两种微藻胞外分泌物与NO2-、NO3-对2，4-D光解的影响

在模拟太阳光照射下,利用旋转式光化学反应装置,研究了海水小球藻(Chlorella vulgaris)和新月菱形藻(Nitzschia closterium)的胞外分泌物(EOM),以及分别在NO-2或(和)NO-3共存条件下对2,4-二氯苯氧乙酸(2,4-D)光解的影响.实验结果表明,2,4-D在海水小球藻和新月菱形藻EOM及分别在NO-2、NO-3共存下的光解过程均符合准一级动力学反应.研究发现,2,4-D的光解速率随海水小球藻和新月菱形藻EOM浓度的增加而减小,表明这两种微藻EOM可抑制海水中2,4-D的光解.当在微藻EOM溶液中分别加入不同浓度的NO-2或NO-3后,微藻EOM对2,4-D光解的抑制作用减弱,且随着NO-2和NO-3浓度的增加,2,4-D光解速率明显增加.特别是当微藻EOM与NO-2或NO-3三者共存时,可进一步促进2,4-D的光解.     

广州地区SO42-、NO3-、NH4+与相关气体污染特征研究

本文获得了2009年12月1日至2011年12月31日广州二次无机离子(SO2-4、NO-3、NH+4)及相关反应性气体(NOx/SO2/HNO2/HNO3等)的小时浓度数据,并分析了其污染特征.研究结果表明:PM2.5的浓度季节变化特征为冬秋春夏,SO2-4的浓度季节变化特征为秋冬春夏,NH+4的为冬秋春夏,NO-3则为冬春秋夏,SO2-4、NO-3和NH+4之和占PM2.5的比重大小为秋夏春冬;硫氧化率(SOR)均大于0.1,秋冬季节的值高于春夏季节,与SO2-4的浓度变化趋势一致;氮氧化率(NOR)日变化呈单峰形式,最大值出现在06时,最小值出现在14时,春冬季节的值高于夏秋季节,与NO-3的浓度变化趋势一致;广州地区NH3/NH+4除10—12月外,其月均值均大于1;在典型过程中,SO2-4、NO-3、NH+4、SOR、NOR和NH3/NH+4与能见度的变化都存在较好的对应关系,说明广州地区低能见度与二次离子(SO2-4、NO-3、NH+4)的生成有关.     

表面活性剂对以污泥为铝源制得的纳米Al（OH）3性质的影响研究

以污泥碳(SC)中回收的铝酸钠为铝源,在制备Al(OH)3的过程中加入表面活性剂PEG-1000(比例在0.01%~0.6%变化),考察其对Al(OH)3表面形貌和结构的影响.研究发现,当加入PEG-1000比例较小时,其空间位阻作用抑制了粒子之间的键合作用,使得Al(OH)3的沉淀效率较高、粒子尺寸较小,也能有效地阻止颗粒的团聚,SBET可以达到340 m2·g-1以上.当PEG-1000加入比例较大时,Al3+的沉淀效率逐渐降低,所得Al(OH)3粒子的尺寸变大,Al(OH)3的SBET和孔体积逐渐变小,平均孔径变大;原因是增多的PEG-1000分子会被包进Al(OH)3的结构中,限制了PEG-1000的表面交联和吸附,使空间位阻效应变差.—CH2—振动峰的出现说明PEG-1000是通过形成化学键的方式连接在Al(OH)3的表面基团上.PEG-1000的使用对于以污泥为铝源制备分散性好、尺寸较小和SBET较大的非晶态Al(OH)3具有重要作用.     

