The additional value of an oblique image plane for MRI of the anterior and posterior distal tibiofibular syndesmosis
The optimal MRI scan planes of collateral ligaments of the ankle have been described extensively, with the exception of the syndesmotic ligaments. We assessed the optimal scan plane for depicting the distal tibiofibular syndesmosis.
Materials and Methods
In order to determine the optimal oblique caudal-cranial and lateral-medial MRI scan plane, two fresh frozen cadaveric ankles were used. The angle of the scan plane that demonstrated the anterior and posterior distal tibiofibular ligament uninterrupted in their full length was determined. In a prospective study this oblique scan plane was then used in addition to the axial and coronal planes, for MRI scans of both ankles in 21 healthy volunteers. Two observers independently evaluated the anterior tibiofibular ligament (ATIFL) and posterior tibiofibular ligament (PTIFL) regarding the continuity of the individual fascicles, thickness and wavy contour of the ligaments in both the axial and the oblique plane. Kappa was calculated to determine the interobserver agreement. McNemar’s test was used to statistically quantify the significance of the two scan planes.
In the axial plane the ATIFL was in 31% (13/42) partly and in 69% (29/42) completely discontinuous; in the oblique plane the ATIFL was continuous in 88% (37/42) and partly discontinuous in 12% (5/42). Compared with the axial plane, the oblique plane demonstrated significantly less discontinuity (p < 0.001), but not significantly less thickening (p = 1.00) or less wavy contour (p = 0.06) of the ATIFL. In the axial scan plane the PTIFL was continuous in 76% (32/42), partially discontinuous in 19% (8/42) and completely discontinuous in 5% (2/42); in the oblique plane the PTIFL was continuous in 100% (42/42). Compared with the axial plane, the oblique plane demonstrated significantly less discontinuity (p = 0.002), but not significantly less thickening (p = 1.00) or less wavy contour (p = 0.50) of the PTIFL. The interobserver agreement score and kappa (κ) regarding the continuity for the ATIFL in the axial and oblique planes was 91% (κ = 0.79) and 91% (κ = 0.55) respectively; for the PTIFL it was 86% (κ = 0.65) and 100% (κ = not defined).
The ATIFL and PTIFL are routinuely scanned in the orthogonal planes. The advantage of MRI scanning in an oblique image plane of about 45 degrees permits a better evaluation of the ligaments compared with the axial plane, particularly a better interpretation of ligament continuity, thickening and wavy contour. This may lead to a reduction in false-positive results, especially regarding partial or complete ligament ruptures. This can be of considerable aid in therapeutic management.
KeywordsAnkle MRI Oblique scan Tibiofibular syndesmosis
Anterior tibiofibular ligament
Posterior tibiofibular ligament
Injury of the distal tibiofibular syndesmosis occurs in approximately 1–11% of all ankle sprains [1, 2, 3]. This number may increase to more than 40% in those actively involved in high contact or collision sporting activities .
Syndesmotic instability in adults can be due to widening of the ankle mortise (complete tibiofibular diastasis) or to posterior translation and external rotation of the fibula (anterior tibiofibular diastasis). The latter is more common and more difficult to recognize. The chronic instability results from increased length of the syndesmotic ligaments that have healed and elongated after an acute rupture that was not adequately treated [5, 6, 7]. Lateral shift of the talus more than 2 mm and external rotation of the talus more than 5° reduce the mean joint contact area and increase the contact pressure in the ankle [8, 9]. Since widening of the ankle mortise by 1 mm decreases the contact area of the tibiotalar joint by 42%  this could lead to early osteoarthritis of the tibiotalar joint.
Radiography, arthrography, ultrasound, and CT have been used to assess the integrity of the syndesmosis. Several authors have described that radiography has limited use in the assessment of syndesmotic integrity [11, 12, 13]. Conventional X-ray arthrography is not routinely used anymore as it is an invasive examination, although it clearly displays syndesmotic and other ligamentous injuries [14, 15, 16]. Ultrasound can clearly depict a torn tibiofibular ligament in the acute stage but is less accurate over time and the results are very dependent on the skills of the radiologist . With the use of CT, widening of the mortise exceeding 3 mm can be reliably assessed, as well as gross deformity . However, external rotation of the distal fibula, such as that seen in anterior tibiofibular diastasis, is not easily recognized, because of the “round” shape of the fibula at that level.
