Conditions:
The sediment samples have been
taken as fast as possible from the core
catcher
or the cut surface during separation of core liners into
sections,
immediately sealed in a headspace vial with a NaCl brine
or NaOH receiver,
shaken for 3 min, and either measured within a few hours
or stored upside down at -18°C.
For measurement, headspace vials are warmed up to room
temperature
and gas samples for analyses are taken from the headspace
above the sediment / brine slurry.
Parameters needed:
VSed - amount of sediment sample
(e.g a syringe sample of 2.5 mL) in L
Vvial - total volume of the
headspace vial Vvial (e.g. 20 mL) in L
Vbrine - amount of NaOH or brine receiver
in the vial to drive CH4 to headspace. (e.g.
7.5 mL ) in L
VGas - amount of headspace gas VGas
(e.g. 10 mL or 0.01 L) in L
VGas = Vvial - Vsed
- Vbrine
VIG - ideal gas volume
at 25°C and 1 bar = 24.789 L/M
CHS - methane concentration
in headspace gas in ppm
por - sediment porosity as a
fraction of 1
Cpw - methane concentration in
pore water in M/L
Cpw = VGas / VIG
* CHS x 10-6 x 1 / (Vsed
x por)
If only sediment density ρsed is known from
e.g. MSCL measurement, porosity may be estimated from
por = (ρrock -
ρsed ) / ( ρrock - ρpw)
Example : Concentration from GC measurement CHS
= 20000 ppm, porosity por = 0.8
Cpw
= 0.01 / 24.789 x 20000 x 10-6
x 1 / (0.0025 x 0.8) = 0.00403 M/L = 4.03 mM/L
In Excel, the densities from MSCL measurements at the
depth of the methane samples
may be extracted from a MSCL dataset using the
VLOOKUP function
assumption:
CH4 sample depth in column A,
MSCL depth and MSCL densities in columns D and E
e.g. from line 2 to line 100
MSCL depths are increasing, no empty readings in E
densitiy at the sample depth found in cell A2 =VLOOKUP
(A2,$D$2:$E$100,2)
if there is no exact match, the VLOOKUP function will use
the previous reading
e.g. Methane sample depth at 2.25 m and only MSCL density
readings at 2.21 m and 2.26 m exist,
VLOOKUP will return the denstiy from column E at 2.21m.
original time stamp 19.December 2022
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