交叉分子束研究氯原子与硅烷的反应动力学

利用通用型交叉分子束研究了氯原子与硅烷的反应,观测到SiH₃Cl+H通道. 测量到产物SiH₃Cl在实验坐标下的角度分辨的飞行时间谱,获得了这个通道质心坐标下的产物角分布和动能分布. 结果表明,相对于氯原子束方向,产物SiH₃Cl主要是后向散射,说明这个通道主要是通过典型的双分子亲核取代反应(S_N2)机理进行的.     

大气NO3自由基损耗率和温度的关系

利用差分吸收光谱系统得到了大气NO₃、NO₂和O₃的浓度,基于NO₃损耗率和温度关系,获得了一种判定NO₃对于VOCs的大气氧化能力和清除大气中NO_x能力的新指示剂,该指示剂用动力学常量和单萜烯释放速率与温度关系来研究NO₃的损耗率．新指示剂应用于研究合肥郊区外场观测的NO₃的氧化能力,分析结果表明,在观测期间单萜烯对于NO₃的损耗贡献约为70%～80%.     

光腔衰荡光谱法测量大气中的NO3和N2O5

本文应用基于二极管激光器的双路光腔衰荡光谱技术，分别对大气中NO₃和N₂O₅浓度进行监测. 通过使用实验室标准样校正有效吸收腔长比R_L和系统的总损耗系数?，并获得了NO₃有效吸收截面. 该装置在时间分辨率为1 s时，对NO₃的测量灵敏度达到1.1 pptv，N₂O₅被在线转换成NO₃，从而被另一路光腔衰荡光谱装置探测. 利用该装置，对合肥市区冬季夜间大气中的NO₃，N₂O₅浓度进行了实时监测. 通过对比一次大气快速清洁过程中氮氧化物、臭氧、PM_2.5等组分的浓度变化，讨论了大气环境下可能影响NO₃及N₂O₅浓度的因素.     

基于LED光源的非相干宽带腔增强吸收光谱技术探测HONO和NO2

介绍了基于近紫外发光二极管LED (中心波长约372 nm,半高宽13 nm) 光源的非相干宽带腔增强吸收光谱技术,同时用于探测痕量气体HONO和NO₂. LED出射光经准直后耦合进入长度为70 cm,由两块高反射率镜片组成的高精密光学腔内. 分别测量了氮气消光谱和氦气消光谱,通过两者瑞利散射截面的差异而引起光谱强度的变化来标定镜片反射率.在360—390 nm反演波段内,镜片反射率在390 nm处最大且为0.99962, 对应测量NO₂/HONO混合物时的最大光程约1.71 km,并利用最小二乘拟合反演出了 HONO和NO₂的浓度值.当光谱采集时间为1000 s时, HONO和NO₂的探测灵敏度(1σ) 分别为0.6 ppbv和1.9 ppbv.实验结果表明,该技术为实现大气痕量气体的高灵敏度在线监测提供了另一种可能的途径.     

直射太阳光差分吸收光谱法测量合肥NO2 整层柱浓度

直射太阳光差分吸收光谱技术(DS-DOAS)近 年来成功应用于大气痕量气体的垂直柱浓度测量. 本文研究了基于被动DOAS算法可用于连续测量NO₂整层垂直柱浓度的DS-DOAS技术, 介绍了测量系统的构成.利用统计最小值外推法减少了由参考谱引入的误差.分析了测量结果的误差来源, 估算了误差大小.报道了该系统在合肥地区对NO₂进行的连续11天的测量, 分析了测量结 果.通过实验验证了算法的可行性, 证实了该技术可实现连续测量NO₂整层垂直柱浓度.     

