Ashley A. Williams1,2, Karyn E. Chappell1,2, and Constance R. Chu1,2
1Orthopaedic Surgery, Stanford University, Stanford, CA, United States, 2Veterans Affairs Palo Alto Health Care System, Palo Alto, CA, United States
Synopsis
This study evaluated deep
cartilage and meniscus UTE-T2* against spatially targeted arthroscopic assessments
in patients with degenerative meniscus tears to further inform interpretation and
utility of in vivo UTE-T2* for different degrees of pathology. While
arthroscopic evaluation confirmed that UTE-T2* was elevated in menisci with
degenerative fraying and tears, increasing intra-operative cartilage grade was not associated with strictly increasing cartilage
UTE-T2*. Instead, in osteoarthritic disease states where the articular surface
of cartilage is disrupted, this report suggests that mono-exponential deep
cartilage UTE-T2* may not be a reliable indicator of tissue pathology.
Introduction
Utility of compositional MRI UTE-T2* for evaluation
of cartilage and meniscus subsurface properties has been shown in
pre-osteoarthritis (pre-OA) where patients largely retain intact articular
surfaces and the underlying tissue is still relatively healthy.1-6
Compared to pre-OA, patients seeking
treatment for degenerative meniscal tears (DMT) exhibit a wider range of cartilage
disease.7 Evaluation of deep cartilage
and meniscus UTE-T2* against spatially targeted arthroscopic assessments in DMT
patients may further inform interpretation and utility of in vivo
UTE-T2* for different degrees of pathology. The hypothesis of this study is
that articular cartilage and meniscus damage in osteoarthritis (OA) manifest as
elevated UTE-T2*. Thus, increasing intra-operative cartilage grade and
worsening meniscus status will be associated with increasing UTE-T2* values in
deep cartilage and menisci of DMT patients.Methods
Sixty-six subjects (32 DMT, mean age
49±15yrs; 34 uninjured controls, mean age 26±7yrs) participated in these
IRB-approved studies and underwent 3T MRI (GE Healthcare) with an 8-channel
knee coil. UTE-T2* maps were calculated via mono-exponential fitting
T2*-weighted images acquired at eight TEs (32μs -16ms, non-uniform echo
spacing) using a radial-out 3-D Cones acquisition.8 Deep articular cartilage
(extending from the bone-cartilage interface through half the cartilage
thickness) was manually segmented in 4 regions to central, weight-bearing medial
and lateral femoral and tibial cartilage (cMFC, cLFC, cMTP, cLTP).4 Anterior and posterior
meniscal horns were segmented from medial and lateral compartments (AMM, PMM,
ALM, PLM).6
UTE-T2* maps and mean values were calculated with MRIMapper (MIT). In DMT subjects, targeted intraoperative
arthroscopic exams, within a median of 11 days following the pre-operative MRI,
were conducted in areas corresponding to MRI study regions and were evaluated
using a modified Outerbridge scale: (0-normal; 1-softening; 2-partial thickness
defect, superficial fissures; 3-fissuring to subchondral bone; 4-exposed subchondral
bone). UTE-T2* values were compared to the surgeon’s assessment of meniscus
status or grade of cartilage damage as the standard. Normality of all data sets
was examined with Shapiro Wilts tests. ANOVA (or Kruskal-Wallis for
non-normally distributed data) was used to assess UTE-T2* differences by
meniscus status (intact, frayed or torn), by DMT cartilage grade (0,1,2,3,4),
and by cartilage status (control, DMT-intact but softened (grade 1), DMT-disrupted
(grade 2+)). Bonferroni adjustment
accounted for multiple comparisons in post-hoc pairwise analyses. Results
The distribution of arthroscopically
confirmed meniscus pathology is shown in Table 1 along with UTE-T2* meniscal
indices, determined by averaging UTE-T2* values across anterior and posterior
horns of each meniscus. Torn medial,
lateral menisci had 37%, 53% higher UTE-T2* indices, respectively, than intact
menisci, and there was a trend for higher UTE-T2* values in torn menisci
compared to frayed, Table 1. Medial and lateral meniscal indices of controls
(n=34) are 39%, 45% lower than those of DMT subjects (n=33; p<0.0005,
0.0005).
The distribution of Outerbridge
cartilage grades, mean UTE-T2* values for each grade, and differences between
grades are shown in Table 2. Additional analyses by cartilage status found that
mean deep cartilage UTE-T2* beneath disrupted articular surfaces (grades 2+) was
not elevated compared to control levels in any region (p>0.05), Figure 1. Although differences
by status did not reach statistical significance, in 3 of 4 regions examined,
mean UTE-T2* values of DMT subjects were higher
in cartilage that was softened-but-intact and were lower in cartilage with a disrupted articular surface, compared to
control levels, Figure 1. Sample DMT and uninjured UTE-T2* maps are shown in
Figure 2.Discussion
Arthroscopic evaluation confirms
that UTE-T2* is elevated in menisci with degenerative fraying and tears. This
finding extends previous observations of elevated meniscal UTE-T2* observed in
ACL-injured patients at heightened risk of developing OA1; 6
to the DMT population where quantitative measures to objectively stratify
intrasubstance pathology are lacking.9; 10 Further, it suggests that elevated UTE-T2* in
intact menisci might be a precursor to subsequent degenerative fraying or tear.
In DMT subjects’ deep cartilage, however,
increasing intra-operative cartilage grade was not associated with increasing UTE-T2*. Instead, DMT cartilage with disrupted
articular surfaces exhibited variable UTE-T2* values with mean levels similar
to or lower than controls. Several
prior reports noted decreased T2* with histologically11; 12
and arthroscopically13
confirmed cartilaginous degeneration. While T2* decreases observed in femoral
acetabular impingement have been attributed to delamination and subsequent fibrocartilage
transformation,14 such phenomena are not commonly
described in idiopathic knee OA. Therefore, relatively low UTE-T2* values in
deep knee cartilage of DMT patients found to have articular disruptions at
arthroscopy may be due to an escape of mobile water from deep cartilage that
occurs with the breach of superficial cartilage. Such an escape may cause greater weighting of
mono-exponentially calculated UTE-T2* values toward the remaining immobile
collagen-bound water protons that exhibit very short T2* relaxation decays.12; 15 Multicomponent T2* analyses may permit better
understanding of the deep molecular changes accompanying surface disruptions. The
distinction between surface-intact pre-OA and more advanced disease with cartilage
surface disruption is important to delineating the potential limitations of
UTE-T2* which has been shown to indicate subsurface changes in pre-OA patients whose
articular surfaces remain largely intact.1-6Conclusion
In OA
disease states where the articular surface is disrupted, this report suggests
that mono-exponential deep cartilage UTE-T2* may not be a reliable indicator of
tissue pathology. Acknowledgements
NIH RO1 AR052784 (PI – CR Chu) and DOD
W81XWH-18-1-0590 (PI-CR Chu) and GE Healthcare for MRI scan time and sequence
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