离子交换膜的制备及发展趋势研究

总结当前离子交换膜制备技术的发展状况.从膜的分类及膜性能出发,讨论均相膜及异相膜的差异和今后各自的发展前景,并就提升膜单方面性能(如:选择透过性、离子交换容量、膜电阻、抗氧化性等)的方式进行归纳总结.离子交换膜的改进制备大多从结构上入手,提出今后膜制备的主要研究方向为:深化均相膜制备技术、结合国内成熟的离子交换树脂制备工艺改进异相膜的制备技术.     

Identification of key factors governing chemistry in groundwater near the water course recharged by reclaimed water at Miyun County, Northern China

Reclaimed water was successfully used to recover the dry Chaobai River in Northern China, but groundwater may be polluted. To ensure groundwater protection, it is therefore critical to identify the governing factors of groundwater chemistry. Samples of reclaimed water, river and groundwater were collected monthly at Chaobai River from January to September in 2010. Fifteen water parameters were analyzed. Two kinds of reclaimed water were different in type (Na-Ca-Mg-Cl-HCO3 or Na-Ca-Cl-HCO3 ) and concentration of nitrogen. The ionic concentration and type in river were similar to reclaimed water. Some shallow wells near the river bed had the same type (Na-Ca-Mg-Cl-HCO3 ) and high concentration as reclaimed water, but others were consistent with the deep wells (Ca-Mg-HCO3 ). Using cluster analysis, the 9 months were divided into two periods (dry and wet seasons), and all samples were grouped into several spatial clusters, indicating different controlling mechanisms. Principal component analysis and conventional ionic plots showed that calcium, magnesium and bicarbonate were controlled by water-rock interaction in all deep and some shallow wells. This included the dissolution of calcite and carbonate weathering. Sodium, potassium, chloride and sulfate in river and some shallow wells recharged by river were governed by evaporation crystallization and mixing of reclaimed water. But groundwater chemistry was not controlled by precipitation. During the infiltration of reclaimed water, cation exchange took place between (sodium, potassium) and (calcium, magnesium). Nitrification and denitrification both happened in most shallow groundwater, but only denitrification in deep groundwater.     

URG-9000型离子色谱仪常见问题及解决办法

介绍了URG-9000型离子色谱仪在运行中常见的问题,URG监测的离子数据部分或全部缺失、数据异常、偏低等情况。并对这些常见问题的出现原因进行了分析说明,通过做校准曲线,考虑背景电导等提出了相应的解决方法。为了提高仪器的运行稳定性保证数据的可靠、准确性,提出了仪器日常维护的一些注意事项。     

新型磁性聚谷氨酸吸附剂对水中Pb2+的吸附去除

德岛大学安澤幹人首次利用γ-PGA在Fe3O4磁性纳米颗粒上进行涂层,制得了γ-聚谷氨酸-Fe3O4磁性纳米颗粒（PG-M）.本实验利用透射电镜以及扫描电镜对PG-M吸附剂的形貌进行了分析,发现PG-M与未涂层的Fe3 O4具有相似的形状以及大小,均为不规则的层状结构,且晶粒直径在120～320 nm之间;实验中针对性地对水溶液中Pb2＋进行了吸附探讨.在振荡实验中,通过主要参数的变化（pH值、吸附时间、竞争离子浓度、腐殖酸浓度）,得到如下结果：吸附最佳pH值为7.0;吸附量随着吸附时间的延长而增长,吸附平衡时间为45 min;Na＋对PG-M去除Pb2＋没有很强的干扰性,而Ca2＋则显示出一定的干扰作用;腐殖酸对吸附效果的影响是复杂的,表现为先增强吸附效果,随后降低吸附效果;最佳条件时Pb2＋的最大吸附量为93.3 mg/g.PG-M对Pb2＋的吸附均能较好地符合Freundlich和Langmuir等温吸附模型,其中Langmuir方程能更好地描述PG-M的吸附特征,说明PG-M在水溶液中对金属离子的吸附为单分子层吸附.PG-M吸附符合准二级动力学模型（r2〉0.99）.不同浓度的HCl和HNO3溶液的再生实验发现,0.1 mol/L的HCl溶液作为吸附再生液,可取得较好的再生效果.表明PG-M是可再生的,具有较好的经济性和可持续性.     

