乙酸/丙酸作为EBPR碳源的动力学模型研究(Ⅱ)——动力学模拟

以乙酸和丙酸作为混合碳源,采用2组序批式反应器(SBR)研究聚磷菌(PAO)和聚糖菌(GAO)代谢过程中的物质转化规律.PAO和GAO动力学模型共包含7个计量学参数和24个动力学参数.根据计量学方程,推导了PAO和GAO动力学模型中的计量学参数.结合试验结果,确定了动力学参数的取值.采用Matlab软件积分计算了PAO和GAO胞内物质的变化规律.SBR运行的实际值与模拟值相吻合,表明基于SCFAs代谢的动力学模型能够很好地模拟PAO和GAO的好氧/厌氧代谢过程.     

夏季南海气溶胶微量元素浓度、溶解度及干沉降通量

搭载国家自然科学基金委南海东北部共享航次（NORC2017-05），于2017年6月9日-8月11日在南海东北部采集气溶胶样品，使用淋溶装置得到气溶胶中微量元素（Al、Fe、Ti、Cr、V、Ba、Mn、Co、Ni、Pb、Cu、Zn）的溶解态浓度和溶解动力学曲线，混酸消解后用高分辨率电感耦合等离子体质谱测得其总浓度，并计算溶解度和干沉降通量.结果表明，夏季南海北部气溶胶中微量元素溶解态浓度、总浓度和干沉降通量均小于大多数陆架边缘海.微量元素溶解度相对较大，原因主要是气溶胶颗粒经过长距离输运后粒径较小，且经历的大气酸过程和云过程对元素溶解度影响显著.气溶胶中微量元素在Milli-Q水中25 min左右达到溶解平衡，后续以pH=2的HCl淋溶.酸淋溶过程中大部分微量金属的溶解度略有增加，约占水溶出量的30%~50%，而Pb在酸溶液中显著溶出，酸溶出量可达水溶出量的140%，表现出潜在的环境效应.夏季大气气溶胶输送的Fe占南海东北部混合层溶解态Fe的0.13%~6.00%，对浮游植物初级生产具有一定的支持功能.     

呼吸计量法测定安庆市城东污水厂污泥特性参数

为了应用活性污泥1号模型模拟生活污水为主的安庆市城东污水处理厂的运行,对该厂的污泥特性参数即化学计量学系数YH、动力学参数bH和μH进行了测定,测定结果分别为0.71、0.40、2.0(10℃),并对YH测试中内源线与呼吸线直线段的差异、bH测定时温度的影响、μH测定前30～60min的大幅OUR上升现象进行了分析。     

重金属铜在黑土和棕壤中解吸行为的比较

采用一次平衡法研究吸附态Cu²⁺在黑土和棕壤上的解吸行为并进行了比较.结果表明,与棕壤相比,黑土吸附态Cu²⁺解吸有更长的滞后阶段,黑土在Cu²⁺的吸附量低于729.00mg·kg^-1(Cu²⁺处理浓度小于40 mg·L^-1),棕壤在Cu²⁺的吸附量低于393.29 mg·kg^-1(Gu²⁺处理浓度小于20 mg·L^-1)时,土壤吸附态Cu²⁺几乎不发生解吸.2种土壤吸附态Cu²⁺的解吸率均较低,尤其是黑土.在试验所采用的Gu²⁺处理浓度范围内,黑土与棕壤吸附态Cu²⁺的最高解吸率分别为6.60%和13.56%.Freundlich方程为描述2种土壤Cu²⁺等温解吸过程的最佳方程.黑土和棕壤吸附态Cu²⁺的解吸速率均较快,在40min左右基本达到平衡.描述黑土和棕壤解吸动力学过程的最优模型为双常数速率方程,其次为Elovich方程.     

The dissolution kinetics of major elements in municipal solid waste incineration bottom ash particles

Leaching and tracer experiments in batches at L/S 20 were performed with 3-month-old MSWI bottom ash separated into eight different particle sizes. The time-dependent leaching of major elements (Ca(2+), K(+), Na(+), Cl(-) and SO(4)(-2)) was monitored for up to 747 h. Physical properties of the particles, the specific surface (BET), pore volume and pore volume distribution over pore sizes (BJH) were determined for all particle classes by N(2) adsorption/desorption experiments. Some common features of physical pore structure for all particles were revealed. The specific surface and the particle pore volume were found to be negatively correlated with particle size, ranging from 3.2 m(2)/g to 25.7 m(2)/g for the surface area and from 0.0086 cm(3)/g to 0.091 cm(3)/g for the pore volume. Not surprisingly, the specific surface area was found to be the major material parameter that governed the leaching behavior for all elements (Ca(2+), K(+), Na(+), Cl(-) and SO(4)(-2)) and particle sizes. The diffusion resistance was determined independently by separate tracer (tritium) experiments. Diffusion gave a significant contribution to the apparent leaching kinetics for all elements during the first 10-40 h (depending on the particle size) of leaching and surface reaction was the overall rate controlling mechanism at late times for all particle sizes. For Ca(2+) and SO(4)(-2), the coupled effect of diffusion resistance and the degree of under-saturation in the intra particle pore volume was found to be a major rate limiting dissolution mechanism for both early and late times. The solubility control in the intra particulate porosity may undermine any attempt to treat bottom ash by washing out the sulfate. Even for high liquid/solid ratios, the solubility in the intra-particular porosity will limit the release rate.     