碳纳米管负载纳米四氧化三铁多相类芬顿降解亚甲基蓝

在课题组前期研究的基础上,以碳纳米管(MWCNTs)为载体制备了Fe3O4/MWCNTs复合物并作为催化剂,以染料亚甲基蓝(MB)为降解对象,研究了该催化剂催化H2O2对亚甲基蓝溶液的降解特性及其影响因素,并考察了催化剂的重复使用效果,探讨了催化反应的机理.结果表明,在pH值3~8的范围内,催化反应体系都能有效降解MB,最佳pH值为3.5.随着催化剂投量的增加,MB的降解率明显提高,500 mg·L-1催化剂投量条件下,MB的降解率最高.随着H2O2初始浓度的增加,MB的降解率增加,10 mmol·L-1时MB的降解率最高.溶液中共存的阴离子会降低MB的降解率.在最佳条件,即温度25℃、H2O2浓度10 mmol·L-1、催化剂浓度500 mg·L-1的条件下,0.20 mmol·L-1MB在30 min内的降解率达到99.1%.催化剂重复使用后仍然具有较好的催化活性,说明Fe3O4在MWCNTs表面负载比较牢固,催化剂具有反复使用的能力.催化反应机理是催化剂催化H2O2产生羟基自由基,高活性的羟基自由基氧化MB.     

Photoassisted Fenton degradation of phthalocyanine dyes from wastewater of printing industry using Fe(Ⅱ)/γ-Al2O3 catalyst in up-flow fluidized-bed

Fe(II)/γ-Al2O3 powders synthesized using the dipping method were produced from a mixed aqueous solution containing aluminium oxide(γ-Al2O3) and iron(II)-precursor(FeSO4), and used for photoFenton degradation of phthalocyanine dyes(PCS) under ultraviolet(UV) irradiation in an up-flow fluidized bed. The catalysts were characterized by XRD, ESCA, BET, EDS and SEM. The results showed that Fe2+ion was compounded on the γ-Al2O3 carrier. The effects of different reaction parameters such as catalyst activity, dosage and solution pH on the decolorization of PCS were assessed. Results indicated that maximum decolorization(more than 95%) of PCS occurred with20 wt% Fe(II)/γ-Al2O3 catalyst(dosage of 60 g/L) using a combination of UV irradiation and heterogeneous Fenton system. The degradation efficiency of PCSincreases as pH decreases, exhibiting a maximum efficiency at pH 3.5. The recycled catalyst was capable of repeating three runs without a significant decrease in treatment efficiency, and this demonstrated the stability and reusability of catalyst.     

三维花状结构α-FeOOH协同H2O2可见光催化降解双氯芬酸钠

采用油浴回流法,在常压回流反应条件下批量制备出三维花状结构的α-Fe OOH纳米材料,并利用XRD、FT-IR和SEM等仪器对其进行分析表征;以双氯芬酸钠为目标污染物,考察三维花状结构α-Fe OOH纳米材料,在模拟太阳光照射下,催化H2O2降解有机污染物的性能.结果表明,三维花状结构α-Fe OOH由纳米棒自组装形成,纳米棒的长度约400~500 nm,直径约40~60 nm.以模拟可见光为光源,三维花状结构α-Fe OOH与H2O2构成光助异相类Fenton体系,对双氯芬酸钠有良好的光催化降解效果,在90 min内对初始浓度为30 mg·L-1的双氯芬酸钠降解去除率达到99%以上,催化降解反应以羟基自由基氧化反应为主.     

Modelling photochemical oxidant formation, transport, deposition and exposure of terrestrial ecosystems

The chemical processes responsible for production of photochemical oxidants within the troposphere have been the subject of laboratory and field study throughout the last three decades. During the same period, models to simulate the atmospheric chemistry, transport and deposition of ozone (O(3)) from individual urban sources and from regions have been developed. The models differ greatly in the complexity of chemical schemes, in the underlying meteorology and in spatial and temporal resolution. Input information from land use, spatial and temporally disaggregated emission inventories and meteorology have all improved considerably in recent years and are not fully implemented in current models. The development of control strategies in both North America and Europe to close the gaps between current exceedances of environmental limits, guide values, critical levels or loads and full compliance with these limits provides the focus for policy makers and the support agencies for the research. The models represent the only method of testing a range of control options in advance of implementation. This paper describes currently applied models of photochemical oxidant production and transport at global and regional scales and their ability to simulate individual episodes as well as photochemical oxidant climatology. The success of current models in quantifying the exposure of terrestrial surfaces and the population to potentially damaging O(3) concentrations (and dose) is examined. The analysis shows the degree to which the underlying processes and their application within the models limit the quality of the model products.     

