3-甲基-3-丁烯基-1-醇与硫酸/过氧化氢混合溶液的吸收反应研究

应用配置有湿式流动反应管的真空紫外激光单光子电离飞行时间质谱研究了3-甲基-3-丁烯基-1-醇气体在硫酸/过氧化氢混合溶液表面的吸收反应,实验中首次测得了反应的摄取系数,并根据气相产物信息推测了其反应机制.3-甲基-3-丁烯基-1-醇与硫酸/过氧化氢混合溶液的吸收反应速率很快,在ω（H2SO4）为40%～60%范围,摄取系数为2.52×10-4～1.05×10-2.在反应过程的气相收集物中检测出3种气相产物：乙醛、丙酮和3-甲基-3,4-环氧-1-丁醇,由此推测了3-甲基-3-丁烯基-1-醇与H2 SO4/H2 O2混合溶液的非均相反应机制.3-甲基-3,4-环氧-1-丁醇可以经过多步转化形成多羟基化合物,同时生成的醛酮化合物在酸性溶液中可进一步反应,这些对大气二次有机气溶胶的形成起着重要作用.因此,3-甲基-3-丁烯基-1-醇的非均相催化氧化过程可能对二次有机气溶胶的形成有重要贡献.     

Chemical composition and size distribution of secondary organic aerosol formed from the photooxidation of isoprene

Photooxidation of isoprene leads to the formation of secondary organic aerosol (SOA). In this study, the chemical composition of SOA formed from OH-initiated photooxidation of isoprene has been investigated with gas chromatography/mass spectrometry (GC/MS) and a home-made aerosol time-of-flight mass spectrometer. Sampling particles generated in a home-made smog chamber. The size distribution of SOA particles was detected by a TSI 3321 aerodynamic particle size spectrometer in real time. Results showed that SOA created by isoprene photooxidation was predominantly in the form of fine particles, which have diameters less than 2.5 m. The obtained mass spectra of individual particles show that products of the OH-initiated oxidation of isoprene contain methyl vinyl ketone, methacrolein, formaldehyde, and some other hydroxycarbonyls. The possible reaction mechanisms leading to these products were also discussed.     

泰山夏季PM2.5中生物源SOA的分子组成及影响因素

为探究泰山夏季PM_2.5中生物源二次有机气溶胶(BSOA)的分子组成、昼夜变化特征、及影响因素,于2016年7-8月在泰山山顶进行PM_2.5样品采集,并对碳质组分、无机离子和BSOA示踪物进行分析.结果表明,元素碳(EC)和左旋葡聚糖质量浓度处于较低水平且昼夜差异较小(t检验,P<0.05),表明采样期间泰山山顶气溶胶受人为污染排放的影响较小.BSOA示踪物的总质量浓度呈昼高夜低的变化特征,表明白天较强的温度和太阳辐射使得气溶胶的氧化程度比夜间强.其中,异戊二烯类SOA示踪物的质量浓度最高达(77.64±51.79)ng/m³,其次为单萜烯类和倍半萜烯类SOA示踪物,分别为(33.68±21.29)和(6 97±3 28)ng/m³.基于示踪物-产率法估算得出SOC_异戊二烯对有机碳(OC)的贡献率(15.3%)最高.由BSOA示踪物与RH(R≤-0.45)和pHi_s(R≤-0.53)的负相关性可知,高湿条件可以降低气溶胶的酸度进而抑制BSOA通过酸催...     

双氧化剂光催化降解水中邻苯二甲酸酯类污染物

采用过硫酸钠/双氧水双氧化体系光催化氧化降解水中邻苯二甲酸酯类有机污染物,考察了过硫酸钠/双氧水的投加比例、紫外光强、溶液pH以及邻苯二甲酸二辛酯(DOP)的初始浓度等因素对降解率的影响,并在优化条件下对降解反应的动力学进行了考察。结果表明:室温下,过硫酸钠和双氧水浓度均为0.2mol/L且体积比为1:1,pH=7.0,光照距离为0.5cm,反应80min,DOP降解率达98%以上,反应动力学研究表明,过硫酸钠/双氧水双氧化体系光催化氧化降解水中DOP反应为表观一级。优于相同条件下两种氧化剂单独使用对DOP的降解效果。     

