碱激发粉煤灰对Cs~+的吸附行为

将粉煤灰进行碱激发改性,运用XRD和SEM技术对碱激发粉煤灰进行了表征,通过静态平衡吸附实验研究了碱激发粉煤灰对Cs+的吸附动力学和热力学特性,并对吸附前后的碱激发粉煤灰进行了FTIR分析。表征结果显示,碱激发处理后,粉煤灰的晶相发生了改变,且粉煤灰表面密实的硬壳层被破坏。实验结果表明:在初始Cs+质量浓度为200 mg/L、吸附温度为25℃、溶液pH为10、碱激发粉煤灰投加量为12.0 g/L的条件下,碱激发粉煤灰对Cs+的平衡吸附率可达80%以上,其吸附能力比碱激发前提高了3倍以上;吸附过程可用准二阶动力学方程来描述,并较好地符合Langmuir等温吸附模型;碱激发粉煤灰对Cs+的吸附是吸热过程,且能自发进行;该过程以物理吸附为主,并伴随化学吸附。     

碱熔融活化固硫灰制备地聚合物

采用碱熔融活化法,由固硫灰制备地聚合物。在前期开展的单因素实验的基础上,采用正交实验,考察了NaOH和固硫灰的质量比、煅烧温度、煅烧时间3个因素对固硫灰基地聚合物的抗压强度的影响。采用XRD,SEM,IR等手段分析固硫灰碱熔融活化前后的物相、微观形貌以及硅铝化学键的变化。实验结果表明,以在NaOH与固硫灰的质量比为0.60、煅烧温度为550 ℃、煅烧时间为60 min的条件下制备的碱熔融固硫灰为原料,制备的固硫灰基地聚合物的抗压强度为38.00 MPa。表征结果显示：通过碱熔融活化固硫灰制备的地聚合物的XRD谱图中出现了地聚合物的特征衍射峰;碱熔融固硫灰的结构松散,在颗粒表面及内部存在大量孔隙;经碱熔融处理后固硫灰的硅酸盐和铝酸盐发生了解聚。     

岷江上游山区聚落生态位地理特征与驱动因子间关系研究

山区聚落生态位反映聚落在山地垂直方向上所处的空间位置及人类生活所能利用的资源空间,是当地居民长期适应山地自然环境的结果。基于岷江上游各民族山区聚落生态位和气象、社会、地形驱动因子的空间分布,借助冗余分析,构建山区聚落生态位地理特征与驱动因子间的多水平贝叶斯模型,定量刻画聚落生态位的民族属性对山区聚落生态位地理特征与驱动因子间关系的影响。结果表明:(1)影响研究区域内1 667个与各民族聚落生态位地理特征的驱动因子有显著差异,海拔和坡度对前者影响较大,海拔、坡度、干季和湿季湿度、距河流距离对后者影响较大,且海拔对两者的影响程度都最大,海拔和坡度地形驱动因子与干、湿季湿度和距河流距离间的相关性较弱。(2)干、湿季湿度气象驱动因子对藏-羌聚落生态位地理特征影响较大,距河流距离和距县城距离社会驱动因子、海拔和坡度地形驱动因子对藏族聚落生态位地理特征影响较大,这与藏族聚落生态位的分布面积和个数有关。(3)民族类型对聚落生态位地理特征指标与气象因子干季湿度间关系的影响最大,对聚落生态位地理特征指标与地形因子坡度间关系的影响最小。岷江上游山区聚落生态位地理特征与驱动因子间关系的研究,为量化山区聚落生态位与山地环境的关系提供了有效的数据支撑。     

二氧化钛颗粒制备及其对水中三价砷的去除

以硫酸氧钛和聚乙烯醇(PVA)为原料,通过冰水浴法制备了二氧化钛(TiO2)颗粒,并研究了其对砷的吸附性能。利用X射线衍射仪(XRD)和扫描电子显微镜(SEM)对TiO2颗粒进行了表征,结果表明,吸附剂为锐钛矿结构,比表面积246 m2/g。TiO2颗粒对模拟地下水中砷(Ⅲ)的吸附动力学研究表明,吸附过程符合准二级动力学。采用Langmuir和Freundlich方程对吸附平衡数据进行了拟合,结果表明,吸附等温线符合Langmuir模型,最大吸附量为22.3 mg/g。TiO2颗粒对三价砷的吸附在pH为9.1时吸附量最大,吸附受CO23-影响较大。将110 g TiO2颗粒装备成过滤滤壶,对山西地下水(总砷含量190μg/L)进行了除砷实验,经过3 600柱体积后,滤液中砷浓度低于10μg/L,符合国家饮用水标准。     

添加牛粪对蚯蚓处理污泥的影响

采用4个相同的塑料装置,将等量的污泥、EM菌、蚯蚓及不同量的牛粪装入其中并混匀后,通过60 d的培养实验,借助对污泥含水率、pH、TP、TOC和TN的监测及蚯蚓生存状况的考察,探究添加牛粪对蚯蚓处理污泥的影响。结果表明:添加牛粪可以抑制污泥含水率的增加,但不同牛粪添加量对污泥含水率的影响无一定规律性;与初始TP相比,1#~4#中污泥TP增长率分别为81%、97%、56%和102%,除3#外,污泥TP增幅随牛粪添加量的增加而增大;因生物作用,1#~4#污泥TOC均呈下降趋势,1#~4#中污泥TOC分别下降了13.6%、22.4%、21.7%和16.1%;1#~4#污泥TN变化与牛粪添加量的变化之间无明显规律。污泥中添加牛粪,对蚯蚓健康有益。     

