Spatial distribution of cadmium over a cyclonic eddy in the southern East China Sea

Eddy systems are a unique ecosystem, usually having high biological masses and primary production in the sea. In this study, both particulate and dissolved phases of cadmium in the water column of 15 stations over a cyclonic eddy in the southern East China Sea were determined to obtain their spatial distributions. This allows us to confirm that cyclonic eddy systems play the role of a Cd pump in the sea.Results showed that particulate Cd (PCd) and dissolved Cd (DCd) concentrations in water varied greatly, ranging over two orders and one order of magnitude, respectively. Large spatial variability was found not only for PCd but also for DCd in the upper water, apparently due to the effects of the cyclonic eddy system on the Cd distributions over the study area. DCd accounts for about 99% of the total Cd. For the surface water, DCd concentration at the eddy center was about five times the average of the water surrounding the eddy center. The depth distributions of DCd exhibited a typical surface depletion and a subsequent increase with depth; however, the PCd distribution showed the opposite, i.e. a surface maximum and a subsequent decline with depth. In general, the DCd maxima were found at depths of 600–1000 m, agreeing well with the literature. It reflected the internal biogeochemical cycling of Cd in the water column, which was driven by the utilization of Cd by plankton in the euphotic zone and by the regeneration of Cd at depth. In addition, a remarkably high DCd concentration existed in near-bottom water around the cyclonic eddy center.The horizontal distributions of both PCd and DCd in the upper water shared a common feature with elevated concentrations centering around the eddy center and a decline in concentration with distance from the eddy center. This shows that the cyclonic eddy could bring up the Cd-rich deep water to the surface water around the eddy center and could then expand toward eddy's vicinity via advection–diffusion. It is thus likely that it produces ample biological masses over the eddy system. Hence, this work can demonstrate that the ascending nutrient-rich water driven by the cyclonic eddies can serve as an important source not only for many nutrients but also for Cd in the sea.     

单层梁格分析宽翼缘箱梁剪力滞效应

由于分析精细、应用简便,平面梁格法已广泛应用于斜弯桥、裤衩高架等异型桥的计算分析中。通过对"Hambly"平面梁格的梁格划分方法与刚度取值的改进,提出更便于杆系有限元软件运用的单层梁格法;通过单层梁格法分析了宽翼缘箱梁的剪力滞效应,并与能量变分法对比,证实了单层梁格法可以有效的计算宽翼缘箱梁剪力滞效应,而这是平面梁格无法解决的。     

连续相位调制信号的检测

本文主要介绍了CPM信号的解调方法,研究了基于最大似然接收原理的网格搜索最优算法—维特比（viterbi）算法,并且通过Matlab计算机仿真,给出了一定信噪比条件下影响CPM调制体系误码率性能的因素。     

舰船惯导航行数据的重构及混沌特性分析

针对现有舰船航行数据处理研究中,对数据内在属性及不同数据间相关性研究不够深入的问题,应用不同方法对舰船惯导航行数据进行了相空间重构及比较分析。分析结果表明,C-C方法对船舶惯导航行数据的重构效果较好。在此基础上,进行了惯导数据的混沌特性定性分析,并计算了惯导数据的最大Lyapunov指数,对舰船惯导数据进行了混沌动力学特性研究。分析结果证实了舰船航行数据具有较为典型的混沌特性,为进一步研究采用混沌控制等方法对舰船航行中的混沌状态进行控制提供必要的数据基础和比较依据。     

二相流模式下JDC4-55可调桨粘性流场分析

运用CFD方法中的汽-液混合二相流模型模拟JDC4-55可调桨的水动力性能和空泡性能。通过改变进速和调节桨叶角度得到相应的水动力性能参数。分析空泡对螺旋桨水动力性能的影响,进行JDC4-55可调桨桨流场模拟分析。相对于单相流模型而言,JDC4-55可调桨汽-液混合二相流模型性能计算结果与实验值吻合得更好。     

水下地形辅助导航新方法仿真

水下地形辅助导航是水下运载体导航定位技术研究的关键技术之一。传统的水下地形辅助导航采用回声测深仪,导航定位精度低,有时甚至失效。本文将多波束测深引入水下地形辅助导航,将水深映射为灰度值,利用快速傅立叶变换将输入灰度图从空间域变换为频率域。先采用相位相关技术进行粗匹配,再采用图像Hu不变矩特征进行精匹配,实现导航定位。对基于不同实验获取的实测海底地形图、惯性导航数据、DGPS数据以及多波束实测数据进行了实验室仿真。仿真结果表明,新方法可以极大地提高水下地形导航定位精度,使INS误差降低到原误差的15%以内,尤其是在INS初始误差较大时(小于3 km)导航定位精度改进更好。     

大悬臂多腹板宽箱梁受力特性研究

结合工程实际,应用有限元软件MIDAS/CIVIL分别建立杆系有限元模型和空间实体模型,对大悬臂、多腹板、宽箱室变截面箱梁在对称荷载作用下的剪力滞效应、偏载作用下的腹板受力不均匀效应进行分析。结果表明,截面上下翼缘剪力滞效应较为显著,按规范提供的有效翼缘宽度折减计算不能完全包络剪力滞效应的影响;同时,箱梁的偏载效应从跨中至支点方向逐渐增大。     

低压配电系统单相接地选择性切除方案研究

本文结合目前飞速发展的单片机及高精度快速采样技术,提出低压配电系统单相接地故障选择性切除的方案。通过理论分析及建模仿真验证了方案的正确可行性。     

大悬臂多腹板宽箱梁受力特性研究

结合工程实际,应用有限元软件MIDAS/CIVIL分别建立杆系有限元模型和空间实体模型,对大悬臂、多腹板、宽箱室变截面箱梁在对称荷载作用下的剪力滞效应、偏载作用下的腹板受力不均匀效应进行分析。结果表明,截面上下翼缘剪力滞效应较为显著,按规范提供的有效翼缘宽度折减计算不能完全包络剪力滞效应的影响;同时,箱梁的偏载效应从跨中至支点方向逐渐增大。