Abstract
Background
The tibiotalar (TT), subtalar (ST), talonavicular (TN), and first metatarsophalangeal (MTP) joints of the foot and ankle are essential for foot mobility and function. Assessing progression of osteoarthritis (OA) in these joints involves subjective radiographic grading that lacks reliability and reproducibility. The purpose of this prospective comparative study was to define normal articular features and joint space width (JSW) in four joints of the foot and ankle using objective analysis of weight-being CT (WBCT) intensity profiles in healthy, non-arthritic subjects.
Methods
This was a cross-sectional IRB-approved study (ID #201904825) where bilateral WBCT scans of the foot and ankle were performed in 20 healthy subjects (40 feet, 9 females, 11 males) with no clinical or radiographic evidence of OA, bony abnormalities, or foot deformities. Five parallel linear spatial projections were generated across the joint space to measure WBCT intensities extending from subchondral bone, to cartilage, through the joint space, then to opposing cartilage and subchondral bone. The software graphically plotted WBCT intensity profiles of these projections which were then interpreted to measure the joint space width (JSW) and Michelson contrast of Hounsfield unit (HU) intensities, two relevant metrics of joint preservation, for each joint.
Results
The average JSW for healthy TT, ST, TN, and first MTP joints were 3.97 (95 % CI 3.73– 4.20), 4.20 (3.96– 4.44), 3.33 (3.07– 3.58), and 3.87 (3.64– 4.12) mm, respectively. The average Michelson contrast was 71.8 (95 % CI 67.32– 76.26), 92.5 (87.82– 97.08), 84.1 (79.25– 88.85), and 101.4 (96.87– 105.81), respectively.
Conclusion
We utilized a novel 3D analysis of WBCT intensity profiles to assess normal JSW and HU intensities in four joints of the foot and ankle to provide a foundation for future work developing an objective grading system for osteoarthritis.
1
Introduction
The prevalence of osteoarthritis (OA) has been steadily increasing due to a rise in the aging population. OA of essential articulations of the body affect at least one third of individuals over the age of 45, leading to pain, disability, and need for specialized care , .
There are four important articulations in the foot and ankle including the tibiotalar (TT), subtalar (ST), talonavicular (TN), and first metatarsophalangeal (MTP) joints. Biomechanically, these joints are key players in bipedalism, representing the joints with the greatest range of motion in the foot and ankle, responsible for dissipating energy during interaction of the foot with the ground, and thus, enabling gait . These joints are particularly susceptible to various foot and ankle pathologies, including OA ,,, . Degenerative changes in these articulations have an immense impact on patients’ function and quality of life, representing a substantial burden on the health care system .
Treatment planning relies upon a grading system to track the progression of OA. With ankle OA, treatments range from physical therapy, bracing, pharmaceuticals, to surgical options . Thus, it is imperative that OA grading systems are reliable and reproducible, supporting the best treatment options for these patients.
One of the first to define OA severity was Kellgren and Lawrence in 1957, which is most widely used today. This system assesses plain radiographic images assigns them into 5 different grading categories ranging from None (0) to Severe (4) based upon the presence and severity of osteophytes, ossicles, joint space narrowing, bony sclerosis, and deformity . Although this classification system is widely used in clinical practice, there are major limitations in their methods. First, the grading system is based on conventional 2D radiographic findings that are limited in their ability to convey the anatomical features of each joint under physiological weight bearing conditions. Second, they rely upon subjective measures whose inter-observer reproducibility ranks from fair to poor when studied , . Objectively staging OA in these essential joints remains a challenge due to the current methods in place.
The recent introduction of weight bearing CT (WBCT) allows for 3D imaging assessments of joints under physiological upright weight-bearing conditions, which is especially imperative in the setting of OA to provide a more accurate representation of local anatomy and disease progression , . This imaging allows for analysis of 3D CT intensity profiles by measuring Hounsfield Units (HU) along the transitions from cancellous bone, to subchondral bone, to the joint space, then back to subchondral bone and cancellous bone on the opposite side of the joint, independent from calibration technique and location of the measurement within the field of view . This can serve as an accurate basis for measuring joint space width (JSW) and bone quality distribution, as line intensity profiles drawn across each joint can capture changes in HU contrast given by bone, subchondral plate, and cartilage , . Tazegul et al. successfully demonstrated this capability of objectively measuring JSW in the tibiotalar joint from WBCT images, resulting in an HU-based algorithm . The purpose of this study was to apply this HU-based algorithm to four important articulations of the foot and ankle (TT, ST, TN, and first MTP joint), aiming to define normal articular features and average JSW in each joint that can serve as reference threshold values for future studies assessing OA severity. We hypothesized that 3D JSW and HU intensities across the joints would be significantly different from each other, respecting local anatomy and unique functional characteristics.
