SO_2在TiO_2颗粒物表面的非均相反应

使用漫反射红外傅里叶变换光谱(DRIFTS)原位反应器研究了SO2在TiO2颗粒物表面的非均相反应.研究了氧气浓度、相对湿度(RH)及紫外光光照对反应的影响.结果表明,SO2在TiO2颗粒物上可转化为亚硫酸盐或被氧化为硫酸盐.水汽或者紫外光照可促进SO2在TiO2颗粒物表面的非均相氧化反应,在两者都存在的情况下,对促进硫酸盐的生成有协同效应.在干态无光照条件下和一定湿度(RH=40%)紫外光照条件下,以硫酸盐的生成来计算,SO2在TiO2颗粒物表面的反应级数分别为二级和一级;反应摄取系数γBET分别为1.94×10-6和1.35×10-5.TiO2颗粒物表面的羟基参与了反应,在紫外光照下表面生成的活性氧物种在反应中起重要作用.     

NO_2在MgO颗粒物表面的非均相反应

氧化镁(MgO)是大气中矿物气溶胶的重要组分之一,对二次污染物的形成有着重要影响.本研究采用原位漫反射红外傅里叶变换光谱(DRIFTS)与离子色谱(IC)技术,研究了二氧化氮(NO2)在MgO颗粒表面的非均相反应.探讨了无光照、紫外光照、臭氧(O3)、温度及相对湿度(RH)等对该反应的影响机制,建立了新的测定摄取系数的方法.结果表明,无光照时,NO2在MgO颗粒表面生成的主要产物为硝酸盐和亚硝酸盐;在NO2-MgO-O3和NO2-MgO-hv两种反应体系中主要产物均为硝酸盐,生成的硝酸根峰面积分别是无光照条件下的1.54倍和3.04倍,O3和紫外光照对硝酸盐的生成均具有促进作用;在紫外光照条件下,NO2在MgO颗粒物表面生成硝酸根的初始速率随温度的升高而呈单峰变化,40℃时初始速率最大;影响NO2与MgO颗粒物反应的敏感因素为紫外光照和臭氧,其次为相对湿度和温度.在25℃,RH为5%时,无光照条件和紫外光照条件下反应初始摄取系数分别为9.01×10-4和5.65×10-3.     

SO_2在ZnO颗粒物表面的非均相反应

使用原位漫反射红外傅里叶变换光谱(DRIFTS)研究了SO2在ZnO颗粒物表面的非均相反应,考察了相对湿度(RH)及紫外光光照对反应的影响.结果表明:无紫外光光照条件下,SO2在ZnO颗粒物表面反应的主要产物为亚硫酸盐,RH与生成的亚硫酸盐量呈负相关关系;有紫外光光照条件下,SO2在ZnO颗粒物表面反应的主要产物为亚硫酸盐和硫酸盐,随着相对湿度和紫外光照强度的增加,亚硫酸盐向硫酸盐转化.光照和水汽对SO2在ZnO颗粒物上的氧化反应起到协同促进作用.以亚硫酸盐生成量计算,干态无光条件下反应对SO2的级数为1.6,接近二级反应;在RH为40%且紫外光光照条件下,反应对SO2的级数为0.91,接近一级反应;使用BET比表面积作为反应有效面积,反应初始摄取系数在干态无光照条件和RH=40%且紫外光照条件下分别为4.87×10-6和2.29×10-5.     

甲醛在α-Al2O3颗粒物表面的非均相反应研究

使用漫反射傅里叶变换红外光谱(DRIFTS)原位反应器研究了273~333 K下甲醛与α-Al2O3颗粒物表面的非均相反应. 结果表明, 甲醛在α-Al2O3颗粒物表面生成产物主要为甲酸盐、二氧亚甲基以及少量多聚甲醛和吸附态甲醛, 甲酸盐是由中间产物二氧亚甲基进一步氧化生成的. 在293 K下, 甲醛在α-Al2O3颗粒物表面的反应级数为0.81±0.05, 以样品池几何面积计算的初始摄取系数γ0GEO为(2.3±0.5)×10-5, 以颗粒物BET面积计算的初始摄取系数γ0BET为(9.4±1.7)×10-9, 表观活化能为33.5 kJ/mol.     