宽带腔增强吸收光谱技术应用于痕量气体探测及气溶胶消光系数测量

基于氙灯的非相干宽带腔增强吸收光谱系统, 并将其应用于痕量气体及气溶胶消光系数的测量. 该系统的探测灵敏度通过测量NO₂在520—560 nm波长范围内的吸收得到验证, 最小可探测灵敏度为1.8× 10^-7cm^-1 (1σ, 0.12 s积分时间, 50次平均), 对应的NO₂探测极限～33 nmol/mol. 结合标准气溶胶粒子发生系统, 测量了不同浓度的单分散硫酸铵气溶胶粒子在532 nm波长处的消光系数, 得到粒径为600 nm的硫酸铵气溶胶的消光截面为1.12× 10^-8cm², 与文献报道值1.167× 10^-8cm²相一致, 验证了气溶胶测量的可行性和准确性.     

机载腔增强吸收光谱系统应用于大气NO_2空间高时间分辨率测量

介绍了一套用于机载平台测量的非相干宽带腔增强吸收光谱(IBBCEAS)系统,并应用于实际大气NO_2空间分布的高时间分辨率观测.为满足机载测量中对时间分辨率的需求,系统采用离轴抛物面镜代替消色差透镜提高光学耦合效率;并运用Allan方差,对系统性能进行了分析.通过腔增强吸收光谱系统与长光程吸收光谱系统对实际大气NO_2的对比测试,两者线性相关系数R~2达到0.86.将IBBCEAS系统应用于机载平台,在时间分辨率为2 s的情况下,探测限达到95 ppt(1σ).通过机载观测,获得了华北地区石家庄等地上空对流层大气NO_2的廓线信息.     

Density Functional Theory Study on Electronic and Magnetic Properties of Mn-doped (MgO)n (n=2～10) Clusters

利用密度泛函理论方法优化了纯的和M_n原子掺杂的(MgO)_n (n=2～10)团簇的几何结构. 在Mn原子掺杂的氧化镁结构中, 获得了一系列的同分异构体和与之相对应的总能量.MnMg_n-1O_n(n=2～10)的几何构型显示Mn原子优先取代低配位的Mg原子. 结构稳定性分析表明,除了(MgO)₁₀团簇外,其它纯的和掺杂结构的平均结合能均随着团簇的增大而增强. MnMg_n-1O_n团簇的二阶能量差结果表明MnMg₅O₆和MnMg₈O₉比相邻的团簇表现出更高的相对稳定性. 除了MnMgO₂团簇的磁矩为3.00 μB外,其它掺杂结构的磁矩均为5 μB左右. 它们的磁性主要受电荷转移大小、原子在结构中的位置以及结构尺寸所影响.     

MgH2(110)表面Pd单原子催化氢脱附反应的第一性原理研究

本文采用第一性原理密度泛函理论计算研究了MgH₂(110)表面吸附单原子Pd后的氢脱附反应. 计算发现,在吸附一个Pd单原子后,MgH₂(110)表面氢脱附反应的能垒可以从1.802 eV显著地降低到1.154 eV,表明Pd单原子对于氢脱附具有很强的催化效应. 并且,Pd单原子催化还可以将氢脱附的温度从573 K显著地降低到了367 K,从而使MgH₂(110)表面的氢脱附反应更加容易和快速地发生. 此外,通过MgH₂(110)表面氢溢出机制的反向过程来讨论了氢脱附反应的微观过程. 该研究表明Pd/MgH₂薄膜在未来的实验中可作为良好的储氢材料.     