异戊二烯和甲苯二次有机示踪物的臭氧非均相氧化

本文基于相对速率法,通过烟雾箱实验测定了异戊二烯和甲苯二次有机示踪物的臭氧非均相氧化的有效速率常数,考察了不同条件(相对湿度和混合状态等)对示踪物臭氧非均相氧化过程的影响,并且分析了由于示踪物被氧化所引起的二次源解析的不确定性.结果表明,赤藓糖醇(analogue of 2-methyl erythritol,AME)和2,3-二羟基-4-氧代戊酸(2,3-dihydroxy-4-oxopentanoic acid,DHOPA)的有效速率常数分别为(4. 60±0. 66)×10-19cm~3·(molecule·s)~(-1)和(6. 57±0. 51)×10-19cm~3·(molecule·s)~(-1);考虑到示踪物不稳定引起的不确定性,采用示踪物产率法解析二次源会对异戊二烯和甲苯二次生成气溶胶低估约16. 5%～44. 8%和18. 3%～47. 3%.     

A clean production process of sodium chlorite from sodium chlorate

This paper presents a novel cleaner production process for producing sodium chlorite by reducing sodium chlorate with hydrogen peroxide. In the new process, chlorine dioxide is generated by reducing chlorate ions with hydrogen peroxide in the presence of sulfuric acid: it then reacts with aqueous sodium hydroxide solution and hydrogen peroxide to produce sodium chlorite. The reaction conditions that were experimentally investigated included: reaction temperatures, concentrations of sodium chlorate solution, molar ratio of NaClO₃:H₂SO₄:H₂O₂, and acidity. Waste acid in the chlorine dioxide generator is dramatically reduced with recycling in the new process. The by-produced sodium sulfate in sulfuric acid is minimized and reclaimed.     

A VUV photoionization mass spectrometric study on the OH-initiated photooxidation of isoprene with synchrotron radiation

The gas-phase organic compounds resulting from OH-initiated photooxidation of isoprene have been investigated on-line by VUV photoionization mass spectrometry based on synchrotron radiation for the first time. The photoionization efficiency curves of the corresponding gaseous products as well as the chosen standards have been deduced by gating the interested peaks in the photoionization mass spectra while scanning the photon energy simultaneously, which permits the identification of the pivotal gaseous products of the photooxidation of isoprene, such as formaldehyde (10.84 eV), formic acid (11.38 eV), acetone (9.68 eV), glyoxal (9.84 eV), acetic acid (10.75 eV), methacrolein (9.91 eV), and methyl vinyl ketone (9.66 eV). Proposed reaction mechanisms leading to the formation of these key products were discussed, which were completely consistent with the previous works of different groups. The capability of synchrotron radiation photoionization mass spectrometry to directly identify the chemical composition of the gaseous products in a simulation chamber has been demonstrated, and its potential application in related studies of atmospheric oxidation of ambient volatile organic compounds is anticipated.     

Compilation of reaction kinetics parameters determined in the Key Development Project for Air Pollution Formation Mechanism and Control Technologies in China

A compilation of new advances made in the research field of laboratory reaction kinetics in China's Key Development Project for Air Pollution Formation Mechanism and Control Technologies was presented. These advances are grouped into six broad, interrelated categories, including volatile organic compound (VOC) oxidation, secondary organic aerosol (SOA) formation, new particle formation (NPF) and gas-particle partitioning, ozone chemistry, model parameters, and secondary inorganic aerosol (SIA) formation, highlighting the laboratory work done by Chinese researchers. For smog chamber applications, the current knowledge gained from laboratory studies is reviewed, with emphasis on summarizing the oxidation mechanisms of long-chain alkanes, aromatics, alkenes, aldehydes/ketones in the atmosphere, SOA formation from anthropogenic emission sources, and oxidation of aromatics, isoprene, and limonene, as well as SIA formation. For flow tube applications, atmospheric oxidation mechanisms of toluene and methacrolein, SOA formation from limonene oxidation by ozone, gas-particle partitioning of peroxides, and sulfuric acid-water (H₂SO₄-H₂O) binary nucleation, methanesulfonic acid-water (MSA-H₂O) binary nucleation, and sulfuric acid-ammonia-water (H₂SO₄-NH₃-H₂O) ternary nucleation are discussed.     

Determination of aerosol strong acidity losses due to interactions of collected particles: Results from laboratory and field studies

Existing methods of measuring atmospheric aerosol strong acidity adequately prevent neutralization of fine-particle acidity by removing course alkaline particles and gaseous ammonia from air samples. However, these techniques do not consider particle interactions on the collection medium; therefore, they may still underestimate the actual aerosol acidity. Assessment of acid neutralization due to such interactions is made possible using annular denuder technology in conjuction with a newly designed filter pack. The amount of sulfate-related acidity neutralized by the collected ammonium nitrate (and possibly ammonium chloride and organic acid ammonium salts) is determined. Laboratory data suggest that large fractions of sulfate-related aerosol acidity are neutralized by ammonium nitrate particles during collection on filter media. Field data from the Harvard Acid Aerosol Health Effects Study also suggest that ammonium nitrate and possibly other ammonium salts, such as ammonium chloride, neutralize collected acid aerosols. For low-acid aerosol concentrations, the correction factor is significant; whereas, for high-acid concentrations, correction is negligible.     