海盐颗粒物表面的NO_2非均相反应

为了深入理解沿海城市大气环境中NO2和海盐颗粒物的非均相反应规律,本研究使用漫反射红外傅立叶变换光谱(DRIFTS)比较研究了0%和20%相对湿度(relative humidty,RH)下NO2在湿海盐颗粒物表面的非均相反应.动力学测量表明硝酸盐的生成对NO2是二级反应,并且0%和20%相对湿度条件下,NO2分子浓度为1.96×1015molcules·cm-3时,反应增长阶段反应摄取系数分别为(5.51±0.19)×10-7和1.26×10-6.结果还显示相对湿度在30%以下时,海盐表面MgCl2·6H2O、CaCl2·2H2O所在点位通过释放结合水和吸附水汽,在海盐表面形成液态水的斑点,增强了反应持续能力.因此氯化钠表面非均相反应的研究可能会低估海盐颗粒物的非均相反应活性.     

2-甲基-2-丁烯乳液氯化反应的研究

研究了温度、时间、紫外光照射等对天然胶乳小分子模型物(2-甲基-2-丁烯乳液)氯化反应的影响,结果表明,在有紫外光照的条件下的氯化反应速率要快于无紫外光照的;温度对氯化反应有着一定影响,在50℃以下,随温度升高产物的氯含量越高,在50℃以上,对产物的氯含量的影响不大;当温度50℃,时间达到7个小时的产物的氯含量能达到6...     

大气复合污染及灰霾形成中非均相化学过程的作用

城市和区域大气复合污染的特征为污染源排放的一次污染物通过大气中的化学反应生成高浓度的氧化剂(臭氧等)及细颗粒物等二次污染物,它们在静稳天气下积累,导致低能见度的灰霾现象并严重影响人体健康和气候.大气复合污染中同时存在高浓度的一次排放和二次转化的气态及颗粒污染物,这为细颗粒表面非均相反应提供了充足的反应物;而气态污染物在细颗粒表面的非均相反应可改变大气氧化性及颗粒物的化学组分、物化性质和光学性质,从而可能对大气复合污染和灰霾的形成起到促进的作用.利用漫反射红外傅里叶变换光谱和单颗粒显微拉曼原位在线技术,我们对大气气态污染物NO2、SO2、O3、甲醛在CaCO3、高岭石、蒙脱石、NaCl、海盐、Al2O3和TiO2等大气主要颗粒物表面的反应进行了系统的反应动力学和机制研究,我们发现反应主要产物为硫酸盐、硝酸盐或甲酸盐,它们可极大改变颗粒物吸湿性和消光性质.通过分析这些非均相反应的动力学过程,我们识别出NO2-颗粒物-H2O、SO2-颗粒物-O3、有机物/SO2-颗粒物-光照等三元反应体系的协同作用机制,这些协同机制对于阐明大气复合污染及灰霾形成的反馈机制和非线性过程提供了实验证据和理论依据.     

NO2在NaCl表面的非均相反应

采用新的样品制备方法和气-固自由扩散的实验方式,使用漫反射傅立叶转换红外光谱原位反应器,结合离子色谱、X-射线光电子能谱、扫描电子显微镜等分析方法,研究了NO2在NaCl表面的非均相反应.研究表明反应不只是发生在颗粒物表面,体相也参与了反应; 颗粒物表面的活性点对反应起决定作用,同时测定了反应级数为二级,反应摄取系数为(1.54±0.70)×10-5.     

无 氧 条 件 下ＴｉＯ２ 薄 膜 界 面 光 催 化 反 应 的ＸＰＳ 研 究

设计利用X射线光电子能谱仪的高真空系统作为无氧条件下光催化反应和分析的场所,研究真空无氧环境和大气有氧环境中紫外光激发TiO2薄膜表面的光催化反应,并对无氧条件下TiO2薄膜降解亚甲基蓝进行初步探索.结果表明,在大气有氧和真空无氧条件下TiO2薄膜经紫外光照后,表面的化学组成和化学状态均发生了变化;在有氧环境中TiO2薄膜表面氧含量增加,而在无氧环境中TiO2薄膜表面氧含量减少.TiO2薄膜表面的吸附氧是维持无氧条件下光催化反应的重要原因,增加薄膜表面吸附氧的含量能提高TiO2薄膜在无氧环境中的催化活性.此外,无氧条件下TiO2薄膜降解亚甲基蓝光催化反应过程中,亚甲基蓝分子只是脱去了某个含氮的基团,生成了中间产物,而并没有完全降解.     

