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.     

微波催化氧化法处理富马酸废水

在活性炭与Fenton试剂存在下,用微波辐射处理多次铁碳微电解处理后的富马酸废水,通过单因素和正交实验对影响因素进行了考察。在100mL水样中,活性炭用量为1．0g、双氧水用量为1．0mL、废水pH为3、微波加热时间为10min、辐射功率为350W的条件下,可以使富马酸废水的COD从300mg／L降至96．6mg／L。     

用喷射鼓泡反应器进行烟气脱硫

介绍了采用喷射鼓泡反应器处理烟气量为7 000~10 000 m3/h的软锰矿浆烟气脱硫中试试验。试验中,对喷射鼓泡反应器及系统的阻力进行了测定,考察了不同品位、不同液固比的软锰矿条件及系统连续运行时的脱硫率和锰浸出率。中试表明,在液固比为(2~3)∶1、矿粉粒度约为100目的连续运行条件下,无论是选用品位高的钦锰矿还是品位低的软锰矿,系统运行稳定,且脱硫率保持在90%以上,锰浸出率在70%以上。吸收液经净化处理后得到的MnSO4.H2O产品可达到国家GB1622—86标准。     

Calcined Oil Shale Semi-coke for Significantly Improved Performance Alginate-Based Film by Crosslinking with Ca2+

Journal of Polymers and the Environment - Oil shale semi-coke (OSSC) is the residual solid waste after refining of oil shale, which principally contains organic matter and minerals. The common...     

Nonisothermal pyrolysis kinetics of waste printed circuit boards and product characterization using TG–MS

Journal of Material Cycles and Waste Management - With characteristics of high resources, complex composition, and high toxicity, the treatment and disposal of waste printed circuit boards (WPCBs)...     

集中排烟公路隧道入口段火灾下诱导风速研究

为研究集中排烟模式下公路隧道入口段发生火灾时的合理诱导风速,以某公路隧道为背景,运用火灾动力学模拟软件FDS对隧道人口段火灾时不同坡度、不同诱导风速的16组火灾工况进行模拟研究,通过对各工况下隧道内的温度场分布及烟气控制效果模拟结果的分析,得到了各工况下的合理诱导风速,研究结果可为公路隧道集中排烟系统关键设计参数提供参考.     

基于GIS的区域干旱灾害风险区划研究

根据自然灾害风险理论,从致灾因子危险性、孕灾环境暴露性、承灾体易损性、防灾减灾能力等4个子系统选取指标,建立干旱灾害风险指数模型,结合GIS中自然断点分类法进行聚类分析,全面综合地分析各地区相关性和差异性.以淮河流域为研究实例,根据拟定的区划原则,采用“自下而上”和“自上而下”相结合的区划方法,将淮河流域分为6个旱灾风险分区,并对区划结果进行分析,为因地制宜地采取工程和非工程的防灾减灾措施,提供参考依据.     

基于应变模态差的海洋平台构件的损伤识别研究

对于具有一定损伤的导管式海洋平台钢管梁来说,实验模态分析得到的位移模态和固有频率难以有效的反应结构损伤的实际状况,特别是对早期的轻微损伤。为了提高损伤识别的效率和效果,根据海洋平台钢管梁架的受力特点,由节点位移模态推到出节点应变模态。然后利用损伤前后的应变模态差作为损伤识别的指标。将这个指标用在海洋平台钢梁构件焊缝和跨中单元的损伤识别上。通过建立钢管梁焊缝损伤的ANSYS模型,进行数据模拟分析,该方法能够在低阶模态条件下,有效的识别早期的轻微损伤。     

基于GIS的松花江干流暴雨洪涝灾害风险评估

以黑龙江省内的松花江干流流域作为研究区,从现代灾害风险理论出发,综合运用GIS空间分析和灾害风险评估数学方法,对松花江干流流域的暴雨洪涝灾害风险进行了定量评价.研究利用遥感数据和社会经济数据,在空间分析基础上,通过对暴雨洪涝灾害的危险性、承灾体的暴露性、脆弱性以及区域防灾减灾能力的分析,确定影响各个县市暴雨洪涝灾害风险的具体方面.并将因子集成为洪涝灾害风险指数(FDRI),在此基础之上绘制出松花江干流流域的洪涝灾害风险区划图,结果表明松花江干流洪涝灾害风险以哈尔滨和佳木斯两市最大,上游洪涝灾害风险大于下游.     

城市防洪工程风险决策方法

本文着重讨论了与城市防洪工程决策制定密切相关的几个问题：①城市防洪工程设计标准的确定；②现有防洪工程的性能评估，③最优防洪工程对策的确定等，并在风险分析的基础上，给出了解决上述问题的方法。所得结论可为城市防洪工程决策的制定提供较为科学的理论依据。