On the influence of sand-wind on atmospheric environment

The authors seek, through tests on simulated sand samples in a wind tunnel and analysis of minerals combination and trace elements, to discover the environmental implications of flying-up, falling-down and concentration variation as a function of natural wind speed and direction, distance of movement, range and extent of influence on the atmospheric environment, of micro-granular components on the ground surface in the Keerqin desert area in northwest Liaoning Province of China.     

浅谈油田开发项目事故风险环境影响和防治措施——以大庆太19区油田开发为例

通过对国内外油田开发的类比事故调查及资料分析,结合大庆太19区油田开采的实际情况,事故风险主要来自于钻井(井下作业)天然气集输管线以及站场等工艺环节,危险其安全的潜在危险因素主要有自然灾害、腐蚀环境、误操作、设备缺陷、施工及人为破坏等同题.在油田开发过程中所发生的事故,不论是人为因素引起的还是自然灾害,其最终结果都是导致原油、天然气或含油污水的泄漏及火灾爆炸事故,并产生不同程度的环境风险,因此采取风险防治措施显得尤为重要.     

Oil spill model development and application for emergency response system

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流域水质监测站对江河重大污染事故的应急监测措施的研究

流域水质监测站对发生在江河中的重大水质污染事故中承担着前哨的重要作用.因此,建立起江河重大污染事故的应急监测体系已迫在眉睫.本文结合多年来松花江水质监测的实际工作,对环境水质监测部门开展重大污染事故应惠监测措施研究的必要性、应急监测工作必需的配置、预警监测断面在应急监测中的功能与作用等进行了较全面的论述.指出,应加大江河水环境监测的投入,切实加强水环境应急监测工作,尽快建成主要江河应急防控体系,提高江河重大污染事件的预警预测、监测、处置、后期评估等方面能力与水平.     

甲烷高温自燃诱导过程实验与数值模拟研究

甲烷的转化在化工产业中具有举足轻重的地位与战略意义,近年来涌现的氧化偶联制烯烃等多种新型化工工艺涉及高温条件的甲烷-纯氧等体系的混合与反应过程,明确甲烷高温自燃诱导与爆炸规律是实现工艺安全设计与运行的前提,然而相关研究与基础数据仍较为欠缺。通过利用基于快速压缩装置的高温高压燃爆测试系统开展甲烷-纯氧等典型混合体系的自燃诱导过程研究,同时基于GRI-Mech 3.0机理的数值模拟方法进行了数值模拟研究。实验结果与数值模拟结果吻合较好,随着温度/压力的增加及氧气含量的下降,混合体系自燃诱导时间均缩短;燃料气中加入乙烷或氢气则会大幅缩短自燃诱导过程。对于多个工艺过程中涉及的低氧含量体系率先开展了研究,得到了不同当量比及温度条件下的典型体系自燃诱导时间,同时考察了惰性气的加入对于自燃诱导过程的延长作用。研究结果有助于深入理解甲烷自燃诱导机理,同时指导高温条件的甲烷转化工艺的本质安全化设计与爆炸防控。     

液氯泄漏事故模拟分析

针对1996年1月21日在西班牙发生的一起液氯泄漏事故的后果进行了模拟分析。模拟分析结果同事故实际所造成的后果是一致的。表明采用基于数学模型的事故后果模拟分析具有一定程度的可靠性。对于救灾和对重大危险源编制应急事故预案有一定程度的指导意义。     

事故前人因失误研究

在安全评价中，人因失误特别是事故后人因失误越来越受到重视；但相对而言，事故前人因失误没有引起足够的重视。本通过对大量核电厂安全分析报告和运行事件报告的考察，系统地阐述了事故前人因失误对系统安全的显影响，并在此基础上，归纳出在核电站开展事故前人因(失误)分析的程序。该程序主要包括系统熟悉，定性分析，筛选，定量计算，与故障树的集成，敏感性分析与不确定性分析，形成分析档等几个步骤。     

2002年我国事故与灾害状况综述

本对我国2002年的安全生产事故及自然灾害情况进行了总结和评述。包括火灾(城乡火灾、森林火灾、草原火灾)、天气气候特征、农业自然灾害(干旱、洪涝、风雹、低温冻害)、海洋灾害(风暴潮、赤潮、海浪)、地质灾害(地震、泥石流、水土流失)等。     

编制企业事故应急预案的实践与探索

企业编制事故应急预案是在新形势下面临的新任务，也是《安全生产法》赋予企业的责任。通过介绍编制《事故应急预案与急救措施》的具体实践，探索了一些编制事故应急预案的程序和原则。     

Numerical Simulation of Synoptic Condition on a Severe Sand Dust Storm

By using observational data and MM5, an observational analysisand numerical study was conducted on the synoptic condition of a severe dust storm that was caused by a Mongolian cyclone whichoccurred from 6 to 8 April 2001. Results illustrated thatthe cyclogenesis was due to the isentropic potential vorticity (IPV) advection in the upper troposphere and the terrain modifiedbaroclinicity in the mid-lower troposphere. The Altai-Sayan complex of mountains blocked the lower level cold air and made the isentropic surface sharply steep. When the air slid down along the isentropic surface the increasing of baroclinicity anddecreasing of stability blew up the vertical vorticity development.The formation of the dust storm was a result of a cyclonic cold front passing across the area. The occurrence of this dust stormwas closely related to the strong surface wind, which was accompanied by a cold front passing, rather than the cyclogenesis, itself. Hence, the reason for the pre-front dust storm formulation was the formation of heating convection. Reasons behind the formation of a black storm (visibilitylower than 50 m), which occurred in the mid-north part ofInner Mongolia, lay in several aspects. Firstly, in thisarea the surface wind was strong, a direct result of thedownward transport in mid-lower troposphere. Secondly,the cold front passed over the effected area near sunsetso the air obtained much more surface heating to form adeeper mixed layer (ML). Thirdly, cooperation between thelower level wind and the terrain made the atmosphere inthis area and acquired the maximum advective contributionnecessary to form a deep post-front ML. The sensitivityexperiment revealed that surface heat flux was important to the frontal lifting. In addition, the forcing of surface heating wasalso seen as the primary forcing mechanism of frontogenesis. Meanwhile, removal of the surface heat flux made the atmosphericstratification became stable and the pre-storm ML very shallow,which weakened the strength of the dust storm.