project
  methods

intro
goals
challenges
background
methane fluxes
the methane barrier
AOM
hydro-acoustics
microbiology
methods
- Seismics
- Coring Equipment
- Sediment physics
- Sediment chemistry
- Process rates
- Microbiology
- Molecular biology
- Water column
modeling
database
work packages
working areas
publications

 

Methanogenesis from CO2+H2 or acetate



Methanogenesis from H2 and CO2 or from acetate is measured experimentally in subcore samples
using 14C-labeled bicarbonate or acetate as tracers.


Field:

At the core processing station sub-sample mini-cores (2.2 cm diameter) are taken with clean Perspex tubes forced into the cut core surface for 10 cm. During this process a vacuum is applied by sucking a tube attached to a stopper at the top of the tube to ensure that the sediment mini-core is not compressed during sampling. The tubes have been pre-drilled with 1 mm ports at 1 cm intervals along their length and these have been sealed with a silicone based aquarium sealant.

The tubes are stoppered with a butyl rubber bung and stored temporarily, at the in situ temperature before being transported to the isotope station.


Amounts of radiotracer injected at each port are approximately;


i)
ii)
At the conclusion of the injections the micro-syringe is thoroughly rinsed with distilled water (10 times), to remove any residual isotope.

After injections all mini-cores are incubated at in situ temperature for 6 hours (acetate) or 18 hours (bicarbonate).

Incubations are terminated by piston extrusion of 2 cm sections of mini-core that are sliced off and put immediately into glass jars containing 7 ml of 0.5 M NaOH. The jars are tightly sealed with a butyl rubber bung, shaken to reduce the core section to a slurry, taped for security and stored upside down at room temperature to await processing.

back to top