荔枝皮对重金属Ni~(2+)的吸附性能

采用批量实验研究了荔枝皮对水中重金属Ni2+吸附的影响因素(如接触时间、pH和吸附剂量)、吸附等温线、吸附动力学和吸附热力学等,并讨论了其吸附机理。结果表明,未改性荔枝皮和改性荔枝皮对Ni2+的吸附平衡时间均为30min;最适pH为6.0~7.0;最佳吸附剂量均为20 g/L。吸附过程均能用Langmuir和Freundlich等温线模型来很好地描述,且均符合假二次动力学模型。改性荔枝皮和未改性荔枝皮对Ni2+的最大比吸附量分别为11.88和5.19 mg/g。此外,热力学研究结果表明,未改性荔枝皮和改性荔枝皮吸附Ni2+均属于非自发的放热过程。     

高效脱硫菌的筛选及其性能研究简

从高硫污染的活性污泥中富集培养,分离纯化得到一株可以降解噻吩的菌株S-4,并对该菌株的形态特征进行观察。应用Design-Expert8.0.5b软件进行响应面优化实验,研究了反应时间、噻吩浓度、微生物浓度3个因素的组合对菌株S-4脱硫效果的影响,并拟合得到多元二次回归方程,得出最佳实验条件。拟合结果表明,当反应时间27.46 h,噻吩浓度为1.04%,微生物浓度4.04%时,预测噻吩降解率为14.8%,通过验证得最佳条件下的降解率为14.3%,与预测值相符。     

Cu-SBA-15催化湿式过氧化氢氧化水溶液中罗丹明B

采用水热晶化法合成了不同含铜量的Cu—SBA-15介孔分子筛,并且用XRD、N2吸附、TEM以及uV—vis对所合成的样品进行表征。以Cu—SBA-15为催化剂,H2O2为氧化剂,催化湿式过氧化水溶液中的罗丹明B,主要考察H2O2浓度、催化剂用量、处理温度、初始pH等因素对罗丹明B氧化效果的影响。结果表明,在同样的处理条件下罗丹明的脱色率明显高于TOC去除率,处理温度、初始pH对罗丹明B的脱色与氧化有重要影响。在罗丹明B初始浓度100mg／L,H2O2初始浓度1．8g／L,催化剂量0．3g／L,温度60℃,pH为7．0,处理时间100min时,罗丹明B的脱色率为98．6％,TOC去除率为62．8％。     

回填土钻孔灌注桩-承台混凝土水化作用效应现场试验

混凝土早期水化作用释放大量热量,会引起桩身温度和桩身应力变化,从而影响桩基承载性能。通过开展现场试验,研究回填土地基中钻孔灌注桩-承台混凝土水化热对桩身及桩基周围土体的影响,实测并分析了桩身及桩基周围土体温度随时间、深度的变化规律和桩基应力随时间的变化规律。研究结果表明,试桩混凝土浇筑完成后,0.7 d时桩体不同深度处的温度均达到最大值,21.4d时其温度基本稳定;桩体温度随时间变化规律可分为快速上升、快速下降、缓慢降低和基本稳定4个阶段。承台混凝土水化热效应仅对桩基周围浅层土体温度有一定影响,当深度大于3 m时,其对土体的温度作用效应基本可以忽略。桩基约束应力变化表现为先迅速增长再缓慢下降最终趋于稳定,最大约束应力值与混凝土轴心抗拉强度十分接近。     

土体环境对微生物诱导碳酸钙沉积加固海相粉土的影响研究

生物地基处理技术利用微生物诱导碳酸钙沉积来加固土体,符合环境保护和可持续发展的要求,具有良好的发展前景。目前已取得的研究成果主要是针对简单离子化学环境下的松散砂土,对不同环境下的细粒土研究的较少。以江苏东部沿海地区的海相吹填粉土为研究对象,选用巴氏芽孢杆菌进行微生物注浆试验,定量分析温度、pH值、氯化盐含量、土体中胶结阳离子含量等土中的环境因素对加固效果的影响规律。结果表明:随着温度的升高、试样中生成的碳酸钙增加,但无侧限抗压强度并不是呈现出一直提高的趋势,而是存在一个峰值。偏碱性的环境有利于巴氏芽孢杆菌的工作,但过高的pH值会影响加固效果。土中的氯化盐含量过高时会抑制细菌的活性从而对加固产生不利影响。土中的胶结阳离子含量对微生物注浆的影响很小,可忽略不计。本次试验研究结果能为现场环境下采用MICP技术加固粉土提供有效的依据。     

