Analytical method:
Quadrupole mass spectrometer is Michael Bender's second instrument, a Pfeiffer Vacuum Prisma. Ion currents measured at masses 18, 28, 29, 32, 40, 44, 45, 64 as well as pressure within mass spectrometer. Inlet capillary switched from equilibrator to air for 10 minutes of every 2 hours for calibration. Quadrupole housing made from PVC pipe with heater and fan controlled at 50oC. Temperature within housing and of electronics unit continuously monitored. Small pump is a Micropump GA-V21.J8FTC. Flowmeter is a McMillan 101 Flo-Sen. Equilibrator cartridge is Membrana LiquiCel MicroModule G569 with flow-through water but only one air-side inlet/outlet. Optode was borrowed from Mike DeGrandpre's group and is model 4175 with analog converter. Ship's electronic's technician made a cable for it which is read by both an RS232 and by the Omega AtoD converter. Tenma EX354D dual power supply 280W suppling 8-8.5V to run the small pump and 12.3V to power the optode. Omega OMB-DAQ-56 AtoD converter being used to read seven thermistors, small pump flow rate, and optode analog signals. Flowmeter calibration applied is 100.39*signal - 5.64. All tubing in air upstream of equilibrator cartridge was insulated with gasketing material to slow warming of water. Capillary is 0.05mm fused silica tubing, catalog 602038 Grace Davison Discovery Science. Capillary length from valco valve to mass spec about 1.15m, capillary lengths from equilibrator cartridge to valco valve and from air to valco valve about 0.85m and closely matched. Air capillary tucked into cable tie or bungee cord holding mass spec housing together. Valco valve is 6 port Cheminert C5 HPLC stream connector valve with microelectric actuator. Used FS1.3-5 ferrules at beginning of cruise and switched to FS1.4-5 ferrules on March 15.
Calculations:
O2/Ar ion currents during each 10-min air standard sampling were averaged together and then interpolated to each water sample time. O2/Ar sat was calculated as the ratio of the ion current for the equilibrator divided by that for the air standard (minus one, and times 100). Data was then binned on one-minute intervals. O2/Ar saturations were corrected for observed offsets from the discrete samples based on an average offset derived for each equilibrator. Optode O2 values were calibrated against discrete O2 detemined by Winkler titration following Uchida et al. (2008). Note that timestamp is only accurate within ~2 minutes as computer clock drifted badly and had to be continually reset to ship's timeserver. Net community oxygen production is calculated from the O2/Arsat data, T, S, and a weighted gas exchange rate. This value approximates the NOP of the mixed layer over 10 days prior to the measurement of O2/Ar. For gas exchnage, we use the Reuer et al. (2007) wind speed weighting over 60 days prior to the measurement using combined QuikSCAT/NCEP wind speeds and the Ho et al. (2006) gas exchange parameterization. For more details see Hamme, R. C., et al. (2012), Dissolved O2/Ar and other methods reveal rapid changes in productivity during a Lagrangian experiment in the Southern Ocean, J. Geophys. Res., 117, C00F12, doi:10.1029/2011JC007046.
BCO-DMO Processing Notes
Original file: "Hamme2012_underway.csv" contributed by Roberta Hamme
Metadata file: "Metadata_report_UnderwayMassSpec_Final.xls" contributed by Roberta Hamme
- year, month, date combined into a single date field formatted as YYYYMMDD
- hour, minute combined into a single time field formatted as HHMM
- Parameter names edited to conform to BCO-DMO parameter naming conventions