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)原位反应器研究了甲醛在TiO2颗粒物表面的非均相反应,结合离子色谱定量分析了反应的主要产物甲酸盐,甲酸盐是由中间产物二氧亚甲基进一步氧化生成.研究了温度和紫外光照对反应的影响,结果表明升高温度和紫外光照可提高反应速率,推测了暗反应和紫外光照下甲醛在TiO2表面的非均相反应机制.结果表明常温下甲醛在TiO2颗粒物表面的反应级数接近2级,初始反应摄取系数为(0.5～5)×10-8([HCHO]:1×1013～2×1014molecule·cm-3),是甲醛浓度的一次函数,同时测定了表观活化能.     

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.     

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.     

MaterialSO2与Fe2O3生成Fe(Ⅱ)(aq)和硫酸盐的复相反应机理

使用DRIFTS, XPS, HPLC和IC考察了常温、常压和氧气存在下SO2与Fe2O3的复相反应, 结果表明, SO2在Fe2O3表面的反应活性与Fe2O3表面含水量密切相关, 表面含水量增加有助于Fe(Ⅱ)(aq)和硫酸盐的生成.室温下(T=291 K, 相对湿度68%), 每毫克Fe2O3在30 min内可消耗53.6 μg SO2, 生成12.6 ng Fe(Ⅱ)(aq)和56.2 μg SO2-4.反应产物 SO2-4的浓度比Fe(Ⅱ)(aq)的浓度高3个数量级, 表明在生成硫酸盐的复相反应中铁对SO2氧化具有非常高的催化活性.提出了Fe(Ⅱ)(aq) 和硫酸盐的生成机理.     

SO2与Fe2O3生成Fe（Ⅱ）（aq）和硫酸盐的复相反应机理

使用DR IFTS,XPS,HPLC和IC考察了常温、常压和氧气存在下SO2与Fe2O3的复相反应,结果表明,SO2在Fe2O3表面的反应活性与Fe2O3表面含水量密切相关,表面含水量增加有助于Fe(Ⅱ)(aq)和硫酸盐的生成.室温下(T=291 K,相对湿度68%),每毫克Fe2O3在30 m in内可消耗53.6μg SO2,生成12.6 ngFe(Ⅱ)(aq)和56.2μg SO42-.反应产物SO42-的浓度比Fe(Ⅱ)(aq)的浓度高3个数量级,表明在生成硫酸盐的复相反应中铁对SO2氧化具有非常高的催化活性.提出了Fe(Ⅱ)(aq)和硫酸盐的生成机理.     

SO2在Fe2O3颗粒表面不同温度下非均相反应的实验模拟

使用漫反射Fourier变换红外光谱(DFTIRS)、离子色谱(IC)及透射电子显微镜(TEM)对不同温度条件下SO2在α-Fe2O3颗粒表面的非均相反应过程进行实验模拟和监测, 并分析了反应剧烈波段(8.7 μm)的产物硫酸盐以及颗粒吸收和后向散射光学系数的变化. 结果表明, 在15-45 ℃内, 硫酸盐生成量、生成速率以及吸收系数、后向散射系数都随反应温度的升高而呈现先增加后减少的趋势; 同一反应温度下, 硫酸盐生成速率随时间呈现先增大后减小, 最后逐渐趋于稳定的演变; 光学系数变化与硫酸盐生成量之间存在较好的指数关系. 在当前全球气候变暖背景下, 研究结果将对深入了解真实大气中SO2与矿尘非均相反应造成的气溶胶光学特性演变, 以及定量评估其辐射强迫影响具有一定意义.     

黑碳颗粒物表面SO2的非均相臭氧氧化

采用漫反射红外傅里叶变换光谱(DRIFTS)结合离子色谱(IC)、 X射线光电子能谱(XPS)研究了常温常压下SO2与O3在黑碳颗粒物(以Printex U为代表, 简称UBC)表面的非均相反应. 研究发现, 在O3和水气存在的情况下, 体系的反应产物主要是SO42-, 反应在一定时间内持续进行. UBC可提供反应活性位点, 促进SO2在其表面的臭氧氧化. O3是关键的氧化剂, 能显著提高SO2非均相氧化生成SO42-的速率. 水气的存在有利于表面活性位点再生, 使反应持续发生. 当SO2和O3的浓度为1014~1015 molecule/cm3、 相对湿度为40%时, SO2在UBC(1: 400, 以NaCl为稀释剂稀释400倍)表面非均相反应生成SO42-的稳态摄取系数(γBET)为1~6×10-6, SO42-的生成速率为1014~1015 ion·s-1·g-1.     

