多层阻尼复合板常温贮存5年性能研究

目的分析多层阻尼复合板常温贮存5年的性能变化。方法对多层阻尼复合板进行常温下贮存5年的减振性能研究,通过贮存前后的正弦扫描试验和随机振动试验,获得贮存前后多层阻尼复合板的减振性能和模态变化,进行对比分析。结果阻尼复合板常温贮存5年后,径向模态有较大的下降,法向模态变化较少,组件上的加速度响应基本无变化。结论该多层阻尼复合板常温贮存5年后仍然满足要求。     

关于“正弦振动试验”现行国家标准与正在修订中的新版标准的解读

正弦振动试验是试验室经常采用的振动方式,对应正弦振动试验国家标准GB／T2423．10应用非常广泛。本文介绍了该标准的用途、制修订背景等,在此基础上分析了现行正弦振动试验国家标准GB／T2423．10—2008与正在修订的6B／T2423．10—201×之间的异同之处,并指明了此标准应用中的几点注意的问题。     

Sustainability and environmental enhancement in changing cirumstances

Natural environment has endured fast economic growth and population explosion sine the 20th century,which has soil erosion,land desertification,ozone layer depletion,bio-diversity reduction and persistent toxic and harmful pollutants are among the major environmental challenges.     

新型复合粘弹阻尼器不同加载波下的性能研究

为了研究新型复合粘弹阻尼器在不同加载波下的力学性能,分别对其施加正弦波与三角波进行抗疲劳与变幅相关性试验,比较2种加载波下新型复合粘弹阻尼器的力学性能变化规律。结果表明:新型复合粘弹阻尼器,在抗疲劳试验中正弦波加载下的力学性能优于三角波加载;变幅试验中,随着应变幅值的增大,三角波加载下的最大剪应力、存储剪切模量和等效刚度均优于正弦波加载,但等效阻尼比小于正弦波加载。     

平板及焊缝中裂纹磁记忆检测技术研究

为了将磁记忆技术用于裂纹缺陷的检测领域,应用试验研究和有限元分析相结合的方法,分析裂纹的深度、埋深、宽度以及扫描角度对平板中裂纹磁记忆检测的影响。针对45号钢板建立深度和宽度2个影响参量与磁记忆信号之间的量化关系。沿焊缝长度方向和垂直焊缝长度方向对焊接裂纹进行磁记忆检测,研究焊接裂纹的检测方法和信号特征。提出根据局部波形呈现正弦波形态判别缺陷的方法。研究结果表明,用磁记忆检测技术能够对裂纹进行定位,并根据波形信号特征量对裂纹深度、宽度进行量化评价。     

舰载机机载设备弹射和拦阻冲击试验条件研究

弹射和拦阻冲击试验是舰载机机载设备必要的考核试验之一,而目前相关标准并未明确试验具体量值,且国内缺少试验经验,这会影响试验工作的开展。基于此,从GJB 150.18A—2009规定的阻尼正弦波出发,结合项目研制过程数据,提出波形频率和振幅的确定方法。波形频率可根据类似机型的地面共振试验数据或全机振动模态分析结果确定,这里利用弹性缩比模型地面动响应试验和带通滤波法来预计瞬态波振幅,并说明了阻尼正弦波实施案例和对试验设备冲程的要求。从累积损伤角度出发,认为采用随机振动试验替代弹射和拦阻冲击试验是可行的,而不能采用常规冲击试验进行替代。根据随机振动3σ响应谱和冲击响应谱的对比分析,提出了采用振动功能试验替代弹射和拦阻冲击试验的前提条件——设备安装频率应高于要求值。     

电子产品共振频率检测方法研究

本文介绍了电子产品共振频率检测方法，主要有目测法、正弦扫描法、随机振动法和模态分析法，并结合工程案例对几种方法进行描述。     

REGIONAL AND TEMPORAL PATTERNS OF TOTAL SOLUTES IN THE SASKATCHEWAN RWER BASIN1

ABSTRACT: In the Saskatchewan River Basin (365,000 km²), which drains the Canadian prairie from the Rocky Mountains east to Manitoba, concentrations of total solutes are usually within the range of 100 to 1000 mg/L. Total solutes levels in tributaries increase markedly from west to east across the basin, as mountain snowmelt and dilute surface runoff are replaced by ion-rich ground water and concentrated prairie runoff as the major influences on solute concentrations. In contrast, total solutes concentrations in main-stem rivers are nearly constant, ranging 200–300 mg/L, with only a small increase across the basin. Dilute mountain runoff dominates solute concentrations in main-stem rivers, despite the influx of increasingly ion-rich water from tributaries. The principal long-term trends in total solute concentrations across the basin, as revealed by linear and sine-curve regressions, were due to the construction of reservoirs, which depress the natural winter maximum in solute concentrations and disrupt the sinusoidal annual pattern, while sharply reducing seasonal variation. These regression methods did not show anticipated anthropogenic increases in salt load in the Red Deer or South Saskatchewan Rivers, but a trend of slowly increasing solutes concentrations (2 mg/L/yr) was detected for autumn flows in the lower Bow River. Municipal wastes from the City of Calgary or irrigation return flows are probably responsible for this increase.