Radiative transfer budgets for scattering and absorbing plumes: Measurements and model predictions

The 1981 VISTTA field study characterized the composition and appearance of particle-rich plumes from three different sources. This paper compares the VISTTA observations with the predictions of two plume visibility models. Observations and predictions are analyzed from the perspective of exact solutions to the equations of radiative transfer for a somewhat idealized atmosphere. These solutions, which explicity relate plume/sky contrast to the composition of plume and background and the geometry of sun, plume and observer, are shown to be consistent with the VISTA observations. The simplified relationships are used as the basis for budgeting radiative transfer by the plume and background, and for analyses of the sensitivity of plume appearance to individual variables.The optics predictions of the two models are less accurate for plumes dominated by particle scattering than they are for plumes dominated by NO₂ absorption. Inaccurate prediction of plume particle size distributions can be identified as an important source of error. Inaccurate prediction of background sky radiance is suspected as another.     

美洲商陆（Phytolacca Americana L.）对铀的富集特征及根际微生物群落功能多样性的响应

在模拟低(25 mg·kg-1)、中(50 mg·kg-1)、高(100 mg·kg-1)剂量铀污染的条件下,采用盆栽试验,研究了美洲商陆富集铀的特点及铀污染对根际微生物群落的影响.结果表明,铀污染对美洲商陆生长的影响可能存在一个阈值,该阈值介于25~50 mg·kg-1之间,低于该阈值时,铀污染能够促进美洲商陆的生长,反之,则会抑制美洲商陆的生长.美洲商陆成熟时,根、茎和叶的最大铀富集量分别为131.69、9.87和45.33μg,是一种较为理想的修复铀尾矿的植物.Biolog-Eco测试结果表明,土壤中铀会对美洲商陆根际微生物群落产生负效应,铀胁迫可使根际微生物代谢迟缓,对碳源的选择发生转移,对糖类、羧酸类和胺类碳源的利用显著减少,对酚酸类碳源的利用显著增加;同时,铀胁迫可导致根际微生物群落功能多样性指数、均匀度指数及优势微生物种类降低.最后,利用培养96 h的平均吸光值进行聚类和主成分分析.结果表明,铀胁迫下美洲商陆根际微生物群落异于对照,美洲商陆根际微生物对铀胁迫的适应是以降低对糖类、羧酸类和胺类等碳源的利用为代价的.     

微波法水处理技术研究进展

简单介绍了微波加热的原理,对微波法水处理技术的研究现状进行了综述,指出了微波法水处理技术的研究方向.     

Microbial diversity accumulates in a downstream direction in the Three Gorges Reservoir

Organic and inorganic materials migrate downstream and have important roles in regulating environmental health in the river networks. However, it remains unclear whether and how a mixture of materials (i.e., microbial species) from various upstream habitats contribute to microbial community coalescence upstream of a dam. Here we track the spatial variation in microbial abundance and diversity in the Three Gorges Reservoir based on quantitative PCR and 16S rRNA gene high-throughput sequencing data. We further quantitatively assess the relative contributions of microbial species from mainstem, its tributaries, and the surrounding riverbank soils to the area immediately upstream of the Three Gorges Dam (TGD). We found an increase of microbial diversity and the convergent microbial distribution pattern in areas immediately upstream of TGD, suggesting this area become a new confluence for microbial diversity immigrating from upstream. Indeed, the number of shared species increased from upstream to TGD but unique species decreased, indicating immigration of various sources of microbial species overwhelms local environmental conditions in structuring microbial community close to TGD. By quantifying the sources of microbial species close to TGD, we found little contribution from soils as compared to tributaries, especially for sites closer to TGD, suggesting tributary microbes have greater influence on microbial diversity and environmental health in the Three Gorges Reservoir. Collectively, our results suggest that tracking microbial geographic origin and evaluating accumulating effects of microbial diversity shed light on the ecological processes in microbial communities and provide information for regulating aquatic ecological health.     

土壤性质对水稻土中外源镉与铅生物有效性的影响

为定量了解土壤理化性质对进入土壤中的外源镉和铅生物有效性的影响,采集了性质相差较大的16个水稻土,通过添加Cd(或Pb)培养和老化处理(Cd的加入量为0、0.2、0.5、1、2和5 mg·kg-1;Pb加入量为0、20、50、100、200和500 mg·kg-1,培养时间为1年),研究了不同土壤中Cd(或Pb)负荷与土壤中水溶态和交换态Cd(或Pb)的关系.结果表明,随着Cd(或Pb)污染水平的提高,土壤中水溶态和交换态Cd(或Pb)均显著增加,但不同土壤中水溶态和交换态Cd(或Pb)随土壤Cd(或Pb)积累的增加幅度有很大的差异.相关分析表明,水稻土中水溶性Cd(或Pb)主要与土壤Cd(或Pb)污染水平和pH值有关;而交换态Cd(或Pb)主要与土壤Cd(或Pb)污染水平、pH值、CEC及质地等有关.数据显示,pH值较高、质地较黏的土壤可大大减缓因污染引起的CA和Pb生物有效性的提高.