带支撑基坑围檩受力性状分析及数值模拟

通过对带支撑基坑围檩受力性状的分析,提出支撑与围檩正交、斜交分别对应的几种基坑围檩轴力分布形式,并以武汉市凯德广场古田项目为例,从实测数据出发,分析了基坑围檩轴力的变化规律,在对基坑内支撑平面有限元计算中设置在围檩上的边界条件的特性进行深入研究的基础上,使用数值模拟手段对基坑围檩轴力进行了计算与数值模拟验证。结果表明:与开挖工况一致,围檩轴力呈现"两阶段"增长过程,地下室主体结构施工完成后,围檩轴力趋于稳定;桩(墙)平行于围檩走向的切向约束客观存在,本例中围檩轴力呈现梯形交替递增分布形式;桩(墙)对围檩的约束方向包括切向和法向,其约束形式表现为线约束和弹性约束。     

离子交换膜的制备及发展趋势研究

总结当前离子交换膜制备技术的发展状况.从膜的分类及膜性能出发,讨论均相膜及异相膜的差异和今后各自的发展前景,并就提升膜单方面性能(如:选择透过性、离子交换容量、膜电阻、抗氧化性等)的方式进行归纳总结.离子交换膜的改进制备大多从结构上入手,提出今后膜制备的主要研究方向为:深化均相膜制备技术、结合国内成熟的离子交换树脂制备工艺改进异相膜的制备技术.     

西安市PM2.5燃煤源谱特征研究

针对西安本地源谱缺乏的现状,总结统计了西安目前灰霾特征和主要成因,对西安市燃煤源进行了测定.研究发现,在煤烟尘PM2.5中SO2-4的含量最高(25%),其次为OC(12%)、NH+4(7%)、Cl-(5%).对固定源燃煤与民用散烧煤,不同脱硫方式、脱硝方式和锅炉类型的固定源成分谱分析得出:1.SO2-4及Al、Si、Ca在固定源煤烟尘PM2.5中含量大于民用燃煤,OC与之相反;2.炉内喷钙法PM2.5中SO2-4明显高于其它脱硫法含量;双碱法PM2.5中Na的含量显著高于其它脱硫工艺流程的含量;氧化镁法PM2.5 中Mg含量为各类脱硫工艺中最高;石灰石膏法颗粒物中Mg、Al、Si、Ca等元素含量均高于大多数工艺;3.不同的脱硝工艺中NO-3离子在各类成分谱中的含量极低;4.链条炉与层燃炉PM2.5中OC、EC含量高于循环流化床炉、煤粉炉.     

超声波有机溶剂萃取法和改进的Bligh-Dyer法提取甘油二烷基甘油四醚类化合物效果对比

由古菌和细菌产生的甘油二烷基甘油四醚类化合物(GDGTs)是微生物学和古环境研究中的一类重要的生物标志化合物。有机溶剂萃取法和改进的Bligh-Dyer法(简称BD法)是两种常用的提取环境样品中GDGTs的方法,然而目前对这两种方法提取效果的对比研究还比较少。本研究分别采用超声波有机溶剂萃取法和BD法对两个土壤样品和两个湖泊沉积物样品的GDGTs进行了提取。对比分析表明,超声波有机溶剂萃取法提取出的核心脂形式的GDGTs(C-GDGTs)含量较高而BD法通常能提取出更多的完整极性膜脂形式的GDGTs(IP-GDGTs)。另外,两种方法得到的C-GDGTs中TEX_(86)、MBT和CBT指标基本相同,但BD法提取的C-GDGTs的BIT值稍微偏高。这些结果将为土壤和湖泊沉积物样品GDGTs提取方法的选择以及不同研究间各指标的对比提供一定的依据。     

