柠檬酸盐法在硫酸尾气治理与资源化中的应用

针对某化工厂硫酸生产中,由于硫酸生产中受冶炼烟气SO2浓度影响波动较大、冶炼系统故障以及自身工艺技术等因素的制约,化工厂硫酸生产系统尾气SO2浓度在烟气非正常条件下(烟气中SO2浓度小于3.5%),甚至在烟气正常条件下(烟气中SO2浓度大于3.5%)有时均难以达标排放,不但造成大量含SO2的尾气超标排入大气,而且使得大...     

线路板蚀刻废液资源化处理零排放新工艺

对广州市白云区南溪化工厂开发出的一套对线路板蚀刻废液集中资源化处理的零排放处理新工艺的工艺条件进行了深入研究,并通过正交试验的方法,优化了最关键的三个工艺条件,即混合生石灰加入量为碱式氯化铜泥重量的0.8倍,焙烧温度为500℃,粉碎粒度为100目。在此条件下处理后的物料,通过摇床分选后得到的氧化铜纯度达96.5%,回收率达97.1%。由于这套工艺通过在固相条件下生成氧化铜并用重力分选的方法将其分离出来,克服了原有工艺的缺陷,使废液中所有的成分能够在较低的处理成本下全部分离回收,完全无“三废”排出,达到了清洁生产的要求。此工艺已经投入运行,效果理想。     

碱性蚀刻废液的综合利用

介绍了利用含铜蚀刻废液回收铜的生产工艺、技术特点、工艺流程和产品质量. 研究了沉淀母液中残余铜的除去方法,使之再生,可回用于碱性蚀刻液的生产.碱性蚀刻废液的综合利用对于资源节约与环境保护都具有重要意义.     

金在热液中的地球化学性质实验研究

通过近百次实验研究表明，金在水热条件下的地球化学行为具有以下几个特点：金在氧化条件下溶解，还原条件下沉淀；金在高温下溶解，低温下沉淀；金在碱性或酸性溶液中溶解，在中性溶液中沉淀；金在低压下溶解，在高压下沉淀；随着fs八的增加，金的溶解度随之增加；金可以[An（HS）4]、[Au（HS）2]-、[Au（Cl4）]、[Au（Cl2）]-等络合物形式存在于热液中；在热液中金普遍以An3＋的络合物形式存在，Aul＋的络合物形式次之，随着温度的升高，热液中Au1＋的含量明显增加。     

土壤硒的生物有效性研究

对黑麦幼苗的试验表明,黑麦幼苗中的总硒(Se)浓度与总干重的乘积与0.1mol/L KH2PO4浸提态Se呈显著相关.对黑油菜的试验表明,在酸性土壤上,当Se(Ⅵ)的量≥0.5mg/kg时,可显著减少黑油菜的产量;而当Se(Ⅳ)的量达到2.0mg/kg时对产量影响不大;黑油菜吸收Se(Ⅵ)的量要大于吸收Se(Ⅳ)的量.通过田间采样分析表明,KH2PO4浸提态Se能反映土壤对植物的供Se状况,推荐用0.1mol/L KH2PO4溶液作为酸性土壤生物有效性Se的浸提溶液.影响土壤Se生物有效性的主要因子是CaCO3,其次是粉粒、有机质、黏粒含量.pH值可通过CaCO3对KH2PO4浸提态Se产生影响.     

纳米铁锰氧化物对钒的吸附特性研究

为寻求处理土壤和地下水钒污染的吸附剂,采用模拟实验,开展了纳米铁锰氧化物(MnFe_2O_4)对五价钒(V~(5+))的吸附特征研究,分析了纳米铁锰氧化物浓度、pH值、时间、温度和初始钒浓度等因素对MnFe_2O_4吸附V~(5+)的影响,以揭示纳米铁锰氧化物的吸附动力学及热力学等特征,并通过扫描电镜(SEM)和红外光谱(IR)等表征方法分析了纳米铁锰氧化物吸附V~(5+)的机理.结果表明,在初始钒溶液为100 mg·L~(-1),MnFe_2O_4加入量为0.1 g,pH=4,温度为25℃的条件下,吸附过程在24 h达到平衡,且此条件下有最大吸附值和吸附率,分别为15.14 mg·g~(-1)和60.54%.纳米铁锰氧化物吸附钒的动力学过程符合伪二级动力学模型,等温吸附线符合Langmuir模型.热力学研究表明,升高温度有利于吸附,吸附过程为吸热过程.由扫描电镜结果可知,纳米铁锰氧化物有较大的比表面积,可提供较多的活性位点.因此,纳米铁锰氧化物可作为一种吸附材料用于钒污染废水处理.     

