蜂窝流道热沉强化传热数值模拟

热沉是模拟太空深冷环境的核心部件。为提高空间深冷环境的模拟效果,更好地满足型号试验需求,设计了一种蜂窝流道热沉。利用流体力学理论和有限元方法对蜂窝热沉内部流体的流动和强化传热进行数值模拟,分析流道结构参数对流体流动和换热的影响,确定最优的流道结构参数。结果表明,同等条件下蜂窝热沉表面温度低于管板式热沉5 K左右,温度均匀性可达到±2 K;流道深度和间距是影响流体在热沉中流动与传热的重要因素,合理选择流道结构参数可以提高热沉的换热性能;需要综合考虑传热和阻力问题来确定最优的流道结构参数,最优的蜂窝热沉流道间距为75 mm,深度为10 mm。     

预富集技术在原子吸收光谱环境分析中的应用

原子吸收光谱法是分析环境水样中金属离子含量的有效方法之一。在测定时往往需要对样品进行前处理,然后再进行测定。文章介绍了近些年较新的一些分离富集技术在原子吸收光谱分析环境中金属离子时的应用,分析了离子交换树脂在样品中金属离子富集分离过程中的研究近况,评述了固相萃取、析相微萃取、单滴液滴微萃取、分散液液微萃取、离子液体萃取、浊点萃取等多种萃取方式在样品预富集中的应用进展,综述了活性炭、纳米粒子、淀粉、分子筛等吸附剂在富集环境水样中金属元素的应用现状,同时还对在线富集技术与流动注射分析技术联用在金属元素分析中的应用进展进行了评述。     

新型单室无质子膜微生物燃料电池性能研究

采用不锈钢金属丝阳极构建了管状单室无质子交换膜空气阴极微生物燃料电池(MFC),并以葡萄糖为唯一电子供体,研究MFC的性能.在室温下,初始ρ(CODCr)为496 mg/L,外接电阻为1 000 Ω时,该MFC可以连续产电,最高电压达235.11 mV,开路电压为461.00 mV,内电阻约2 820 Ω.实验条件下测得该MFC的最大功率密度为137.1 mW/m2,库仑效率为32.4%.采用该MFC进行了啤酒酿造废水处理对比实验,在进水ρ(CODCr)为15 900 mg/L,停留时间为96 h下,MFC对废水CODCr的去除率达40%～55%,比厌氧生物处理效率高5%～10%.表明MFC技术可以在获得电能的同时,强化有机废水的生物处理过程.     

对我国减灾战略的几点建议

本文从我国的灾害特点徊灾害防治中的困难的角度出发,参照灾害防治的经验教训,提出建立管理国家紧急事物的职能机构;设立防灾科研和教育基金;积极开展国际交流和协作;尽快成立灾害信息情报中心和进行必要的救灾物资储备。     

固体废物管理技术进展

概述了固体废物管理技术近年来的主要进展,这些进展包括,固体废物从“摇蓝到坟墓”的全过程管理,即从废物产生到收集、运输贮存,再循环,再利用,处理直至最终处理过程所涉及到的：废物最小量化管理技术;废物转移跟踪管理中产生者,运输者,处理处理者,主管当局的职责、主管当局的职责,义务和管理方式;废物经营者向主管当局申请许可证的程序和申请。时,对废物交换制度和废物管理信息系统也作了概要介绍。     

串联式氨解脱离子交换法处理味精等电点废母液

提出了一种味精生产污染物控制新技术。采用四只串联的离子交换柱连续、交替吸附味精生产等电点废母液中残留的谷氨酸，通氨洗脱树脂吸附的谷氨酸，回收谷氨酸生产味精。这一技术可使味精得率提高４５％，污染物ＣＯＤＣｒ排放量减少２５６％。     

船舶在航更换压载水方法浅析

介绍了船舶在航更换压载水的各种方法，包括逐一更换法，注入顶出法和稀释法。并将各种方法从对船舶和船员的安全所造成的影响两方面进行了比较。     

Impact of urbanization on hydrochemical evolution of groundwater and on unsaturated-zone gas composition in the coastal city of Tel Aviv, Israel

The coastal city of Tel Aviv was founded at the beginning of the 20th century. The number of its inhabitants and its water consumption increased rapidly. This study analyses a 15-year record (1934-1948) of pre-industrial development of groundwater chemistry in the urban area. Archive data on concentrations of major ions, dissolved gases (CO2 and O2), organic matter, and pH were available for each half-year during the period of 1934-1948. The major factors causing changes in the chemistry of groundwater flowing in three sandy sub-aquifers have been seawater encroachment due to overpumping, and infiltration of effluents from pit-latrine collectors. Influence of these factors decreases with depth. Landward-penetrating seawater passed through clayey coastal sediments, interbedded among sands and calcareous sandstones, and spread into the Kurkar Group aquifer. This has led to exchange of sodium (dominant in seawater) with calcium adsorbed on clay particles, enriching groundwater with calcium. Intensity of cation exchange decreases inland and with depth. Infiltration of pit-latrine effluents has introduced large amounts of ammonium into the unsaturated zone. Its rapid oxidation in unsaturated sediments has caused massive nitrate production, accompanied by pore-water acidification. This process induces dissolution of vadose carbonate, resulting in enrichment of groundwater recharge in calcium. Anthropogenically induced dissolution of calcite in the unsaturated zone has been the major factor for the increase of Ca2+ concentration in groundwater, accounting for about 80% of this increase. In the interface zone, an additional 20% of calcium has been supplied by cation exchange. Owing to pH increase caused by denitrification in the aquifer, Ca(2+)-rich waters supersaturated with calcite could be formed, especially in the capillary fringe of the uppermost sub-aquifer, which could induce calcite precipitation and ultimately lead to the cementation of sandy aquifers. Urban development has caused drastic changes in the gas content in the unsaturated zone and in groundwater. Carbon dioxide was intensively generated by nitrification-denitrification processes, by hydration of urea, to a lesser degree by oxidation of organic matter, and probably by anoxic biodegradation of organics. Between 1934 and 1948, concentrations of CO2 in unsaturated sediment air rose from 3.2% to 7.6%. In the unsaturated zone, oxygen consumption for oxidation of ammonium and organic matter lowered O2 concentrations in sediment air to unusually low values of 3.9-12.9%. Nitrification in the urban unsaturated zone could thus serve as a pump, sucking in atmospheric oxygen at a rate of about 0.3-0.5 g m-2 day-1. The extreme concentrations of CO2 and O2 in unsaturated sediments have been preserved due to production and consumption of gas under conditions of diminishing areas open to the atmosphere, uncovered by buildings and by roads.     

沸石滤料曝气生物滤池启动性能研究

沸石滤料曝气生物滤池 (ZBAF)对氨氮的去除包括生物硝化和离子交换两种作用。中试装置启动试验表明 ,初期对氨氮的去除以离子交换作用为主 ,末期以硝化作用为主 ,不能以氨氮总去除率达到稳定作为启动过程结束的标志 ,而应以氨氮硝化去除率达到稳定作为标志。沿程试验表明 ,硝化细菌对沸石的“生物再生功能” ,实质是已被沸石交换的氨氮被水中浓度较大的其他阳离子交换下来后 ,被硝化菌所利用的现象 ;沸石表面有生物膜时 ,仍具有交换氨氮能力     

离子交换树脂及其在废水处理中的应用

介绍了离子交换树脂及其在多种废水处理中的应用研究。离子交换树脂法处理废水具有可深度净化、处理效率高和能实现多种金属综合回收的优点，在水处理领域必将得到更为深入的应用。