模拟太阳光-过氧化氢作用下冰相中苯酚的光转化

以模拟太阳光为照射光源,对冰相中苯酚在过氧化氢(H2O2)存在条件下的光转化反应进行了研究,考察了影响苯酚光转化反应的主要因素并探讨了光转化动力学过程.研究结果表明,光强度越高或H2O2初始浓度越大,苯酚在冰相介质中的光转化率越快,而苯酚初始浓度越高则会导致苯酚的光转化率减慢.p H值对苯酚的光转化率的影响则表现为酸性导致减小,碱性导致加快.应用气相色谱-质谱联用仪(GC-MS)分析了苯酚的光解产物,推断苯酚在冰相中的光解过程中主要发生了羟基化反应.     

NO2-存在条件下冰相中对氯苯酚的光转化

以125 W高压汞灯为光源, 在低温(-12—-14 ℃)条件下研究了冰相中有亚硝酸盐存在时对氯苯酚(4-CP)的光转化反应. 考察了各种因素对冰相中4-CP光转化的影响以及冰相中4-CP光转化的动力学和机理. 实验结果表明, 4-CP初始浓度、亚硝酸盐初始浓度、pH值和光强对冰相中4-CP光转化均有较大影响. 在180 min内, 4-CP和总有机碳(TOC)的转化率分别达到80%和32%, 在实验条件下, NO2-的存在能够改变4-CP在冰相中光转化的产物和机理.     

光-Fe3+-草酸体系中对氯苯酚的冰相光转化

本文利用室内低温反应装置研究了在模拟太阳光-Fe3+-草酸作用下冰相中对氯苯酚（4-CP）的光转化。结果表明,Fe3+-草酸存在条件对冰相中4-CP的光转化有促进作用。Fe3+和草酸初始浓度、Fe3+与草酸的初始浓度比以及初始pH值对体系中4-CP的转化率具有较大影响。当溶液初始pH值为6.50,Fe3+和草酸的初始浓度比是1/5,草酸初始浓度为0.80mmol/L时,4-CP光照7.5h转化率可达39.1%。在光转化过程中,TOC的转化率滞后于4-CP的光转化率。4-CP的光转化符合一级动力学模型。分别利用直接萃取法和衍生化法富集了反应中间产物,并采用GC-MS进行了分析,据此推断了冰相中模拟太阳光-Fe3+-草酸作用下4-CP光转化的反应机理。     

NO-2存在条件下冰相中对氯苯酚光转化机理

以125 W高压汞灯为光源,在低温(-14～-12 ℃)条件下,研究了紫外光作用下,冰相中有亚硝酸盐存在时,0.8 mmol/L对氯苯酚(4-CP)的光转化反应. 结果表明,在180 min内,4-CP的转化率达到80%. 在此实验条件下,得到的主要产物为5-氯联苯-2,4'-二醇、苯酚、4-(4-氯-2-硝基苯氧)酚和4-氯-2-硝基酚. 由此推断,NO-2的存在能够改变4-CP在冰相中光转化的产物和机理.     

六氯苯在水相、冰相和有机相中的光化学转化

以低压汞灯为光源研究了六氯苯(HCB)在水相、 冰相和有机溶剂中光转化的动力学过程, 分析了反应产物, 探讨了反应机理, 考察了H₂O₂, NO₂^-, Fe²⁺对水相/冰相中HCB光转化的影响. 结果表明, 在低压汞灯照射下, HCB在3个体系中的光转化速率大小为有机相>水相>冰相; H₂O₂ 促进水相中HCB的光转化而抑制冰相中HCB的光转化; NO₂^-对HCB在水相/冰相中的光化学转化均起抑制作用; Fe²⁺对水相中HCB的光转化有促进作用, 而对其在冰相中的光转化无影响; 六氯苯在3个体系中光转化的机理均为逐级脱氯过程.     

