静电火灾的成因与认定

所谓静电火灾。是批电静电放电火花引燃可燃气体，可燃液体蒸气等易燃易物而造成的火灾或爆炸事故。静电火灾的非常复杂，火灾发生往往是各种最不利因素的偶然组合所致火灾现场又常遭到严重破坏，所以，静电火灾原因的认定是很难由火场痕迹和遗贸物来取得直接证据，这就给静电火灾调查带来了一定的困难。     

地震的社会经济影响

在查阅前人研究成果的基础上,分析了地震造成社会灾害严重、影响地区经济发展的现象,认为地震灾害对一个地区所造成的影响程度与该地区的承灾力有关,并影响地区经济的可持续发展.     

地铁运营系统安全综合评价指标体系研究

分析地铁运营系统的特点、运营模式、系统故障模式,并运用系统工程的理论原则,从系统外部因素、系统指挥因素、设备设施因素、运营管理因素4个方面,确立地铁运营系统安全综合评价指标体系,利用模糊数学综合评价法,建立了地铁运营系统安全综合评价模型,并通过典型实例进行综合分析评价,进而证明将模糊数学理论应用于地铁安全综合评价的可行性。通过地铁运营系统安全指标体系和评价方法的研究和探索,对正确评价地铁系统运营安全现状,修正偏差,提高地铁系统安全总体水平具有十分重要的意义。     

开放型历史文化名城主题公园的建设

长期以来,历史文化名城的保护工作受到以商住房地产开发为主要形式、"投资者主导型"为开发模式的旧城改造浪潮的冲击.历史文化名城主题公园以保护古城风貌、延续城市历史文脉为宗旨,运用主题公园的规划设计、经营管理等方法和开发模式,以保留、修复、移植和改造古城建筑为技术手段,建设成为集名城风貌观光、史籍博览、特色商品购物、民俗文化娱乐为一体的旅游目的地,从而达到保护历史古城风貌,树立文化名城形象的目的.     

系统评价天然蛭石吸附氨氮的效果

采用在人工配置含氨氮的污水中投加蛭石的方法,系统研究了天然蛭石吸附污水中氨氮的饱和吸附容量以及蛭石吸附氨氮的等温吸附曲线,探讨了污水的pH值、温度、浓度对氨氮去除率的影响及各影响因子的大小,结果表明,蛭石的饱和吸附量为20 8mg/g;蛭石吸附量在pH2 0～6 0范围内随着pH的增大而增大,最佳pH为4 0～6 0;温度在15～35℃范围内,吸附量随温度的升高减小,氨氮的去除率随着蛭石用量的增加而增加,影响因素的大小顺序为:pH>蛭石的用量>吸附时间>温度。这为蛭石作为一种新型氨氮吸附材料提供了基础参数。     

地铁运营系统危险有害因素辨识分析

地铁系统发生事故,后果不堪设想。笔者在对国内外63起地铁典型事故分析的基础上,确定了地铁火灾、列车脱轨、拥挤踩踏、中毒窒息、列车撞车等危险有害因素,并对影响事故的后果严重度和发生频率进行了分析,给出了危险度计算查阅赋值表,从而确定了影响地铁运营的危险度,作出了量化分级,同时对可能导致事故的危险有害因素进行了分析,并对危险有害因素的防治对策进行了探讨。     

地震应急的影响因素分析

本文在理论分析、国内外历史震例和救灾案例研究的基础上,同时参照我国的相关政策和法律法规文件,对影响地震应急(包括震前准备和震后应急行动)的因素进行了初步分类,并系统讨论了这些因素影响地震应急的方式、途径和程度.以期为地震应急的理论研究和地震应急的实际工作提供部分补充和指导.     

