Original contributionsMagnetic resonance imaging of cortical bone with ultrashort TE pulse sequences
Introduction
With virtually all forms of proton imaging used in clinical practice normal adult cortical bone has a short T2 and shows no signal. This lack of signal provides a constant background against which abnormalities can be recognised by their increase in signal, but it has meant that there has been no signal available to explore different conspicuity options with surrounding tissues, or to characterise normal cortical bone by measuring its relaxation times and studying the effect of contrast agent administration.
A potential method for detecting signal from cortical bone is the use of ultrashort echo time (UTE) pulse sequences where TE is reduced from the usual values for conventional T1-weighted clinical sequences of about 4–10 ms to 0.07–0.20 ms [1], [2], [3], [4], [5]. Using this approach it is possible to detect signal from cortical bone before it has decayed to zero. We report our initial experience using this technique in normal volunteers and patients.
Section snippets
Subjects and methods
Studies were approved by the institutional review board. Seven adult volunteers [aged 29–85 years, four males (M) and three females (F)], two children with congenital muscular dystrophy [aged 7 years (F) and 10 years (M)], two patients with fractured tibias and fibulas [aged 56 years (F) and 18 years (M)], one with malunion of a tibial fracture 4 years after injury [aged 31 years (F)], one with osteoporosis following childhood polio [aged 32 years (F)], one with idiopathic osteoporosis [aged 55
Results
Using fat saturation and a surface coil, moderate signal was seen from the cortical bone in the tibia (Fig. 1A). The signal from cortical bone was much lower on the second echo (TE=5.95 ms) but was rendered more obvious by the subtraction of the second echo from the first (Fig. 1C).
Fig. 2A is a ds STUTE image (TR=650, TE=0.08, TI=80 ms image with the later echo [TE=5.95 ms] image subtracted from it). Cortical bone has a positive signal and is surrounded by a rebound (or cancellation) line from
Discussion
Signal was detected from cortical bone in all cases. In general, signal was apparent with the first echo (UTE) image but very low or zero on subsequent echoes. Intravenous contrast enhancement produced an increase in signal on the first echo and difference images.
Difference images were useful. Even though cortical bone had only a moderate signal on the first echo with many sequences, it had the shortest T2 of the tissues examined and generally showed the largest difference in signal between the
Conclusion
Signal from cortical bone is now detectable in clinical MR studies and may show changes in disease of diagnostic value. These may prove to be complementary to the detailed studies already performed on trabecular bone [23] and provide a clinical application for findings already demonstrated in studies of in vitro bone samples [24], [25], [26] and with UTE phosphorus imaging [27].
Acknowledgments
We wish to thank Dulcie Rodrigues for preparation of this manuscript as well as the Arthritis Research Council for their support.
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