2
Methods
2.1
Participants
This was a cross-sectional IRB-approved study (ID #201904825) where patients signed a written informed consent. We enrolled healthy volunteers with no history of prior injury or surgeries in the foot and ankle. Inclusion criteria comprised of patients 18–70 years of age at the time of the WBCT scan. Each volunteer underwent bilateral WBCT imaging of the foot and ankle. The WBCT scan of each patient was evaluated at 4 joint sites (TT, ST, TN, and first MTP). Joints with no clinical or radiographic signs of OA or other bony abnormalities were selected to be included in the study for computational analysis of JSW using a HU-based algorithm . We excluded from the analysis patients with foot deformities (cavovarus, flatfoot, hallux valgus). A total of 20 volunteers (40 feet, 9 females/11 males) were initially enrolled. Three patients were excluded secondary to recognition of the presence of foot deformities. After excluding from analysis joints that had minor osteophytes or any other early OA signs, we finally analyzed 30 TT joints (13 L, 17 R), 28 ST joints (12 R, 16 L), 26 TN joints (11 R, 15 L), and 30 first MTP joints (14 R, 16 L). The average age and body mass index (BMI) for patients analyzed can be found in Table 1 .
Table 1
Age and BMI of included volunteers per joint analyzed.
| Joint | Number of joints analyzed | Age (Average, Range) | BMI (Average and SD) |
|---|---|---|---|
| Ankle | 30 | 37.5 (18– 64) years | 26.37 (±3.6) kg/m 2 |
| Subtalar | 28 | 36.5 (18– 64) years | 26.74 (±3.4) kg/m 2 |
| Talonavicular | 26 | 39.1 (18– 64) years | 27.00 (±3.3) kg/m 2 |
| 1 st Metatarsophalangeal | 30 | 37.3 (18– 64) years | 26.47 (±3.7) kg/m 2 |
2.2
WBCT imaging protocol
All volunteers were imaged using a cone-beam WBCT scanner (HiRise®, LLC, Warrington, PA, USA) with a kVp = 120 and an mA = 5. Images were acquired bilaterally while patients stood using full weight bearing capabilities and both feet pointing forward, shoulder-width apart, dividing the body weight evenly in both lower extremities. Images were reconstructed into 533 slices using 0.37 mm voxels with the reconstruction software provided with the scanner .
2.3
WBCT image analysis
When analyzing WBCT images, we used the method previously described by Tazegul et al. . CubeVue® software (CurveBeam LLC, Warrington, PA, USA), was used to reconstruct the images and present the 3D images in axial, sagittal, and coronal planes that could be adjusted.
Axial, sagittal, and coronal planes were defined by first positioning the multiplanar cross-sectional tool at the center of each joint, using midpoint linear measurements in the coronal and sagittal planes of the talar dome, talar posterior facet, navicular articular surface, and articular surface of the first toe proximal phalanx for the TT, TN, ST, and first MTP joints, respectively ( Fig. 1 ). The sagittal and coronal planes were selected by positioning crosshairs at the midpoint of the anteroposterior and mediolateral portion of the articular surface of the joint analyzed. Once the crosshairs were positioned in the center of the joint, they were rotated accordingly to ensure that the axial plane was always parallel to the articular surface of each of the joints.
Sagittal (A), coronal (B), and axial (C) plane positioning of the multiplanar cross-section in the central aspect of the tibiotalar, subtalar, talonavicular and first metatarsophalangeal joints.
Once the crosshairs were placed at the center of the joint space, the volume of interest (VOI) function of the software was used. This tool generated a 3D cube with a predefined VOI whose center was positioned in the crosshair location previously placed. For the TT, ST, TN, and first MTP joints, the VOI cube dimensions were 20x20x20mm, 20x20x20mm, 15x15x15mm, and 10x10x10mm, respectively. This software tool allowed the assessment of voxel intensity distributions within the selected VOI.
