阶梯状来流中立管的涡激振动响应预报

将变参数受拉柔性梁的有限元模态分析与涡激振动预报结合在一起,建立了变参数柔性立管的横向涡激振动预报模型,考虑到海洋立管的模态信息与涡激振动响应高度耦合,为合理计算附加质量对模态信息的影响,模态分析与涡激振动响应预报迭代进行.其中,使用有限元方法对立管进行模态分析,考虑了质量、拉力、抗弯刚度沿立管轴向的变化;在此基础上,涡激振动响应计算在各个模态上分别进行.在出现多模态参与的情况时,比较各模态的振幅,对模态受力进行折减.与近期阶梯状来流作用下立管涡激振动实验结果的比较显示,本文模型是有效的.     

露天浅孔爆破震动反应谱特征

结合汕头华能电厂爆破监测阶段所得数据进行分析,对露天浅孔爆破地震反应谱特征进行了分析研究。所得结果不仅对建筑物抗震设计提供依据,还将对爆破振动的研究有推动作用。     

沁河流域地表水与地下水转换的模拟

黄河中游的沁河流域中下游水文地质情况复杂,地表水地下水转换频繁。为研究该流域水资源形成转换规律,建立了一个基于相似水文响应单元的物理性分布式水文模型,模拟了人类活动用水影响下的水文过程,用简化的渗流模型模拟成层岩溶地区地下水运动。经参数率定和1986—1998年长系列模拟,结果显示:沁河流域水资源量主要受降水影响,地表水与地下水转换量占地下水资源量80%以上。超采地下水导致地下水位下降,引起地表径流量显著减少。成层岩溶影响到多个水文过程,地表水与地下水转换随着岩溶发育而动态变化。     

Analyzing Nonstationary Random Response of a SDOF System under the Evolutionary Random Excitation by Wavelet Transform

For evolutionary random excitations, a general method of analyzing nonstationary random responses of systems was presented in this paper. Firstly, for the evolutionary random excitation model, the evolutionary power spectrum density function （EPSD） of a random excitation was given by wavelet transform. Based on the EPSD, the nonstationary responses of a SDOF system subjected to evolutionary random excitations were studied. The application and validity of presented method were illustrated by numerical examples. In numerical examples, the recently developed stochastic models for El Centro （1934） and Mexico City （1985） earthquakes which preserve the nonstationary evolutions of amplitude and frequency content of ground accelerations were used as excitations. The nonstationary random mean-square responses of a SDOF system under these two excitations were evaluated and compared with simulated results.     

Optimization of Multi-Criteria Experiments with Fuzzy Results

Introduction To reach a best quality product, experiments and an op- timized design of experiments are required in an inte- grated quality management system. The best quality level of a manufacturing process or product is defined not only by one, but by m…     

Synthesis and photocurrent response of porphyrin-containing conjugated polymers

In recent years conjugated polymers have attracted considerable attention because of their potential appli- cations in the fields of light emitting diodes, photo- voltaic devices, and sensors[1―7]. In the fabrication of semiconductor photovoltaic devices…     

Climate change and hydrologic process response in the Tarim River Basin over the past 50 years

Climate change and hydrologic process response in the Tarim River Basin over the past 50 years are the focus of more and more researchers＇ attention. In this paper, both temperature and precipitation time series were found to present a monotonic increasing trend using nonparametric tests. Noticeably, a significant step change in both temperature and precipitation time series occurred in 1986. By contrasting the trends of natural water process in headstream and mainstream, we found that it was anthropogenic activities not climate change that caused the river dried up and vegetation degenerated in the lower reaches of Tarim River. The results of gray correlation analysis show that the runoff of higher latitude distributing river is more closely associated with winter snow stocking, while that of lower latitude is more closely related to summer temperature. Runoff in the headstream is more sensitive to precipitation, while that in the mainstream is more sensitive to evaporation. The strong evaporation caused by increasing temperature weakened runoff to some extent in spite of the fact that precipitation increased over the past 50 years.     

共射-共基电路的高频响应

频率响应是放大电路的一个重要参数，也是选择电路组态的一个重要依据．该文对常用的共射-共基放大电路进行了高频响应的详细分析，给出了此电路的上限截止频率与共基放大电路上限截止频率的关系，并分析了此电路的特点．     

自适应无限冲激响应陷波器抑制窄带干扰的误差补偿算法

考虑到直接序列扩频(DS-SS)系统中无限深度格型陷波器在去除窄带干扰的同时对扩频信号的损伤,在无限深度格型陷波器上添加一自适应横向滤波器,其输出作为对受损扩频信号的误差补偿.仿真结果证实,新设计的误差补偿滤波器改善了无限深度格型陷波器的性能,而系统计算复杂度只有少量增加.     

Depositional environments of Bathonian sediments from the Jaisalmer Basin, Rajasthan, western India

The pericratonic sedimentary Jaisalmer Basin, west of the Aravalli Ranges, on the westerly dipping eastern flank of the Indus Shelf, is a principal structural element of Rajasthan. Jurassic sediments in the SE comprise non-marine sandstones and conglomerates to nearshore, brackish to marine sands, silts, clays and carbonates, grouped lithostratigraphically into the Lathi, Jaisalmer, Baisakhi, and Bhadasar formations. The Late Bajocian to Oxfordian Jaisalmer Formation is divided, in ascending order, into the Hamira, Joyan, Fort, Badabag, Kuldhar, and Jajiya members. Fossil records providing a Bajocian to Bathonian age for the lower and middle parts of the formation include: a Late Bajocian coral Isastraea bernardiana (d’Orbigny) in the uppermost Joyan Member; Bathonian ammonite Clydoniceras in the basal part of the Badabag Member; Bathonian foraminiferal/bivalve assemblages in the Fort Member. The topmost bed of the Joyan Member represents the peak of first marine transgression of the Jaisalmer Basin, probably contemporaneous with the Late Bajocian one in the neighbouring Kachchh Basin. Based on faunal studies Bajocian to Bathonian sediments of the Jaisalmer Basin can be broadly correlated with those of the Kachchh Basin. The Fort and Badabag members represent the following depositional environments, in chronological order: (a) brackish to shallow fully marine; (b) fully marine with rapidly fluctuating water energy and sedimentation rates; (c) near-shore to lower shoreface with fluctuating energy conditions, salinity and sedimentation rates; (d) near-shore to shoreface channels and storm-dominated marine above fair-weather wave-base; (e) lagoon with fluctuating low to moderate energy, salinity and sedimentation rates; (f) stormdominated shelf to lower shoreface.