首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Acetone and acetonitrile in the tropical Indian Ocean boundary layer and free troposphere: Aircraft-based intercomparison of AP-CIMS and PTR-MS measurements
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Acetone and acetonitrile in the tropical Indian Ocean boundary layer and free troposphere: Aircraft-based intercomparison of AP-CIMS and PTR-MS measurements

机译:热带印度洋边界层和对流层中的丙酮和乙腈:基于飞机的AP-CIMS和PTR-MS测量的比对

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We have performed aircraft-borne intercomparison measurements of acetone and acetonitrile using two different mass spectrometric techniques: A Proton Transfer Reaction Mass Spectrometer (PTR-MS) operated and developed by the Institute of Ion Physics, University of Innsbruck, and an Atmospheric Pressure Chemical Ionization Mass Spectrometer (AP-CIMS) operated and developed by the Max Planck Institute for Chemistry, Mainz. The two devices were employed for atmospheric trace gas measurements over the Indian Ocean on board the National Center for Atmospheric Research C-130 research aircraft during the Indian Ocean Experiment (INDOEX) intensive field phase in February and March 1999. Both instruments use reactions of ions with atmospheric trace gas molecules and mass spectrometric detection techniques for the determination of trace gas concentrations. For the detection of acetone and acetonitrile, both mass spectrometers operate in the positive ion mode and detect the protonated species of these compounds. One difference of the two systems is the operating pressure of the reaction chamber, where the ion molecule reactions take place. While the PTR-MS uses a low-pressure (2.2 hPa) drift tube, a much higher pressure of 300 hPa is used by the AP-CIMS. Other differences are the determination of background concentrations and the calibration procedure. The AP-CIMS uses a charcoal filter, and the PTR-MS uses a Pt catalyst. For the AP-CIMS an on-line calibration is necessary, which is performed during the flights. The intercomparison measurements described here were carried out on two research flights along a north-south transect along 73 degreesE between 6 degreesN and 8 degreesS. Altitudes between 100 in and 6500 in above sea level were covered. Backward trajectory analyses indicate that the sampled air was taken from polluted air masses originating from India and the Bay of Bengal as well as from remote southern hemispheric air. During the two flights on February 20 and 24 the position of the Intertropical Convergence Zone was located around 1.5 degreesS in the investigated area. The measurements of both instruments of acetone and acetonitrile indicate a strong gradient in the boundary layer and a weaker one in the free troposphere. The values measured by the PTR-MS are higher than the ones by the AP-CIMS, but are within the combined error range of +/- 20-30% for each instrument. Acetone mixing ratios up to 2.5 parts per billion (ppb) and acetonitrile up to 0.4 ppb were measured in the northern hemispheric boundary layer. The measurements in the free troposphere give values between 0.3 ppb and 1.0 ppb for acetone and 0.12 ppb and 0.3 ppb for acetonitrile. [References: 54]
机译:我们已经使用两种不同的质谱技术对丙酮和乙腈进行了机载比对测量:由因斯布鲁克大学离子物理研究所操作和开发的质子转移反应质谱仪(PTR-MS),以及大气压化学电离质谱仪(AP-CIMS)由美因茨的马克斯·普朗克化学研究所操作和开发。在1999年2月和3月的印度洋实验(INDOEX)密集场阶段期间,这两种设备被用于美国国家大气研究中心C-130研究飞机上印度洋上的大气痕量气体测量。这两种仪器均使用离子反应结合大气中痕量气体分子和质谱检测技术来测定痕量气体浓度。为了检测丙酮和乙腈,两个质谱仪均以正离子模式运行,并检测这些化合物的质子化物种。两种系统的区别之一是发生离子分子反应的反应室的工作压力。 PTR-MS使用低压(2.2 hPa)漂移管,而AP-CIMS使用300 hPa更高的压力。其他差异是背景浓度的确定和校准程序。 AP-CIMS使用木炭过滤器,而PTR-MS使用Pt催化剂。对于AP-CIMS,需要在飞行过程中进行在线校准。此处描述的比对测量是在沿着南北横断面的两次研究飞行中进行的,该横断面在6°N和8°S之间的73°E。海拔高度介于100英寸至6500之间。向后的轨迹分析表明,采样空气取自源自印度和孟加拉湾的污染空气团以及偏远的南半球空气。在2月20日和24日的两次飞行中,热带气旋收敛区的位置在被调查区域内约1.5度。丙酮和乙腈这两种仪器的测量结果表明,边界层中的梯度很大,而对流层中的梯度则较弱。 PTR-MS测得的值高于AP-CIMS测得的值,但在每台仪器的综合误差范围内为+/- 20-30%。在北半球边界层测得的丙酮混合比高达2.5十亿(ppb),乙腈高达0.4 ppb。在对流层中的测量值得出,丙酮的值介于0.3 ppb和1.0 ppb之间,乙腈的值介于0.12 ppb和0.3 ppb之间。 [参考:54]

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