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首页> 外文期刊>Biogeosciences >Technical note: Seamless gas measurements across the land–ocean aquatic continuum – corrections and evaluation of sensor data for CO 2 , CH 4 and O 2 from field deployments in contrasting environments
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Technical note: Seamless gas measurements across the land–ocean aquatic continuum – corrections and evaluation of sensor data for CO 2 , CH 4 and O 2 from field deployments in contrasting environments

机译:技术说明:陆地海洋水生型连续体的无缝气体测量 - 在对比环境中从现场部署到CO 2,CH 4和O 2的传感器数据的校正和评估

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The ocean and inland waters are two separate regimes, with concentrations in greenhouse gases differing on orders of magnitude between them. Together, they create the land–ocean aquatic continuum (LOAC), which comprises itself largely of areas with little to no data with regards to understanding the global carbon system. Reasons for this include remote and inaccessible sample locations, often tedious methods that require collection of water samples and subsequent analysis in the lab, and the complex interplay of biological, physical and chemical processes. This has led to large inconsistencies, increasing errors and has inevitably lead to potentially false upscaling. A set-up of multiple pre-existing oceanographic sensors allowing for highly detailed and accurate measurements was successfully deployed in oceanic to remote inland regions over extreme concentration ranges. The set-up consists of four sensors simultaneously measuring p CO 2 , p CH 4 (both flow-through, membrane-based non-dispersive infrared (NDIR) or tunable diode laser absorption spectroscopy (TDLAS) sensors), O 2 and a thermosalinograph at high resolution from the same water source. The flexibility of the system allowed for deployment from freshwater to open ocean conditions on varying vessel sizes, where we managed to capture day–night cycles, repeat transects and also delineate small-scale variability. Our work demonstrates the need for increased spatiotemporal monitoring and shows a way of homogenizing methods and data streams in the ocean and limnic realms.
机译:海洋和内陆水域是两个单独的制度,温室气体浓度与它们之间的数量级不同。他们共同创造了土地 - 海洋水生连续体(LOAC),这在很大程度上包括在没有关于了解全球碳系统的情况下没有数据的地区。其中的原因包括远程和无法进入的样本位置,通常需要收集水样和随后在实验室分析的繁琐方法,以及生物,物理和化学过程的复杂相互作用。这导致了巨大的不一致,增加了错误,并且不可避免地导致可能是虚假的升级。多种预先存在的海洋传感器的设置,允许高度详细和准确的测量在海洋中成功部署到远程内陆地区,以极端浓度范围。设置由四个传感器同时测量P CO 2,P CH 4(流通式,基于膜的非分散红外(Ndir)或可调谐二极管激光吸收光谱(TDLA)传感器),O 2和ThermositInograph在同一水源的高分辨率下。系统的灵活性允许从淡水部署到不同血管尺寸的海洋状况,在那里我们设法捕获日夜周期,重复横断面,并描绘小规模的变化。我们的作品表明需要增加时空监测,并显示出海洋和石质境界的均质方法和数据流的方式。

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