Sarkozy Laszlo C, Clouser Benjamin W, Lamb Kara D, Stutz Eric J, Saathoff Harald, Möhler Ottmar, Ebert Volker, Moyer Elisabeth J
Department of the Geophysical Sciences, University of Chicago, Chicago, Illinois 60637, USA.
Department of Physics, University of Chicago, Chicago, Illinois 60637, USA.
Rev Sci Instrum. 2020 Apr 1;91(4):045120. doi: 10.1063/1.5139244.
We describe a new tunable diode laser (TDL) absorption instrument, the Chicago Water Isotope Spectrometer, designed for measurements of vapor-phase water isotopologues in conditions characteristic of the upper troposphere [190-235 K temperature and 2-500 parts per million volume (ppmv) water vapor]. The instrument is primarily targeted for measuring the evolving ratio of HDO/HO during experiments in the "Aerosol Interaction and Dynamics in the Atmosphere" (AIDA) cloud chamber. The spectrometer scans absorption lines of both HO and HDO near the 2.64 µm wavelength in a single current sweep, increasing the accuracy of isotopic ratio measurements. At AIDA, the instrument is configured with a 256-m path length White cell for in situ measurements, and effective sensitivity can be augmented by enhancing the HDO content of chamber water vapor by an order of magnitude. The instrument has participated to date in the 2012-2013 IsoCloud campaigns studying isotopic partitioning during the formation of cirrus clouds and in the AquaVIT-II instrument intercomparison campaign. Realized precisions for 1-s measurements during these campaigns were 22 ppbv for HO and 16 ppbv for HDO, equivalent to relative precisions of less than 0.5% for each species at 8 ppmv water vapor. The 1-s precision of the [HDO]/[HO] ratio measurement ranged from 1.6‰ to 5.6‰ over the range of experimental conditions. HO measurements showed agreement with calculated saturation vapor pressure to within 1% in conditions of sublimating ice and agreement with other AIDA instruments (the AIDA SP-APicT reference TDL instrument and an MBW 373LX chilled mirror hygrometer) to within 2.5% and 3.8%, respectively, over conditions suitable for all instruments (temperatures from 204 K to 234 K and HO content equivalent to 15-700 ppmv at 200 hPa).
我们介绍了一种新型可调谐二极管激光(TDL)吸收仪器——芝加哥水同位素光谱仪,该仪器设计用于在对流层上部典型条件下(温度为190 - 235K,水汽体积分数为2 - 500ppm)测量气相水同位素分子。该仪器主要用于在“大气气溶胶相互作用与动力学”(AIDA)云室实验中测量HDO/H₂O不断变化的比率。光谱仪在单次电流扫描中扫描2.64μm波长附近H₂O和HDO的吸收线,提高了同位素比率测量的准确性。在AIDA中,该仪器配置了一个256米光程的怀特池用于原位测量,通过将云室水汽中的HDO含量提高一个数量级,可增强有效灵敏度。该仪器迄今已参与了2012 - 2013年的IsoCloud活动,研究卷云形成过程中的同位素分配,以及参与了AquaVIT - II仪器比对活动。在这些活动中,1秒测量的实际精度对于H₂O为22ppbv,对于HDO为16ppbv,相当于在8ppmv水汽条件下,每种物质的相对精度小于0.5%。在实验条件范围内,[HDO]/[H₂O]比率测量的1秒精度范围为1.6‰至5.6‰。在升华冰的条件下,H₂O测量结果与计算的饱和蒸气压的一致性在1%以内,在适合所有仪器的条件下(温度从204K到234K,在200hPa下H₂O含量相当于15 - 700ppmv),与其他AIDA仪器(AIDA SP - APicT参考TDL仪器和MBW 373LX冷镜湿度计)的一致性分别在2.5%和3.8%以内。