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Fast spin echo MRI of reservoir core plugs with a variable field magnet
Rheya Rajeev1, Andrés Ramírez Aguilera2, Florea Marica2
1UNB MRI Centre, Department of Physics, University of New Brunswick, Fredericton, New Brunswick, E3B 5A3, Canada; Department of Chemical Engineering, University of New Brunswick, Fredericton, NB E3B 5A3, Canada.
Abstract:
Fast Spin Echo MRI is now widely employed in biomedicine for proton density and T2 contrast imaging. Fast Spin Echo methods provide rapid data acquisition by employing multiple echoes to determine multiple k-space lines with single excitations. Due to the multi-exponential behavior of T2 in typical porous media, and the strong dependence of T2 on the details of the experiment, acquiring a proton density image with Fast Spin Echo methods requires favorable sample and acquisition parameters. In recent years, we have shown the value of pure phase encode Free Induction Decay based methods such as SPRITE. However, in a reservoir rock, a typical T2* is hundreds of µs, whereas a typical T2 is hundreds of ms. Hence, there is merit in considering spin echo-based MRI measurements such as the Fast Spin Echo for rock core plug studies. A variable field superconducting magnet was employed in this study. This is a new class of magnet for MR/MRI. These magnets have the flexibility of operation in the field range of 0.01 Tesla to 3 Tesla. This is advantageous when working with rock core plugs, as it allows one to maximize sample magnetization, by increasing the static field while controlling magnetic susceptibility mismatch effects, and thereby T2 and T2*, through reducing the static field. The magnetic fields employed in the study were 0.79, 1.5, and 3 Tesla. Measurements were undertaken on five brine-saturated reservoir rock core plugs (Bentheimer, Berea, Buff Berea, Nugget, and Wallace). The results show that Fast Spin Echo measurements are more sensitive than SPRITE methods in amenable samples and usually feature higher resolution. Quantification of saturation with Fast Spin Echo methods requires correction for T2 attenuation. The results also show that 3 Tesla is too high a static field in general for rock core MRI studies with either method. While the current study is focused on five representative reservoir rock cores, the conclusions which result are general for MRI of fluids in porous media.
Insights
Fast Spin Echo MRI offers higher resolution and sensitivity for porous media studies compared to SPRITE methods. However, 3 Tesla magnetic fields are generally too high for accurate rock core MRI analysis.
Area of Science:
- Geophysics
- Materials Science
- Biomedical Engineering
Background:
- Fast Spin Echo (FSE) MRI is crucial for proton density and T2 contrast imaging in porous media.
- Acquiring accurate proton density images with FSE requires optimized parameters due to multi-exponential T2 behavior.
- Previous studies highlighted the utility of Free Induction Decay methods like SPRITE for reservoir rock analysis.
Purpose of the Study:
- To evaluate the efficacy of Fast Spin Echo MRI for studying fluids in reservoir rock core plugs.
- To compare the performance of FSE with SPRITE methods across various magnetic field strengths.
- To determine optimal magnetic field conditions for MRI of porous media.
Main Methods:
- Utilized a variable field superconducting magnet (0.01 T to 3 T) for MRI measurements.
- Conducted experiments on five brine-saturated reservoir rock core plugs (Bentheimer, Berea, Buff Berea, Nugget, Wallace).
- Employed magnetic fields of 0.79 T, 1.5 T, and 3 T for comparative analysis.
Main Results:
- Fast Spin Echo MRI demonstrated superior sensitivity and resolution over SPRITE in suitable samples.
- T2 attenuation requires correction for accurate saturation quantification using FSE.
- A 3 Tesla field strength was found to be generally excessive for rock core MRI studies with both FSE and SPRITE.
Conclusions:
- Fast Spin Echo MRI is a valuable technique for analyzing fluids in porous media, offering enhanced resolution.
- Variable field magnets provide flexibility in optimizing MRI experiments for specific samples like rock cores.
- Careful selection of magnetic field strength is critical for accurate MRI characterization of porous materials.
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