宽带腔增强吸收光谱法测量大气NO2定标方法研究

非相干宽带腔增强吸收光谱法定量探测大气痕量气体浓度需要准确定标。以定量探测大气NO₂为目的,建立了基于蓝色发光二极管光源的非相干宽带腔增强吸收光谱测量系统,研究了(1)仅使用浓度已知的NO₂吸收光谱、(2)同时使用浓度已知的NO₂和纯氧气中氧气二聚体O₂-O₂吸收光谱、(3)利用纯氮气和纯氦气的瑞利散射消光差异等三种方法,分别获取非相干宽带腔增强吸收光谱在430～490 nm波段的镜片反射率定标曲线。三种方法得到的镜片反射率最大值对应波长均约为460 nm,但这些最大值存在一定差异,分别为0.999 25,0.999 33和0.999 37。利用NO₂样气吸收测量对比了三种定标方法,发现方法(1)与另外两种方法的测量结果不一致性分别约为14%和19%,而后两种方法所测结果的不一致性仅为4%。测量结果表明,NO₂标准气体浓度的不准确性以及壁损耗等因素恶化了方法(1)的定标精度,应尽量避免使用该定标方法。通过对实际大气中NO₂和O₂-O₂在440～485 nm波段内的同时测量,进一步验证了非相干宽带腔增强吸收光谱法的高灵敏度以及所用标定方法的有效性。     

Gain versus tuning issues to Q-switch with Yb<Superscript>3+</Superscript>:LSO and amplify broad-bandwidth pulses

We report on the development of Incoherent Broadband Cavity Enhanced Absorption Spectroscopy (IBBCEAS) using a blue light emitting diode (LED) for the detection of NO₂ in laboratory ambient air. Absorption of the oxygen collisional pair in the atmosphere was also detected in the same spectral range. The mirror reflectivity was determined using a standard gas sample mixture of NO₂, and calibrated with the help of the absorption spectrum of the oxygen collisional pair in pure oxygen at atmospheric pressure. Optimization of the experimental parameters was investigated and is discussed in detail. For the first time in IBBCEAS involving broadband absorption spectra, averaging time for signal-to-noise ratio enhancement has been optimized using Allan variance plot. 18.1 ppbv NO₂ in laboratory ambient air has been retrieved from the absorption spectra using differential fitting method over a 40 nm spectral region centered at 470 nm. A minimum detection sensitivity of about 2.2 ppbv (1σ) for NO₂ at atmospheric pressure has been achieved using the optimal averaging time of 100 s by means of a high finesse optical cavity formed with two moderate reflectivity (∼99.55%) mirrors. No purging of the cavity mirrors by high purity He or N₂ gas streams was necessary to prevent contamination of the mirror faces for the in situ measurements.     

Self-, N2-, O2-broadening coefficients and line parameters of HFC-32 for ν7 band and ground state transitions from infrared and microwave spectroscopy

Hydrofluorocarbons have been used as replacement gases of chlorofluorocarbons, since the latter have been phased out by the Montreal Protocol due to their environmental hazardous ozone-depleting effects. This is also the case of difluoromethane (CH₂F₂, HFC-32), which nowadays is widely used in refrigerant mixtures together with CF₃CH₃, CF₃CH₂F, and CF₃CHF₂. Due to its commercial use, in the last years, the atmospheric concentration of HFC-32 has increased significantly. However, this molecule presents strong absorptions within the 8–12 μm atmospheric window, and hence it is a greenhouse gas which contributes to global warming. Although over the years several experimental and theoretical investigations dealt with the spectroscopic properties of CH₂F₂, up to now pressure broadening coefficients have never been determined. In the present work, the line-by-line parameters of CH₂F₂ are retrieved for either ground state or ν₇ band transitions by means of microwave (MW) and infrared (IR) absorption spectroscopy, respectively. In particular, laboratory experiments are carried out on 9 pure rotational transitions of the ground state and 26 ro-vibrational transitions belonging to the ν₇ band lying around 8.2 μm within the atmospheric region. Measurements are carried out at room temperature on self-perturbed CH₂F₂ as well as on CH₂F₂ perturbed by N₂ and O₂. The line shape analysis leads to the first determination of self-, N₂-, O₂-, and air-broadening coefficients, and also of line intensities (IR). Upon comparison, broadening coefficients of ground state transitions are larger than those of the ν₇ band, and no clear dependence on the rotational quantum numbers can be reported. The obtained results represent basic information for the atmospheric modelling of this compound as well as for remote sensing applications.     