The value of MRI in acute and chronic syndesmotic injuries has been described in several papers [19, 20, 21, 22, 23]. In these papers the usual three orthogonal scan planes (axial, coronal, and sagittal) and the position of the foot during imaging (neutral, 10–20° dorsiflexion or 40–50° plantar flexion) have been used to evaluate the optimal scan plane of both the collateral and the syndesmotic ankle ligaments [21, 23]. However, since the anterior and posterior distal tibiofibular ligaments run obliquely to the orthogonal planes , the axial scan plane may lead to a false-positive interpretation regarding the presence of a syndesmotic injury when MRI results are compared with operative findings [20, 25].
In the present study we assessed the additional value of an oblique scan plane for depicting the anterior and posterior distal tibiofibular syndesmotic ligaments in cadaveric specimens and validated this in healthy volunteers. The clinical relevance is illustrated with three clinical cases.
Materials and methods
In two fresh frozen cadaveric lower legs, amputated below the knee, we obtained images of the ankle in a 1.5 T MR (Philips Gyroscan, Best, The Netherlands). The legs were thawed for 24 h before scanning. We used a wrap-around surface coil (E1 coil). A T1-weighted turbo spin echo (TSE) sequence was acquired (TR 500 ms; TE 15 ms; TF 5) with a FOV of 12 × 12 cm, a matrix of 512 × 512 and slice thickness of 2.5 mm with a gap of 0.2 mm and NSA of 2.
After determination of the optimal angle of the oblique MRI scan plane, this plane was used in addition to the axial and coronal views to scan the syndesmosis of both ankles in 21 healthy volunteers (9 men, range 21–30 years, and 12 women, range 21–30 years). Inclusion criteria for the volunteers were: age over 18 years, no history of trauma in the past year, no previous surgery and no inflammatory disease of the ankle or foot. The same MR scanner and T1-weighted TSE sequences as in the cadaveric legs were applied. The anterior and posterior distal tibiofibular ligaments were evaluated with respect to continuity of the separate fascicles, thickening of the fascicles, and a wavy contour of the ligament . Regarding the continuity of the fascicles the ATIFL and PTIFL were assigned a score in both the axial and the oblique image planes: “zero” when none of the fascicles of the ligament between the tibia and fibula was interrupted (i.e., continuous), “one” when one or more, but not all of the fascicles, were interrupted (i.e., partly interrupted), and “two” when all fascicles were interrupted (i.e., completely interrupted). Thickening of the fascicles and a wavy contour of the ligament were scored as either present or absent.
The images were independently analyzed by two musculoskeletal radiologists with 10 (JH) and 30 (AG) years’ experience. The interobserver agreement was determined by the kappa agreement score (0.00–0.20: poor; 0.21–0.40: fair; 0.41–0.60 moderate; 0.61–0.80 good; 0.81–0.90: very good; 0.91–1.00: extra good). McNemar’s test was used to statistically quantify the significance of the axial and oblique scan planes regarding the continuity, thickening and wavy contour of the anterior and posterior distal tibiofibular ligaments, with a p value less than 0.05 considered significant. Statistical analysis was performed with Statistical Package for Social Sciences (SPSS) 15.0.
In three clinical cases the additional value of the oblique scan plane was demonstrated with respect to diagnosis and treatment.
When the ankle joint was imaged in the axial plane the fascicles of the anterior distal tibiofibular ligament appeared to be discontinuous between the anterior tubercle of the tibia and the anterior tubercle of the fibula. This apparent discontinuity slowly decreased when the 30° angle of the scan plane was increased by steps of 5°. At about 35° the uninterrupted ATIFL became visible and showed the multifascicular aspect of the ligament to good advantage. With a scan angle greater than 55° the fascicles appeared to be discontinuous again. The plane of 45° also demonstrated the posterior distal tibiofibular ligament in its full length. In both the coronal and sagittal planes the ATIFL and PTIFL were not depicted with as much detail as in the oblique plane.
