Shellac-coated iron oxide nanoparticles for removal of cadmium(II) ions from aqueous solution

This study describes a new effective adsorbent for cadmium removal from aqueous solution synthesized by coating a shellac layer, a natural biodegradable and renewable resin with abundant hydroxyl and carboxylic groups, on the surface of iron oxide magnetic nanoparticles. Transmission Electron Microscopy (TEM) imaging showed shellac-coated magnetic nanoparticle (SCMN) adsorbents had a core-shell structure with a core of 20 nm and shell of 5 nm. Fourier Transform Infrared Spectroscopic analysis suggested the occurrence of reaction between carboxyl groups on the SCMN adsorbent surface and cadmium ions in aqueous solution. Kinetic data were well described by pseudo second-order model and adsorption isotherms were fitted with both Langmuir and Freundlich models with maximum adsorption capacity of 18.80 mg/g. SCMN adsorbents provided a favorable adsorption capacity under high salinity conditions, and cadmium could easily be desorbed using mild organic acid solutions at low concentration.     

磁性纳米铁对厌氧颗粒污泥特性及其微生物群落的影响

考察了磁性纳米铁(Fe3O4NPs)对厌氧颗粒污泥溶解性微生物产物(SMP)、疏松胞外聚合物(LB-EPS)、紧密胞外聚合物(TB-EPS)的影响,同时利用高通量测序技术对厌氧颗粒污泥内微生物群落结构的变化进行了分析.结果表明,在长期接触实验过程中,投加Fe3O4NPs的反应器对COD去除率为83.6%,与对照组相比降低了5.7%.对照组与实验组中厌氧颗粒污泥TB-EPS含量(以VSS计)分别为178.20 mg·g-1和138.24 mg·g-1,而SMP含量分别为34.88 mg·L-1和27.44 mg·L-1;同时投加Fe3O4NPs后,在LB-EPS三维荧光(EEM)光谱中,紫外光区类腐殖酸荧光峰消失,辅酶F420荧光峰强度有所降低.在长期接触实验后,甲烷杆菌属(Methanobacterium)所占比例从76.15%增至86.76%,而甲烷丝菌属(Methanothrix)所占比例从17.1%降至7.51%,Methanothrix对于Fe3O4NPs更为敏感;总细菌群落变化明显,其中变形菌门(Proteobacteria)所占比例从66.44%降至47.16%,放线菌门(Actinobacteria)所占比例从8.97%增至17.33%,拟杆菌门(Bacteroidetes)所占比例从8.07%增至17.74%,厚壁菌门和拟杆菌门比例的增加对有机物的厌氧水解过程发挥积极的作用.     

Fe3O4@SiO2-Chitosan的制备及其对水中Cu2+的吸附效能研究

以SiO_2包覆Fe_3O_4,戊二醛为交联剂,交联壳聚糖(Chitosan, CTS),制得Fe_3O_4@SiO_2-Chitosan复合磁性纳米粒子.以Fe_3O_4和Fe_3O_4@SiO_2为对照,采用X射线衍射、透射电镜和傅立叶红外光谱对其进行表征分析,并测定了投加量、pH值、吸附时间和温度等因素对Cu~(2+)吸附效果的影响,从动力学、热力学以及再生回用性能评价等方面对其吸附性能进行了探究.结果表明Fe_3O_4@SiO_2-Chitosan对Cu~(2+)的吸附过程符合准二级吸附动力学模型和Langmuir模型,为自发、放热、优惠型的单分子层化学吸附.在pH为6.0, 298 K下达到最大吸附量154.8 mg·g~(-1),吸附解吸4次后吸附容量变化不大,说明Fe_3O_4@SiO_2-Chitosan具有较高的吸附容量,可作为处理含铜废水和回收铜的高效吸附剂.     