SO2在Fe2O3颗粒表面不同温度下非均相反应的实验模拟

使用漫反射Fourier变换红外光谱(DFTIRS)、离子色谱(IC)及透射电子显微镜(TEM)对不同温度条件下SO2在α-Fe2O3颗粒表面的非均相反应过程进行实验模拟和监测,并分析了反应剧烈波段(8.7μm)的产物硫酸盐以及颗粒吸收和后向散射光学系数的变化.结果表明,在15-45℃内,硫酸盐生成量、生成速率以及吸收系数、后向散射系数都随反应温度的升高而呈现先增加后减少的趋势;同一反应温度下,硫酸盐生成速率随时间呈现先增大后减小,最后逐渐趋于稳定的演变;光学系数变化与硫酸盐生成量之间存在较好的指数关系.在当前全球气候变暖背景下,研究结果将对深入了解真实大气中SO2与矿尘非均相反应造成的气溶胶光学特性演变,以及定量评估其辐射强迫影响具有一定意义.     

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.     

Heterogeneous reaction of SO2 on TiO2 particles

The heterogeneous reaction of SO₂ on TiO₂ particles was studied using in situ diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS). The influences of the oxygen concentration, relative humidity (RH), and ultraviolet (UV) light illumination (λ ≈ 365 nm) intensity on the reaction were investigated. The main product of the heterogeneous reaction of SO₂ on TiO₂ particles was sulfate with UV illumination and sulfite without it. The production of sulfate was promoted significantly with UV illumination or water, and there was a synergistic effect when both were present. In the dry system without UV, the heterogeneous reaction of SO₂ on TiO₂ particles was found to be second-order for SO₂ and the initial uptake coefficient, γ_BET, was determined to be 1.94 × 10^?6. With UV and RH = 40%, the reaction order was first-order and the initial uptake coefficient was 1.35 × 10^?5.     

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.     

紫外光下纳米TiO2 薄膜亲水性机理的电化学研究

The nanometer films of TiO2 were prepared by sol-gel method on ITO（Indium-tin oxide,SnO2:In） substrate. The TiO2 film was the anatase phase with a particle size of 100 nm from the measurements of X-ray diffraction and AFM（Atomic-Force-Microscope）. Electrochemical characteristics of ITO/ TiO2 electrode under UV（ultraviolet）irradiation were investigated using the method of cyclic voltammetry. A new oxidative peak was observed at 0.035 V when the TiO2 electrode was irradiated by 253.7 nm UV light for a certain time. The peak current increased with the irradiation time. It was assumed that the new oxidative peak resulted from Ti3+,which was formed during the UV illumination. The changes of hydrophilicity of the TiO2 thin film on ITO under UV light were also observed. It was assumed that the changes of hydrophilicity of the films may be related with the formation of Ti3+ on the surface when the film was irradiated by UV light.     

NaCl与Fe2O3混合物对SO2的有效吸收

采用DRIFTS和XPS等方法研究了SO2在NaCl和α-Fe2O3混合物表面的复相反应, 并计算了反应的吸附常数. 结果表明, 反应生成物主要为硫酸盐、硫酸氢盐以及少量的亚硫酸(氢)盐; SO2与NaCl和α-Fe2O3混合物的反应符合零级反应动力学规律; NaCl的含量对反应有影响, 随着混合物中NaCl含量的增加, BET吸附常数呈现先上升而后再下降的变化规律, 当NaCl的质量分数达到70%左右时, BET吸附常数达到最大(4.62×10-6), 是纯α-Fe2O3(5.72×10-7)的8.08倍; 反应生成的FeCl2-SO3-中间体作为SO2的储存库, 促进了更多的硫酸盐生成.     

Two Photoelectrochemical Processes for TiO2 Electrode under UV Illumination

TiO2 thin film electrode was prepared by a sol-gel method on ITO substrates. Cyclic voltammetric behavior of the ITO/TiO2 electrode under ultraviolet (UV) illumination was investigated in the solution of Na2SO4.There are two photoelectrochemical processes for TiO2 electrode under UV illumination.One is a fast process,which results in the appearance of anodic photocurrent.The anodic photocurrent will appear and disappear with the light on and off.The other is a slow process,which will be responsible for the appearance of an oxidative peak. When the electrode is illuminated under UV light for a long time,a new oxidative peak can be observed.The peak current increases with the increase of UV illumination time.It is assumed that the new peak belongs to the oxidation of Ti^3 ,which formed and accumulated on the electrode surface during the UV illumination.A detailed mechanism is proposed on the base of these two photoelectrochemical processes.It is assumed that the change of hydrophilicity of TiO2 thin film may be related to the slow process while the film irradiated by UV light.