Agreement score (AS [%]) and kappa (κ), regarding continuity, thickening, and wavy contour of the anterior tibiofibular ligament (ATIFL) and posterior tibiofibular ligament (PTIFL) in the axial and oblique planes of both ankles in 21 volunteers
Frequencies of ligament characteristics of ATIFL and PTIFL in the axial and oblique planes of both ankles in 21 volunteers. The fascicles are continuous (CO), or partially or completely interrupted (PI or CI)
Many studies have been carried out to determine the optimal plane for scanning the lateral collateral ankle ligaments with MRI. Only a few studies have been performed regarding the optimal scan plane for the syndesmotic ligaments [21, 23]. According to the literature the axial and coronal scan planes are optimal for depicting the ATIFL, PTIFL, and transverse ligaments, and the axial plane for the interosseous ligament. The basic concept is that a ligament is depicted best when the scan plane runs parallel to the direction of that ligament. Since the ATIFL and PTIFL run in an oblique direction with respect to the tibial plafond, imaging of the ATIFL and PTIFL should be optimal in an oblique plane, instead of the commonly used axial and coronal planes. As one can expect, an obliquely running ligament will likely show a partial or complete discontinuity when imaged in an axial plane.
The ATIFL has anteroposteriorly a triangular shape, is about 1 cm in height and has a thickness of 5 mm. It consists of three bundles, separated by 2-mm wide gaps that slightly converge in the laterodistal direction . The superficial anterior fibers are 2–3 cm long; the deeper posterior fibers are somewhat shorter . It extends in an oblique way between the anterior tubercle of the distal tibia and the anterior tubercle of the distal fibula and runs from medial-superior to lateral-inferior and crosses the anterolateral corner of the talus. The angle formed between a line along the tibial plafond in the coronal view and a line along the ATIFL varies from 30 to 50° [24, 28, 29, 30].
The PTIFL has a quadrilateral shape, is about 1 cm in height, 6 mm thick and 18 mm wide. Its fibers extend between the posterior tibial malleolus and the posterior tubercle of the fibula from medial-superior to lateral-inferior. It runs slightly more horizontally than the ATIFL .
Based on these data it seemed a logical step to introduce an oblique image plane for depicting the ATIFL and PTIFL. To find the optimal angle of this oblique plane we first used two cadaveric lower legs. We increased the angle gradually from 30 to 60° in steps of 5°. In the range of 35–55°, the individual fascicles of both the ATIFL and PTIFL were visible in their entire length. We finally chose an angle of 45° (in consensus JH, NW) as the optimal angle for the oblique image plane, as this angle has an upper and lower range of about 10° without the risk of not depicting the ligaments properly.
In our volunteers we analyzed the ATIFL and PTIFL with regard to continuity, thickening, and a wavy aspect of the ligament, since these are characteristics of ligamentous injury . In the axial plane the ATIFL and PTIFL were continuous in 0% and 76% respectively, while they were continuous in 88% and 100% respectively in the oblique plane. In the axial plane the fascicles were depicted as partly or completely interrupted. This could easily give the impression of a rupture of the ligament . An example of this problem is demonstrated in the paper by Oae et al. , where axial MRI images showed a rupture of the ATIFL in one patient and a rupture of the PTIFL in another, both of which proved to be incorrect at ankle arthroscopy. Since the range in the angle of the anterior distal tibiofibular ligament varies, not all of its fascicles will always lie in the oblique image plane of 45°, as occurred in 12% of the healthy volunteers.
