纳米FeO作用下4-氯酚的脱氯特性及机理

采用化学还原法制备了纳米Fe^O, ESEM测定结果表明其颗粒在1～100 nm内. 实验表明这些纳米Fe^O能在20 h内将初始浓度为20 mg/L的4-氯酚完全降解, Fe^O对4-CP的还原脱氯是主要去除途径. 苯酚是脱氯反应的主要产物. 当4-CP的初始浓度由20　mg/L增大到50, 100, 150　mg/L时, 其相对去除率明显降低, 但绝对降解量有较大提高. 温度不仅影响脱氯速率, 而且影响4-CP去除的途径. 30℃时, 脱氯反应为主要反应; １０℃时, 较易产生氧化产物. Fe原子的迁移过程在4-CP的降解中也是一个重要的限速步骤. 此外, 纳米Fe^O具有很好的稳定性, 在受试的379　h内, 纳米Fe^O能够应对不同浓度冲击及反复投加的4-氯酚冲击的能力.     

纳米Fe3O4负载的浮游球衣菌去除重金属离子的工艺研究

以纳米Fe₃O₄负载浮游球衣菌（Sphaerotilus natans）制备复合生物吸附剂,对此吸附剂进行表征并考察了其吸附水中重金属离子的性能.红外光谱分析表明,此复合生物吸附剂表面的主要活性基团为酰胺基（—CONH—）和羟基（—OH）.吸附性能研究表明,菌含量和流量是影响复合生物吸附剂吸附重金属离子的主要因素,在Cu²⁺初始浓度c₀<20 mg/L,菌含量1.5 g/L（菌/ Fe₃O₄＝3∶2）,流量0.96 L/h 时吸附剂对Cu²⁺的吸附效果最好;用稀盐酸对复合生物吸附剂进行再生,吸附剂可重复使用10次以上,再生液可重复使用3次; 吸附选择性为：Pb²⁺ > Cu²⁺ > Zn²⁺>Cd²⁺.     

高铁低铝煤矸石酸法提取铝、铁研究

以高铁低铝煤矸石为原料,经机械活化,酸浸提取有价元素铝、铁.首先利用硫酸盐在不同温度和不同硫酸质量分数条件下的溶解度差异,通过结晶分离法从酸浸液中转移出硫酸盐,然后利用新鲜煤矸石中和酸浸液中的游离酸,调节pH值至1.5～2.0,制备酸浸初步净化液.以初步净化液为研究对象,利用不同离子水解pH值的差异进行物质分离,再经纯化处理制备相应产品.用XRD对原料和产品进行了表征.结果表明,在硫酸质量分数为75％的条件下,反应液固比为4、温度为125℃、3h时煤矸石中铝、铁溶出率分别为92.5％、99.7％.通过项目经济效益分析可知,该法可以产生良好的环境效益、社会效益,同时可实现煤矸石增值,产生较好的经济效益.     

烧结烟气中氨-络合法同步脱硫脱硝络合剂再生的实验研究

对氨-络合法同步脱硫脱硝废液中络合剂再生进行了实验研究。结果表明,在50℃、p H值为5.65、Fe(Ⅱ)-EDTA浓度为0.04 mol/L、再生剂/Fe(Ⅱ)EDTA为2∶1的条件下,经铁粉再生后吸收液最高脱硫脱硝效率分别达到99%和75%;焦粉再生最高脱硫脱硝效率达到97%和46%;而乙二醛再生最高脱硫脱硝效率仅为80%和20%。同时铁粉再生中试结果也还表明脱硫效果可以稳定在100%,脱硝效果可维持在60%。     

钢铁企业大气污染环保提升技术措施

针对2015年1月1日新《中华人民共和国环境保护法》和钢铁排放系列新标准(2012版)实施的新形势,指出了钢铁企业面临的五大考验,分析了大气污染物治理的技术现状,提出实现钢铁工业大气污染环保提升的技术措施。     

熔融铜渣中的金属提取及尾渣制矿棉探索试验

目前铜渣资源化利用主要采用选矿法,处理后仍有大量尾渣无法有效利用。故将铜渣视为含有铜铁金属、高氧化硅无机材料且含高热值的资源,对铜渣进行资源化处理。熔融条件下对铜渣进行还原处理回收含铜铸铁,尾渣用于制备矿棉,实现了熔融铜渣的高附加值利用。该技术处理铜渣产品附加值高、能耗低,且具备一定的市场空间,具有较好的发展前景,可进行推广应用。     

Interaction between Cu2+ and different types of surface-modified nanoscale zero-valent iron during their transport in porous media

This study investigated the interaction between Cu²⁺ and nano zero-valent iron (NZVI) coated with three types of stabilizers (i.e., polyacrylic acid [PAA], Tween-20 and starch) by examining the Cu²⁺ uptake, colloidal stability and mobility of surface-modified NZVI (SM-NZVI) in the presence of Cu²⁺. The uptake of Cu²⁺ by SM-NZVI and the colloidal stability of the Cu-bearing SM-NZVI were examined in batch tests. The results showed that NZVI coated with different modifiers exhibited different affinities for Cu²⁺, which resulted in varying colloidal stability of different SM-NZVI in the presence of Cu²⁺. The presence of Cu²⁺ exerted a slight influence on the aggregation and settling of NZVI modified with PAA or Tween-20. However, the presence of Cu²⁺ caused significant aggregation and sedimentation of starch-modified NZVI, which is due to Cu²⁺ complexation with the starch molecules coated on the surface of the particles. Column experiments were conducted to investigate the co-transport of Cu²⁺ in association with SM-NZVI in water-saturated quartz sand. It was presumed that a physical straining mechanism accounted for the retention of Cu-bearing SM-NZVI in the porous media. Moreover, the enhanced aggregation of SM-NZVI in the presence of Cu²⁺ may be contributing to this straining effect.     

