29.12.2014 Views

Ingrid T. Luijkx, R.E.M. Neubert, S. van der Laan, and H.A.J. Meijer ...

Ingrid T. Luijkx, R.E.M. Neubert, S. van der Laan, and H.A.J. Meijer ...

Ingrid T. Luijkx, R.E.M. Neubert, S. van der Laan, and H.A.J. Meijer ...

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Continuous measurements of atmospheric oxygen<br />

<strong>and</strong> carbon dioxide on a North Sea gas platform<br />

<strong>Ingrid</strong> <strong>Luijkx</strong>, R.E.M. <strong>Neubert</strong>, S. <strong>van</strong> <strong>der</strong> <strong>Laan</strong>, H.A.J. <strong>Meijer</strong><br />

Centre for Isotope Research, University of Groningen, the Netherl<strong>and</strong>s<br />

AMTD 2, 1693-1724, 2009


Outline<br />

• Measurement site description<br />

• Instrumental setup<br />

• Measurement precision<br />

• Initial results of continuous onsite<br />

measurements at F3 North Sea Platform<br />

9 September 2009 CO 2 Experts Meeting Jena 2/ 22


Measurement site: general information<br />

F3 North Sea Platform<br />

- 54º51’N, 4º44’E<br />

- 200 km from l<strong>and</strong><br />

- Oil <strong>and</strong> gas platform<br />

- Air inlet on South-West corner,<br />

46 meters above sea-level<br />

- North Sea depth 44 meters<br />

9 September 2009 CO 2 Experts Meeting Jena 3/ 22


Measurement site: additional equipment<br />

• Flask AutoSampler (<strong>Neubert</strong> et al., 2004)<br />

• Meteorological facilities<br />

9 September 2009 CO 2 Experts Meeting Jena 4/ 22


Outline<br />

• Measurement site description<br />

• Instrumental setup<br />

• Measurement precision<br />

• Initial results of continuous onsite<br />

measurements at F3 North Sea Platform<br />

9 September 2009 CO 2 Experts Meeting Jena 5/ 22


Instrumental setup O 2 <strong>and</strong> CO 2<br />

• O 2 : Oxzilla II similar to e.g. Stephens et al.<br />

(2007), Thompson et al. (2007) <strong>and</strong> Patecki &<br />

Manning (2007).<br />

• CO 2 : Vaisala CarboCap<br />

Infrared absorption,<br />

use two in differential<br />

mode to increase accuracy<br />

9 September 2009 CO 2 Experts Meeting Jena 6/ 22


Instrumental setup O 2 <strong>and</strong> CO 2<br />

Oxzilla + Vaisala = Oxzala<br />

9 September 2009 CO 2 Experts Meeting Jena 7/ 22


Instrumental setup O 2 <strong>and</strong> CO 2<br />

9 September 2009 CO Experts Meeting Jena 8/ 22<br />

2


Instrumental setup O 2 <strong>and</strong> CO 2<br />

• Calibration of all working <strong>and</strong> reference<br />

cylin<strong>der</strong>s is performed in our lab, using Air<br />

Optima.<br />

• Until now local Groningen scale.<br />

• The Air Optima measurements have recently<br />

been transferred to Scripps scale. F3 data in<br />

this presentation is however still on local<br />

scale.<br />

9 September 2009 CO 2 Experts Meeting Jena 9/ 22


Outline<br />

• Measurement site description<br />

• Instrumental setup<br />

• Measurement precision<br />

• Initial results of continuous onsite<br />

measurements at F3 North Sea Platform<br />

9 September 2009 CO 2 Experts Meeting Jena 10/ 22


Measurement precision: Lab tests<br />

Lab results have shown adequate stability (9 days):<br />

O 2 : σ = 5 per meg<br />

Short term<br />

(0.5 hour):<br />

O 2 : σ = 4 per meg<br />

CO 2 : σ = 0.28 ppm<br />

CO 2 : σ = 0.3 ppm<br />

9 September 2009 CO 2 Experts Meeting Jena 11/ 22


Measurement precision: Target<br />

9 September 2009 CO 2 Experts Meeting Jena 12/ 22


Outline<br />

• Measurement site description<br />

• Instrumental setup<br />

• Measurement precision<br />

• Initial results of continuous onsite<br />

measurements at F3 North Sea Platform<br />

9 September 2009 CO 2 Experts Meeting Jena 13/ 22


Continuous observations from F3 platform<br />

• Measurement system installed on F3 platform<br />

in August 2008.<br />

