Leonardo Brizi1, Marco Barbieri1, Claudia Testa1, and Paola Fantazzini1
1Physics and Astronomy, University of Bologna, Bologna, Italy
Synopsis
There is increasing interest in the study of water
content, compartmentalization, exchange and its interaction with collagen in
cortical bone for the evaluation of bone fracture risk. Here, we present the
NMR characterization of 1H nuclei signals of the cortical bone. Different
components (collagen, lipid, water) and different water compartments are
identified measuring NMR properties and self-diffusion coefficients. The exchange between collagen and water protons is observed and an average
residence time in the collagen is estimated. The results can contribute to optimize MRI protocols
specifically for bone imaging and to characterize the role of water in this
tissue.
INTRODUCTION
Reduced bone strength is associated to a loss of bone
mass, usually evaluated by the estimation of the Bone Mineral Density (BMD)
with Dual energy X-ray absorptiometry technique. BMD cannot fully explain the
mechanical properties for this tissue as well, since other determinants are
involved, and there is evidence of the significant role of water in its
mechanical properties (1, 2). There is increasing interest in the study of water
content, compartmentalization, exchange and its interaction with collagen in
cortical bone for the evaluation of bone fracture risk (3).
Recently, NMR/MRI studies (1, 4-5) have enabled
clinical imaging of cortical bone, giving a new perspective to the diagnosis of
bone diseases. Moreover, there is increasing awareness that also water content
have a role in determining the so- called “quality” of the bone. Here, we
present the NMR characterization of 1H nuclei signals, including water
content, compartmentalization, exchange and diffusion, whose knowledge may help
to optimize MRI protocols, and to characterize to role of water in the cortical
bone system by low field- low cost portable devices (6).
METHODS
One and two dimensional
1H-NMR analyses were performed on cylindrical pig cortical bone samples (diameter~ 1 cm, height~ 1.5 cm) cored from the pig shoulder as shown in Figure 1. NMR measurements were executed by both a laboratory device (JEOL C60 - homogeneous magnetic field B
0=0.473 T) and a low field portable, NMR single-sided device (MOUSE PM10, Magritek - inhomogeneous magnetic field with an average B
0= 0.327 T). In the homogeneous field, a one pulse sequence was acquired to determine the FID behavior and a IR-FID sequence to study the longitudinal relaxation time. By the single-sided device, the STE-CPMG sequence was performed to estimate
D-
T2 correlation function. Data inversions were performed using UPEN for 1D Inverse Laplace Transform (ILT) and I2DUPEN for the 2D ILT (7, 8).
RESULTS AND DISCUSSION
We characterized 1H spin pools as low and high mobility protons and water compartments (bound water and pore water) by means of the different combinations of the measured parameters. FID analysis identified a fast quasi-Gaussian (solid-like) component due to low-mobility nuclei (almost all collagen protons) with a relaxation time Tgauss in the range 10 μs – 20 μs and a slower exponential decay component due to the high-mobility 1H nuclei (tentatively water and lipid) as shown in Figure 2. The analysis of IR-FID data indicated that all the FIDs, obtained at the different inversion times, revealed the presence of two 1H spin groups. The filtering technique (9-10) allowed us to separate the signal of the solid-like and the liquid-like components for which the quasi-continuous T1 distributions were computed. Because a cross-relaxation effect was expected, we performed the inversion without imposing the usual non-negative amplitude constraint. The results, shown in Figure 3, indicated magnetization and/or proton exchange between the two spin pools. Moreover, the exchange of magnetization between low and high mobility protons was detected by a spin-group analysis. The exchange between collagen and water protons has been demonstrated with an average residence time in the collagen of ~220 µs (Figure 4). The results of the 2D inversion of the D-T2 raw data, obtained by the single-sided device, are depicted in Figure 5. The diffusion coefficient of liquid-like components in cortical bone had D values in the range (1.2 – 0.03) µm2/ms. Three main compartments were found: pore water, lipids and bound water; the latter was presumably constituted by a slower component, (loosely-bound water) and a faster one (bound water).CONCLUSION
Our results have further clarified compartmentalization, diffusion and exchange of water in cortical bone. Different components (collagen, lipid, water) and different water compartments, can be identified measuring different NMR properties (signal intensity and relaxation times) and self-diffusion coefficients, by diffusion-relaxation measurements. Therefore, our results show the possibility to develop a NMR method, based on low-cost, mobile and non-ionizing single-sided devices for the characterization of bone tissue properties, which can change in pathological conditions.
The longitudinal magnetization transfer and the proton chemical exchange
suggest caution in the interpretation of T2 data in cortical bone.
These results can contribute to optimize MRI protocols specifically for bone
imaging and to characterize the role of water in this tissue.
Acknowledgements
We acknowledge Ms
Roberta Fognani, Laboratory of Medical Technology, IRCCS Istituto Ortopedico
Rizzoli, Bologna IT, for the preparation of the samples, and
Fondazione del Monte di Bologna e Ravenna for the financial support to this project.References
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