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.     

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.     

荧光探针法研究铜离子-姜黄素体系中1O2的反应机理及在O2·-存在下1O2的测定

以1,3-二苯基异苯并呋喃(1,3-Diphenylisobenzofuran, DPBF)为荧光探针, 研究了姜黄素(Curcumin, CUR)在铜离子催化下产生的单线态氧(1O2), 其反应机理为姜黄素与溶液中的氧分子快速作用产生O2·-和H2O2等活性氧物种, 同时Cu2+与姜黄素形成复合物, 再与H2O2形成过氧化物过渡态, 过氧化物进一步与H2O2发生类Haber-Weiss反应生成1O2, 且只有Cu2+和Cu+离子可催化姜黄素并产生1O2. 1O2在1.37×10-8～3.66×10-7 mol/L浓度范围内与荧光强度下降值ΔIF有良好的线性关系, 检出限为4.12×10-9 mol/L.     

SO2气体对质子交换膜燃料电池阴极性能的影响

将5×10-8~3.2×10-6(空气中的体积含量)的SO2通入质子交换膜燃料电池(PEMFC)单电池阴极, 研究了SO2对PEMFC性能的影响. 实验得到的电压-时间(V-t)曲线和极化(V-I)曲线表明, 空气中SO2含量达到5×10-7时, 将对PEMFC的性能产生显著的和不可逆的影响, 且SO2浓度越大电池性能的下降幅度越大. 对SO2影响前后的电化学交流阻抗谱(EIS)的解析表明, 电池电荷传递阻抗(Rct)的变化可逆, 而阴极的表面状态发生了不完全可逆的变化. 循环伏安(CV)实验数据进一步证明, SO2毒化后阴极的活性电化学表面积(EAS)缩小.     

Cr2O3催化剂上甲烷部分氧化制备合成气

分别采用柠檬酸络合法和直接分解法制备了Cr2O3催化剂, 采用XRD, BET, TPR, XPS, TEM和TGA表征了催化剂的物理化学性质, 在常压固定床石英管(内径5 mm)反应器中考察了Cr2O3催化剂对甲烷部分氧化反应的催化性能. 在500~750 ℃, V(CH4)∶V(O2)=2, 空速12×104 h-1的条件下, O2几乎完全转化, CH4转化率及H2和CO选择性随着温度的升高而增加. 700 ℃下CH4转化率及H2, CO选择性随着空速(6.0×104~24×104 h-1)的升高而增加. 在500 h稳定性实验中, 随着反应时间的延长, CH4转化率及H2, CO选择性缓慢下降, XRD, TEM和BET结果表明, 催化剂的活性下降与烧结和团聚有关, TGA分析表明催化剂具有良好的抗积炭性. 通过CH4脉冲反应, 推测在反应过程中CO, H2, CO2和H2O是直接生成的.     

NH2 + HNCO反应机理的从头计算

在6-311G(d,p)基组水平上, 采用全电子的UMP2和UQCISD(T)方法对自由基NH₂和HNCO反应机理进行了研究, 结果表明, 反应存在如下两条反应通道: NH₂ + HNCO→NH₃ + NCO (1)和NH₂ + HNCO→N₂H₃ + CO (2). 反应(1)是吸氢反应, QCISD(T,full)// MP2(full)/6-311G(d,p) 计算位垒是29.04 kJ/mol. 与实验估计值29.09 kJ/mol一致. 在反应的温度区间(2300～2700 K),传统过渡态理论得出的速率常数值的范～围是1.68×1011～3.29×10¹¹cm³·mol^-1·s^-1, 支持了反应速率常数应小于等于5.0×10¹¹cm³·mol^-1·s^-1的实验结论. 对反应(1), 理论研究还得出反应物分子可通过分子间作用生成氢键复合物(HBC), 其能量相对于反应物降低32.41 kJ/mol. 反应(2)是一个可经过顺式或反式方式进行的分步反应, 在反应分子间第1步生成N—N键, 再经过一个C—N键断裂过渡态生成产物. 反应(2)控速步骤的位垒为92.79 kJ/mol(顺式)或147.43 kJ/mol(反式). 反应(2)位垒高于反应(1).     

298.16 K时Na+, Mg2+//Cl-, SO42-, NO3-, H2O体系中NaCl饱和区域相平衡

采用等温溶解平衡法研究了五元体系Na+, Mg2+//Cl-, SO42-, NO3-, H2O在298.16 K下氯化钠饱和平衡体系的溶解度, 获得了相应的投影干盐图、氯图和水图. 研究结果表明, 在298.16 K下氯化钠饱和时, 该五元体系投影干盐图由8个二盐共饱和的双变面、13条三盐共饱的单变线和6个四盐共饱的零变点构成, 存在两种复盐, 8个二盐共饱双变面分别对应于NaCl+NaNO3, NaCl+Na2SO4, NaCl+MgCl2·6H2O, NaCl+MgSO4·Na2SO4·4H2O, NaCl+Mg(NO3)2·6H2O, NaCl+NaNO3·Na2SO4·2H2O, NaCl+MgSO4·7H2O 和NaCl+MgSO4·(1—6)H2O. 讨论了该相图在新疆硝酸盐矿开发利用过程中的应用.     