Degradation of 2,4-dichlorophenol with a novel TiO2/Ti-Fe-graphite felt photoelectrocatalytic oxidation process

Degradation of 2,4-dichlorophenol(2,4-DCP)was studied in a novel three-electrode photoelectrocatalytic(PEC)integrative oxidation process,and the factors influencing the degradation rate,such as applied current,flow speed of O_2,pH,adscititious voltage and initial 2,4-DCP concentration were investigated and optimized.H_2O_2 was produced nearby cathode and Fe~(2 )continuously generated from Fe anode in solution when current and O_2 were applied,so,main reactions,H_2O_2-assisted TiO_2 PEC oxidation and E-Fenton reaction,occurred during degradation of 2,4-DCP in this integrative system.The degradation ratio of 2,4-DCP was 93% in this integrative oxidation process,while it was only 31% in E-Fenton process and 46% in H_2O_2-assisted TiO_2 PEC process.So,it revealed that the degradation of 2,4-DCP was improved greatly by photoelectrical cooperation effect.By the investigation of pH,it showed that this integrative process could work well in a wide pH range from pH 3 to pH 9.     

溶液环境对荷电超滤膜和传统中性超滤膜去除天然有机物的影响

以Aldrich 腐殖酸溶液为水样,研究比较了溶液环境(pH值、离子强度和钙离子)对荷电改性再生纤维素超滤膜和传统中性未改性再生纤维素超滤膜过滤过程的影响.结果表明, ①pH值主要通过质子化作用影响荷电膜以及腐殖酸分子的荷电量,进而影响荷电超滤过程.溶液pH值从7.5下降到3.5时,荷电超滤膜对腐殖酸的截留率从92%减少到79%,超滤4 h时,膜通量下降从26%增加到36%.②离子强度的改变是通过影响腐殖酸分子的物化性质和静电屏蔽作用来影响超滤过程的.当溶液离子强度为0、 3和100 mmol/L时,初始截留率依次降低,分别为92%、 87%和48%,超滤4 h时,荷电超滤膜的通量下降依次增加,分别为26%、 35%和63%.③Ca2+浓度的影响,需要综合考虑静电屏蔽作用、Ca2+的架桥作用以及滤饼层的压实性等各方面的影响.④pH值、离子强度和钙离子对中性超滤膜过滤行为的影响趋势与荷电超滤膜相似,但其影响程度有着较大的差别.研究结果对荷电超滤膜技术在实际应用中选择合适环境条件提供了参考.     

土壤与酸性含氟溶液相互作用特征及机理研究

通过反复多次提取实验方法模拟了酸性含氟溶液与红壤和赤红壤相互作用过程。结果表明：在相互作用过程中，土壤中氟含量不同对土壤溶液pH有明显不同的影响。当氟含量较低时氟离子对土壤溶液pH的影响不明显；当浓度较高时则可大大提高土壤溶液的pH，缓冲土壤酸化。在第一次提取中因氟的大量吸附可减少溶液中铝的浓度，且氟含量越高铝浓度越少量越大。随提取次数增加土壤溶液中铝、氟浓度同时增加，且氟含量越高铝浓度越大，其中氟以AI－F络合物为主。     

Dynamics of soil inorganic nitrogen and their responses to nitrogen additions in three subtropical forests, south China

Three forests with different historical land-use, forest age, and species assemblages in subtropical China were selected to evaluate current soil N status and investigate the responses of soil inorganic N dynamics to monthly ammonium nitrate additions. Results showed that the mature monsoon evergreen broadleaved forest that has been protected for more than 400 years exhibited an advanced soil N status than the pine （Pinus massoniana） and pine-broadleaf mixed forests, both originated from the 1930＇s clear-cut and pine plantation. Mature forests had greater extractable inorganic N pool, lower N retention capacity, higher inorganic N leaching, and higher soil C/N ratios. Mineral soil extractable NH4^＋-N and NO3-N concentrations were significantly increased by experimental N additions on several sampling dates, but repeated ANOVA showed that the effect was not significant over the whole year except NH4^＋-N in the mature forest. In contrast, inorganic N （both NH4^＋-N and NO3^--N） in soil 20-cm below the surface was significantly elevated by the N additions. From 42% to 74% of N added was retained by the upper 20 cm soils in the pine and mixed forests, while 0%-70% was retained in the mature forest. Our results suggest that land-use history, forest age and species composition were likely to be some of the important factors that determine differing forest N retention responses to elevated N deposition in the study region.