流化床O2/CO2气氛下添加SiO2对燃煤PM2.5的控制

采用小型流化床研究了在O2/CO2气氛下添加SiO2对PM2.5(空气动力学直径小于2.5 μm的颗粒物)的控制,试验在1123 K、O2/CO2气氛下进行,并采用荷电低压撞击器(ELPI)采集和分析燃烧后的PM2.5.结果表明,添加SiO2是燃烧过程中影响PM2.5生成的重要因素.添加SiO2后,生成PM1的质量浓度均降低,而PM1-2.5的质量浓度均略有增加;PM2.5质量粒径分布均呈双峰分布,峰值分别出现在0.2 μm和2.0μm左右.随着SiO2添加量的增加,PM2.5中的S、K、Na、Cu和Pb元素的含量呈减少的趋势;随着颗粒粒径减小,S、K、Na、Cu和Pb元素的含量有增高的趋势.     

酱糟与醋糟混合发酵产沼气研究

酱糟、醋糟是我国食品酿造行业产生的废弃物,通过厌氧发酵不仅可以解决废糟处理问题又可获取能源.因此本研究在中温(35±1)℃的条件下,根据C/N比的不同,进行了酱糟/醋糟干物质(TS)比分别为1∶0(N1)、1∶1.5(N2)、1∶3(N3)、1∶7(N4)、1∶18(N5)和0∶1(N6)的混合发酵实验.结果表明,单一酱渣的延滞期为17.46 d,混合发酵明显缩短了延滞期,为3.00-3.83 d;混合发酵组(N2～N5)累计产甲烷量的实验结果比计算结果分别提高了1％、16％、14％和10％,其中,N3组C/N比为25.7∶1,提高最为明显;各组发酵产生的沼气的甲烷体积分数在65％～ 70％之间;Gompertz模型拟合可以用于酱糟和醋糟混合发酵产甲烷的过程;酱、醋糟发酵的产酸类型以乙酸型发酵为主.     

流化床焚烧含盐苯胺废液的NOx排放特性

在流化床焚烧实验装置上进行含盐苯胺(C6H5NH2)废液的焚烧实验研究,用IMR-IMR2800P废气分析仪对焚烧尾气成分进行了在线监测,考察了焚烧工艺条件对NOx排放浓度的影响规律.结果显示:采用分级燃烧工艺和提高焚烧温度,可以降低NOx浓度;增大进料速率却导致NOx排放浓度的增加.当过剩空气系数(α)低于1.0时,NOx排放浓度随着α的增大急剧上升;大于1.1时,NOx排放浓度随α增加而减小.苯胺废液高温焚烧时添加氯化钠能降低NOx排放.     

高岭土负载纳米Fe/Ni同时去除水中Cu2+和NO3-

工业废水常含有不同污染物如重金属离子和无机阴离子,而如何有效去除复合污染物就成为环境科学前沿研究的挑战性课题.这些污染物因化学性质不同而导致去除机理和途径也不同.本文采用合成高岭土负载纳米双金属Fe/Ni(K-Fe/Ni)同步去除水中Cu2+和NO-3.结果表明K-Fe/Ni能有效去除水中Cu2+和NO-3,但它们的去除效果却会相互受到影响.在Cu2+浓度为200mg·L-1时,NO-3的去除率达到42.5%;而未加入Cu2+时,NO-3的去除率仅有26.9%,说明Cu2+的存在提高了NO-3降解效率.同样,水中NO-3的存在也影响Cu2+的去除(Cu2+去除率从99.7%降到96.5%).但NO-3浓度对去除Cu2+的影响小于Cu2+浓度对NO-3的影响.通过BET比表面积、X射线衍射(XRD)、扫描电镜(SEM)、X射线能量散射(EDS)和X射线光电分析(XPS)对K-Fe/Ni表征的结果显示,反应后K-Fe/Ni的表面存在铁的氧化物、Ni0和被还原的Cu0.基于以上结果,我们发现K-Fe/Ni同步去除水中Cu2+和NO-3的机理是:高岭土负载下的纳米Fe0作为还原剂,在Ni0的催化产氢作用下将Cu2+还原成Cu0并沉积在K-Fe/Ni上而形成纳米Fe/Ni/Cu三金属催化剂,从而加速催化水中NO-3降解.     

