Andrew C Yung1, Emily Sullivan2,3, Jessica C Küpper2,4, Kirsten Bale1, Piotr Kozlowski1, and David Wilson2,4
1UBC MRI Research Centre, Radiology, University of British Columbia, Vancouver, BC, Canada, 2Centre for Hip Health and Mobility, Vancouver, BC, Canada, 3School of Biomedical Engineering, University of British Columbia, Vancouver, BC, Canada, 4Orthopaedics, University of British Columbia, Vancouver, BC, Canada
Synopsis
Keywords: Cartilage, Osteoarthritis, Strain
We present
a novel approach to cartilage multi-echo data where T2 reflects focal
changes in strain along the cartilage depth, and the signal
amplitude reflects a measure of water content which presents a simpler pattern of
change that reflects strain. Ex vivo
bovine knee samples were scanned at 9.4T while under load, with high resolution along the cartilage depth to allow
direct measurement of strain. Changes in water content were found to be more
spatially uniform than the complex depth dependence shown by T2, and showed a
high degree of correlation to whole-cartilage averages of bulk strain.
Introduction
Mapping of transverse relaxation time (T2)
has been investigated as a surrogate measure of strain in articular cartilage. This mapping may allow for the indirect detection
of abnormal tissue load response that has been implicated in the onset or
progression of osteoarthritis1,2. Cartilage T2 depends on a complex combination of proton density,
compartmental differences in water mobility, and collagen fibril orientation that
varies between the different zonal layers3. The resultant depth
dependence may complicate the detection of strain-related changes, especially
at clinically feasible resolutions where partial volume artifact across the
cartilage depth becomes significant.
This work explores the T2 response to strain at high resolution in ex
vivo bovine knee cartilage samples at 9.4T, and extracts a water content metric
which shows a simpler pattern of change that reflects strain.Methods
Five
previously frozen medial femoral and tibial osteochondral block pairs were
submerged in phosphate-buffered saline (PBS) within a uniaxial compressive
loading actuator4. Specimens were scanned in a
9.4 Tesla Bruker MRI scanner using a quadrature volume RF coil (inner diameter
= 72mm). Specimens were
scanned uncompressed and three more times at step loads with target bulk
compressive strains of 10%, 20%, and 30% with a 20-minute delay after initial
load application to allow creep to occur5. MSME data were acquired
(TE/TR = 9.22/4000 ms, 36 echoes, NA=3, scan time = 32 minutes, resolution = 0.0625x0.250
mm, slice thickness=1.6mm, 3 slices). Data was denoised6 and processed using NNLS with stimulated echo correction7, which produces T2 distributions that reflect both the weighted T2
average of the signal peak, and a water content metric that is calculated from
the integral under the signal peak. The
water content metric WC was calculated as
$$WC=\frac{signal\;integral\;under\;T2\;peak}{pixelwise\;average\;of\;signal\;integral\;from\;all\;pixels\;in\;femoral\;unloaded\;cartilage\;in\;the\;same\;slice}$$
This
normalization was undertaken mainly to account for signal differences between
slices due to magnetization transfer effects on cartilage in the interleaved
slices8. However, WC should still be considered a relative metric of water
content, since it does not fully account for all other scaling factors that affect
the absolute signal intensity.
Tibial
and femoral cartilage within regions of contact were manually segmented. The bulk strain εbulk as well as the relative change in the MRI metric mean ΔT2 or ΔWC was
calculated as follows:
$$ \epsilon_{bulk} = \frac{thickness_{compressed}-thickness_{uncompressed}}{thickness_{uncompressed}}$$
$$\Delta{metric} = \frac{metric_{compressed}-metric_{uncompressed}}{metric_{uncompressed}}$$
Results
Figure 1 shows
typical T2 distributions at the different load conditions (from the midpoint of
tibial cartilage depth, along the column marked with the green arrow in Figure
2), showing one salient T2 component in the distribution. Sagittal unloaded T2 maps in Figure 2a show a
depth dependence that roughly follows the cartilage zones as previously
reported9, with an initial T2 peak near the surface which decreases with
depth. Cartilage compression causes the T2
maxima to extend deeper into the cartilage in an arc that roughly follows the strain
profile along the cartilage length (Figure 2c).
Representative depth profiles in Figure 3a (located at the green arrows
in Figure 2) show that the T2 peak decreases in value as it moves deeper into
the cartilage with increasing load.
Conversely, WC shows a decrease with load that is much more uniform
throughout the cartilage, with a more gradual decrease with depth (Figures 2b,
3b). The scatterplot in Figure 4 shows
that for one representative specimen, ΔT2 extends
across a larger dynamic range but has higher variability, whereas ΔWC is
relatively smaller and more independent of strain. However, when overall cartilage averages of strain and
MRI metric changes from all samples were pooled together (Figure 5), ΔWC showed
a higher linear correlation with strain than ΔT2 (R2
= 0.60 vs. 0.27). The grouped femoral whole-cartilage
means showed no relationship between strain and changes in either MRI metric. Discussion
We observed a T2
depth dependence on strain that reproduces prior work10. Specifically, the changes under load were related to the changing
orientation of collagen fibrils, therefore changing their dipolar interaction
with the main magnetic field. The shape
of the T2 depth profile provides much information that could be used to quantify
local strain, but much of this utility is lost to partial volume artifact at
low image resolutions.
The spatial patterns and changes observed for the water
content matches well with our expectation that water concentration in unloaded
cartilage decreases monotonically with cartilage depth3, and further decreases with load as the increased hydrostatic
pressure causes fluid efflux. ΔWC showed a weak dependence on columnwise strain in the individual specimen but showed a stronger inter-specimen correlation with overall strain, suggesting that ΔWC is related more to global measures of strain. The water
content metric calculated in this study does not represent a true proton
density because it does not account for factors such as coil sensitivity and T1. Measurement of water content would be improved
by use of reference water phantoms and with more efficient pulse sequences11.Conclusion
We have identified
a novel approach to multi-echo spin-echo data analysis which uses T2 to
identify focal changes in strain along the cartilage depth, while also
detecting the overall whole-cartilage strain with the water content metric, in
a more robust manner that may be valuable at clinical resolutions.Acknowledgements
This research is funded by the Arthritis Society (Grant # 21-0000000129), a NSERC Discovery Grant (RGPIN-2019-06347), and Michael Smith Health Research BC.References
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