Once the VOI tool was selected, a HU heatmap automatically opened in a separate window of the software to visually represent the mean intensity of the voxels in the axial plane ( Fig. 2 ). For each joint analyzed, 5 parallel linear spatial HU projections were hand-placed on the heatmap perpendicular to the axial plane, traversing the joint. One projection was placed in the center of each quadrant of the cube, and one additional projection was placed in the center of the cube. Fig. 3 shows a 3D schematic of the VOI cube placed for the TT joint with the location of the 5 projections indicated . For the TT and ST joint, the four projections were placed in the anteromedial, anterolateral, posteromedial, and posterolateral quadrants of the joint. For the TN and first MTP joints, the four projections were placed in the superomedial, superolateral, inferomedial, and inferolateral quadrants.
Heat map (A) and graphical plots (B) of Hounsfield Unit (HU) intensity profiles for each projection placed inside the cubic volume of interest (VOI). Five points marked to generate HU distribution lines. Points 1–4 marked on the center of four quadrants (anteromedial, anterolateral, posteromedial and posterolateral for the ankle joint depicted in this image) (C) and Point 5 on the central aspect of the cube (D).
Three-dimensional volume of interest (VOI) in the shape of a cube, and positioning of a total of five Hounsfield Unit lines on the central aspect of four quadrants and central aspect of the entire cube. VOI for tibiotalar and subtalar joints as depicted here, measuring 20x20x20 mm. Dimensions for the talonavicular and first metatarsophalangeal joints were respectively 15x15x15 mm and 10x10x10 mm.
The software then generated a summary of the WBCT image HU intensities along the placed projection lines going across the joint space and graphed the intensities on a plot ( Fig. 2 B) . For example, the image intensity graph for the TT joint corresponds to the transition of distal tibia cancellous and subchondral bone, to the joint space, to talar subchondral and cancellous bone . These graphical plots of the image intensity profiles and HU distributions for each projection were then used to calculate JSW and HU contrast.
2.4
Computation of articular features
Each projection allowed for the computation of JSW and HU contrast at that specific location across each assessed joint ( Fig. 4 ). First, the two maximum intensity values (I max1 and I max2 ) on the graphical plot, coinciding with the opposing subchondral bone surfaces, were manually selected (two peak points on the graphical plot, Figs. 4 B and 4 C). Next, the minimum value within the same plot, corresponding to the joint space, was manually selected (I min ), corresponding to the lowest point on the HU intensity graph ( Fig. 4 C). To calculate JSW in millimeters, we calculated the voxel distance between the two maximum points selected (I max1 and I max2 ), multiplied by 20/54, which corresponds to the scale of millimeters for each voxel. Each joint had 5 different JSW values in millimeters corresponding to the 4 quadrants and center of the joint.
Example of a Hounsfield Unit (HU) intensity projection line crossing the tibiotalar joint (A). Graphical plot of the HU line/projection demonstrating the transition between cancellous bone, subchondral bone (peak), joint (valley), subchondral bone (peak) and cancellous bone (B). Calculation of Joint Space Width is performed in-between the two peaks in the graphical plot (subchondral bone to subchondral bone distance). HU Contrast is calculated following the depicted mathematical formula that takes into consideration the maximum and minimum HU values in the HU projection line.
To calculate the HU Michelson Contrast, which measures the difference in image intensity between the densest subchondral bone and that within the joint space, first the I max,avg was calculated by finding the average of I max1 and I max2 . Next, the following formula was used: HU Contrast = (I max,avg – I min )/(I max,avg + I min ) * 100.
2.5
Statistical analysis
Continuous data were analyzed for normality by the Shapiro-Wilk test. Descriptive statistics were utilized to describe distributions, mean/median values, standard deviations (SD) and 95 % confidence intervals (CI). JSW and HU Contrast data were then compared between each joint and among the different HU projections (four quadrants and joint center) by utilizing One-Way ANOVA followed by paired T-test analysis, or Kruskal-Wallis Rank Sum test, followed by paired-Wilcoxon depending on the distribution parameters of the data. P-values less than 0.05 were considered significant. All statistical analyses were performed using JMP Pro 16® software by an independent observer.
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