滇池水葫芦规模化控养生态环境效应分析

水葫芦规模化控养是"十二五"期间滇池治理的重要措施之一。首先介绍了滇池水葫芦规模化控养现状,比较了滇池草海和外海在水葫芦控养前后水质的变化情况,指出滇池水葫芦规模化控养对草海水体生态恢复效果显著,可以在滇池选择适宜水葫芦生长的水域继续扩大水葫芦控养面积,使水葫芦在滇池生态治理中发挥更大的作用。     

Interface-mediated synthesis of monodisperse ZnS nanoparticles with sulfate-reducing bacterium culture

We have created a new method of ZnS nanospheres synthesis. By interface-mediated precipitation method (IMPM), monodisperse ZnS nanoparticles was synthesized on the particle surface of sulfate-reducing bacterium nutritious agar culture. Sulfate-reducing bacterium (SRB) was used as a sulfide producer because of its dissimilatory sulfate reduction capability, meanwhile produced a variety of amino acids acting as templates for nanomaterials synthesis. Then zinc acetate was dispersed into nutritious agar plate. Subsequently agar plate was broken into particles bearing much external surface, which successfully mediated the synthesis of monodisperse ZnS nanoparticles. The morphology of monodisperse ZnS nanospheres and SRB were examined by scanning electron microscopy (SEM), and the microstructure was investigated by X-ray diffraction (XRD). The thermostability of ZnS nanoparticles was determined by thermo gravimetric-differential thermo gravimetric (TG-DTG). The maximum absorption wavelengh was analysed with an ultraviolet-visible spectrophotometer within a range of 199–700 nm. As a result, monodisperse ZnS nanoparticles were successfully synthesized, with an average diameter of 80 nm. Maximum absorption wavelengh was 228 nm, and heat decomposed temperature of monodisperse ZnS nanoparticles was 596°C.     

Numerical simulation of alga growth and control in Dalian Bay

WAHMO model was used to simulate the distribution of pollutants in Dalian Bay, China as to predict well as the growth and control of alga. The observed and predicted values of main pollutants showed a good trend at all study locations and the different between them can be ignored. Simulation results illustrated that phosphate was one of limited factors to control algal growth at the location near the sewage outfall, meanwhile, away from the sewage outfall, the synergy of ammonium nitrogen and phosphate was the limited factor.     

Interface-mediated synthesis of monodisperse ZnS nanoparticles with sulfate-reducing bacterium culture

We have created a new method of ZnS nanospheres synthesis. By interface-mediated precipitation method (IMPM), monodisperse ZnS nanoparticles was synthesized on the particle surface of sulfate-reducing bacterium nutritious agar culture. Sulfate-reducing bacterium (SRB) was used as a sulfide producer because of its dissimilatory sulfate reduction capability, meanwhile produced a variety of amino acids acting as templates for nanomaterials synthesis. Then zinc acetate was dispersed into nutritious agar plate. Subsequently agar plate was broken into particles bearing much external surface, which successfully mediated the synthesis of monodisperse ZnS nanoparticles. The morphology of monodisperse ZnS nanospheres and SRB were examined by scanning electron microscopy (SEM), and the microstructure was investigated by X-ray diffraction (XRD). The thermostability of ZnS nanoparticles was determined by thermo gravimetric-differential thermo gravimetric (TG-DTG). The maximum absorption wavelengh was analysed with an ultravioletvisible spectrophotometer within a range of 199-700 nm. As a result, monodisperse ZnS nanoparticles were successfully synthesized, with an average diameter of 80 nm. Maximum absorption wavelengh was 228 nm, and heat decomposed temperature of monodisperse ZnS nanoparticles was 596℃.     

日本沼虾与秀丽白虾的营养生态位

为科学评估虾类的营养关系及资源的保护,利用稳定同位素技术研究了2种淡水虾类在大型通江湖泊——洞庭湖和鄱阳湖中的营养生态位和生态宽幅大小.结果表明,日本沼虾与秀丽白虾的δ13C值呈显著差异,而δ15N值无明显差异.同时,由于营养状况及水文的差异,虾类同位素值的差异在2个湖泊中表现不同.日本沼虾的δ13C值范围比秀丽白虾大,频率分布相对集中在-25.0‰～-23.0‰区间,表明其摄食的食物来源更广,对某些饵料生物有所偏好.另外,日本沼虾与秀丽白虾的营养生态位重叠程度较大,表明二者的主要食物来源相同,在食物网中占据的营养级相近,存在着激烈的种间竞争.在鄱阳湖中,日本沼虾占有的营养生态位和生态宽幅大于秀丽白虾;而在洞庭湖的研究结果则相反,主要是由于采样区域生境的差异及人类活动干扰的程度不同所致.     

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.