沸石强化生化装置脱氮功能的效果及机理初探

针对石化工业废水开展沸石强化脱氮处理试验研究,通过比较沸石浓度25mg/L与空白,以及沸石浓度25 mg/L与50mg/L两阶段脱氮效果,探讨沸石促进脱氮功能的机理,结果表明,曝气池中投加沸石可明显提高氨氮和总氮的去除率,硝化细菌总数和硝化功能也得到增强。与空白对照组相比, 沸石浓度25mg/L的试验组运行稳定后,氨氮去除率提高约10%~13%,总氮去除率约提高13%,出水中NO3--N含量约提高100%,氨氮与总氮之比下降6%,内源硝化耗氧呼吸速率可提高138%,硝化细菌总数是空白对照组2.2folds。沸石浓度提高到50mg/L后,试验组的脱氮效果略有增加,但效果不明显。通过对试验结果的关联分析,认为沸石提高系统脱氮能力的原因一方面是因为沸石对NH4+及硝态氮的交换吸附,另一方面NH4+离子富集于沸石表面及内部、沸石颗粒独特的好氧-缺氧微环境,以及沸石离解出CO32- 或HCO3-增加碱度等条件,促进了硝化细菌和反硝化细菌的生长,从而提高了系统脱氮能力。     

Environmental and economic assessment of a greenhouse waste heat exchange

As the economic costs of energy and the negative externalities associated with the combustion of fossil fuels threaten the economic viability of greenhouses in northern climates there is a renewed interest in the use of waste heat. This paper presents a technical and economic methodology to determine the viability of establishing waste heat greenhouses using the waste heat from industrial processes in northern climates. A case study is presented of an exchange between a tomato greenhouse and a flat glass manufacturing plant, which found the waste heat system is significantly more economic to operate than a purely natural gas system.     

琉基纤维素对水中Cr(VI)离子的吸附研究

制备了巯基纤维素并用其对含Cr(VI)离子的溶液进行了静态吸附实验.研究了pH值、吸附时间、反应温度、吸附剂用量等因素对吸附性能的影响.结果表明:在pH值为2、Cr(VI)浓度为50 mg/L和吸附剂为0.5 g时,常温条件下吸附6h后,Cr(VI)去除率达到99.2%,吸附反应符合Langmuir和Freundlic...     

Lindet ypeF(K)沸石对Zn~(2+)的吸附研究

利用粉煤灰合成Linde type F(K)沸石吸附重金属Zn2+,考察吸附剂量、pH值、反应温度对Zn 2+吸附效果影响,研究沸石吸附Zn2+的等温线与动力学,得到了相应的模型。结果表明:吸附剂量、pH值、反应温度均对Zn2+去除效果影响显著。随着吸附剂量增大,Zn 2+去除效果不断提高,饱和吸附量逐渐减小。初始pH值为3~7时,沸石对Zn2+去除率随pH值升高迅速提高。反应温度越高,沸石吸附Zn2+到达平衡时间越短。沸石对Zn2+吸附过程符合Langmuir吸附等温式,其吸附为单分子层吸附;准二级反应动力学方程能很好描述沸石对Zn2+的吸附行为。     

春、夏季长江口及其邻近海域溶解N2O的分布和海-气交换通量

分别于2012年3月和7月对长江口及其邻近海域进行了调查,对水体中溶解氧化亚氮(N2O)的分布及海-气交换通量进行了研究.结果表明,春季长江口及其邻近海域表层海水中溶解N2O浓度范围为9.34~49.08 nmol·L-1,平均值为(13.27±6.40)nmol·L-1.夏季表层溶解N2O浓度范围为7.27~27.81 nmol·L-1、平均值为(10.62±5.03)nmol·L-1.两航次表、底层海水中溶解N2O浓度相差不大.长江口溶解N2O浓度由近岸向外海逐渐降低,受陆源输入影响显著.溶解N2O浓度高值出现在长江口最大浑浊带附近,这主要是由于水体中较高的硝化速率造成的.温度是影响N2O分布的另一个重要因素,对溶解N2O浓度有双重作用.春季和夏季表层海水中N2O饱和度范围分别为86.9%~351.3%和111.7%~396.0%,平均值分别为(111.5±41.4)%和(155.9±68.4)%,大部分站位处于过饱和状态.利用LM86、W92和RC01公式分别计算了长江口及其邻近海域N2O的海-气交换通量,春季分别为(3.2±10.9)、(5.5±19.3)和(12.2±52.3)μmol·(m2·d)-1,夏季分别为(7.3±12.4)、(12.7±20.4)和(20.4±35.9)μmol·(m2·d)-1,初步估算出长江口及其邻近海域的年平均释放量分别为0.6×10-2Tg·a-1(LM86)、1.1×10-2Tg·a-1(W92)、2.0×10-2Tg·a-1(RC01).长江口及其邻近海域虽然只占全球海洋总面积的0.02%,但其释放的N2O占全球海洋释放量的0.06%,表明长江口及其邻近海域是产生和释放N2O的活跃区域.     

分光光度法与离子色谱法测定降水中铵离子的对比

采用分光光度法和离子色谱法测定降水中铵离子,比对研究两种方法的测定原理、标准曲线和检出限。结果表明,两种方法对标准样品和实际样品分析测定均能达到质控要求,测定结果基本一致。离子色谱法方便快捷,污染少,结果准确可靠,可以同时测定多种阳离子。