用味精生产废水培养好氧颗粒污泥

以厌氧颗粒污泥为接种污泥,采用味精生产废水进行培养,在SBR中以逐渐降低污泥沉淀时间的方法成功培养出好氧颗粒污泥。实验结果表明：污泥接种65 d后,出现细小的好氧颗粒污泥,呈黄褐色,95 d后颗粒污泥趋于成熟,粒径达0.6 mm左右,且周围存在大量原生动物;运行95 d后MLSS提高至8.00 g/L,SVI降至30.00 mL/g左右;成熟后的好氧颗粒污泥对味精生产废水中的COD和NH₃-N具有良好的去除效果,出水COD和ρ（NH₃-N）分别为80 mg/L和2 mg/L左右。     

紫外催化湿式双氧水氧化处理化学镀铜废液

利用化学镀铜废液自身含有的铜作为催化剂,应用紫外催化湿式双氧水氧化工艺处理化学镀铜废液取得了良好效果。通过单因素实验确定的推荐工艺条件为：pH=2.0（保持原始值不变）;不额外投加铜催化剂;H₂O₂用量为2倍理论量。在此条件下处理化学镀铜废液180 min,COD去除率可达到96.6%;之后采用沉淀法回收铜,调节处理后废水pH到9.5,铜的回收率可达到99.8%。     

温度对亚硝化及氧化亚氮释放的影响

采用批次实验的方法探讨了3种不同温度(15℃,25℃,35℃)对亚硝化及其过程中温室气体氧化亚氮释放情况。结果表明,温度对亚硝化过程及氧化亚氮的释放有显著影响。在15～35℃范围内,随着温度的升高,氨氧化率和亚硝化积累率逐渐升高,N2O释放量也逐渐增大,35℃可以作为适宜的亚硝化温度,平均氨氧化率为50.9%,亚硝化积累率为55.6%,NO2--N与NH4+-N出水浓度比为1.1,氨氧化率,亚硝化积累率和出水中亚硝氮与氨氮浓度比较合适,从而可以为厌氧氨氧化工艺提供合适的进水,但在此温度下平均N2O释放量相对较高,为1.494μg/g MLSS。     

Organochlorine pesticides in the dust fall around Lake Chaohu, the fifth largest lake in China

The residual levels of organochlorine pesticides (OCPs) in the dust fall around Lake Chaohu were measured using gas chromatography mass spectrometry from April 2010 to March 2011. The fluxes, components, temporal–spatial variations, and sources of OCPs were also analyzed. Twenty-one types of OCPs were detected in the dust fall samples around Lake Chaohu, with a total concentration of 51.54?±?36.31 ng/g and a total flux of 10.01?±?13.69 ng/(m² day). Aldrin (35.3 %), endosulfan (39.1 %), dichlorodiphenyltrichloroethanes (DDTs) (49.8 %), and isodrin (37.1 %) were the major OCPs in the spring, summer, autumn, and winter, respectively. Both the residual level and the flux were higher in the spring than in other seasons and higher at the outer lake sampling sites than inner lake sampling site. The potential source of the hexachlorcyclohexanes in the dust fall may be recent lindane usage. The DDTs mainly came from historical dicofol usage, and a significant input of DDT was found during April and June. The presence of endosulfan may be due to the present use of technical endosulfan. The aldrin in the dust might be due to its occasional usage, and isodrin may be a result of long-distance transport from other countries.     

Variations in global temperature and precipitation for the period of 1948 to 2010

Climate change has impacts on both natural and human systems. Accurate information regarding variations in precipitation and temperature is essential for identifying and understanding these potential impacts. This research applied Mann–Kendall, rescaled range analysis and wave transform methods to analyze the trends and periodic properties of global and regional surface air temperature (SAT) and precipitation (PR) over the period of 1948 to 2010. The results show that 65.34 % of the area studied exhibits significant warming trends (p?<?0.05) while only 3.18 % of the area exhibits significant cooling trends. The greatest warming trends are observed in Antarctica (0.32 °C per decade) and Middle Africa (0.21 °C per decade). Notably, 62.26 % of the area became wetter, while 22.01 % of the area shows drying trends. Northern Europe shows the largest precipitation increase, 12.49 mm per decade. Western Africa shows the fastest drying, ?21.05 mm per decade. The rescaled range analysis reveals large areas that show persistent warming trends; this behavior in SAT is more obvious than that in PR. Wave transform results show that a 1-year period of SAT variation dominates in all regions, while inconsistent 0.5-year bands are observed in East Asia, Middle Africa, and Southeast Asia. In PR, significant power in the wavelet power spectrum at a 1-year period was observed in 17 regions, i.e., in all regions studied except Western Europe, where precipitation is instead characterized by 0.5-year and 0.25-year periods. Overall, the variations in SAT and PR can be consistent with the combined impacts of natural and anthropogenic factors, such as atmospheric concentrations of greenhouse gases, the internal variability of climate system, and volcanic eruptions.