NO2在NaCl表面的非均相反应研究

采用新的样品制备方法和气-固自由扩散的实验方式, 使用漫反射傅立叶转换红外光谱原位反应器, 结合离子色谱、X-射线光电子能谱、扫描电子显微镜等分析方法, 研究了NO₂在NaCl表面的非均相反应. 研究表明反应不只是发生在颗粒物表面, 体相也参与了反应; 颗粒物表面的活性点对反应起决定作用, 同时测定了反应级数为二级, 反应摄取系数为(1.54±0.70)× 10NO^−5.     

Heterogeneous reaction of formaldehyde on the surface of TiO2 particles

The heterogeneous reaction of formaldehyde (HCHO) on the surface of titanium dioxide (TiO₂) was investigated in situ using diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS) combined with ion chromatography (IC), X-ray diffraction (XRD), and transmission electron microscopy (TEM). Formate, dioxymethylene, methoxy, and polyoxymethylene were observed in the infrared spectra of TiO₂ particles during the reaction. On the surface of TiO₂, the adsorbed HCHO was first oxidized to dioxymethylene and further oxidized to formate. The effects of temperature and ultraviolet radiation (UV) on the reaction products and reactive uptake coefficients were studied, and the results indicate that the reaction rate can be accelerated at increasing temperatures as well as under UV. The heterogeneous reaction mechanisms of HCHO on the surface of TiO₂ in the dark and under UV irradiation are proposed. Kinetic measurements show that formate formation on TiO₂ is second order in HCHO concentration and the initial reactive uptake coefficients at room temperature calculated with the Brunauer-Emmett- Teller specific surface area are (0.5–5) × 10^?8 ([HCHO]: 1 × 10¹³?2 × 10¹⁴ molecules/cm³). A linear function relationship exists between the uptake coefficient and the concentration. The apparent activation energy of the reaction was also determined.     

Heterogeneous Interaction of H(2)O(2) with TiO(2) Surface under Dark and UV Light Irradiation Conditions

The heterogeneous interaction of H(2)O(2) with TiO(2) surface was investigated under dark conditions and in the presence of UV light using a low pressure flow tube reactor coupled with a quadrupole mass spectrometer. The uptake coefficients were measured as a function of the initial concentration of gaseous H(2)O(2) ([H(2)O(2)](0) = (0.17-120) × 10(12) molecules cm(-3)), irradiance intensity (J(NO(2)) = 0.002-0.012 s(-1)), relative humidity (RH = 0.003-82%), and temperature (T = 275-320 K). Under dark conditions, a deactivation of TiO(2) surface upon exposure to H(2)O(2) was observed, and only initial uptake coefficient of H(2)O(2) was measured, given by the following expression: γ(0)(dark) = 4.1 × 10(-3)/(1 + RH(0.65)) (calculated using BET surface area, estimated conservative uncertainty of 30%) at T = 300 K. The steady-state uptake coefficient measured on UV irradiated TiO(2) surface, γ(ss)(UV), was found to be independent of RH and showed a strong inverse dependence on [H(2)O(2)] and linear dependence on photon flux. In addition, slight negative temperature dependence, γ(ss)(UV) = 7.2 × 10(-4) exp[(460 ± 80)/T], was observed in the temperature range (275-320) K (with [H(2)O(2)] ≈ 5 × 10(11) molecules cm(-3) and J(NO(2)) = 0.012 s(-1)). Experiments with NO addition into the reactive system provided indirect evidence for HO(2) radical formation upon H(2)O(2) uptake, and the possible reaction mechanism is proposed. Finally, the atmospheric lifetime of H(2)O(2) with respect to the heterogeneous loss on mineral dust was estimated (using the uptake data for TiO(2)) to be in the range of hours during daytime, i.e., comparable to H(2)O(2) photolysis lifetime (～1 day), which is the major removal process of hydrogen peroxide in the atmosphere. These data indicate a strong potential impact of H(2)O(2) uptake on mineral aerosol on the HO(x) chemistry in the troposphere.     

