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Marine Geochemistry - Laboratory Methods

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Methane analysis
method  Methane in sediment is analyzed by headspace GC analysis with FID detection.

instrument:

Varian Star 3400

Column: J+W Scientific #115 3432 30m x 0.53mmID Phase:GSO Film:THK.

bottled gas Hydrogen 5.0, Nitrogen 4.6, synthetic air, methane (min. 99.9%)
work solution prepare a 1.2 M NaCl solution, artificial seawater
methane standard stock Headspace vial with pure methane
work standards work standards are prepared by injecting different amounts (i.e. 5, 10, 20, 50 µl of pure methane into headspace of sealed 50 ml vials filled with 25 ml of artificial seawater
GC conditions AIR = synth air, FID gas = Hydrogen, Carrier = nitrogen, Make up = nitrogen, Inj 50°, Detection 150° Column 30°C)
calibration 10 to 50 µl are drawn from the headspace of standard vials by a headspace syringe and injected into GC
conversion conversion of GC readings in ppm to pore water concentration in mole per Liter
sediment is sampled using a 10ml standard syringe with cut tip such that the whole diameter is open. The piston is carefully pulled back while pushing the syringe into the sediment. sediment samples for methane analysis are taken from the core catcher directly after recovery

sample preparation:

50 ml Headspace vials are filled with 20 ml of NaCl/HgCl2 work solution. 5 ml sediment are added and the vials are sealed immediately samples are then homogenized by shaking for 3 min. Analysis should be performed within a few hours
or samples stored
upside down at -18°C

tips + tricks

Sediment has to be sampled as fast as possible. We obtained the most reliable results by sampling directly from the core catcher and from the open liner ends when the core is cut into segments on deck. These first samples give a good idea of the real methane concentrations and allow location of the Sulfate methane transition zone (SMTZ) which then may be sampled at higher resolution. In the cool lab we used to cut little windows into the liner and take syringe samples for methane analysis prior to opening the whole core in the glovebox. Since we now almost exclusively take rhizon pore water samples directly through the liner prior to opening the core we avoid using glove boxes. It is virtually unavoidable to lose some methane, so measured concentrations will be smaller than real concentrations.

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