Microcollection of Gases in a Capillary Tube: Preservation of Spatial and Temporal Resolution

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• 作者：Kristin Herrmann Favela ; Pieter Tans ; Thomas H. Jaeckle ; William S. Williamson
• 刊名：Analytical Chemistry
• 出版年：2012
• 出版时间：October 2, 2012
• 年：2012
• 卷：84
• 期：19
• 页码：8310-8316
• 全文大小：340K
• 年卷期：v.84,no.19(October 2, 2012)
• ISSN：1520-6882

文摘

Researchers at the National Oceanic and Atmospheric Administration (NOAA) have recently developed and reported a novel air collection device for measuring vertical profiles of trace gases in the atmosphere, which has been applied to carbon dioxide and methane so far. The device consists of a long stainless steel tube that is prefilled with calibrated gas and allowed to ascend on a weather balloon. During ascent, the device is evacuated as it equilibrates with the decreasing atmospheric pressure. During descent, the tube is filled with atmospheric gas in an ordered manner. The diffusion rate inside the tube is slow enough that the collected gas remains ordered. Here is reported a miniaturization of the device described above, in which the stainless steel tube is replaced with Hydroguard fused silica tubing (0.53 mm 脳 30 m) and two lightweight valves having a total mass of less than 28 g. This micro-AirCore device was deployed on the SwRI-developed unmanned SkyWisp glider. Profiling of carbon dioxide in the atmosphere proceeded via mass spectrometric detection. A laboratory-based validation system was used for evaluating the micro-AirCore function, including accuracy and precision, for carbon dioxide. The diffusion profiles of carbon dioxide, argon, oxygen, and methane were also investigated. Overall, the micro-AirCore demonstrated an accuracy error of 2% (¹²CO₂) and minimal diffusion over a period of 16 h (peak width increased by a factor of 1.6). Even after 63 h, mixing of the gases inside the tube was not complete. A triplet of micro-AirCores was deployed on the SkyWisp glider yielding a relative standard deviation of 0.08%, or 0.3 ppm, for CO₂. The profile collected resulted in observation of the boundary layer with elevated CO₂ levels, a region in the free troposphere with relatively constant CO₂ mole fraction, and a gradual decrease in CO₂ above 10鈥?00 m. This microdevice has broad applications extending beyond vertical profiling. Fitting the device with a metering device could enable horizontal collection of gases.