Reactive uptake of HONO to TiO2 surface: "dark" reaction

The interaction of HONO with TiO(2) solid films was studied under dark conditions using a low pressure flow reactor (1-10 Torr) combined with a modulated molecular beam mass spectrometer for monitoring of the gaseous species involved. The reactive uptake of HONO to TiO(2) was studied as a function of HONO concentration ([HONO)(0) = (0.3-3.3) × 10(12) molecules cm(-3)), water concentration (RH = 3 × 10(-4) to 13%), and temperature (T = 275-320 K). TiO(2) surface deactivation upon exposure to HONO was observed. The measured initial uptake coefficient of HONO on TiO(2) surface was independent of the HONO concentration and showed slight negative temperature dependence (activation factor = -1405 ± 110 K). In contrast, the relative humidity (RH) was found to have a strong impact on the uptake coefficient: γ(0) = 1.8 × 10(-5) (RH)(-0.63) (calculated using BET surface area, 40% uncertainty) at T = 300 K. NO(2) and NO were observed as products of the HONO reaction with TiO(2) surface with sum of their yields corresponding to nearly 100% of the nitrogen mass balance. The yields of the NO and NO(2) products were found to be 42 ± 7% and 60 ± 9%, respectively, independent of relative humidity, temperature, and concentration of HONO under experimental conditions used. The contribution of aerosol to the total HONO loss in the boundary layer (calculated with initial uptake data for HONO on TiO(2) surface) showed the unimportance of this process in the atmosphere. In addition, the diffusion coefficient of HONO in He was determined to be D(HONO-He) = 490 ± 50 Torr cm(2) s(-1) at T = 300 K.     

In situ FTIR Study of the Adsorption of Formaldehyde, Formic Acid, and Methyl Formiate at the Surface of TiO2 (Anatase)

The catalytic properties of TiO₂ (anatase) in the reactions of formaldehyde oxidation and formic acid decomposition are examined. At 100–150°C, formaldehyde is converted into methyl formate with high selectivity regardless of the presence of oxygen in the reaction mixture. Formic acid is decomposed to CO and water. Surface compounds formed in the reactions of formaldehyde, formic acid, and methyl formate with TiO₂ (anatase) are identified by in situ FTIR spectroscopy. In a flow of a formaldehyde-containing mixture at 100°C, H-bonded HCHO, dioxymethylene species, bidentate formate, and coordinatively bonded HCHO are observed on the TiO₂ surface. In the adsorption of formic acid, H-bonded HCOOH and two types of formates (bidentate and unsymmetrical formates) are formed. In the adsorption of methyl formate, H-bonded HCOOCH₃, HCOOCH₃ coordinatively bonded via the carbonyl oxygen, and bidentate formate are identified.     

具有广谱紫外屏蔽性能的三元共聚物微球的制备

以醋酸乙烯酯(VA)、 马来酸酐(MA)和商品化的紫外吸收剂2-{2-羟基-5-[2-(甲基丙烯酰氧)乙基]苯基}-2H-苯并三唑(NB)为单体, 偶氮二异丁腈(AIBN)为引发剂, 通过自稳定沉淀聚合法(2SP)制备了具有广谱紫外屏蔽性能的单分散三元共聚物微球(PVMN); 研究了溶剂、 单体配比、 引发剂用量、 单体浓度、 反应温度和反应时间对共聚物微球形态和性能的影响. 研究结果表明, 体积比为7∶3的苯甲酸乙酯/正庚烷混合溶剂是2SP法合成单分散PVMN微球的理想溶剂. 随着单体配比中紫外吸收单体NB比例的增加, 引发剂用量、 单体浓度、 反应温度的提高和反应时间的延长, 微球的粒径随之增大, 进而改变了微球的紫外屏蔽性能. 本文制备的微球的粒径范围为(249±19)~(1434±213) nm, 优化得到的PVMN微球可屏蔽约90%的紫外光. 该策略还可扩展到其它可用作紫外吸收剂的乙烯基单体, 是一种制备稳定高分子紫外屏蔽剂的通用方法.     

甲醛还原Pt/TiO2催化剂用于温和条件下高效催化氧化甲醛

通过浸渍法(IM)和沉积-沉淀(DP)法制备了一系列Pt/TiO2(P25)催化剂,并分别用甲醛溶液和氢气还原处理催化剂.利用原位红外监测催化剂表面吸附物种在反应过程中的变化,探究了催化剂制备和还原条件及Pt负载量对催化剂结构和催化氧化甲醛活性的影响.结果显示,用DP法制备并用甲醛还原的Pt/P25催化剂中Pt颗粒分散均匀,并具有合适的粒径和高浓度的表面活性氧,显示出良好的甲醛氧化活性.在空速30000 ml/(g·h)、反应温度30°C和甲醛初始浓度50 mg/m3的条件下,0.4%Pt/P25(DP-HCHO)上的甲醛转化率达到98%,并能稳定运行100 h以上.相比之下, Pt/P25(DP-H2)由于表面活性氧较少,不利于甲酸盐氧化,活性较低. Pt/P25(IM-H2)虽然具有高浓度的表面活性氧,却同时具有最大的Pt颗粒粒径,在甲醛转化为甲酸盐和甲酸盐氧化两步反应中的活性均较差,因而甲醛氧化活性最差.