振戎中学食堂楼耗能减震分析与设计(Ⅰ)一反应谱法

本文采用耗能减震技术，根据建筑结构抗震规范规定的反应谱法，利用ＣＴＡＢ程序对云南省洱源县振戎中学食堂进行了抗震计算分析和设计验算．首先对未加耗能减震装置的空框架结构进行了小震下的位移和强度验算以及大震下的位移验算；其次，介绍了本工程选用的Ｔ字芯板摩擦耗能器的工作原理，并对耗能器进行了足尺性能试验；第三，根据工程结构的环境特点和建筑使用功能要求，确定了耗能减震方案；最后，对耗能减震结构进行了抗震验算和分析，结果表明，附加耗能器后的工程结构抗震性能得到了明显改善．     

多级变刚度滞变耗能的设计思想和可行性实验研究

本文提出了一种多级变刚度滞变耗能器，讨论了其设计的基本思想，并进行了初步的试验研究。结果表明，不管是增刚度型还是减刚度型多级变刚度耗能器均具有很好的滞变耗能能力，可以应用于被动自适应（或称为智能）控制。     

Relationship between energy dissipation rate and channel morphology in the development of the model braided channel

1 IntroductionA certain pattern of channel is the product of its self-adjustment under given boundary, discharge and sediment conditions[1]. A lot of experiments have been performed in flumes, usually with an initially-regulated straight channel being constructed in the flume, to determine the impact of these conditions on channel morphologies and patterns[2-6]. Schumm's experiments[3] demonstrated that when the bed-load channels transport only sand at constant discharge, channels develop from…     

采用耗能减震装置修复震后有损伤钢筋混凝土框架的试验研究

本文通过地震模拟振动台试验研究用耗能减震装置修复后震后有损伤钢筋混凝土框架的效果和可行性，文中制作了两层和三层两座钢筋混凝土剪切型框架，首先进行了地震损伤模拟试验，其次提出了震后有损伤结构的参数识别方法，修复准则和修复用耗能减震装置的设计准则；在此基础上，采用了软钢屈服型耗能器驿两座试验框架在地震损伤后进行修复，并再次对修复后的框架模型进行地震模拟试验，证实了采用这种修复措施可以恢复震后有损伤结构     

A modified profile method for determining the vertical fluxes of NO,NO2, ozone,and HNO3 in the atmospheric surface layer

A modified profile method for determining the vertical deposition (or/and exhalation) fluxes of NO, NO₂, ozone, and HNO₃ in the atmospheric surface layer is presented. This method is based on the generally accepted micrometeorological ideas of the transfer of momentum, sensible heat and matter near the Earth's surface and the chemical reactions among these trace gases. The analysis (aerodynamic profile method) includes a detailed determination of the micrometeorological quantities (such as the friction velocity, the fluxes of sensible and latent heat, the roughness length and the zero plane displacement), and of the height-invariant fluxes of the composed chemically conservative trace gases with group concentrations c ₁=[NO]+[NO₂]+[HNO₃], c ₂=[NO₂]+[O₃]+3/2·[HNO₃], and c ₃=[NO]–[O₃]–1/2·[HNO₃]. The fluxes of the individual species are finally determined by the numerical solution of a system of coupled nonlinear ordinary differential equations for the concentrations of ozone and HNO₃ (decoding method). The parameterization of the fluxes is based on the flux-gradient relationships in the turbulent region of the atmospheric surface layer. The model requires only the vertical profile data of wind velocity, temperature and humidity and concentrations of NO, NO₂, ozone, and HNO₃.The method has been applied to vertical profile data obtained at Jülich (September 1984) and collected in the BIATEX joint field experiment LOVENOX (Halvergate, U.K., September 1989).     

考虑波能耗散的近岸波浪传播数学模型

基于考虑能耗的定常缓坡方程，推导得出包含波能耗散的近岸水域波浪传播变形数学模型，并用所得模型对浅水中波浪的传播进行了计算，将计算结构与Berkhoff的实验数据进行比较，表明二者吻合很好。该数学模型能较好地解决波浪在浅水中的传播变形问题。     

Nonlinear saturation-based whitecapping dissipation in SWAN for deep and shallow water

This study investigates the effectiveness of a revised whitecapping source term in the spectral wind wave model SWAN (Simulating WAves Nearshore) that is local in frequency space, nonlinear with respect to the variance density and weakly dependent on the wave age. It is investigated whether this alternative whitecapping expression is able to correct the tendency towards underprediction of period measures that has been identified in the default SWAN model. This whitecapping expression is combined with an alternative wind input source term that is more accurate for young waves than the default expression. The shallow water source terms of bottom friction, depth-induced breaking and triad interaction are left unaltered. It is demonstrated that this alternative source term combination yields improved agreement with fetch- and depth-limited growth curves. Moreover, it is shown, by means of a field case over a shelf sea, that the investigated model corrects the erroneous overprediction of wind-sea energy displayed by the default model under combined swell-sea conditions. For a selection of field cases recorded at two shallow lakes, the investigated model generally improves the agreement with observed spectra and integral parameters. The improvement is most notable in the prediction of period measures.     

Bottom friction caused by boundary layer streaming beneath random waves for laminar and smooth turbulent flow

The effect of boundary layer streaming on the sea bed shear stresses, beneath random waves, is investigated for laminar flow as well as smooth turbulent flow. It is demonstrated how bottom friction formulas for regular waves can be used to obtain the bed shear stresses resulting from steady streaming under random waves. As a result, friction factors for steady streaming under random waves are provided, and the effect of streaming versus the effect of linear waves is discussed. For laminar flow the effect of second order Stokes waves is also included. Examples are included to illustrate the applicability of the present practical method, and results are obtained using data typical for field conditions.     

An Extented Wave Action Equation

1 .IntroductionWaves,oneofthemostimportantdynamicfactorsincoastalengineering ,havesignificanteffectsonthesafetyofconstructionandthecostofcoastalstructures.Thevariationofwave inducednearshorecurrentsandlongcyclicoscillationofwatersurfaceresultsinbankerosion ,sedimenttransportinestu aries ,siltationofharborsandchannels ,protectivestructureaccidents ,shipmooringfailuresanddiffu sionofpollutants ,andthushavedrawnscientificresearchers’attention .Alargenumberofresearchresultsonwavesandwave inducedc…