腐植酸作用下γ-六氯环己烷在冰相中的光转化

研究了腐植酸(HA)存在下冰相体系中γ-六氯环己烷(γ-HCH)的光转化规律.结果表明,HA浓度对γ-HCH的光转化率呈现低浓度促进而高浓度抑制的现象;盐离子浓度、NO_2~-及NO_3~-对γ-HCH的光转化率均有促进作用;低浓度Fe~(3+)对γ-HCH的光转化率有促进作用,当Fe~(3+)的浓度增大到50μmol/L时,呈现抑制效应;γ-HCH在不同p H值条件下光转化速率的大小顺序为碱性中性酸性.冰相中HA通过产生单线态氧(~1O_2)、羟基自由基(·OH)及三重激发态(HA*)加速γ-HCH的光转化.HA存在下γ-HCH的光转化产物主要是五氯环己烯、邻二氯苯和对二氯苯、一氯苯,光转化过程中~1O_2通过消耗中间产物间接加速了γ-HCH的光转化过程.     

苯酚在含氯体系中的电化学氧化

以Ru-Ir/Ti三元电极作阳极电解处理苯酚废水,研究废水中Cl-初始浓度对处理效果的影响.结果表明,在一定的电解时间内,苯酚的电化学氧化符合一级动力学方程;废水中Cl-的初始浓度越大,苯酚完全被氧化所需的时间也越短,即其表观速率常数越大.苯酚在Cl-体系中降解的中间产物主要有4-氯苯酚,1-氯苯酚,2,4-二氯苯酚,2,6二氯苯酚,2,4,6-三氯苯酚及各种短链脂肪酸和氯代醇等;最终产物是CO2、CHCl2和CHCl3.电解中间体的生成和降解速率随废水中Cl-初始浓度的增加而增大.据此,导出苯酚在含Cl-体系中电化学氧化的反应途径.     

离子液体内耦合液膜迁移苯酚的研究

本文以N-甲基咪唑为原料,采用微波合成法,制备了疏水性离子液体1-丁基-3-甲基咪唑六氟磷酸盐([BMIM]PF6),并将其作为液膜,对苯酚的内耦合液膜迁移进行了研究,考察了温度、搅拌速度、料液相酸度、初始浓度及解析相NaOH浓度等因素对苯酚迁移的影响,得出了最佳迁移条件:温度300 K,搅拌速度350 r/min,料液相pH为3.65,解析相NaOH浓度为0.8 mol/L.在最佳液膜条件下,对于10 mg/L苯酚溶液,迁移110 min,迁移率可以达到97.3%,膜相中有少量苯酚滞留.离子液体可循环使用.     

硝酸分解磷矿的宏观动力学研究

在间歇反应器中 ,反应温度为 30～ 6 0℃ ,硝酸初始浓度 30～ 5 4 % ,磷矿初始粒径 0 .375～ 1.0 75毫米 ,搅拌强度 4 0 0转 分的条件下研究了硝酸分解磷矿的反应过程机理及宏观动力学。结果表明 ,磷矿分解速率及转化率随着搅拌强度、反应温度、硝酸浓度和颗粒细度的增加而增加 ;氢离子通过液膜的扩散传质是该过程的速率控制步骤。应用固体粒径减小的缩芯模型 ,将上述各影响因素的实验数据回归得到如下的宏观动力学模型 :1- (1-xB) 2 3=8.36 6exp - 6 .198× 10 3RT c1 .31 1AO R- 0 .1 0 91S lnτ活化能Ea=6 .198kJ mol,属液膜扩散传质控制     

利用TiO2/SO42-光触媒催化还原CO2之参数影响与反应路径探讨

将改良式溶胶-凝胶法制备的酸性触媒TiO2/SO24-涂布于不锈钢网上,并利用自行设计之批次式光催化反应器,在三组近紫外灯管(波长为365nm,光强度为2.0mW/cm2)照射下,进行CO2光催化还原反应操作参数(还原剂种类、CO2初始浓度和反应温度)之影响研究.结果显示,使用氢气为还原剂可获得最高的光催化还原速率,光还原反应之主要气态产物为CO和甲烷,其次为微量的乙烯与乙烷.同时,光催化还原速率亦随着CO2初始浓度及反应温度的提高而增加.FT-IR光谱分析发现,TiO2/SO42-光触媒表面有甲酸、甲醇、碳酸盐、甲酸盐及甲酸甲酯等产物之存在.TiO2/SO42-光触媒催化还原CO2有两种可能反应路径,其中一种反应路径生成CO,CH4,C2H4及C2H6等气态产物;而另一种反应路径则生成CO23a-ds,CH3OHads,HCOOa-ds,HCOOHads,HCOHads与HCOOCH3ads等吸附在光触媒表面的产物.     