BiOCl/SiO2/Fe3O4复合材料可见光催化去除水中亚甲基蓝

以FeCl_3·6H_2O、FeCl_2·4H_2O、(C_2H_5)_4SiO_4、Bi(NO_3)_3·5H_2O、KCl为主要原料,采用化学共沉淀法和水热法制备了BiOCl/SiO_2/Fe_3O_4光催化剂,并对其进行EDS、TEM、XRD、FT-IR、UV-Vis表征,最后通过亚甲基蓝降解实验,研究了催化剂在合成过程中pH及催化剂投加量对其光催化性能的影响.结果表明,在pH=6、催化剂初始投加量为0.5 g·L~(-1)时,对亚甲基蓝的可见光催化效果最佳,光照120 min后对10 mg·L~(-1)的亚甲基蓝溶液的脱色率达到93.2%.BiOCl/SiO_2/Fe_3O_4经过简单的无水乙醇和水洗后,可高效重复利用4次.综合表明,BiOCl/SiO_2/Fe_3O_4是一种在处理染料废水中具有应用前景的磁性光催化剂.     

埕岛油田海底管道漏磁检测与安全评估

提出了埕岛油田海底管道内缺陷漏磁检测需解决的主要问题,研发了325 mm管道内缺陷漏磁检测装置,确定了海底管道漏磁检测工艺流程,配套了管道检测发射装置、接受装置等相关设施,实现了海底管道的漏磁检测、缺陷分析和安全评估。     

Fly ash content and distribution in lake sediments around a large power station: inferences from magnetic susceptibility analysis

The bulk magnetic susceptibility of sediments from artificial and natural lakes around a large coal-fired power station in NE Spain has been measured. Higher magnetic susceptibility values are found in lake sediments located SE of the power station. This distribution of susceptibility values is compatible with environmental and meterological studies of emissions from the power station, which indicate a dominant SE plume direction. Mineralogical studies, by means of X-ray diffraction and scanning electron microscopy, show that the highest susceptibility values found in the sediments are caused by magnetic iron spinels in the fly ash that is transferred to the environment by the power station particulate emissions. After the quantitative mineralogical studies of fly ash, two different methods of fly ash content determination in the sediments have been devised, showing very similar results. The low background magnetic susceptibility of the sediments in the study area and the high susceptibility resulting from the input of magnetic fly ash particles allows both delimitation of the polluted area around the power station, and quantification of the fly ash input into the natural sediments.     

台湾泥岩地区不同刺竹林景观下之土壤与植被变异

台湾西南部泥岩恶地,由于其特殊之土壤,地力流失消耗与区域微气候型态之间的因果循环,在水土保持与景观上形成不易植生绿化的地区及特殊之世界地形。泥岩地区之不同刺林林相之土壤,其林相皆伐后复层植被区土壤性质变异高于其它位置,而其它区之土壤理化性质在时间及空间上之变异不大,可明显区分林相不同之显著差异。不同林相对泥岩地浅层土壤(0~20cm)理化性质的差异,以植物营养元素与植生覆盖因子可充分说明(约占变异范围之62%)。泥岩试区区中移动性物质(交换性钙、钠与镁)明显较少出现在复层林相处区,而易出现于淋洗、冲蚀量较大之刺林相保留区与隔丛择伐区。长效性植物营养元素因子(pH值与有效性磷),因长时间之林相不同,使其较明显趋于复层林相区堆积,并影响地表植生之种类、分布与覆盖情形。0～20cm土壤性质的分布和离子间的移动特性有关,移动性高的钠、镁离子会在冲蚀量高之区域出现,20～40cm土壤性质的分布则和土壤中之母质与植生有关并与因素分析结果相似,其次为可移动性离子的影响,且应用地理统计印证土壤性质在空间之变化,其分布确实与不同林相位置有关,即植生营养元素(pH值、有效性磷)大都朝向复层植被区之趋势。典型相关分析结果,地表覆盖度与入侵植物数量两变量主要系透过第一个典型因素与第二个典型因素而影响到复层植被区之pH值、有机质等土壤理化性质。