工程弃渣型坡面泥石流形成过程试验

从试验模型、试验材料、试验装置及测试内容等方面制定了工程弃渣型坡面泥石流试验方案,拟定了模型试验过程,降雨历时16-18 h,其中0～13h属于前期降雨阶段,降雨强度控制在6.8 mm/( 10 min),分4次完成,每次降1h,停2h;13h以后属于短历时强降雨阶段,降雨强度控制在16.7 mm/(10 min);分...     

关于湿陷性黄土路基处理方法的探讨

阐述了湿陷性黄土的定义、湿陷机理;并以闻合高速为例,介绍了常用湿陷性黄土处理方法,分析了各种方法各自的优缺点,并结合规范对湿陷性路基等处理要求,通过工程经济等综合比选,提出了各种方法的适用原则,以供交流、参考。     

上海世博会公共客运系统设计

世博参观游客交通的合理组织是办好世博会的关键问题之一。在总结上海世博会交通条件的基础上,提出以公共交通为核心的世博会客流集散策略,并采用由整体到局部系统化分析的方法,进行了世博公共交通系统的总体设计。基于世博游客集散的三条对策,以提高公共交通系统吸引力为目标,建立了世博公共交通系统的总体框架;接着就世博公共交通系统两个主要子系统“交通转换系统”和“EXPOBUS系统”,进行了系统的功能分析、服务流程分解和服务对象分类;最后梳理了系统设施需求,提出了各子系统的系统设计与规划方案。通过研究,期望能建立高效的、具有吸引力的公共交通系统,保障上海世博会的成功举办。     

不同加筋形式对结构声辐射性能的影响

本文基于统计能量法分析了横向加筋板,纵向加筋板,斜加筋板,圆心在板角的圆弧形加筋板,圆心在板中轴的圆弧形加筋板,正交加筋板等六种不同加筋形式板在100Hz至1000Hz内的声辐射特性,研究表明正交加筋板的平均辐射声压级要低于另外五种形式的加筋板.研究了两类改变加强筋间距的横向加筋板的声辐射性能,研究表明对于固定左侧的一根加强筋改变加强筋间距,随着加强筋间距的增大,辐射声压级先增大后减小,而对于板中线为基准改变加强筋间距,对辐射声压级影响不大.最后,本文研究加筋板在主机舱中的实际应用,建立了三种主机舱模型,分析模型的声辐射特性,研究表明复合加筋形式的主机舱辐射声压级最小,相对于无加筋形式,要低4~5dB左右.     

船舶机舱空气质量监测评价仪的设计及实现

机舱多模式空气质量监测评价仪是对机舱气体进行实时监测并做出评价的智能化产品.本仪器通过多种传感器对机舱气体中部分物质的含量进行采集,利用单片机进行数据整理和分析,实时给出评价.该仪器对于监测机舱环境的空气品质,为轮机人员提供自我防护决策提供了依据和保障,有较大的意义和实用价值.     

基于CFD的船舶货舱通风数值模拟

以某集装箱船的货舱通风系统为研究对象,根据船舶舱室的通风系统的特点,采用合理的数值模拟方法,并利用拉格朗日粒子示踪的方法描述舱室中的气体流动状况.在此基础上,分析比较3种不同的通风设计方案,通过对比分析研究送风管上开孔朝向和数目对通风效果的影响,确定对通风最有利的方案.模拟结果表明,应用CFD技术进行通风系统分析,可以很好地从流场的分布特性以及空气粒子的运动追踪等方面来评估设计方案的优劣,为通风系统的设计、优化提供有力的工具.     

基于流形理论的数据分类挖掘

数据挖掘技术应用于作战指挥挖掘系统,能为指挥员的决策分析提供智能化的、自动化的辅助手段。在分析数据挖掘问题中的分类算法的基础上,利用流形结构对分类算法进行了改进。从而避免全局线性对分类信息造成的丢失,保留完整的数据结构信息,在一般意义下完成针对数据集的各项任务。     

QNX4原理及其启动过程分析

介绍QNX4操作系统的架构和工作原理。并对其启动过程进行了详细分析。     

基于功能损伤的复杂电磁环境下炮兵目标毁伤评估

为适应复杂电磁环境,提高炮兵指挥员“科学决策,量敌用兵”的水平,依据目标在复杂电磁环境下的特点,综合利用了指数法和D-S理论等方法,分别对典型目标、电磁敏感目标和系统目标进行了功能损伤性毁伤评估。     

Seasonal and interannual variation of physical and biological processes during 1994–2001 in the Sea of Japan/East Sea: A three-dimensional physical–biogeochemical modeling study

A Pacific basin-wide physical–biogeochemical model has been used to investigate the seasonal and interannual variation of physical and biological fields with analyses focusing on the Sea of Japan/East Sea (JES). The physical model is based on the Regional Ocean Model System (ROMS), and the biogeochemical model is based on the Carbon, Si(OH)₄, Nitrogen Ecosystem (CoSiNE) model. The coupled ROMS–CoSiNE model is forced with the daily air–sea fluxes derived from the National Centers for Environmental Prediction (NCEP) and the National Center for Atmospheric Research (NCAR) reanalysis for the period of 1994 to 2001, and the model results are used to evaluate climate impact on nutrient transport in Mixed Layer Depth (MLD) and phytoplankton spring bloom dynamics in the JES.The model reproduces several key features of sea surface temperature (SST) and surface currents, which are consistent with the previous modeling and observational results in the JES. The calculated volume transports through the three major straits show that the Korea Strait (KS) dominates the inflow to the JES with 2.46 Sv annually, and the Tsugaru Strait (TS) and the Soya Strait (SS) are major outflows with 1.85 Sv and 0.64 Sv, respectively. Domain-averaged phytoplankton biomass in the JES reaches its spring peak 1.8 mmol N m^− 3 in May and shows a relatively weak autumn increase in November. Strong summer stratification and intense consumption of nitrate by phytoplankton during the spring result in very low nitrate concentration at the upper layer, which limits phytoplankton growth in the JES during the summer. On the other hand, the higher grazer abundance likely contributes to the strong suppression of phytoplankton biomass after the spring bloom in the JES. The model results show strong interannual variability of SST, nutrients, and phytoplankton biomass with sudden changes in 1998, which correspond to large-scale changes of the Pacific Decadal Oscillation (PDO). Regional comparisons of interannual variations in springtime were made for the southern and northern JES. Variations of nutrients and phytoplankton biomass related to the PDO warm/cold phase changes were detected in both the southern and northern JES, and there were regional differences with respect to the mechanisms and timing. During the warm PDO, the nutrients integrated in the MLD increased in the south and decreased in the north in winter. Conversely, during the cold PDO, the nutrients integrated in the MLD decreased in the south and increased in the north. Wind divergence/convergence likely drives the differences in the southern and northern regions when northerly and northwesterly monsoon dominates in winter in the JES. Subjected to the nutrient change, the growth of phytoplankton biomass appears to be limited neither by nutrient nor by light consistently both in the southern and northern regions. Namely, the JES is at the transition zone of the lower trophic-level ecosystem between light-limited and nutrient-limited zones.