Secondary organic aerosol formation and transport

A Lagrangian trajectory model simulating the formation, transport and deposition of secondary organic aerosol is developed and applied to the Los Angeles area, for the air pollution episode of 27–28 August 1987. The predicted secondary organic aerosol on 28 August 1987 represents 15–22% of the measured particulate organic carbon at inland locations in the base case simulations, and 5–8% of that at coastal locations. A maximum secondary organic aerosol concentration of 6.8 μg m⁻³ is predicted for Claremont, CA, during this episode. On a daily average basis at Claremont about 46% of this secondary organic aerosol is predicted to be a result of the oxidation of non-toluene aromatics (xylenes, alkylbenzenes, etc.), 19% from toluene, 16% from biogenic hydrocarbons (α-pinene, ß-pinene, etc.), 15% from alkanes and 4% from alkenes. The major uncertainties in predicting secondary organic aerosol concentrations are the reactive organic gas emissions, the aerosol yields and the partitioning of the condensable gases between the two phases. Doubling the reactive organic gas (ROG) emissions results in an increase of the secondary organic aerosol predicted at Claremont by a factor of 2.3. Predicted secondary organic aerosol levels are less sensitive to changes in secondary organic aerosol deposition and NO_x emissions than to ROG emissions.     

Size distribution and chemical composition of secondary organic aerosol formed from Cl-initiated oxidation of toluene

Secondary organic aerosol (SOA) formed from Cl-initiated oxidation of toluene was investigated in a home-made smog chamber. The size distribution and chemical composition of SOA particles were measured using aerodynamic particle sizer spectrometer and the aerosol laser time-of-flight mass spectrometer (ALTOFMS), respectively. According to a large number of single aerosol diameter and mass spectra, the size distribution and chemical composition of SOA were obtained statistically. Experimental results showed that SOA particles created by Cl-initiated oxidation of toluene is predominantly in the form of fine particles, which have diameters less than 2.5 m (i.e., PM2.5), and glyoxal, benzaldehyde, benzyl alcohol, benzoquinone, benzoic acid, benzyl hydroperoxide and benzyl methyl nitrate are the major products components in the SOA. The possible reaction mechanisms leading to these products are also proposed.     

Reinvestigation of the Henry’s law constant for hydrogen peroxide with temperature and acidity variation

Hydrogen peroxide is not only an important oxidant in itself;it also serves as both sink and temporary reservoir for other important oxidants including HOx(OH and HO2) radicals and O3 in the atmosphere.Its partitioning between gas and aqueous phases in the atmosphere,usually described by its Henry's law constant(KH),significantly influences its role in atmospheric processes.Large discrepancies between the KH values reported in previous work,however,have created uncertainty for atmospheric modelers.Based on our newly developed online instrumentation,we have re-determined the temperature and acidity dependence of KH for hydrogen peroxide at an air pressure of(0.960 ± 0.013) atm(1 atm = 1.01325 × 105 Pa).The results indicated that the temperature dependence of KH for hydrogen peroxide fits to the Van't Hoff equation form,expressed as lnKH = a/T-b,and a =-ΔH/R,where KH is in M/atm(M is mol/L),T is in degrees Kelvin,R is the ideal gas constant,and ΔH is the standard heat of solution.For acidity dependence,results demonstrated that the KH value of hydrogen peroxide appeared to have no obvious dependence on decreasing pH level(from pH 7 to pH 1).Combining the dependence of both temperature and acidity,the obtained a and b were 7024 ± 138 and 11.97 ± 0.48,respectively,ΔH was(58.40 ± 1.15) kJ/(K·mol),and the uncertainties represent σ.Our determined KH values for hydrogen peroxide will therefore be of great use in atmospheric models.     

