化工企业储运系统恒功率电伴热带的应用及风险控制

通过不同类型电伴热带的特性比较,分析化工储运的生产特点和对电伴热适应性要求,找出储运系统电伴热应用过程存在的主要风险因素,从风险控制的角度提出恒功率电伴热带的方案设计、安装、运行管理、故障排除、应急管理5个方面的优化措施,以提高恒功率电伴热系统的安全性、稳定性。     

抑食金球藻对翡翠贻贝生长及摄食的影响研究

在室内以翡翠贻贝（Perna viridis）为对象,研究单种抑食金球藻（Aureocuccos anophagefferens）及其与亚心形四爿藻（Tetraselmis subcordiformis）混合藻液条件下抑食金球藻对贻贝的生长和摄食的影响。结果表明,抑食金球藻对翡翠贻贝的生长和摄食均有显著的负面影响。单种高、中浓度抑食金球藻组贻贝的鲜重、干重及无灰分干重均显著低于混合藻组,贻贝的个体生长条件指数（CI）下降明显,其下降率甚至高于饥饿组。混合藻组中贻贝的CI、软组织的鲜重、干重、无灰分干重等均显著低于对照组,其抑制程度与混合藻组中抑食金球藻浓度有关,当混合藻组中抑食金球藻浓度较大时（≥ 4×105 cells/mL）,贻贝的上述指标更低。四组混合藻中贻贝的摄食率也均显著低于对照组,抑食金球藻对贻贝的抑食作用也与其藻细胞密度有关,混有较高密度抑食金球藻组中贻贝的摄食率更低,说明抑食金球藻并非因其个体太小而不能被贝类正常摄食,可能产生了某种生物活性物质抑制了贻贝的摄食和生长,亚心形四爿藻能在一定程度上可以缓解抑食金球藻对贝类摄食和生长的抑制作用。     

Flexible options to provide energy for capturing carbon dioxide in coal-fired power plants under the Clean Development Mechanism

Mitigation and Adaptation Strategies for Global Change - Operators of coal-fired power plants with carbon dioxide capture and storage (CCS) can provide energy for carbon dioxide (CO2) capture by...     

南京市校园室内空气微生物特征

为调查南京市学校教室内空气微生物污染状况,本研究各选一所幼儿园、小学、初中和大学,每所学校分别随机选取10间教室,采用六级安德森采样器进行空气微生物采样.研究发现,在南京地区所调研的这4所不同类型的学校中,幼儿园室内空气微生物浓度最高,细菌和真菌浓度均值分别为605CFU/m³和648CFU/m³,均显著高于其余3所学校.室内细菌和真菌粒径分布趋同,峰值均出现在Ⅴ级（1.1~2.1μm）.仅在大学教室内,发现环境参数与空气微生物浓度存在显著相关性.幼儿园教室内学生每天吸入的细菌和真菌剂量分别为150.2CFU/kg和160.9CFU/kg,均显著高于其他学校学生.     

污泥含碳有机官能团分布及其模型化合物构建

污泥有机结构体系中碳属于活泼元素,化学活性较强,能源转化处理过程时易发生热化学反应,对污泥能源转化产物的化学特征及生成规律有重大影响.本研究采用傅里叶变换红外光谱（FTIR）和X射线光电子能谱（XPS）开展了污泥含碳官能团分布特征分析,污泥中的主要含碳官能团为烯基（C-C）、苯环（π-π^*）、醚（C-O-C）、羧基（-COOH）.基于污泥中主要含碳官能团分布和污水中常见有机物组成,构建了污泥典型含碳官能团模型化合物：间二甲苯（π-π^*）,四氢呋喃（C-O-C）,乙酸（-COOH）和环戊烯（C=C）.此外采用热解仪与气相色谱/质谱联用技术（Py-GC/MS）对比分析了不同温度下污泥与含碳模型化合物的热解规律,验证了所构建的含碳模型化合物基本合理可靠.     

稻壳基活性炭催化剂的低温NH3-SCR抗硫性能

以稻壳基活性炭（DAC）为载体,利用等体积浸渍法制备了DAC负载Mn、Ce氧化物的Mn-Ce/DAC脱硝催化剂,并用于氨法SCR反应.采用N₂吸附、X射线衍射（XRD）、X射线光电子能谱（XPS）和程序升温吸附脱附（TPR/TPD）等手段对催化剂的物理化学性能进行了表征.结果发现与商业木屑基活性炭负载Mn、Ce氧化物催化剂（Mn-Ce/MAC）相比,Mn-Ce/DAC具有更高的Ce³⁺/Ce⁴⁺比率、表面化学吸附氧含量以及表面Brønsted酸性位点,这与其优良的低温SCR活性及抗硫抗水性能直接相关.原位红外光谱结果显示在含硫气氛中Mn-Ce/DAC表面的硫酸盐含量明显低于Mn-Ce/MAC,表明前者具有优良抗硫性能.     

