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％。     

BF4-废水水解法实验

常温下用水解法处理ＢＦ４废水．实验采用铝盐作主水解剂，试剂Ａ作助水解剂，ｐＨ值小于３，在常温条件下实现了对ＢＦ４的高效水解．研究结果表明，ＢＦ４∶Ａｌ３＋∶Ａ的质量比为１∶０．８∶０．１，水解时间６～３ｈ，水解率达到９９．５％以上．使用助水解剂Ａ，缩短了水解时间，减少了铝盐用量，对高浓度的ＢＦ４废水效果尤为显著，水解时间可缩短一半，主水解剂用量可减少１／５，处理后出水中的ＢＦ４含量可降到１０ｍｇ／Ｌ以下．     

我国低纬度、亚热带地区的降水化学及其雨水酸化趋势分析

在世界上酸沉降研究尚为空白的低纬度、亚热带地区建立了酸沉降监测网。通过两年的监测，结果表明降水中酸度和离子总浓度季节变化明显，Ｃａ￣（２＋）和ＮＨ在降水离子构成中占百分率较高，阳离子总和略大于阴离子总和。两广地区降水酸度是雨水中多种阴、阳离子综合作用的结果，降水中ＳＯ浓度高的地区是ＳＯ＿２排放量高的地区，控制雨水逐年酸化趋势的唯一途径是限制ＳＯ＿２排放。     

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。     

离子色谱法同时测定有机和无机阴离子

用离子色谱法同时测定有机阴离子和无机阴离子，实验中采用一种新型高容量分离柱，灵敏度高，选择性好。讨论了最佳实验条件的选择测定了Ｆ＾－，Ｃｌ＾－，ＳＯ４＾２－，ＮＯ２＾－，ＳｅＯ３＾２－、Ｃ２Ｏ４＾２－、甲酸奶和乙酸根等阴离子，并且分析了沈阳地区雪样中的几种阴离子。     

土壤对SO_4~(2-)的吸附-解吸特征

研究区两类主要农业土壤在实验温度和吸附平衡液浓度相同时,酸性淋溶土(红壤、黄红壤)SO_4~(2-)吸附量均高于近中性水成土 (水稻土、潮土),与土壤游离Fe,Al含最呈显著正相关,吸附过程均符合Freundlich和Ternkin方程描述规律:低温(10℃)时吸附量均高于常温 (25℃),表明吸附系放热反应,有利于冬,春酸雨频仍季节土壤对SO_4~(2-)的固定,研究表明土壤吸附过程由快速反应(0—4h)和慢速反应(4—48h)两部份组成,且符合反映吸附机制较复杂的多级动力学反应规律,0.01mol/l Ca(NO_3)_2和1.0mol/l NaCl对土壤吸附态SO_4~(2-)的解吸率较高,表明SO_4~(2-)主要被土壤吸附于带正电荷的氧化物胶体表面,离子交换可逆吸附机制似占较大优势。     

~(35)S标记法研究土壤中SO_4~(2-)的吸附-解吸行为

本文比较了~35S同位素标记法和两种常规化学分析、一种电化学分析法测定环境样品中SO_4~2-的优劣.用本法和BaCrO_4分光光度法研究土壤对SO_4~2-的吸附-解吸特征,表明两者测定结果接近,且所得规律一致.酸雨研究中,在样品数量多、SO_4~2-分析任务重且仪器、设备条件具备时,本法为便捷、准确、较理想的SO_4~2-测定技术.     

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