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HomeMy WebLinkAboutGMC Data Report No. 245
Pyromat kinetic model of coal from cuttings (9,220' - 9,260') of the Norton Sound
Exxon Corporation DCS Y-0407-1 (Yellow Pup No.1) well.
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See GMC Data Report No. 242
Received 24 June 1995
Total of 3 pages in report
Alaska Geologic Materials Center Data Report No. 245
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18 ..
16 -
14 -
Norton Sound Coal
Exxon #1 9220-60'
12 -
10 -
8 -
6 -
4 -
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0 0 0 0 0 0 0 0 0 0 0 0 0 0
C\J C\J C'I C'I C\J C\J C'I C'I C\J C'I C'I C\J C\J C'I
LC? LO LC? LC? LC? LC? LC? LC? LC? It) LC? LC? LC? LC?
0 ; C'I C':) -:t LC? CD ¡-.. co CJ) 0 ,.... C\J C':)
-:t -:t -:t -:t -:t -:t -:t -:t -:t LC? LC? LC? LC?
E, cal/m 01
o 0 000 000 0 0
C'I C'I C\J C\J C\J C'I C'I C\J C'I C'I
LC? LC? LC? LC? LC? LC? LC? LC? Il) Il)
-:t LC? CD ¡-.. co CJ) 0 ,.... C'I C':)
Il) LC? Il) Il) LC? Il) CD CD CD CD
Corrected Pyromat Kinetic Model
A = 1 X 1014S·1
1.00.............................................................··...........·...·..........·..............................................................................mm.........m.......................;
Fraction cal/mol
0.13 40520
0.36 41520
0.31 42520
0.42 43520
0.56 44520
0.76 45520
0.26 46520
2.12 47520
0 48520
4.26 49520
13.25 50520
16.64 51520
15.32 52520
12.6 53520
5.12 54520
7.58 55520
1.46 56520
5.82 57520
0 58520
3.63 59520
2.66 60520
0 61520
0 62520
6.73 63520
0.90 .
O.BO .
0.70 .
0.60 .
0.50 .
0.40 .
0.30 .
0.20 .
0.10 .
0.00
70
GMC Data Report No. 245
3"C/My Heating Rate
Kimmeridge Clay Fm.
Norton Sound Coal
90
110
130
Tern perllture. ·C
Herrin Coal
150
170
190
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Mobil Exploration, and Producing Technical Center
FARMERS BRANCH
P.O. BOX 819047
DALLAS. TEXAS 75381·9047
Date: May 19, 1995
To: Fred Stone, MEPTEC
George Claypool, l\1EPTEC
PYROMAT KINETIC MODEL OF
COAL FROM NORTON SOUND,
EXXON #1 WELL Ve..l 10 t..J f'v.f' .:Ji L
JOB NO. BGWOOA o<:_-s Y -... ($4.1· ~:>'~1
As you requested, I have determined a kerogen decomposition kinetic model for the coal from
Norton Sound (Exxon #1, 9220-9260 feet) using the Pyromat II micropyrolyzer. This technique
was developed by geochemists at the Lawrence Livermore National Laboratory. I Small quantities
(l0-100 mg) of rock or kerogen are pyrolyzed at different temperature ramp rates (1 to
56°C/min). The pyrograms are then fitted using a program called KINETICS resulting in a
distribution of activation energies (E, kcal/mol) for either a single predetermined or best-fit
frequency factor (A, sec·I).
The kinetic parameters derived from Pyromat experiments are inaccurate for direct use in basin
modeling. When compared to field observations, Pyromat kinetics are "too slow" and will result
in lower kerogen conversion than measured. In a tield study of Maracaibo Basin, Venezuela,
LLNL researchers found that the Pyromat activation energies should be shifted downwards by ~2
kcal/mol for the modeled results to agree with the field data.2.3 This correction is required
because of an experimental artifact associated with the inefficient volati1ization and transport of
the pyrolysates at low temperatures « 350°C). We have recently calibrated kinetic models
derived from Pyromat, hydrous pyrolysis, and MSSV methodology to a set of field test data on
the Kimmeridge Clay Formation and have developed a means of correcting the Pyromat kinetic
parameters based on the reactivity of the kerogen.4
I Braun R.L.. Burnham A.K., Reynolds J.O. and Clarkson J.E. (1991) Pyrolysis kinetics for lacustrine and
marine source rocks by programmed micropyrolysis. Energy & Fuels 5, 192-204.
2 Sweeney 1., Burnham A., Talukdar S. and Valejos e. (1989) Pyrolysis kinetics applied to prediction of oil
generation in the Maracaibo Basin, Venezuela. Org. Geochem.16, 189-196.
3 Burnham A.K., Braun R.L.. Sweeney J.1., Reynolds 1.0., Vallejos G. and Talukdar S. (1992) Kinetic
modeling of petroleum formation in the Maracaibo Basin: Final report, Annex XII. US DOE Report No.
DOEfBC-92001051, July.
4 Walters e.e., Claypool G.B., Theis N.K.. Acholla F. and Mitchell T.O. (1995) A method to correct
Pyromat kinetic models to conform with field observations. MEPTEC Lab. Memorandum. in
preparation.
GMC Data Report No. 245
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The corrected kinetic model for the Norton Sound Coal is shown and listed below. The
distribution of activation energies is typical of other vitrinitic coals that we have analyzed by the
Pyromat technique. When a 3°C/My heating rate is applied, the Norton Sound Coal behaves
much more like the reference Herrin Coal sample than the Kimmeridge Clay Formation sample.
Please contact me (BM 381-8456) if you have any questions concerning the data or their
interpretation.
~¿d~
Clifford C. Walters
Supervisor, Geochemistry Labs
Petroleum Systems
cc: B.C. Griffiths
S.J. Moncrieff
J.W. Stinnett
M.B. Toon (Geochemistry Files)
Technical Information
CCWalters
Enclosures
GMC Data Report No. 245
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