低强度超声波强化污水生物处理中超声辐照污泥比例的优化选择

通过超声波的SBR反应器与对照反应器处理人工配制生活污水的对比试验,研究了利用低强度超声波强化污水生物处理的另一个重要工艺参数———超声处理污泥比例(即超声处理污泥量占反应器内总污泥量的百分比).设置超声波反应器采用频率35kHz、声强0.3W/cm²超声波每隔8h取反应器中一定比例的活性污泥辐照10min后再返回反应器.结果表明,超声处理污泥比例为10%时,其COD和NH₃-N去除率可分别提高5%和0.5%左右,以好氧呼吸速率(Oxygen Uptake Rate,OUR)表示的污泥活性可提高12%以上.通过对污泥增长率的研究表明,当超声污泥比例为10%,超声波反应器内污泥的增长率比对照反应器降低了11%左右,减轻了后续污泥处理工序的负荷.随着超声处理污泥比例的增加,污泥体积指数SVI持续增大,但是超声污泥比例不超过10%对污泥沉降性能影响不大.因此,在超声强化污水生物处理工艺中,可采用强度0.3W/cm²超声波每隔8h取反应器中的10%的活性污泥辐照10min后再返回反应器,来提高反应器的生物处理效率.     

河套灌区春小麦-萝卜复种模式下土壤NO3--N动态

研究了河套灌区春小麦-萝卜复种模式下,土壤、土壤溶液和地下水NO₃^--N浓度的动态变化.结果表明:随着试验时间的延长,土壤表层NO₃^--N含量降低,深层(100～150cm)增加;土壤溶液中、下层NO₃^--N浓度(70、120cm)显著高于上层(30cm),尤其是在萝卜生长季.当前的灌溉条件下,不同年度、不同生长季土壤NO₃^--N淋失量的多少与土壤水分的下渗量密切相关,且输入的氮素中有30%以上以NO₃^--N的形式淋失掉.施肥区地下水NO₃^--N浓度显著高于未施肥区,且65.5%的水样超过WHO规定的上限(11.3mg/L).总之,经过连续2a的春小麦与萝卜复种可使表层土壤NO₃^--N含量明显降低,但由于中、下层土壤剖面中残留大量的NO₃^--N,因此在当前灌溉措施下,短期内NO₃^--N淋失是不可避免的.     

Effects of elevated pO3 on carbon cycle between above and belowground organs of trees

Translocation of carbohydrate from leaves to roots via phloem and reallocation from roots to leaves via xylem regulate the allocation of carbon （C） between above and belowground organs of trees. To quantitatively analyze effects of elevated ozone concentrations pO3 on the internal cycle of C, juvenile beech and spruce were grown in phytotrons and exposed to ambient and elevated pO3 （i.e. twice-ambient O3 levels, restricted to 〈 150 ppb） for two growing seasons. The translocation of C in the phloem and xylem was quantitatively studied by investigating the phloem/xylem-loading of sugars, the differentiation of stem conductive tissue and the hourly water flow through the stem. Results in the present study shown, elevated pO3 significantly decreased C translocation from shoot to roots in beech by reducing both sugar concentration in the phloem and conductive phloem area. Elevated pO3 also significantly decreased C reallocation from the roots to the shoot in beech by reducing both of sugar concentration in the xylem and transpiration rate. The adverse effects of elevated pO3 on C translocation in the phloem and xylem, however, were small in spruce. Contrasting to beech, spruce is less sensitive to elevated pO3, regarding to phloem differentiation and sugar concentrations in the phloem and xylem.