Soo Hyun Shin1, Dina Moazamian1, Arya Suprana1,2, Eddie Fu1,3, Saeed Jerban1, Hyungseok Jang1, Charles Ginsberg4, Susan V Bukata5, Yajun Ma1, Eric Y. Chang1,3, and Jiang Du1,2,3
1Department of Radiology, University of California, San Diego, La Jolla, CA, United States, 2Department of Bioengineering, University of California, San Diego, La Jolla, CA, United States, 3Radiology Service, VA San Diego Healthcare System, La Jolla, CA, United States, 4Department of Medicine, University of California, San Diego, La Jolla, CA, United States, 5Department of Orthopedic Surgery, University of California, San Diego, La Jolla, CA, United States
Synopsis
Keywords: Bone, Diabetes, Bone
Motivation: There is no standardized method to probe bone quality, a key determinant of bone fracture risk of type 2 diabetes patients.
Goal(s): We tested whether UTE quantitative MT (UTE-qMT) imaging and UTE-based water pool measurement can distinguish diabetic bones from healthy ones.
Approach: Twenty-two ex vivo human diabetic bones and 13 healthy ones were scanned with UTE-MT, proton density UTE, and inversion recovery UTE sequences to measure qMT parameters and fractions of pore and bound water pools.
Results: The proton exchange rates from UTE-qMT showed a significant decrease in diabetic bones.
Impact: The proton exchange rate
measured via UTE-qMT can distinguish diabetic bones from healthy ones. UTE-qMT
may provide insight into molecular-scale bone quality that explains the
increased fracture risk in type 2 diabetes patients despite the increased bone
mineral density.
Introduction
Diabetes is often followed
by an increased risk of bone fracture, assessed via measurement of bone mineral
density (BMD) by DXA and CT scans1. Yet, in the case of type 2
diabetes, a counterintuitive BMD increase is often reported despite the
increased risk of fracture2. While it is well known that not only
bone quantity but also quality, such as the degree of collagen crosslinking, is
a significant factor determining the fracture risk, there are no established
methods to noninvasively monitor such molecular scale features3.
Quantitative magnetization transfer (qMT) MRI has been widely studied not only
for quantifying macromolecular proton fraction (MMF) but also for probing
tissue microenvironment by measuring their exchange with surrounding water
protons4. The qMT technique was combined with ultrashort echo time
(UTE) MRI to acquire molecular information of short T2 tissues,
including cortical bones5. In this study, we examined whether
UTE-qMT can distinguish diabetic cortical bones from healthy ones. We also
tested the diagnostic potential of UTE-based measurements of pore and bound
water pools for diabetic bones.Methods
A total of 43 human ex vivo
femoral and tibial bone samples were scanned at 3T (MR750, GE Healthcare), of
which 8 samples were excluded from analysis due to other confounding complications
reported (control: n = 13, age = 46.4±10.9; type 2 diabetic: n = 22, age =
69.4±13.8). The bone samples were placed in Fomblin for a susceptibility-matching
purpose (Figure 1). An 8-channel head coil was used for scans, and MT-weighted
images, dual-echo proton density images, and inversion recovery (IR) images
were acquired. B1 maps and T1 maps were also acquired via
actual flip angle with variable repetition time (AFI-VTR) method for qMT
analysis6. Detailed scan parameters are summarized in Table 1.
Region of interest (ROI)-based UTE-qMT fitting was applied to a series of
MT-weighted images for measuring qMT parameters for each bone sample7. Porosity
index (PI) and suppression ratio (SR) were calculated by normalizing the PD-UTE
image by the second echo of the PD image (PI) and normalizing the IR image by the
PD-UTE image (SR), respectively8-10. A two-tailed t-test was
performed for statistical comparison between two groups with a significance
level of 0.05. The normality of the data was confirmed via the Shapiro-Wilk
test.Results
All the UTE scans
generated images with sufficient signal-to-noise ratio for quantitative
analysis (Figure 1). IR images effectively suppressed the long T2
signals from residual trabecular bones and fat. MT-weighted images generated
reliable ROI-based UTE-qMT fitting (normalized mean squared error < 1%,
Figure 2A) and subsequent qMT parameter measurements (Figure 2B). While other
qMT parameters did not show a significant difference between diabetic and
control bones, magnetization exchange rates showed a substantial difference
between the two groups (kab: 4.09±1.21 vs. 5.33±1.48 Hz, P = 0.011;
kba: 7.40±1.71 vs. 9.19±2.34 Hz, P = 0.013). While there were no
differences in PI and SR, T1 relaxation time showed a significant,
but not substantial difference between diabetic and control bones (368.05±23.08
vs. 351.48±22.58 ms, P = 0.047). Discussion
UTE-qMT, PD, and IR
sequences generated images with sufficient qualities for accurate quantitative
analysis. UTE-qMT analysis showed a reduced proton exchange rate between the water pool and macromolecular pool in diabetic bones while MMF
was preserved. The unchanged MMF may be
explained by the similar body mass index (BMI) of tissue donors between the two
groups (Diabetic: 24.8±5.2 vs. Control: 25.7±8.1, P = 0.686) in this study, as
BMI has been shown to be positively correlated with BMD11. The preserved MMF also aligns with the unchanged PI and SR. The
decreased exchange rates in diabetic bones may be due to the
glycation-associated collagen crosslinking, as proton exchange rates are
affected by the degree of crosslinking of macromolecules12,13. The
small increase of T1 relaxation time in diabetic bones despite the
preserved PI and SR may be due to altered water distribution after collagen crosslinking,
but further systematic investigation is needed to correlate these observations
with underlying pathology14. The UTE-qMT and water pool measurements
should also be compared with BMD in the future.
Conclusion
The proton exchange rate
between water and macromolecular pool measured by UTE-qMT is a potential
imaging marker for assessing the quality of diabetic bones, which cannot be
achieved by currently available diagnostic tools. Acknowledgements
The authors acknowledge grant support from National
Institutes of Health (R01AR062581, R01AR068987, R01AR075825, K01AR080257 and
R01AR079484, and RF1AG075717), VA Research and Development Services (Merit
Awards I01CX001388, I01CX002211, and I01BX005952), DFG (SE 3272/1-1) and GE
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