Université Grenoble Alpes, CNRS, IRD, Grenoble INP Institute of Engineering Université Grenoble Alpes, IGE, F-38000 Grenoble , France.
CNRS DT INSU, 29280 Plouzané , France.
Environ Sci Technol. 2018 Sep 18;52(18):10543-10551. doi: 10.1021/acs.est.7b06171. Epub 2018 Aug 28.
We present a novel instrument, the Sub-Ocean probe, allowing in situ and continuous measurements of dissolved methane in seawater. It relies on an optical feedback cavity enhanced absorption technique designed for trace gas measurements and coupled to a patent-pending sample extraction method. The considerable advantage of the instrument compared with existing ones lies in its fast response time of the order of 30 s, that makes this probe ideal for fast and continuous 3D-mapping of dissolved methane in water. It could work up to 40 MPa of external pressure, and it provides a large dynamic range, from subnmol of CH per liter of seawater to mmol L. In this work, we present laboratory calibration of the instrument, intercomparison with standard method and field results on methane detection. The good agreement with the headspace equilibration technique followed by gas-chromatography analysis supports the utility and accuracy of the instrument. A continuous 620-m depth vertical profile in the Mediterranean Sea was obtained within only 10 min, and it indicates background dissolved CH values between 1 and 2 nmol L below the pycnocline, similar to previous observations conducted in different ocean settings. It also reveals a methane maximum at around 6 m of depth, that may reflect local production from bacterial transformation of dissolved organic matter.
我们介绍了一种新型仪器,即海底探头,可实现海水中溶解甲烷的原位和连续测量。它依赖于一种为痕量气体测量设计的光学反馈腔增强吸收技术,并与一项待审专利的样品提取方法相结合。与现有仪器相比,该仪器的一个显著优势在于其快速响应时间,约为 30 秒,这使得该探头非常适合对水中溶解甲烷进行快速连续的 3D 测绘。它可以承受高达 40 MPa 的外部压力,并且具有从亚纳摩尔每升海水中的 CH 到毫摩尔每升的大动态范围。在这项工作中,我们介绍了仪器的实验室校准、与标准方法的相互比较以及甲烷检测的现场结果。与随后进行的气相色谱分析的顶空平衡技术的良好一致性支持了该仪器的实用性和准确性。在短短 10 分钟内,我们在地中海获得了一个 620 米的连续垂直深度剖面,表明在密度跃层下方,背景溶解 CH 值在 1 到 2 纳摩尔每升之间,与在不同海洋环境中进行的先前观测结果相似。它还揭示了约 6 米深处的甲烷最大值,这可能反映了细菌对溶解有机物的转化产生的局部产量。