SO2 oxidation in an entraining cloud model with explicit microphysics

A model of the chemical evolution of the droplets in a hill-cap cloud is presented. The chemistry of individual droplets forming on cloud condensation nuclei of differing size and chemical composition is considered, and the take-up of species from the gas phase by the droplets is treated explicity for the droplet population. Oxidation of S(IV) dissolved in cloud droplets is assumed to be dominated by hydrogen peroxide and ozone.Hydrogen peroxide is normally found to be the dominant oxidant for the oxidation of sulphur dioxide (except in the presence of substantial concentrations of ammonia gas, which increases droplet pH and the contribution made by the oxidant ozone). The entrainment of hydrogen peroxide from above the cloud top increases the amount of sulphate produced in conditions where the reaction is otherwise oxidant limited by the availability hydrogen peroxide. These conditions occur when there are high concentrations of sulphur dioxide accompanied by low cloudwater pH values.Within droplets formed on sodium chloride aerosol, reduced levels of acidity lead to an increase in sulphate production as a result of an enhanced reaction between SO₂ and the oxidant ozone. This results in an overall higher increase in cloudwater sulphate than would be expected assuming an even distribution of all reactants amongst the droplets. In addition, concentrations of the hydrogen sulphite ion predicted to occur in the cloudwater can be substantially in excess of those predicted from the bulk cloudwater pH. This is consistent with recent observations.     

Recovery of molybdenum, phosphorus and arsenic fromleaching solution of molybdenum residues by solvent extraction with primary amine and tributylphosphate

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氯化钙种子气溶胶对甲苯二次有机气溶胶与氨形成含氮有机物的影响

苯系物光氧化反应形成的二次有机气溶胶(SOA)是大气细粒子的重要组成部分.SOA羧酸和二元醛组分能与氨反应形成有机酸铵和咪唑类含氮有机物,它们能够吸收205 nm和270 nm的紫外辐射,是棕色碳的主要组分.氯化钙等无机种子气溶胶具有较大的比表面积,可为气相羰基化合物和氨提供凝结与反应载体,从而影响含氮有机物的形成.基于此,本文利用烟雾腔研究氯化钙种子气溶胶存在时甲苯SOA与氨的反应,采用紫外-可见分光光度计测量产物溶液在205 nm和270 nm处的吸光度,并定性研究不同浓度、湿度和酸度的氯化钙种子气溶胶对含氮有机物形成的影响.结果表明:氯化钙种子气溶胶能够促进甲苯SOA含氮有机物的形成;含氮有机物的生成浓度随着氯化钙种子气溶胶浓度和pH值的增加而逐渐增大.但当氯化钙种子气溶胶为碱性时,OH~-会与凝结的有机酸发生酸碱中和反应并抑制二元醛化合物水合形成四醇产物,从而不利于含氮有机物的生成;水分子的增加占据了氯化钙种子气溶胶表面的吸附活性位点,氨被吸附和凝结的量减少,从而导致含氮有机物的生成浓度随着相对湿度的增大而降低.本研究可为人为源SOA棕色碳的形成机制和化学组成研究提供实验依据.     

O3/H2O2法降解甲基叔丁基醚（MTBE）的试验研究

采用自制鼓泡反应器对臭氧/双氧水(O3/H2O2)降解水中甲基叔丁基醚(MTBE)进行了试验研究,考察了进气(含O3)流量、H2O2 投加量、MTBE初始浓度、pH、温度等因素对MTBE降解的影响.结果表明,在MTBE初始浓度为10 mg·L-1,气体流量为0.5 L·min-1,温度293K, pH=6.5, H2O2 添加量为2.4mg·L1 条件下,反应30 min后, MTBE去除率可达75.5%, COD去除率为68.0%.降解得到的中间产物主要有叔丁基甲酯(TBF)、叔丁醇(TBA)、乙酸甲酯(MA)和丙酮(AC)等,据此探讨了O3/H2O2氧化MTBE的可能反应机理和降解途径.     

中国植被对氮和盐基阳离子吸收速率及其在土壤酸化中的作用

植被对氮和盐基阳离子的吸收是除酸沉降外另一个重要的土壤酸度来源.本研究基于中国植被的净初级生产力和元素化学组成确定了中国植被对氮和盐基阳离子的吸收速率.结果表明中国东南部,包括东北、华北、华东和华南地区,植被对氮的吸收速率普遍较低,而在中国的西北部吸收速率较高,并且由东南向西北逐渐递减对盐基阳离子来说,吸收速率较高(>2.0 keq·(hm²·a)^-1)的植被有亚热带、热带常绿阔叶林、温带石灰岩落叶阔叶林、温带落叶灌丛和亚热带、热带稀树灌木草原等,它们主要分布在华北西北部、云南南部和海南岛西部,而吸收速率较低(<0.5 keq·hm²·a)^-1)的植被则主要包括分布在东部亚热带地区的常绿针叶林以及分布在西部干旱地区的各种荒漠和草原尽管中国大多数地区不会因为植被吸收而造成显著的土壤酸度增加,但在少数地区,植物吸收造成的土壤酸度输入却不容忽视(>0.5 keq·(hm²·a)^-1)由于这些地区植被吸收造成的土壤酸度输入已经大于或相当于目前的酸沉降水平,而且两者之和也超过了土壤的风化速率,这些地区可能面临土壤的酸化问题.     

