Title: NMR Measurement of Bitumen at Different Temperatures
1NMR Measurement of Bitumen at Different
Temperatures
- Elton Yang, George J. Hirasaki
Rice Consortium Rice University, Houston,
TX March 26th, 2008
2Introduction
- Bitumen is characterized by its high viscosity
and density, which is a major obstacle to both
its recovery and property investigations. - Due to the loss of T2 information shorter than
echo spacing (TE) and interference of water
signal, estimation of heavy oil saturation and
viscosity from NMR T2 measurements is problematic.
3Sample
- Athabasca Bitumen sample (bitumen water
clay), contained in a cylinder glass tube. - Tube I.D. 4.66 cm
- Sample height 3.70 cm
- Sample volume 63.1 mL
4CPMG Measurement for Bitumen at 30 oC
5Approach to Compensation of Lost T2 Information
- Determine initial magnetization M0 from FID.
- Supplement M0 into the regular CPMG data and do
the interpretation.
6Mo and T2 Can be Estimated from FID
7Interpretation of Supplemented CPMG Data by Using
Standard Multi-exponential Model
8Approach to Solution
- Distinguish oil and water response by using
contrast in relaxation. - Assume relaxation time of emulsified water is
correct as interpreted in standard way. - Assume ?f of bitumen is equal to difference
between M0 and ?f of water. - Assume lognormal distribution for bitumen and
redo the interpretation. Here, unknowns are log
mean T2 and standard deviation.
9Fitting Supplemented CPMG Data at 30 oC
- CPMG data is supplemented with a specified Mo
from FID. - Assume lognormal distribution for bitumen T2
distribution.
10Corrected T2 of Bitumen from Lognormal
Distribution Model has Little Dependence on TE
11T2 Estimated from CPMG is Echo Spacing Dependent.
This can be Fixed by Specifying Mo from FID and
Assuming Lognormal Distribution for Bitumen
12Apply this method for the estimation of T2 at
different temperatures.
13Experimental Method
- Sample is placed in thermal water bath with
interested temperature for gt 4 hours before NMR
measurement. - Sample tube is wrapped with a 4-layer paper
insulation during NMR measurement. The
temperature of magnetic field is kept at 30 oC. - FID is performed before each CPMG. The total time
for making one measurement (FID CPMG) lt 1 min. - Measurement is repeated for at least 3 times to
ensure the reliability of experimental data. - The interested temperature range is 8 90 oC,
which is adequate for Canadian bitumen logging.
14Temperature Change of Athabasca Bitumen Sample in
90 oC Case
Fig. (a) Heating Process It only took about 90
min. to heat the bitumen sample from room
temperature to 90 oC.
Fig. (b) NMR Measurement Process For the 90 oC
case, the sample temperature deviation was 1.6
within 1 min.
15Change of Mo with Temperature is Governed by
Curies Law
(1)
Curies Law
Given a sample system, each parameter on the
right side of above equation is constant except
for the temperature, thus equation (1) becomes
(2)
16Estimate Mo from FID at 8 60 oC
- Apparent Mo extrapolated from FID increases with
temperature. - Extrapolated Mo reaches a constant when
temperature gt 40 oC (indicated by arrow).
- FID signals probably attenuate much faster within
first 80 msec dead time. Loss of FID information.
17FID of Bitumen Sample at 8 and 20 oC, Obtained by
Using 20 MHz Bruker Spectrometer with a Dead Time
of 50 msec
18Estimate Mo from FID at 60 90 oC
- Estimated M0 of bitumen at T 60 oC starts
decreasing as temperature increases
19Mo of Bitumen Sample at 8 90 oC
- Difference between 60 oC-based prediction and 90
oC-based prediction is 3.2 . - Correct M0 by using Curies Law on the basis of
60 oC value.
20Fitting CPMG Signal at Different T, Constrained
by Curies Law Corrected M0 and Assuming
Lognormal Distribution for Bitumen
21Interpretation of CPMG, Supplemented with Curies
Law Corrected M0
22Interpretation of CPMG, Supplemented with
Apparent M0 without Curies Law Correction
23Calculate Bitumen HI and Water Saturation
Definition
Here, assume the difference of sample volume
within our interested temperature range is
negligible, thus
? f b/bw sum of f of bitumen part in the
mixture sample M0,w initial
magnetization of pure water as standard Vb/bw
volume of bitumen part in the mixture
sample Vt total volume of mixture
sample, assumed to equal to volume of pure water
as standard Tstandard standard
temperature, K Tinterest
temperature of interest, K
24Estimated Water Saturation of Bitumen Sample
25T2 Distribution of Bitumen Sample at 60, 70, 80,
90 oC
26Bitumen HI has Incorrect Dependence on
Temperature unless Constrained by Proper Mo from
Curies Law
0.82
27Viscosity of Bitumen Estimated from Current
Correlation has Significant Discrepancy from
Experimental Value
28Intramolecular Dipole-Dipole Interactions
- Normalize relaxation time, viscosity and
viscosity/temperature ratio with respect to 2 MHz
- Rotational correlation time (McConnell, 1980)
- Normalized relaxation times by intramolecular
dipole-dipole interaction for spherical molecule
Here
29T1,LM T2,LM Normalized with 2MHz Larmor
Frequency
30Conclusions
- The echo spacing restriction of regular CPMG
measurement on highly viscous bitumen can be
overcome by specifying the M0 in CPMG raw data
and assuming lognormal distribution for bitumen
during the interpretation. - Apparent Mo of bitumen at low temperatures has
incorrect dependence on temperature due to the
loss of FID signal within initial decay period.
This can be fixed by using Curies Law. - Given proper Mo and cut-off between oil and
water, the HI and Sw can be evaluated by using
the new method. - The T1 and T2 of Athabasca bitumen follow the
trend of previous literature data. The existing
T2 vs. viscosity correlations, which are good for
the oil with relatively low viscosity, are not
suitable for the samples with extremely high
viscosity like Canadian bitumen.
31Acknowledgements
- The financial support of Consortium on
Processes in Porous Media at Rice University and
DOE is gratefully acknowledged. - Dr. Harold Vinegar is acknowledged for his
important advices. - Dr. Zvi Taicher is acknowledged for the use of
his 20 MHz Bruker spectrometer.