生物质分类表征蔬菜废物好氧降解模型中试检验

为发展可支持生产性堆肥设施控制的有机废物好氧降解模型,对生物质分类蔬菜废物好氧降解速率模型(即:六因子的生物质分类一级降解动力学模型Mt=M0e-kt),以及通过主因子分析法(PCA)和生物质组分归类2种方法简化得到的二因子和三因子模型,利用太湖农村生活垃圾现场堆肥中试的一次发酵试验结果,进行了模拟检验.结果表明,生物质分类表征蔬菜废物好氧降解模型能有效地模拟中试的实际降解率,模拟与实测值的pearson相关系数r＞0.966(p＜0.001);且模拟效果基本不受原料生物质组成与堆肥工况控制条件的影响.而简化模型的模拟效果明显劣于六因子模型,这可能源于各类生物质好氧降解受温度影响的机制不同,组分的动力学参数难以合并简化.     

骨炭对Pb(Ⅱ)的吸附特性

通过间歇实验研究了骨炭对重金属Pb(Ⅱ)的吸附特性。探讨了固液比、pH、离子强度、反应时间、温度及初始浓度等因素的影响。实验结果表明,pH与固液比显著影响去除率,温度与离子强度的影响较小。当温度为20℃,pH=2.5,Pb(Ⅱ)的初始浓度为200 mg/L,固液比为1 g/L时,最大去除率近100%。动力学实验结果表明,骨炭对Pb(Ⅱ)的吸附为快速反应,在30 min内可达到平衡,准二级动力学模型可较好地拟合实验结果。等温吸附实验结果表明,Freundlich模型与Langmuir模型均可较好地拟合等温吸附实验结果。骨炭对Pb(Ⅱ)的吸附机制主要为表面络合反应与分解置换-沉淀反应。     

Photolysis of oxyfluorfen in aqueous methanol

Photolysis of oxyfluorfen, an herbicide of the nitrodiphenyl ether class, was studied in aqueous methanol under UV and sunlight. UV irradiation was carried out in a borosilicate glass photoreactor (containing 250 ppm oxyfluorfen in 50% aqueous methanol) equipped with a quartz filter and 125 watt mercury lamp (maximum output 254 nm) at 25 ± 1°C. Sunlight irradiation was conducted at 28 ± 1°C in borosilicate Erlenmeyer flasks containing 250 ppm oxyfluorfen in 50% aqueous methanol. The samples from both the irradiated conditions were withdrawn at a definite time interval and extracted to measure oxyfluorfen content by gas chromatography-flame ionization detector for rate study. The half-life values were 20 hours and 2.7 days under UV and sunlight exposure, respectively. Photolysis of oxyfluorfen yielded 13 photoproducts of which three were characterized by infrared spectrophotometer and ¹H NMR and ¹³C NMR spectroscopy. The rest of the photoproducts were identified by gas chromatography-mass spectrometry (GC-MS) and thin layer chromatography (TLC). An ionization potential 70 eV was used for electron impact-mass spectrometry (EI-MS) and methane was used as reagent gas for chemical ionization-mass spectrometry (CI-MS). Two of the photoproducts were also synthesized for comparison. The main phototransformation pathways of oxyfluorfen involved nitro reduction, dechlorination, and hydrolysis as well as nucleophiles displacement reaction.     

碱性水对煤自燃特性影响实验研究

为了研究碱性水对煤自燃特性的影响,选取葫芦素煤矿102工作面煤样作为实验煤样,利用STA-449C型同步热分析仪进行热重实验,研究加入PH=8 NaOH的煤样与原煤以及加入蒸馏水煤样在空气氛围中燃烧失重、放热量、特征温度点等变化规律,并根据Coats-Redfern积分模型计算了3种煤样燃烧反应动力学参数（活化能、指前因子）。研究结果表明:加入碱性水的2号煤样失重量较1,3号少,燃烧失重速率更低;2号煤氧化燃烧温度区间缩短,着火温度点升高,放热量少,比1,3号煤分别少485.0,480.4 J/g;3种煤样反应机理基本遵循一级化学反应函数,2号煤各段活化能高于1,3号煤,但2号煤失水活化能小于3号,表明碱性水具有抑制煤自燃效应。     

缙云山不同林分下土壤有机碳及矿化特征

土壤有机碳库是陆地最大的有机碳储存库,其微弱的变化就能影响大气CO2浓度的显著变化,其中森林土壤碳库约占全球土壤碳库的70%,因此如何实现森林生态系统土壤有机碳库的高效管理成为目前的研究热点.本研究以缙云山5种典型林分:阔叶林、针叶林、针阔叶混交林、竹林及研究区内弃耕15 a的荒草地(对照土壤)为对象,采用矿化培养实验,分析了不同林分的土壤在不同土层(0～20、20～40、40～60、60～100 cm)中的有机碳矿化特征.结果表明,林分类型、培养时长和土层深度均对土壤有机碳矿化速率有显著影响.不同林分土壤有机碳矿化速率均随着土层加深而降低,其中0～20 cm土层的矿化速率[11. 97～25. 12 mg·(kg·d)-1]均显著高于其他土层(P 0. 05),其他土层间矿化速率[4. 79～6. 51mg·(kg·d)-1]无显著性差异. 5种林分的土壤有机碳累积矿化量均随着土层加深而降低,0～20 cm土层中竹林和阔叶林土壤有机碳累积矿化量最高,分别为177. 66 mg·kg~(-1)和120. 38 mg·kg~(-1),随着土层加深在60～100 cm土层中,针叶林累计矿化量最高达到了46. 96 mg·kg~(-1).双库一级动力学方程可以较好地拟合缙云山不同林分下土壤有机碳矿化过程,不同林分下土壤易分解有机碳含量均随土层加深而降低,针叶林土壤矿化能力较强,对难分解有机碳库的利用程度较高,而竹林和阔叶林土壤微生物活性较高,可以有效促进碳循环,提高土壤固碳能力.