基于O2-O2吸收的非相干宽带腔增强吸收光谱浓度反演方法研究

针对传统非相干宽带腔增强吸收光谱浓度反演方法的定量结果易受镜片反射率标定误差的影响问题, 提出了一种基于测量大气O₂-O₂吸收的浓度反演方法. 该方法是将非相干宽带腔增强吸收光谱技术的光学增强腔等效成吸收光程不随波长变化的多次反射池, 首先根据测得的宽带腔增强大气吸收谱和参考谱计算出光学厚度, 并应用差分光学吸收光谱算法拟合修正后的气体吸收截面到光学厚度, 反演得到大气中O₂-O₂以及被测气体的柱浓度, 然后根据O₂-O₂在大气中的含量已知且相对稳定这一特性, 确定出等效多次反射池的吸收光程, 最后从被测气体的柱浓度中扣除吸收光程信息得到被测气体的浓度值. 以监测大气中NO₂实验为例, 应用该方法在454-487 nm波段反演得到了大气NO₂的浓度(1-30 ppbv范围内), 并将反演结果与传统浓度反演方法的结果进行了对比, 发现两者的不一致性在7%以内. 实验结果表明, 非相干宽带腔增强吸收光谱技术可以利用大气O₂-O₂的吸收来定量其他被测气体的浓度, 而且定量结果对镜片反射率的标定误差不敏感.     

Analysis of influence of atmosphere extinction to Raman lidar monitoring CO2 concentration profile

Lidar （Light detection and ranging） system monitoring of the atmosphere is a novel and powerful technique tool. The Raman lidar is well established today as a leading research tool in the study of numerous important areas in the atmospheric sciences. In this paper, the principle of Raman lidar technique measurement CO2 concentration profile is presented and the errors caused by molecular and aerosol extinction for CO2 concentration profile measurement with Raman lidar are also presented. The standard atmosphere extinction profile and ＇real-time＇ Hefei area extinction profile are used to conduct correction and the corresponding results are yielded. Simulation results with standard atmosphere mode correction indicate that the errors caused by molecule and aerosol extinction should be counted for the reason that they could reach about 8 ppm and 5 ppm respectively. The relative error caused by Hefei area extinction correction could reach about 6%. The errors caused by the two components extinction influence could produce significant changes for CO2 concentration profile and need to be counted in data processing which could improve the measurement accuracies.     

锐钛矿型TiO2(001)-(1×4)表面还原型缺陷对乙醛偶联反应的作用

本文利用程序升温脱附技术(TPD)研究了乙醛吸附在锐钛矿型TiO₂(001)-(1×4)表面的化学性质. 实验结果表明完整晶格位点对乙醛反应表现极为惰性,而表面上的还原型缺陷位点在热驱动下可有效地使乙醛分子通过碳-碳偶联反应生成2-丁酮和丁烯. 提出了乙醛在锐钛矿型TiO₂(001)-(1×4)表面偶联反应主要是通过表面还原型缺陷位吸附成对的乙醛分子,因为表面已有的钛原子对还原型缺陷为乙醛分子提供了合适的吸附位点.     

非相干宽带腔增强吸收光谱技术应用于实际大气亚硝酸的测量

介绍了基于紫外发光二极管光源的非相干宽带腔增强吸收光谱技术, 并用于实际大气亚硝酸(HONO)和二氧化氮(NO₂)的同时测量. 分析了腔内气体的瑞利散射对测量的影响, 测试了紫外发光二极管光源的稳定性, 使用氦气和氮气的瑞利散射差异性标定了镜片反射率随波长的变化曲线, 在HONO吸收峰(368.2 nm)处镜片反射率约为0.99965. 应用Allan方差统计方法确定出测量光谱最佳采集时间为320 s, 对应的HONO和NO₂的探测限(1σ)分别为0.22 ppb 和0.45 ppb. 使用非相干宽带腔增强吸收光谱测量装置对大气HONO和NO₂进行了连续三日的实际观测, 将测量得到的HONO浓度变化与差分吸收光谱测量装置的测量结果进行对比, 线性相关系数R²为0.917.     