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.     

NO2和HSO反应的机理及动力学研究

本文采用CCSD(T)/aug-cc-pVTZ//B3LYP/aug-cc-pVTZ方法构建了NO2 + HSO反应的单、三重态势能面,并对主通道速率常数进行了计算。研究结果表明,该反应在单[R1(HN(O)O + 1SO)、R2(cis-HONO + 1SO)和R3 (trans-HONO + 1SO)]、三重态[R6(HN(O)O + 3SO)、R7(cis-HONO + 3SO)和R8(trans-HONO + 3SO)]均存在3条抽氢反应通道,在单[R4(NO + HS(O)O)和R5(H + SO2 + NO)]、三重态[R9(HS(O)O + NO)和R10(H + SO2 + NO)]均存在两条抽氧通道,其中单重态抽氢通道R2 (cis-HONO + 1SO)是NO2 + HSO反应主通道。利用传统过渡态理论(TST)并结合Wigner校正,计算了上述10条通道在200 ~ 1000 K温度范围内的速率常数。计算结果表明,NO2 + HSO反应主通道在298 K时的速率常数(7.78×10-13cm3?molecule-1?s-1)与实验值(9.6×10-12 cm3?molecule-1?s-1)相吻合。此外,水分子影响主通道R2(cis-HONO + 1SO)经历了NO2 + H2O…HSO和 NO2 + H2O…HSO(HSO + NO2…H2O)两条反应通道,且两条通道的能垒分别比R2升高了49.97和20.43 kcal?mol-1,说明在实际大气环境中水分子对NO2 + HSO反应几乎没有影响。     

α-Fe_2O_3空心球的水热法制备及其对苯酚的吸附性能

以铁氰化钾、磷酸二氢铵等为反应物,采用水热法合成了α-Fe2O3空心球,并用XRD,TEM,FESEM(场发射扫描电镜)、UV-Vis和低温氮吸附脱附对其进行了表征。结果表明,α-Fe2O3空心球直径在200～560nm之间,其BET比表面积为80m2·g-1,平均孔径为8.5nm。考察了反应时间、反应物用量和反应温度等对α-Fe2O3空心球形貌和大小的影响,提出了其可能的形成机理。研究了室温下α-Fe2O3空心球吸附苯酚的性能,吸附达平衡时,其吸附苯酚的量达97mg·g-1。     

Synergistic reaction between SO2 and NO2 on mineral oxides: a potential formation pathway of sulfate aerosol

Sulfate is one of the most important aerosols in the atmosphere. A new sulfate formation pathway via synergistic reactions between SO(2) and NO(2) on mineral oxides was proposed. The heterogeneous reactions of SO(2) and NO(2) on CaO, α-Fe(2)O(3), ZnO, MgO, α-Al(2)O(3), TiO(2), and SiO(2) were investigated by in situ Diffuse Reflectance Infrared Fourier Transform Spectroscopy (in situ DRIFTS) at ambient temperature. Formation of sulfate from adsorbed SO(2) was promoted by the coexisting NO(2), while surface N(2)O(4) was observed as the crucial oxidant for the oxidation of surface sulfite. This process was significantly promoted by the presence of O(2). The synergistic effect between SO(2) and NO(2) was not observed on other mineral particles (such as CaCO(3) and CaSO(4)) probably due to the lack of the surface reactive oxygen sites. The synergistic reaction between SO(2) and NO(2) on mineral oxides resulted in the formation of internal mixtures of sulfate, nitrate, and mineral oxides. The change of mixture state will affect the physicochemical properties of atmospheric particles and therefore further influence their environmental and climate effects.     

Heterogeneous reactions of sulfur dioxide on typical mineral particles

The heterogeneous reaction of SO2 on Al2O3, CaO, TiO2, MgO, FeOOH, Fe2O3, MnO2, and SiO2, as well as authentic aerosol sample, was investigated by using a White Cell coupled with in situ-FTIR and Diffuse Reflectance Infrared Fourier Transform Spectroscopy (DRIFTS). Simultaneous observations of reactants and products were performed to obtain full information on the mechanism and kinetics of the reactions. SO2 was irreversibly adsorbed to form surface sulfite (SO3(2-)), bisulfite (HSO3(-)), and sulfate (SO4(2-)). The reactivity order of these particles is the following: FeOOH >Al2O3 > mixture > MgO > Fe2O3 > SiO2. Field-collected aerosol showed significant activity for the oxidation of SO2. The uptake coefficient of SO2 on Al2O3 with different acidity varied in the order of basic Al2O3 > neutral Al2O3 > acidic Al2O3. The surface-active oxygen and hydroxyl might be the key factors for the conversion of SO2 to SO4(2-). The faster reaction rate could be achieved with greater surface area on particles with the same mass. On the basis of the same surface area Fe2O3 could be most reactive in the reaction with SO2 compared with all other particles. The apparent rate constants were determined to be 1.35 x 10(-2) and 9.4 x 10(-3) for uptake on Al2O3 and MgO, respectively, which are the same as the results of other scientists.     