Photoinduced release of nitroxyl and nitric oxide from diazeniumdiolates

Aqueous photochemistry of diazen-1-ium-1,2,2-triolate (Angeli's anion) and (Z)-1[N-(3-aminopropyl)-N-(3-aminopropyl)amino]diazen-1-ium-1,2-diolate (DPTA NONOate) has been investigated by laser kinetic spectroscopy. In neutral aqueous solutions, 266 nm photolysis of these diazeniumdiolates generates a unique spectrum of primary products including the ground-state triplet (3NO-) and singlet (1HNO) nitroxyl species and nitric oxide (NO*). Formation of these spectrophotometrically invisible products is revealed and quantitatively assayed by analyzing a complex set of their cross-reactions leading to the formation of colored intermediates, the N2O2*- radical and N3O3- anion. The experimental design employed takes advantage of the extremely slow spin-forbidden protic equilibration between 3NO- and 1HNO and the vast difference in their reactivity toward NO*. To account for the kinetic data, a novel combination reaction, 3NO-+1HNO, is introduced, and its rate constant of 6.6x10(9) M-1 s-1 is measured by competition with the reduction of methyl viologen by 3NO-. The latter reaction occurring with 2.1x10(9) M-1 s-1 rate constant and leading to the stable, colored methyl viologen radical cation is useful for detection of 3NO-. The distributions of the primary photolysis products (Angeli's anion: 22% 3NO-, 58% 1HNO, and 20% NO*; DPTA NONOate: 3% 3NO-, 12% 1HNO, and 85% NO*) show that neither diazeniumdiolate is a highly selective photochemical generator of nitroxyl species or nitric oxide, although the selectivity of DPTA NONOate for NO* generation is clearly greater.     

Ice photolysis of 2,2′,4,4′,6-pentabromodiphenyl ether (BDE-100): Laboratory investigations using solid phase microextraction

Here, we report for the first time a laboratory investigation into the photochemical degradation of 2,2′,4,4′,6-pentabromodiphenyl ether (BDE-100) in ice solid samples using an artificial UV light source. Solid phase microextraction (SPME) was used as a sensitive extraction technique for monitoring trace amounts of the hydrophobic pollutant and its photoproducts. The results showed that ice photolysis kinetics for BDE-100 is similar to the one observed in the aqueous counterpart. The eight photoproducts identified consisted of brominated diphenyl ethers with lower bromine content and polybrominated dibenzofurans, suggesting two important photodegradation pathways for BDE-100 in ice solid samples: (i) stepwise reductive debromination and (ii) intramolecular elimination of HBr. Similarities in photochemical product arrays observed in the ice and water photolysis of BDE-100 were attributed to a similar mechanism for photochemical decomposition for both phases. Possible involvement of the water molecules in the reactions has been excluded by performing photolysis in D₂O ice solid and water samples. Taking advantage of the high preconcentration factor obtained with SPME at low temperatures, a SPME fiber cooled with liquid carbon dioxide down to 0 °C was used as a photoreaction support for BDE-100 allowing the identification of a greater number of photoproducts.     

The primary photodynamics of aqueous nitrate: formation of peroxynitrite

We have examined the photochemical reactions occurring after irradiation at 200 nm of the aqueous nitrate ion, NO3(-)(aq). Using femtosecond transient absorption spectroscopy over the range 194-388 nm, we have characterized the formation and subsequent relaxation of the primary photoproducts of nitrate photolysis. The dominant photoproduct is the cis-isomer of peroxynitrite, which accounts for 48% of the excited state molecules initially produced. A slightly smaller fraction, 44%, of the excited molecules return to the electronic ground state of NO3(-) and relax to the vibrational ground state in 2 ps. The remaining 8% of the molecules initially excited react via the *NO + *O2(-) or the NO- + O2 dissociation channels. Formation of NO2(-) and *NO2 is not observed, suggesting that the previous observations of these species in steady-state photolysis are caused by reactions occurring on a longer time scale.     