典型水库型湖泊中CDOM吸收及荧光光谱变化特征:基于沿岸生态系统分析

为进一步了解水库型湖泊溶解性有机质(DOM)的地球化学特征,本文以三峡库区典型内陆水库型湖泊——长寿湖为研究对象,利用紫外-可见和三维荧光光谱,并结合湖区周边生态系统分析,讨论了长寿湖水体中CDOM的组成、来源和空间分布特征.结果表明,长寿湖不同采样点DOM浓度(DOC和CDOM)存在一定程度的空间分布差异,但各点FDOM分布较为稳定.回水区出现DOM累积,由于受陆源输入影响有限,水体内源活动主导,具有较明显"内源控制"特征,芳香性和分子量相对较低;而周边陆地以人工林兼旅游开发为主的采样点,陆源输入在带入较多腐殖化(高芳香性)组分的同时,人为活动排放也是导致其类蛋白组分丰富的重要原因;入湖区尽管周边果林和居民生活对水体DOM有一定影响,但上游河流输入的影响也不容忽视.另外,各采样点也出现了不受周边生态系统影响的独立的相关性特征,例如芳香性特征常数(SUVA280)和光谱斜率[S(275~295)]显著负相关、CDOM和FDOM极显著正相关、CDOM和S(275~295)负相关等.同时,长寿湖水体中CDOM的生色团主要由具有芳香性结构的大分子组分构成;至少51%的CDOM波动可以通过FDOM变化来进行解释,其中回水区荧光组分对CDOM变动的影响最为明显.在采用传统FI值无法区分DOM来源差异性时,结合采样点沿岸生态系统,综合紫外-可见和荧光光谱特征,有助于对DOM组成及来源进行解析.     

适用于中国燃煤电厂的汞监测及排放控制技术

随着GB 13223—2011《火电厂大气污染物排放标准》的颁布,汞排放问题正式列入了控制目标,这必将对燃煤电厂的环保设施提出新的更高的要求。在综述国外汞监测技术的前提下,总结脱硫脱硝污染物监测的经验,针对中国的具体情况分析了新形势下我国燃煤电厂汞监测技术的发展方向和关键技术的开发重点。同时分析了在最大化地利用燃煤电厂现有环保设施和设备的情况下,如何开发在今后一段时期内最适宜在我国广泛应用的汞排放控制技术,也对国内今后的政策发展进行了预测。     

餐厨垃圾与污水污泥共消化产酸试验研究

研究了餐厨垃圾与污水污泥在不同混合比例、不同污泥停留时间条件下的共消化产酸效果。试验结果表明:当餐厨垃圾与污水污泥TS比为1∶3时,SRT=1 d的反应器酸化效率最高,且乙酸含量占优,产酸效果较佳;当TS之比为1∶1时,各反应器产酸量普遍高于1∶3时,其中SRT=5 d产酸反应器,最高酸化效率达5.94,产酸量最大,且乙酸含量占优,运行效果最佳。     

Enhanced photocatalytic activity of quantum-dot-sensitized one-dimensionally-ordered ZnO nanorod photocatalyst

An efficient photocatalyst was fabricated by assembling quantum dots （QDs） onto one-dimensionally-ordered ZnO nanorods, and the photocatalytic properties for Methyl Orange degradation were investigated by scanning electron microscopy, transmission electron microscopy, X-ray diffraction, UV-Vis-NIR absorption spectroscopy and photoluminescence. The results indicate that the catalyst with assembled QDs is more favorable for the degradation than the pristine ZnO nanorods. The QDs with core-shell structure lower the photocatalytic ability due to the higher carder transport barrier of the ZnS shell layer. Besides its degradation efficiency, the photocatalyst has several advantages given that the one-dimensionally-ordered ZnO nanorods have been grown directly on indium tin oxide substrates. The article provides a new method to design an effective and easily recyclable photocatalyst.     

Preparation of MgO/B2O3 coatings by plasma spraying on SUS304 surface and effects of heat-resistant

This study mainly deals with the preparation of MgO/B₂O₃ coatings by plasma spraying on the SUS304 surface and the effects of heatresistant. The power materials of low thermal conductivity were selected to control the heat divergent performance of high temperature parts. The reticular micro-structure between the cover thermal layer and the substrate was prepared by using the plasma spraying method. The powder mixture of MgO and B₂O₃ were selected as spraying materials and the SUS304 was used as the substrate material. The MgO/B₂O₃ coating was prepared on the surface of the SUS304 to provide better cover thermal performance. The properties of the microstructures and the morphologies were studied by Optical Microscope, Scanning Electron Microscope, Electron Probe Microanalyzer, and X-ray Diffraction. The results showed that the cover thermal performance has been improved.     

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.