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.     

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.     

A new approach to studying aqueous reactions using diffuse reflectance infrared Fourier transform spectrometry: application to the uptake and oxidation of SO2 on OH-processed model sea salt aerosol

Diffuse reflectance infrared Fourier transform spectrometry (DRIFTS) is a powerful technique for analyzing solid powders and for following their reactions in real time. We demonstrate that it can also be applied to studying the uptake and reactions of gases in liquid films. Within the DRIFTS cell, a 10%(w/w) mixture of MgCl(2) x 6H(2)O in NaCl was equilibrated with air at 50% RH, which is above the deliquescence point of the magnesium salt but below that of NaCl. This mixture of NaCl coated with an aqueous magnesium chloride solution was then reacted with gas phase OH to generate hydroxide ions via a previously identified interface reaction. This treatment, hereafter referred to as OH-processing, was sufficient to convert some of the magnesium chloride to Mg(OH)(2) and Mg(2)(OH)(3)Cl x 4H(2)O, making the aqueous film basic and providing a reservoir of alkalinity. Subsequent addition of SO(2) to the basic processed mixture resulted in its uptake and conversion to sulfite which was measured by FTIR. The sulfite was simultaneously oxidized to sulfate by HOCl/OCl(-) that was formed in the initial OH-processing of the salt. Further uptake and oxidation of SO(2) in the aqueous film took place when the salt was subsequently exposed to O(3). These studies demonstrate that DRIFTS can be used to study the chemistry in liquid films in real time, and are consistent with the hypothesis that the reaction of gaseous OH with chloride ions generates alkalinity that enhances the uptake and oxidation of SO(2) under these laboratory conditions.     

Model of uptake of OH radicals on nonreactive solids

A model of adsorption and recombination of OH radicals was developed for nonreactive solid surfaces of atmospheric interest. A parametrization of this heterogeneous mechanism was carried out to determine the role of the catalytic properties of these solid surfaces, taking into account the adsorption energy, defects, surface diffusion, and chemical reactions in the gas-solid interface. The uptake process was simulated for diffusion-controlled chemical reactions on the surface on the basis of Langmuir-Hinshelwood and Eley-Rideal mechanisms. Using an analytical approach and the Monte Carlo technique, we show the dependencies of the uptake probability of the heterogeneous reactions on the OH concentration and adsorption energy. The model is employed in the analysis of the empirically derived uptake coefficient for water ice, Al(2)O(3), NaCl, NH(4)NO(3), NH(4)HSO(4), and (NH(4))(2)SO(4). We found the following values for the free energy of adsorption of OH radicals: E(ice) = 7.3-7.6 kcal/mol, E(Al)(2)(O)(3) = 11-11.7 kcal/mol, E(NH)(4)(NO)(3) = 10.2 kcal/mol, E(NaCl) = 10.2 kcal/mol, E(NH)(4)(HSO)(4) = 9.8 kcal/mol, and E((NH)(4))(2)(SO)(4) = 9.8 kcal/mol. The atmospheric implications of the catalytic reactions of OH with adsorbed reactive molecules are discussed. The results of the modeling of the uptake process showed that the heterogeneous decay rate can exceed the corresponding gas-phase reaction rate under atmospheric conditions.     

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.     

Synergistic effect between NO2 and SO2 in their adsorption and reaction on gamma-alumina

Field measurements showed that there exists a correlation between nitrate and sulfate on mineral dust. In this work, the synergistic mechanism of adsorption and reaction between SO2 and NO2 on gamma-alumina was studied using in situ diffusion reflectance infrared Fourier spectroscopy (in situ DRIFTS) and temperature programmed desorption (TPD). The results revealed that the reaction pathway of NO2 adsorbed on alumina was altered in the presence of SO2. In the absence of SO2, nitrite was found to be an intermediate in the oxidation of NO2 to surface nitrate species. However, in the presence of SO2, the formation of nitrite was inhibited and a new intermediate, dinitrogen tetraoxide (N2O4), was observed. On the other hand, surface tetravalent sulfur species S(IV), including bisulfite and sulfite, were oxidized to sulfate in air condition when NO2 was present. The atmospheric implication of this synergistic effect was also discussed.     

Heterogeneous reactions of sulfur dioxide on dust

In urban atmospheric environment, SO2 is the prin- cipal sulfur-containing anthropogenic pollutant, with concentrations reaching into hundreds of parts per bil- lion[1]. Atmospheric SO2 can be adsorbed and oxidized to sulfate on the surface of particles and subsequently involved in the formation of secondary inorganic aerosol in the atmosphere[2―4]. Sulfate particles are known to affect climate by scattering solar radiation, resulting in a net cooling effect, as well as acting as cloud conde…