Absorption spectra and photolysis of methyl peroxide in liquid and frozen water

Methyl peroxide (CH(3)OOH) is commonly found in atmospheric waters and ices in significant concentrations. It is the simplest organic peroxide and an important precursor to hydroxyl radical. Many studies have examined the photochemical behavior of gaseous CH(3)OOH; however, the photochemistry of liquid and frozen water solutions is poorly understood. We present a series of experiments and theoretical calculations designed to elucidate the photochemical behavior of CH(3)OOH dissolved in liquid water and ice over a range of temperatures. The molar extinction coefficients of aqueous CH(3)OOH are different from the gas phase, and they do not change upon freezing. Between -12 and 43 °C, the quantum yield of CH(3)OOH photolysis is described by the following equation: Φ(T) = exp((-2175 ± 448)1/T) + 7.66 ± 1.56). We use on-the-fly ab initio molecular dynamics simulations to model structures and absorption spectra of a bare CH(3)OOH molecule and a CH(3)OOH molecule immersed inside 20 water molecules at 50, 200, and 220 K. The simulations predict large sensitivity in the absorption spectrum of CH(3)OOH to temperature, with the spectrum narrowing and shifting to the blue under cryogenic conditions because of constrained dihedral motion around the O-O bond. The shift in the absorption spectrum is not observed in the experiment when the CH(3)OOH solution is frozen suggesting that CH(3)OOH remains in a liquid layer between the ice grains. Using the extinction coefficients and photolysis quantum yields obtained in this work, we show that under conditions with low temperatures, in the presence of clouds with a high liquid-water content and large solar zenith angles, the loss of CH(3)OOH by aqueous photolysis is responsible for up to 20% of the total loss of CH(3)OOH due to photolysis. Gas phase photolysis of CH(3)OOH dominates under all other conditions.     

Formation of hydroxyl radical from the photolysis of frozen hydrogen peroxide

Hydrogen peroxide (HOOH) in ice and snow is an important chemical tracer for the oxidative capacities of past atmospheres. However, photolysis in ice and snow will destroy HOOH and form the hydroxyl radical (*OH), which can react with snowpack trace species. Reactions of *OH in snow and ice will affect the composition of both the overlying atmosphere (e.g., by the release of volatile species such as formaldehyde to the boundary layer) and the snow and ice (e.g., by the *OH-mediated destruction of trace organics). To help understand these impacts, we have measured the quantum yield of *OH from the photolysis of HOOH on ice. Our measured quantum yields (Phi(HOOH --> *OH)) are independent of ionic strength, pH, and wavelength, but are dependent upon temperature. This temperature dependence for both solution and ice data is best described by the relationship ln(Phi(HOOH --> *OH)) = -(684 +/- 17)(1/T) + (2.27 +/- 0.064) (where errors represent 1 standard error). The corresponding activation energy (Ea) for HOOH (5.7 kJ mol(-1)) is much smaller than that for nitrate photolysis, indicating that the photochemistry of HOOH is less affected by changes in temperature. Using our measured quantum yields, we calculate that the photolytic lifetimes of HOOH in surface snow grains under midday, summer solstice sunlight are approximately 140 h at representative sites on the Greenland and Antarctic ice sheets. In addition, our calculations reveal that the majority of *OH radicals formed on polar snow grains are from HOOH photolysis, while nitrate photolysis is only a minor contributor. Similarly, HOOH appears to be much more important than nitrate as a photochemical source of *OH on cirrus ice clouds, where reactions of the photochemically formed hydroxyl radical could lead to the release of oxygenated volatile organic compounds to the upper troposphere.     

Parahalogenated phenols accelerate the photochemical release of nitrogen oxides from frozen solutions containing nitrate

The photolysis of nitrate anion (NO(3)(-)) contained in surface ice and snow can be a regionally significant source of gas-phase nitrogen oxides and affect the composition of the planetary boundary layer. In this study, the photochemical release of nitrogen oxides from frozen solutions containing NO(3)(-) in the presence of organic compounds was investigated. Gas-phase nitrogen oxides were quantified primarily by NO-O(3) chemiluminescence detection of NO and NO(y) (=NO + NO(2) + HONO + HNO(3) + ∑PAN + ∑AN ...) and cavity ring-down spectroscopy of NO(2) and total alkyl nitrates (∑AN). The photochemical production of gas-phase NO(y) was suppressed by the presence of formate, methanesulfonate, toluene, or phenol. In contrast, para-halogenated phenols (in the order of Cl > Br > F) promoted the conversion of NO(3)(-) to gas-phase NO(y), rationalized by acidification of the ice surface.     

