate is much more unfavorable to the landslide than an increase of the water level rising rate. In addition, the landslide was found to have an adaptive ability to resist subsequent water level fluctuations after undergoing large deformation during a water level fluctuation. The landslide deformation and observations in the field were found to support the test results well.     

Determination of water level design for an estuarine city

Based on the extreme value theory,self-affinity,and scale invariance,we studied the temporal and spatial relationship and the variation of water level and established a model of Gumbel-Pareto distribution for designed flood calculation.The model includes the previous extreme value models,the over-threshold data,and the fractal features shared by previous extreme value models.The model was simplified into a logarithmic normal distribution and a Pareto distribution for specific parameter values,and was used to calculate the designed flood values for the Shanghai Wusong Station in 100-and 1 000-year return periods.The calculated results show that the value of the designed flood height calculated in the Gumbel-Pareto distribution is between those in the Gumbel and Pearson-III distributions.The designed flood values in the100-and 1 000-year return periods of the model were 0.0 3%and 0.11%lower,respectively,than the Gumbel distribution and 0.06%and 1.54%higher,respectively,than the Pearson-III distribution.Compared to the traditional model based solely on extreme probability,the Gumbel-Pareto distribution model could better describe the probabilistic characteristics of extreme marine elements and better use the data.     

针对EJB测试特殊性扩充JUnit 框架

简要介绍了单元测试编程框架JUnit和J2EE体系架构中的EJB组件,对EJB组件类测试的特点进行分析.针对EJB组件类的并发性和不确定性,利用JUnit框架,进行一定的扩充,实现系统测试集的自动构建和并发多线程测试用例类.     

An enhanced underwater camera apparatus for seabed observation of megabenthic epifauna in the northern Yellow Sea

Journal of Oceanology and Limnology - Seabed photographing has been applied with various underwater camera apparatuses (UCAs) for observations of megabenthic epifauna, which reveals more details...     

Coast sea level and Asian monsoon system a downscaling exercise for Chinese coast

In this study, the authors examined the relationship between monthly sea level data and concurrent large-scale monthly mean sea level pressure and SST data for 1960 to 1990, which are reasonably well simulated by present day climate models; sea level variations due to variations of regional atmospheric forcing and oceanic circulation, are not adequately simulated by a global climate model because of insufficient spatial resolution. The authours applied a statistical “down scaling” strategy to sea level along the Chinese coast. Two interrelated processes were identified: one process is the local wind or wave set-up of water due to Asian monsoon wind anomalies; the other is the rainfall diluting effect in spring. At interdecadal time scale, the later becomes more important and most likely plays a major role in the planetary scale atmosphere-ocean interaction taking place in the eastern North Pacific. Contribution No. 3236 from the Institute of Oceanology, Chinese Academy of Sciences. Key project 39630060 and Project 49476274 supported by NSFC, and also supported by president's fund of Chinese Academy of Sciences.     

A physical simulation test for the rockburst in tunnels

According to the test results of the physical and mechanical properties of similar materials in various quality mixture, a type of material with obvious tendency of rockburst was selected to produce a large-size model to simulate rockburst phenomena in tunnels. The prototype model comes from a typical section of diversion tunnels in Jinping Hydropower Station in China. The simulation of excavating tunnels is carried out by opening a hole in the model after loading. The modeling results indicated that under the condition of normal stresses in the model boundaries the arch top, spandrel and side walls of the tunnel produced an obvious jump reaction of stress and strain and the acoustic emission counts of the surrounding rock also increased rapidly in a different time period after the "tunnel" excavation, showing the clear features of rockburst. The spalling, buckling and breaking occurred in the surrounding rock of model in conditions of over loading. It is concluded that the modeling tunnel segment in Jinping Hydropower Station is expected to form the tensile rockburst with the pattern of spalling, buckling and breaking.     

Influence of sea level rise on Shanghai astronomical tide and storm surge and estimation of probable water level

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Global sea level change and thermal contribution

The global long-term sea level trend is obtained from the analysis of tide gauge data and TOPEX/Poseidon data. The linear trend of global mean sea level is highly non-umiform spatially, with an average rate of 2.2 mm year-1 in T/P sea-level rise from October 1992 to September 2002. Sea level change duc to temperature vanation (the thermosteric sea level) is discussed. The results are compared with TOPEX/Poseidon altimeter data in the same temporal span at different spatial scales. It is indicated that the ther-mal effect accounts for 86% and 73% of the observed seasonal variability in the northern and southern hemispheres, respectively. The TOPEX/Poseidon observed sea level lags behind the TSI, by 2 months in the zonal band of 40°-60° in both the northern and southern hemispheres. Systematic differences of about 1-2cm between TOPEX/Poseidon observations and thermosteric sea level data are obtained. The potential causes for these differences include water exchange among the atmosphere, land, and oceans, and some pos-sible deviations in thermosteric contribution estimates and geophysical corrections to the TOPEX/Poseidon data.