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采用平衡进样质谱仪进行连续高频溶解氧/氩测量。

Continuous high-frequency dissolved O2/Ar measurements by equilibrator inlet mass spectrometry.

机构信息

Department of Geosciences, Princeton University, Princeton, New Jersey 08544, USA.

出版信息

Anal Chem. 2009 Mar 1;81(5):1855-64. doi: 10.1021/ac802300u.

Abstract

The oxygen (O(2)) concentration in the surface ocean is influenced by biological and physical processes. With concurrent measurements of argon (Ar), which has similar solubility properties as oxygen, we can remove the physical contribution to O(2) supersaturation and determine the biological oxygen supersaturation. Biological O(2) supersaturation in the surface ocean reflects the net metabolic balance between photosynthesis and respiration, i.e., the net community productivity (NCP). We present a new method for continuous shipboard measurements of O(2)/Ar by equilibrator inlet mass spectrometry (EIMS). From these measurements and an appropriate gas exchange parametrization, NCP can be estimated at high spatial and temporal resolution. In the EIMS configuration, seawater from the ship's continuous intake flows through a cartridge enclosing a gas-permeable microporous membrane contactor. Gases in the headspace of the cartridge equilibrate with dissolved gases in the flowing seawater. A fused-silica capillary continuously samples headspace gases, and the O(2)/Ar ratio is measured by mass spectrometry. The ion current measurements on the mass spectrometer reflect the partial pressures of dissolved gases in the water flowing through the equilibrator. Calibration of the O(2)/Ar ion current ratio (32/40) is performed automatically every 2 h by sampling ambient air through a second capillary. A conceptual model demonstrates that the ratio of gases reaching the mass spectrometer is dependent on several parameters, such as the differences in molecular diffusivities and solubilities of the gases. Laboratory experiments and field observations performed by EIMS are discussed. We also present preliminary evidence that other gas measurements, such as N(2)/Ar and pCO(2) measurements, may potentially be performed with EIMS. Finally, we compare the characteristics of the EIMS with the previously described membrane inlet mass spectrometry (MIMS) approach.

摘要

表层海水中的氧气(O(2))浓度受生物和物理过程的影响。通过同时测量氩(Ar),由于其具有与氧气相似的溶解度特性,我们可以消除氧气过饱和的物理贡献,并确定生物氧气过饱和。表层海洋中的生物氧气过饱和度反映了光合作用和呼吸作用之间的净代谢平衡,即净群落生产力(NCP)。我们提出了一种新的连续船载测量 O(2)/Ar 的方法,即平衡进气质谱法(EIMS)。通过这些测量和适当的气体交换参数化,可以以高时空分辨率估算 NCP。在 EIMS 配置中,来自船舶连续进水的海水流经一个装有透气微孔膜接触器的墨盒。墨盒顶空的气体与流动海水中的溶解气体达到平衡。一根熔融石英毛细管连续抽取顶空气体,并通过质谱法测量 O(2)/Ar 比。质谱仪上的离子电流测量反映了通过平衡器流动的水中溶解气体的分压。每隔 2 小时,通过第二根毛细管抽取环境空气,自动对 O(2)/Ar 离子电流比(32/40)进行校准。概念模型表明,到达质谱仪的气体比例取决于几个参数,例如气体的分子扩散率和溶解度差异。讨论了通过 EIMS 进行的实验室实验和现场观测。我们还初步证明,其他气体测量,如 N(2)/Ar 和 pCO(2)测量,可能可以通过 EIMS 进行。最后,我们比较了 EIMS 的特点与之前描述的膜进样质谱法(MIMS)方法的特点。

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