Determination of the photochemical efficiency of o-quinodimethane ring closure in room-temperature solutions by using time-delayed, two-color photolysis technique

Photochemical efficiency of o-quinodimethane (3) ring closure at room temperature was determined by using a time-delayed, two-color photolysis technique. o-Quinodimethane (3) was generated by the photolysis of 1,2-bis[(phenylseleno)methyl]benzene (1) by a KrF (248 nm) laser pulse and thus-generated 3 was photolyzed by a subsequent XeCl (308 nm)/XeF (351 nm) laser pulse with varying delay time of 0 to 3 s. The time profile of 3 was monitored by the chemical analyses of benzocyclobutene (5) (a photochemical product of 3), which was formed by a one-photon process, and the spiro dimer of 3 (4) (a thermal product of 3) in the two-color photolysis experiments. The time profile of 3 followed a second-order decay kinetics. The photochemical efficiency was obtained by the analysis of the delay-time dependence of the product yields; those of the consumption of 3 and the conversion 3-->5 by a single pulse of the excimer laser were 81% and 5.7% for the XeCl laser, and 73% and 2.3% for the XeF laser. This difference was attributed to the different excited states involved in the photolysis. In contrast to the photolysis of 3 in argon or rigid organic matrixes, it was revealed that photochemical conversion 3-->5 was not the main path in the solutions, and intermolecular reactions predominated.     

Nitrate radical quantum yield from peroxyacetyl nitrate photolysis

Peroxyacetyl nitrate (PAN, CH3C(O)OONO2) is a ubiquitous pollutant that is primarily destroyed by either thermal or photochemical mechanisms. We have investigated the photochemical destruction of PAN using a combination of laser pulsed photolysis and cavity ring-down spectroscopic detection of the NO3 photoproduct. We find that the nitrate radical quantum yield from the 289 nm photolysis of PAN is Phi(NO3)PAN = 0.31 +/- 0.08 (+/-2 sigma). The quantum yield is determined relative to that of dinitrogen pentoxide, which is assumed to be unity, under identical experimental conditions. The instrument design and experimental procedure are discussed as well as auxiliary experiments performed to further characterize the performance of the optical cavity and photolysis system.     

Photolysis of 2,6-dimethyl-3,5-dicarboethoxy- 1,4-dihydropyridine-4-carboxylic acid

The photolysis of 2,6-dimethyl-3,5-dicarboethoxy-1,4-dihydropyridine-4-carboxylic acid 1 gives with a pyrex filter pyridine 2 and glycol 3. At low concentration, aldehyde 4 accumulates. The photochemical dimerization of this aldehyde gives glycol 3 in methanol or ethanol. The aldehydic hydrogen in aldehyde 4 is replaced by deuterium on performing the photolysis of acid 1 in MeOD as is the case for the photolysis of 2,6-dimethyl-3,5-diacetyl-1,4-dihydropyridine. A concerted mechanism for the decarboxylation of acid 1 to aldehyde 4 is possible. When the photolysis of 1 is performed in quartz, another reaction occurs leading to 1,2-dihydropyridine 8.     

Photolysis of polycyclic aromatic hydrocarbons on water and ice surfaces

Laser-induced fluorescence detection was used to measure photolysis rates of anthracene and naphthalene at the air-ice interface, and the kinetics were compared to those observed in water solution and at the air-water interface. Direct photolysis proceeds much more quickly at the air-ice interface than at the air-water interface, whereas indirect photolysis due to the presence of nitrate or hydrogen peroxide appears to be suppressed at the ice surface with respect to the liquid water surface. Both naphthalene and anthracene self-associate readily on the ice surface, but not on the water surface. The increase in photolysis rates observed on ice surfaces is not due to this self-association, however. The wavelength dependence of the photolysis indicates that it is due to absorption by the PAH. No dependence of the rate on temperature is seen, either at the liquid water surface or at the ice surface. Molecular oxygen appears to play a complex role in the photolytic loss mechanism, increasing or decreasing the photolysis rate depending on its concentration.