Other characteristics of an injured ligament are thickening and a wavy aspect. In two volunteers, one or more of the fascicles of the ATIFL appeared to be thickened in the axial plane (in only one in the oblique plane). Bassett et al. described a thick inferior fascicle of the ATIFL as a possible cause of anterolateral tibiotalar impingement . The ATIFL consisted of two or three rather thick fascicles in some, and multiple thin fascicles in other volunteers. Since none of the volunteers had a history of serious ankle trauma or current ankle complaints, it is reasonable to assume that a thickened aspect of one or more of the fascicles, especially when present in both ankles, could be a normal variant. Possibly, the ATIFL is composed of a variable number of fascicles, with variable thickness, instead of the three mentioned by Bartonicek . Subhas et al. also mention a thickened inferior ligament (i.e., Bassett’s) in the presence of a normal ATIFL .
Although the agreement score regarding the different characteristics of the ATIFL and PTIFL was generally good (86–100%), the kappa value (κ), however, varied from fair to good (0.23–0.90; Table 1). For example, the agreement score regarding continuity of the PTIFL in the oblique plane was 100%, while kappa was only 0.65. Discrepancies between the percentage agreement and kappa values in our case can be explained by the skewed distribution of categories. In such cases kappa is known to have poor properties as an index for measuring agreement. With regard to continuity and the wavy aspect of the PTIFL in the oblique plane, the value for kappa could not even be determined .
We compared the oblique plane only with the axial plane and not with the coronal plane. The oblique and axial planes differ in only one parameter, i.e., the angle in which the ligaments are depicted, while the cross-sectional direction is the same; the oblique and coronal planes differ in two parameters, i.e., both in different cross-sectional directions as well as a different plane. Although the coronal view is good for depicting the multifascicular aspect of the ATIFL and PTIFL, in our volunteers the fascicles of the ATIFL and PTIFL were never entirely visible along their full length between their insertion onto the tibia and fibula. The coronal plane is therefore less suited for analysis of traumatic changes.
Our study has several shortcomings. First, we only used two cadaveric legs. It would be better to determine the range of angles of the ATIFL and PTIFL in a larger number cadaveric legs or volunteers. The ATIFL and PTIFL should perhaps each be scanned with a different optimal angle. Second, ideally, the best way to analyze the ATIFL and PTIFL would be to determine the exact angle of both ligaments in each individual separately. This would mean that in each individual first an axial and a coronal dataset should be acquired. Subsequently, in the axial plane the angle with the coronal plane could be established and next in the coronal images the angle with the axial plane. However, this would make it an elaborate and time-consuming procedure and not very practical. We therefore chose a fixed angle of 45° for the oblique MRI scan plane and accepted a small percentage (12%) of partly interrupted ligaments. Third, although the volunteers are healthy, it is unlikely that they had never had any previous ankle trauma. On average, almost everyone sustains an inversion injury of the ankle once during their lifetime. Thirty-nine percent of the volunteers had signs of minor injury of the collateral ankle ligaments, visible as a slight thickening of one or more of the collateral ankle ligaments. Although isolated injury of the syndesmosis, known as a high sprain, can occur, it often has a more protracted recovery period and therefore would be more easily remembered. On the other hand, minor syndesmotic injury could also go undetected and heal with a slight thickening or maybe wavy aspect of the ATIFL.
Clinically, information about the integrity of the syndesmotic ligaments is of importance, because it determines the kind of therapy the patient gets. The ATIFL in particular plays an important role in the stability of the syndesmosis. In the case of an isolated injury of the ATIFL (a high sprain), a complete rupture of the ATIFL should be treated with a non-weight-bearing cast or surgery, while a partly ruptured ATIFL can be treated functionally with a weight-bearing cast.
The MRI scans for the syndesmotic ligaments, ATIFL and PTIFL, have been carried out in the three usual orthogonal scan planes. The advantage of scanning in an oblique image plane of about 45° lies in better depiction of both ligaments compared with the axial plane, and with it a better interpretation of continuity, thickening, and wavy contour. This may lead to a reduction in false-positive results, especially regarding partly or completely ruptured ligaments, and can be of considerable aid in therapeutic management, as demonstrated by the three clinical cases.
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