基于GIS的长江中下游地区洪灾风险分区及评价

国内外近几年的发展表明,在所有可能避免和减轻自然灾害的措施中,最简单有效的方法就是通过在科学研究基础上进行风险区划,将自然灾害管理提高到风险管理的水平.在长江流域数字化地图的基础上,选取不同重复期(20,50,100年),及包括1870年历史洪水和1931,1935,1954,1991,1995,1996,1998,1999和2002年共10次洪水,借助Arcview地理信息系统的空间分析和叠加功能,对长江中下游地区的洪水灾害危险性进行了初步评价.首先参考洪水灾害淹没图和相关历史文献记录资料,构建10次洪水受灾县(市)分布图;其次对这10次洪水受灾县(市)分布图进行叠加,得到长江中下游地区洪涝灾害风险性评价图.分析表明:长江中下游地区洪水风险的分布是有规律的,而且具有明显的地理意义.有4个明显的高危风险区,分别是洞庭湖、鄱阳湖两湖平原的湖滨地区和公安以下的长江中游河段的沿江一带,尤其是荆江河段以及两江相夹地势低洼的江汉平原;沿高危风险区外侧为高风险地区,重点在汉江下游、资、沅、澧水、清江流域、皖沿江地区以及太湖流域的部分地区;沿长江于高危风险和高风险地区两侧分别为风险较小地区;其他地区对于洪水灾害而言则为安全地区.评价结果与长江中下游的实际情况基本吻合.     

Reaction kinetics of waste sulfuric acid using H2O2 catalytic oxidation

The process of recovering waste sulfuric acids using H₂O₂ catalytic oxidation is studied in this paper. Activated carbon was used as catalyst. Main operating parameters, such as temperature, feed rate of H₂O₂, and catalyst dosage, have effects on the removal of impurities from waste sulfuric acids. The reaction kinetics of H₂O₂ catalytic oxidation on impurities are discussed. At a temperature of 90°C, H₂O₂ feeding rate of 50 g (kg waste acid)^?1 per hour, and catalyst dosage of 0.2 wt% (waste acid weight), the removal efficiencies of COD and chrominance were both more than 99%, the recovery ratio of sulfuric acid was more than 95%, and the utilization ratio of H₂O₂ was 88.57%.

Implications: Waste sulfuric acid is a big environmental problem in China. The amount of waste sulfuric acid is huge every year. Many small and medium-sized businesses produced lots of waste acids, but they don’t have an appropriate method to treat and recover them. H₂O₂ catalytic oxidation has been used to treat and recover waste sulfuric acid and activated carbon is the catalyst here. Main parameters, such as temperature, feed rate of H₂O₂, and catalyst dosage, have been investigated. The reaction kinetics are discussed. This method can be economical and feasible for most small and medium-sized businesses.     

Contamination status and potential release of trace metals in a mangrove forest sediment in Ho Chi Minh City,Vietnam

Can Gio district is located in the coastal area of Ho Chi Minh City, southern Vietnam. Discharge of wastewater from Ho Chi Minh City and neighboring provinces to the rivers of Can Gio has led to concerns about the accumulation of trace metals (As, Cu, Cr, Ni, Pb, and Zn) in the coastal sediments. The main objective of this study was to assess the distribution of As, Cu, Cr, Ni, Pb, and Zn in surface and core sediments and to evaluate the contamination status in relation to local background values, as well as the potential release of these selected trace metals from sediments to the water environment. Sediment characteristization, including determination of fine fraction, pH, organic matter, and major elements (Al, Fe, Ca, K, Mg, and S), was carried out to investigate which parameters affect the trace metal enrichment. Fine fraction and Al contents were found to be the controlling proxies affecting the distribution of trace metals while other sediment characteristics did not show any clear influence on trace metals’ distribution. Although As concentrations in the sediments were much higher compared to its reference value in other areas, the enrichment factor based on local background values suggests minor contamination of this element as well as for Cr, Cu, and Pb. Risk assessment suggested a medium to very high risk of Mn, Zn, and Ni under acidification. Of importance is also that trace metals in sediments were not easily mobilized by organic complexation based on their low extractabilities by ammonium-EDTA extraction.