Resource conservation strategies for rice‐wheat cropping systems on partially reclaimed sodic soils of the Indo‐Gangetic region,and their effects on soil carbon

The Indo‐Gangetic plain is characterized by intensive agriculture, largely by resource‐poor small and marginal farmers. Vast swathes of salt‐affected areas in the region provide both challenges and opportunities to bolster food security and sequester carbon after reclamation. Sustainable management of reclaimed soils via resource conservation strategies, such as residue retention, is key to the prosperity of the farmer, as well as increases the efficiency of expensive initiatives to further reclaim sodic land areas, which currently lay barren. After five years of experimentation on resource conservation strategies for rice‐wheat systems on partially reclaimed sodic soils of the Indo‐Gangetic region, we evaluated changes in different soil carbon pools and crop yield. Out of all resource conservation techniques which were tested, rice‐wheat crop residue addition (30% of total production) was most effective in increasing soil organic carbon (SOC). In rice, without crop residue addition (WCR), soils under zero‐tillage with transplanting, summer ploughing with transplanting and direct seeding with brown manuring showed a significant increase in SOC over the control (puddling in rice, conventional tillage in wheat). In these treatments relatively higher levels of carbon were attained in all aggregate fractions compared to the control. Soil aggregate sizes in meso (0.25‐2.0 mm) and macro (2‐8 mm) ranges increased, whereas micro (< 0.25 mm) fractions decreased in soils under zero‐till practices, both with and without crop residue addition. Direct seeding with brown manuring and zero tillage with transplanting also showed an increase of 135% and 95%, respectively, over the control in microbial biomass carbon, without crop residue incorporation. In zero tillage with transplanting treatment, both with and without crop residue showed significant increase in soil carbon sequestration potential. Though the changes in accrued soil carbon did not bring about significant differences in terms of grain yield, overall synthesis in terms of balance between yield and carbon sequestration indicated that summer ploughing with transplanting and zero tillage with transplanting sequestered significantly higher rates of carbon, yet yielded on par with conventional practices. These could be appropriate alternatives to immediately replace conventional tillage and planting practices for rice‐wheat cropping systems in the sodic soils of the Indo‐Gangetic region.     

Fe~0-厌氧微生物降解2,4-二氯酚的效应及机理

以2,4-二氯酚(2,4-DCP)为目标污染物,采用间歇试验,接种厌氧混合微生物,考察葡萄糖共基质条件下不同pH值时零价铁(Fe)0对2,4-DCP生物降解的效应,并对Fe0与厌氧微生物联合体系的作用机理进行探讨。结果表明:Fe0与厌氧微生物联合作用可提高2,4-DCP的降解效果,且中性或偏碱性环境下联合体系对目标污染物的促进效果较酸性环境明显,初始pH值为8时目标污染物的降解效果最好。Fe0在厌氧条件下腐蚀产生的OH-可有效平衡葡萄糖发酵产生的有机酸,使体系挥发性脂肪酸(VFA)的浓度维持在较低水平(300 mg/L),同时促使联合体系pH值上升从而利于目标物2,4-DCP的降解。Fe0在酸性环境的腐蚀较强,腐蚀产物以Fe2+为主,Fe3+含量较少。不同pH值时"Fe0+微生物"体系的COD去除率与目标物降解效果有一定相关性。     

北京市密云水库上游金铁矿区土壤重金属污染特征及对比研究

不同金属矿山选冶活动造成的矿区及周边土壤中重金属的分布累积特征不同.为了解密云水库上游金矿和铁矿矿区土壤中重金属地球化学特征的异同及污染状况,对区域内典型的金矿和铁矿矿区进行土壤样品采集,应用地球化学方法研究了2种土壤中重金属的污染特征,并应用地累积指数法评价了其污染状况.结果表明,2种土壤中除As外的其它重金属含量明显高于北京市土壤重金属背景值,金矿矿区土壤重金属含量普遍高于铁矿矿区.相关性分析表明,金矿矿区土壤中Cu含量与Pb、Zn(p<0.01)及Cr、有机质(OM)含量(p<0.05)之间显著相关,pH值与Pb含量(p<0.01)及Hg含量(p<0.05)呈显著负相关,而铁矿矿区土壤中重金属含量之间的相关性不显著.金矿尾砂中重金属含量明显高于铁矿尾砂,与矿区土壤污染状况一致.地累积指数法评价结果显示,金铁矿区土壤中重金属的污染程度均已十分严重,金矿矿区土壤污染程度高于铁矿,金矿矿区土壤重金属的污染程度由高到低依次为:Pb>Hg>Cd>Cr>Cu>Zn>Co>As;铁矿矿区土壤重金属的污染程度由高到低依次为:Pb>Cd>Cr>Co>Cu>Zn>Hg>As.该研究数据可为同一区域内不同金属矿区重金属污染的有效监控与治理提供科学依据.