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Continuous measurements of atmospheric oxygen and carbon dioxide on a North Sea gas platform

机译:在北海天然气平台上连续测量大气中的氧气和二氧化碳

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A new atmospheric measurement station has been established on the North Seaoil and gas production platform F3, 200 km north off the Dutch coast(5°51' N, 4°44' E). Atmospheric concentrations of O2 andCO2 are continuously measured using fuel cell technology and compactinfrared absorption instruments, respectively. Furthermore, the stationincludes an automated air flask sampler for laboratory analysis of theatmospheric concentrations of CO2, CH4, CO and O2 and isotopemeasurements of δ13C, δ18O and Δ14Cfrom CO2. This station is the first fixed sea based station withon-site continuous O2 and CO2 measurements and therefore yieldsvaluable information about the CO2 uptake in coastal marine regions,specifically the North Sea. This paper presents the measurement station andthe used methodologies in detail. In comparison to land-based stations, thedata show low day-to-day variability, as they are practically free ofnightly inversions as well as human influences, due to the station'sremoteness. Therefore, the data set collected at this measurement stationserves directly as background data for the coastal northwest Europeanregion. Additionally, the first data are presented showing the seasonalcycle as expected during August 2008 through June 2009. Furthermore, someshort-term O2 and CO2 signals are presented. The observations atthe platform include several large and fast changing negative atmosphericO2 excursions without an accompanying change in the CO2 signal,which most likely indicate marine O2 uptake.
机译:在距荷兰海岸以北200公里(北纬5°51',东经4°44')的北海油气生产平台F3上建立了一个新的大气测量站。分别使用燃料电池技术和紧凑型红外吸收仪连续测量O 2 和CO 2 的大气浓度。此外,该站还包括一个自动烧瓶采样器,用于实验室分析CO 2 ,CH 4 ,CO和O 2 的大气浓度以及同位素测量来自CO 2 的δ 13 C,δ 18 O和Δ 14 C。该站是第一个在现场连续进行O 2 和CO 2 测量的固定海基站,因此可得出有关CO 2 吸收的有价值信息。沿海海洋地区,特别是北海。本文详细介绍了测量站及其使用的方法。与陆基气象站相比,该数据显示出较低的日常变化,因为由于气象站的远程性,它们几乎不受夜间反转和人类影响。因此,在该测量站收集的数据集可直接用作西北欧洲沿海地区的背景数据。此外,还提供了第一个数据,显示了预期的2008年8月至2009年6月的季节性周期。此外,还提供了一些短期O 2 和CO 2 信号。平台上的观测结果包括几次快速变化的负大气压O 2 偏移,而CO 2 信号却没有随之变化,这很可能表明海洋O 2 吸收。

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