Evaluation of natural goethite on the removal of arsenate and selenite from water

Elevated arsenic and selenium concentrations in water cause health problems to both humans and wildlife. Natural and anthropogenic activities have caused contamination of these elements in waters worldwide, making the development of efficient cost-effective methods in their removal essential. In this work, removal of arsenate and selenite from water by adsorption onto a natural goethite(α-FeO OH) sample was studied at varying conditions. The data was then compared with other arsenate, selenite/goethite adsorption systems as much of literature shows discrepancies due to varying adsorption conditions. Characterization of the goethite was completed using inductively coupled plasma mass spectrometry, X-ray diffraction, Fouriertransform infrared spectroscopy, scanning electron microscopy, and Brunauer–Emmett–Teller surface area analysis. Pseudo-first order(PFO) and pseudo-second order(PSO) kinetic models were applied; including comparisons of different regression methods. Various adsorption isotherm models were applied to determine the best fitting model and to compare adsorption capacitates with other works. Desorption/leaching of arsenate and selenite was studied though the addition of phosphate and hydroxyl ions. Langmuir isotherm modeling resulted in maximum adsorption capacities of 6.204 and 7.740 mg/g for arsenate and selenite adsorption,respectively. The PSO model applied with a non-linear regression resulted in the best kinetic fits for both adsorption and desorption of arsenate and selenite. Adsorption decreased with increasing pH. Phosphate induced desorption resulted in the highest percentage of arsenate and selenite desorbed, while hydroxide induced resulted in the fastest desorption kinetics.     

Thiocyanate-induced labilization of schwertmannite: Impacts and mechanisms

Schwertmannite is an amorphous iron(III)-oxyhydroxysulfate that forms in acid mine drainage(AMD) environments. The characteristic of high heavy metal adsorption capability makes schwertmannite a potentially useful, environmentally friendly material in wastewater treatment. Unstable schwertmannite is prone to recrystallization.Understanding the mechanisms that induce schwertmannite labilization and affect its capacity to remove heavy metals are of great environmental and geochemical significance.Thiocyanate(SCNˉ) is a hazardous pseudohalide that is also normally found in AMD.However, little is known about the impact of Fe(III)-binding ligand SCNˉ on schwertmannite stability and its subsequent capacity to bind trace elements. Here, we investigated the adsorption of SCNˉ on schwertmannite and subsequent mineral transformation to characterize this little-known process. The appearance of Fe2+indicated that the interactions between schwertmannite and SCNˉ may involve complexation and reduction reactions. Results showed that the majority of the adsorbed-SCNˉ was immobilized on schwertmannite during the 60-days transformation. The transformation rates of schwertmannite increased with increasing concentrations of SCNˉ. Goethite was detected as the dominant transformation product with or without SCNˉ. The mechanisms of SCNˉ-promoted dissolution of schwertmannite can be described as follows:(1) formation of Fe(III)–NCS complexes on the schwertmannite surface and in solution, a process which increases the reactivity of solid phase Fe(III);(2) the extraction of Fe(III) from schwertmannite by SCNˉ and subsequent schwertmannite dissolution; and(3) the formation of secondary minerals from extracted Fe(III). These findings may improve AMD treatment strategies and provide insight into the use and potential reuse of schwertmannite as a trace element sorbent.     

2014年北京地区云内云下的降水化学分析

为了解现阶段北京地区降水的化学特征和云下/云内的清除作用,于2014年采用分段采样的方式针对25场降水进行收集,分析了降水中各离子组分浓度.结果发现,2014年北京地区降水中NH₄⁺、SO₄^2-、NO₃^-和Ca²⁺浓度最高,雨量加权平均离子浓度分别为240、162、91和65 μeq·L^-1,与早期研究相比均有所下降.SO₄^2-/NO₃^-比值为1.8,NO₃^-和NH₄⁺的比重显著增加.综合利用相关性分析、主因子分析及后向轨迹等方法,探讨了北京地区降水中各离子组分的来源.结果表明,东南气团中主要离子NO₃^-、SO₄^2-及NH₄⁺的浓度较高,主要受人为活动排放的影响.总体上各离子的云下冲刷作用略大于云内清除,其中,Na⁺、Ca²⁺及NO₃^-云下冲刷的贡献大于SO₄^2-和NH₄⁺.与其他城市相比,北京地区云内清除的贡献略大,表明长距离输送的影响不可忽视.     

Case study of dust event sources from the Gobi and Taklamakan deserts: An investigation of the horizontal evolution and topographical effect using numerical modeling and remote sensing

A severe dust event occurred from April 23 to April 27, 2014, in East Asia. A state-of-the-art online atmospheric chemistry model, WRF/Chem, was combined with a dust model, GOCART, to better understand the entire process of this event. The natural color images and aerosol optical depth (AOD) over the dust source region are derived from datasets of moderate resolution imaging spectroradiometer (MODIS) loaded on a NASA Aqua satellite to trace the dust variation and to verify the model results. Several meteorological conditions, such as pressure, temperature, wind vectors and relative humidity, are used to analyze meteorological dynamic. The results suggest that the dust emission occurred only on April 23 and 24, although this event lasted for 5 days. The Gobi Desert was the main source for this event, and the Taklamakan Desert played no important role. This study also suggested that the landform of the source region could remarkably interfere with a dust event. The Tarim Basin has a topographical effect as a “dust reservoir” and can store unsettled dust, which can be released again as a second source, making a dust event longer and heavier.