电镀含铬废水的处理和利用

论述了电镀含铬废水的处理和以铬污泥为原料制取红帆钠的原理和条件。经处理后的废水Ｃｒ（Ⅳ）、Ｃｒ（总）含量均达到规定的排放标准：产生的铬污泥可用于制取红矾钠，不会产生二次污染。整个流程简单，铬的转化率高，经济效益与社会效益明显。     

钛酸四丁酯水解制备TiO_2半导体光催化剂研究

研究了钛酸四丁酯水解制备TiO2 粉末的两大影响因素R值 (R是水和钛酸四丁酯的摩尔比 )和烧结温度 .通过光催化氧化五氯苯酚钠实验 ,结合对催化剂晶型结构、比表面积的表征分析 ,综合评价所制备的催化剂 .实验结果表明 ,当R =10 0、烧结温度为 6 5 0℃、烧结时间为 1h ,钛酸四丁酯水解所制备的TiO2 半导体光催化剂催化活性和使用寿命均比较理想 .从晶型结构分析 ,当催化剂中锐钛矿和金红石按一定比例共存时 ,其催化活性较单一金红石或锐钛矿高 .实验认为锐钛矿与金红石的最佳比约为 2∶1     

麦草低污染制浆新技术

麦草低污染制浆新工艺采用亚硫酸钠-甲醛-蒽醌（加入少量催化剂）制浆（SFP-AQ法）,生产吨浆的COD排放总量下降30％,色度下降60％,悬浮物总量下降50％,制浆黑液的pH值下降至7～8。采用该新工艺同时还可产生表面活性好、便于利用的木素磺酸钠和其他产品,使纤维资源得到综合利用,为解决中小型草浆造纸厂的污染问题提供一条有效途径。j     

制浆,黑液碱回收试验研究

本文对造纸工业制浆黑液中的碱回收问题进行了探讨,在实验的基础上,提出了一种切实可行而且比传统的燃烧法投资更省的碱回收工艺,即将多效蒸发后的浓缩黑液经等离子处理后得到的黑粉,稀释后用离心过滤脱水的办法再进行碱回收。     

地下水中钠形成的控制因素及其与人群健康的关系

利用国家科技攻关成果并根据国内外的研究现状，论证了地下水中钠元素形成的控制因素及其与人群健康的关系。     

多相抽提和原位化学氧化联合修复技术应用——某有机复合污染场地地下水修复工程案例

某电子机械厂搬迁后原址约1 500 m区域地下水受到了多种类型的有机物复合污染,包括石油烃、苯系物和多环芳烃,并且部分区域发现有明显轻质非水溶相流体(LNAPL)。该案例首先应用多相抽提技术强化回收地下水中的LNAPL,并去除土壤气体和地下水中溶解态的污染物。当地下水中不存在明显LNAPL且污染物浓度不再明显降低后,继续应用原位化学氧化技术进行修复,所使用氧化剂为"过硫酸钠+Na OH"。经过45 d的多相抽提以及4t过硫酸盐氧化剂注射之后,验收监测表明污染区域地下水污染物浓度均达到了修复目标。该案例表明,多种修复技术的联合应用能够明显加快修复进度、提高修复效率、节约修复成本。对于存在LNAPL,且修复目标较严格的有机复合污染场地,多相抽提结合原位化学氧化联合修复是一种较好的修复技术选择。     

不同有机碳源对小球藻的生长与产油量的影响

该研究探讨了葡萄糖和乙酸钠两种碳源对小球藻（Chlorella protothecoides）的生长与产油量的影响,并对小球藻在两种碳源混合培养下的生长与产油情况进行了分析.研究结果表明,葡萄糖和乙酸钠的浓度对小球藻的生物量和产油量都有较大的影响,最优的浓度分别为15 g/L和20.5 g/L.相对于以葡萄糖为碳源的小球藻,以乙酸钠为碳源的小球藻的生物量与含油量均较低.在混合培养条件下,葡萄糖最先被小球藻吸收利用.图5,表1,参8.     

The influence of metam sodium on soil respiration

Abstract

A laboratory experiment was performed in order to evaluate the extent to which metam sodium (MS) applied at two different recommended rates and its degradation product, methyl isothiocyanate ( MITC ), affect soil respiration. Results suggest that MS degradation to MITC was complete within 4 hours and that MITC decomposed quickly in a few days, except in the soil containing high organic matter where it was still present after 15 days. Following the addition of MS, a lag phase appeared in CO₂‐C evolution in the soil. It was longer for the higher dose of MS added and for the two soils with low organic C content. The dynamics of the process was described by the Bonde and Rosswall model and by the Gompertz RS E model for the untreated and the MS‐treated soils, respectively.     

Hygroscopic properties of sodium and potassium salts as related to saline mineral dusts and sea salt aerosols

Mineral dust, soil, and sea salt aerosols are among the most abundant primary inorganic aerosols in the atmosphere, and their hygroscopicity affects the hydrological cycle and global climate. We investigated the hygroscopic behaviors of six Na- and K-containing salts commonly found in those primary organic aerosols. Their hygroscopic growths as a function of relative humidity (RH) agree well with thermodynamic model prediction. Temperature dependence of deliquescence RH (DRH) values for five of those salts was also investigated, which are comparable to those in literature within 1%–2% RH, most showing negative dependence on temperature. Hygroscopic growth curves of real-world soil and sea salt samples were also measured. The hygroscopic growths of two more-hydroscopic saline soil samples and of sea salt can be predicted by the thermodynamic model based on the measured water-soluble ionic composition. The substantial amounts of water-soluble ions, including Na⁺ and K⁺, in saline soil samples imply that even nascent saline soil samples are quite hygroscopic at high-RH (>80%) conditions. For three less-hygroscopic dust samples, however, measurements showed higher water uptake ability than that predicted by the thermodynamic model. The small amount of water taken up by less-hygroscopic dust samples suggests that dust particles might contain thin layers of water even to very low RH. The results of this study provide a comprehensive characterization of the hygroscopicity of Na- and K-containing salts as related to their roles in the hygroscopic behaviors of saline mineral dusts and sea salt aerosols.