• Continuous measurements at F3 platform<br />

started in September 2008.<br />

• First preliminary results:<br />

9 September 2009 CO 2 Experts Meeting Jena 14/ 22


Continuous observations from F3 platform<br />

Seas. amplitude<br />

O 2 : 110 per meg<br />

CO 2 : 16 ppm<br />

9 September 2009 CO 2 Experts Meeting Jena 15/ 22


Continuous observations from F3 platform<br />

Small scale event:<br />

Oxidative ratio<br />

1 : -1.31±0.09<br />

9 September 2009 CO 2 Experts Meeting Jena 16/ 22


Continuous observations from F3 platform<br />

Small scale events:<br />

9 September 2009 CO 2 Experts Meeting Jena 17/ 22


Continuous observations from F3 platform<br />

• Huge, fast changing O 2 signal<br />

• Little cloud cover, high solar irradiance<br />

• Since there is no concurrent CO 2 signal, most effects can be<br />

ruled out immediately<br />

• No use of liquid N 2 <strong>and</strong> (thermal) fractionation is unlikely<br />

since signal does not fit temperature/cloud cover<br />

• Signal does fit wave period<br />

measurements at F3<br />

• Therefore likely marine O 2 uptake:<br />

• Signal corresponds to a marine<br />

un<strong>der</strong>saturation of 10%<br />

9 September 2009 CO 2 Experts Meeting Jena 18/22


Continuous observations from F3 platform<br />

APO:<br />

Seas. amplitude:<br />

75 per meg<br />

9 September 2009 CO 2 Experts Meeting Jena 19/ 22


Discussion<br />

• The measurement system does yield<br />

important observations, but needs<br />

improvement in measurement precision<br />

• Improvements can be achieved by: shorter<br />

flushing by minimizing volumes of e.g. air<br />

drying system <strong>and</strong> increasing the amount of<br />

working cylin<strong>der</strong>s<br />

9 September 2009 CO 2 Experts Meeting Jena 20/ 22


Conclusion<br />

• Continuous observations are available since<br />

one year.<br />

• Flasks have been filled during 2006-2009, this<br />

data is presented at ICDC8, poster session T1-<br />

059.<br />

• F3 is an ideal location for atmospheric<br />

observations in the North Sea area, since it is<br />

at the boundary of the shallower southern<br />

North Sea <strong>and</strong> the deeper northern part. The<br />

shallower part is a CO 2 source in summer<br />

whereas the deeper part is a sink for CO 2 .<br />

9 September 2009 CO 2 Experts Meeting Jena 21/ 22


Thanks for your attention!<br />

Questions<br />

Comments to AMTD can be<br />

submitted until 1 October<br />

CIO is looking for PhD student<br />

to continue measurements at F3<br />

9 September 2009 CO 2 Experts Meeting Jena 22/ 22


References<br />

• <strong>Neubert</strong>, R. E. M., Spijkervet, L. L., Schut, J. K., Been, H. A., <strong>and</strong> <strong>Meijer</strong>,<br />

H. A. J.: A computer-controlled continuous air drying <strong>and</strong> flask<br />

sampling system, J. Atmos. Ocean. Technol., 21, 651–659, 2004.<br />

• Patecki, M. <strong>and</strong> Manning, A. C.: First results from shipboard<br />

atmospheric O2 <strong>and</strong> CO2 measurements over the North Atlantic<br />

Ocean, OCEANS 2007 – Europe, Aberdeen, UK, 18-21 June 2007, 2007.<br />

• Stephens, B. B., Bakwin, P. S., Tans, P. P., Teclaw, R. M., <strong>and</strong> Baumann,<br />

D. D.: Application of a differential fuel-cell analyzer for measuring<br />

atmospheric oxygen variations, J. Atmos. Ocean.15 Technol., 24, 82–94,<br />

doi:10.1175/JTECH1959.1, 2007.<br />

• Thompson, R. L., Manning, A. C., Lowe, D. C., <strong>and</strong> Weatherburn, D. C.:<br />

A ship-based methodology for high precision atmospheric oxygen<br />

measurements <strong>and</strong> its application in the Southern Ocean region, Tellus<br />

B, 59, 643–653, 2007.<br />

9 September 2009 CO 2 Experts Meeting Jena A1

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!