Dy掺杂对Sr2Bi4Ti5O18铁电陶瓷性能的影响

用传统固相烧结法制备了Sr₂Bi_4-xDy_xTi₅ O₁₈(SBDT-x, x=0—0.20)陶瓷样品. x射线衍射分析表明, 微量的Dy掺杂没有影 响Sr₂Bi₄Ti₅O₁₈(SBTi) 原有的层状钙钛 矿结构. 通过研究样品的介电特性, 发现Dy掺杂减小了材料的损耗因子, 降低了样品铁电- 顺电相转变的居里温度. 铁电性能测量结果表明, 随Dy含量的增加, SBDT-x系列样品的剩余 极化先增大, 后减小. 当Dy掺杂量为0.01时, 剩余极化达到最大值, 约为20.1 μC·cm^-2. 掺杂引起剩余极化的变化, 与材料中缺陷浓度、内应力以及晶格畸变程度等因 素有关, 是多种作用机理相互竞争的结果. (Bi₂O₂)²⁺ 层通常被看作是绝缘层和空间电荷库, 对材料的铁电性能起关键作用. 掺杂离子进入(Bi2O₂)²⁺层会导致铁电性能变差. 关键词： 2Bi₄Ti₅O₁₈陶瓷')" href="#">Sr₂Bi₄Ti₅O₁₈陶瓷 Dy掺 杂 铁电性能 居里温度     

开放光路非相干宽带腔增强吸收光谱技术测量大气NO2

采用蓝色发光二极管(LED)作为非相干宽带腔增强吸收光谱技术(IBBCEAS)系统光源,测量了436～470nm波段内NO2样气的吸收,验证IBBCEAS的高探测灵敏度。通过氮气和氦气两者瑞利散射截面的差异标定了镜片在430～490nm波段内的反射率,并利用纯氧中氧气二聚体(O2-O2)在477nm处的吸收验证了镜片反射率标定的准确性。镜片反射率在461nm处最大且为0.99937,光学腔长度为73.5cm时的最大有效光程为1.17km。当光谱采集时间为20s时,NO2的探测灵敏度(1σ)达到了0.25×10-9。进行了开放光路下环境大气中NO2和O2-O2在454～486nm波段内的吸收测量,结果表明大气中气溶胶等颗粒物的Mie散射消光降低了IBBCEAS仪器的探测灵敏度(1.04×10-9)。大气中O2-O2的测量为IBBCEAS吸收光程的在线标定提供了一种可行的途径。     

Hydrogen and Deuterium Analysis Using Laser‐Induced Plasma Spectroscopy

Abstract

Hydrogen emission in laser plasma has been studied by focusing a TEA CO₂ laser and Nd‐YAG lasers on various types of samples, such as glass, quartz, and zircaloy pipes doped with hydrogen. It was found that H_α emission with a narrow spectral width occurs with high efficiency when the laser plasma is produced in low‐pressure host gas. In contrast, the conventional well‐known laser‐induced breakdown spectroscopy (LIBS), which operates at atmospheric air pressure, cannot be applied for the analysis of hydrogen as impurity. The specific characteristic of hydrogen emission in low‐pressure plasma is interpreted on the basis of our shock wave model, taking account of the fact that the hydrogen mass is extremely light compared to that of the host target. Another experimental study on gas analysis was conducted using an Nd‐YAG laser and helium host gas at atmospheric pressure on a sample of mixed water (H₂O) and heavy water (D₂O) in vapor form. It was shown that completely resolved hydrogen (H_α) and deuterium (D_α) emission lines that are separated by only 0.179 nm could be obtained at a properly delayed detection time when the charged particles responsible for the strong Stark broadening effect in the plasma have mostly disappeared. It is argued that a helium metastable excited state plays the important role in the hydrogen excitation process.