交通事故再现技术研究现状与发展趋势

道路交通事故再现不仅是交通事故责任鉴定和原因分析的重要方法,也是交通事故防治的重要内容。在详细介绍国内外事故再现计算机仿真技术的基础上,分析目前事故再现系统开发中事故现场数据采集技术、碰撞前后速度估算的技术、碰撞过程进行模拟的虚拟现实技术的研究现状与存在的问题,提出进一步优化的方向,进而达到完善交通事故模拟再现的目的。最后指出我国交通事故再现技术进一步研究的内容和发展趋势。     

我国民航实施安全管理体系(SMS)的思考

中国民航的快速发展需要一种系统的安全管理方法。本文总结了我国民航管理现状和所处的水平，分析了安全管理体系（SMS）方法的本质。同时笔者指出我国在SMS建设中一些人对SMS的建设重点、自愿报告系统等问题的认识上存在误区，最后提出了几点具有实践意义的操作方法帮助实施SMS建设。     

钢铁企业总排口废水回用新工艺应用

就当前国内几个典型的钢铁企业总排口废水水质特性作了分析,探索钢铁企业废水回收利用的工艺路线,提出在吸收国外新技术的基础上研究开发出符合国情的新工艺技术.     

环境条件对浮游藻色素特征的影响及应用研究进展

基于色素分析的浮游藻化学分类方法已经成为从宏观上对浮游藻群落组成和丰度进行定量研究的良好工具。浮游藻化学分类方法的应用需要对藻类色素特征及其在不同环境条件下的变化特点有较充分的了解。本文对在实验室培养条件下,光照和营养盐条件对不同藻种单位细胞色素含量、特征色素对叶绿素a比值的色素特征的影响,以及在淡水、高浑浊河口环境下,多种因素的综合作用、非藻类色素引起的误差等因素的研究进展进行了综述,并阐述了相关应用、存在的问题及未来的展望。     

浅谈钢制氮封储罐泄漏防治措施

从消除储罐泄漏点、加强日常管理方面阐述了如何做好氮封储罐泄漏治理与预防,并对加强储罐泄漏防治提出建议。     

Reassessment of the Ocean-To-Atmosphere Flux of Carbon Monoxide

Carbon monoxide (CO) in the surface sea waters is produced predominantly by photochemical processes, oxidized by micro-organisms and outgassed to the atmosphere. to assess carbon monoxide flux from the oceans to the atmosphere, the photochemical production and microbial oxidation of carbon monoxide in the oceanic mixed-layer was investigated during several oeanographic cruises and in the laboratory. the photoproduction rate of carbon monoxide was found to be well correlated to the concentration of dissolved organic carbon (DOC) in coastal and open ocean surface waters. Taking a global average carbon monoxide production rate of 10 ± 2 nmole litre^-1 (mg DOC hr)^-1 in the surface open ocean water, and 25 ± 7 nmole litre^-1 (mg DOC hr)^-1 in coastal sea water, at cloud-free summer solar noon, the photochemical production of carbon monoxide in the global oceans is estimated to be at a rate of 1200 ± 200 Tg CO y^-1. the microbial carbon monoxide turnover time in the mixed-layer was observed to range from hours in a coastal estuary to 16 days in the Pacific along 1057deg; W in dark incubations. Natural sunlight can largely inhibit the microbial consumption of carbon monoxide in surface water. On a global scale, microbial consumption is responsible for the loss of less than 10% of photochemical produced carbon monoxide in the surface ocean. Field measurements have shown that the net transport of carbon monoxide from the euphotic zone to the underlying deeper ocean water is limited and that the overall life time in surface sea waters is less than 3-4 hours. When combined, these field measurements with the photoproduction and microbial consumption rates obtained, we estimate the oceanic flux to the atmosphere is about 1000 ± 200 Tg CO y^-1, which represents the largest single source of atmospheric carbon monoxide.