几种低分子量有机酸对石灰岩溶蚀作用的室内模拟试验

在室内进行了几种低分子量有机酸对石灰岩颗粒(粒径0.45～1mm)的溶蚀试验,同时用盐酸进行对比试验。结果表明:各有机酸对石灰岩颗粒溶蚀作用大小的顺序为:乳酸>乙酸>柠檬酸>甲酸>草酸>丙酮酸,同类型酸中如醇酸或羧酸中,酸性较弱的酸溶蚀力反而较大。这几种酸混合后对石灰岩颗粒的溶蚀作用并未比单个酸的作用强。乳酸、乙酸、柠檬酸的溶蚀力大于盐酸。不管是有机酸还是盐酸,溶蚀石灰岩后溶液中钙离子浓度都呈对数增长,且与溶液pH值呈极显著正相关(P<0.0001);草酸反应液中的钙离子浓度与电导值呈极显著负相关(P<0.0001),其他种类酸溶液钙离子浓度则与电导值呈极显著正相关;除乙酸外,其他酸溶液电导值在反应初始阶段稍微下降后迅速上升。有机酸对石灰岩的溶蚀能力不仅与溶液中的H+和有机配位体浓度有关,而且与酸的类型、酸的强弱及反应后形成的盐的溶解度有关。     

苯乙烯在有机-水两相界面上的分子氧选择性光氧化

以水为介质的氧化反应是一种有效的烯烃选择性绿色氧化和有机物的绿色处理过程.以苯乙烯为反应底物,开展了苯乙烯在室温、紫外光照射下的有机-水两相界面上的分子氧选择性光氧化反应.结果表明:在水溶液中,苯乙烯被选择性地光氧化成苯甲醛,苯甲醛的产率和选择性分别为28.5%和90.8%;而在无氧状态下,水溶液和有机溶剂中的苯乙烯光氧化反应都只得到非常少量的苯甲醛,产率仅有0.2%~0.4%.芳香端基烯烃（如3-甲基苯乙烯、4-甲氧基苯乙烯、1,1-二苯基乙烯）也能在水溶液中被分子氧选择性地光氧化,生成相应的羰基化合物;以双氧水为氧化剂,在水溶液中苯乙烯光氧化反应的苯甲醛产率为0.4%,以双氧水或分子氧为氧化剂时,醇溶剂中苯甲醛的产率均为0.6%~0.7%.研究显示,分子氧和水是苯乙烯光氧化反应的必须因素.      

Selective oxidation of benzyl alcohols to benzoic acid catalyzed by eco-friendly cobalt thioporphyrazine catalyst supported on silica-coated magnetic nanospheres

A novel magnetically recoverable thioporphyrazine catalyst (CoPz(S-Bu)8/SiO2@Fe3O4) was prepared by immobilization of the cobalt octkis(butylthio) porphyrazine complex (CoPz(S-Bu)8) on silica-coated magnetic nanospheres (SiO2@Fe3O4). The composite CoPz(S-Bu)8/SiO2@Fe3O4 appeared to be an active catalyst in the oxidation of benzyl alcohol in aqueous solution using hydrogen peroxide (H2O2) as oxidant under Xe-lamp irradiation, with 36.4% conversion of benzyl alcohol, about 99% selectivity for benzoic acid and turnover number (TON) of 61.7 at ambient temperature. The biomimetic catalyst CoPz(S-Bu)8 was supported on the magnetic carrier SiO2@Fe3O4 so as to suspend it in aqueous solution to react with substrates, utilizing its lipophilicity. Meanwhile the CoPz(S-Bu)8 can use its unique advantages to control the selectivity of photocatalytic oxidation without the substrate being subjected to deep oxidation. The influence of various reaction parameters on the conversion rate of benzyl alcohol and selectivity of benzoic acid was investigated in detail. Moreover, photocatalytic oxidation of substituted benzyl alcohols was obtained with high conversion and excellent selectivity, specifically conversion close to 70%, selectivity close to 100% and TON of 113.6 for para-position electron-donating groups. The selectivity and eco-friendliness of the biomimetic photocatalyst give it great potential for practical applications.