California Current Ecosystem LTER

Membrane Inlet Mass Spectrometry, vertical O2/Ar profiles

Title
Three ~50m vertical profiles of the dissolved O2/Ar ion current ratio in seawater with depth, measured at high vertical resolution using Membrane Inlet Mass Spectrometry. 2017.

Abstract
Seawater was sampled via tubing with depth between the surface and ~50m, then measured for the ion current ratio of dissolved O2/Ar using Membrane Inlet Mass Spectrometry (Tortell, 2005; Kaiser et al., 2005). Measurements were conducted during the P1706 CCE-CalCOFI Process Cruise (1 Jun - 2 Jul 2017). Profiles were taken on 11 June, 15 June, and 25 June during Cycle 1, Cycle 2, and Cycle 4, respectively. Oxygen saturation and solubility were separately and concurrently measured from sampled seawater using an Aanderaa optode oxygen sensor. The ratio of seawater O2/Ar to the O2/Ar ratio at equlibration with the atmosphere is also reported. Vertical profiles of O2/Ar are used to correct surface measurements of productivity using O2/Ar for vertical influences, and can also be used to qualitatively assess profiles of community metabolic activity with depth.

Keywords
marine, measurements, oceans, seawater, O2/Ar, MIMS, profiles, ions

LTER Data System Record
http://dx.doi.org/10.6073/pasta/f37ebc2664eafe83fa9f81eeb256a74f
Projects
California Current Ecosystem LTER

Creators
Kranz, Sven (skranz@rice.edu)
Kelly, Thomas (tbkelly@alaska.edu)
Wang, Seaver (seaver.wang@duke.edu)
Cassar, Nicolas (nicolas.cassar@duke.edu)

Contact
CCE LTER Information Manager (ccelter.im@gmail.com)

Other Personnel
Stukel, Mike Co-author

Data

table vertical profiles
primary data table for dataset
Rows: 699
Columns: 10
View / Download

Methods


Membrane Inlet Mass Spectrometry
Sample seawater was pumped aboard ship via tubing with one end fixed to a cable being lowered to progressively deeper depths. A custom-made MIMS cuvette consisted of a stainless-steel baseplate in which a frit inlay (gas permeable 50 µm PTFE), overlaid with a 10 µm PTFE membrane (RTC Reichelt Chemietechnik GmbH, Germany) and a flow through cuvette which transported water along the membrane. To avoid large temperature changes, a heating coil was wrapped around the MIMS cuvette which kept the stainless-steel base plate at 45 °C. For calibration purposes, a 4 L polycarbonate bottle of filtered seawater was equilibrated continuously using an aquarium air pump. The calibration bottle was placed in the flow-through water intake reservoir to keep water temperatures close to the environmental temperatures. Every 4 hours, automated solenoid valves switched the water intake from the flow through to the air equilibrated water which was subsequently measured by the MIMS. A calibration step lasted 25 minutes after which the system changed back to the seawater intake. These automatic calibrations were used for the atmospheric O2/Ar ratio baseline correction. Subsequent to each calibration, the calibration water-bottle was automatically topped off with filtered water from the seawater intake using a peristaltic pump. Equilibration with room air for >3 hours and constant monitoring of the O2 concentration using O2 optodes (Firesting, P2 optodes) ensured that the water was equilibrated. For further details, see Tortell, 2005 and Kaiser et al., 2005.