- Original Article
- Open Access
A radiological classification system for talocalcaneal coalition based on a multi-planar imaging study using CT and MRI
Insights into Imaging volume 4, pages 563–567 (2013)
To develop a radiological classification system for talocalcaneal coalition suitable for adults.
Methods and materials
A retrospective review was performed on patients diagnosed with talocalcaneal coalition from July 2001 to November 2011. Based on the cartilaginous or bony nature, facet joint orientation and bony structure morphology, we classified talocalcaneal coalitions into four types: I (linear with or without posterior hooking), II (talar overgrowth), III (calcaneal overgrowth) and IV (complete osseous).
Seventy feet (59 patients) with talocalcaneal coalition were evaluated by CT (61/70 feet) using multi-planar reformation and/or magnetic resonance imaging (43/70 feet). Type I, II, III and IV coalitions were detected in 45 (64 %), 10 (14 %), 13 (19 %), and 2 feet (3 %), respectively. Fracture fragments were observed in 16 feet (seven Type I and nine Type III coalitions) with hooked or overgrown calcanei and in one foot in the talus (Type I). Eleven patients had bilateral talocalcaneal coalitions; ten patients had coalitions of the same type and one had both Type I and Type III coalitions. Among 48 patients with unilateral involvement, the left and right feet were affected in 26 and 22 patients, respectively.
A classification system for talocalcaneal coalition based on multi-planar imaging studies was developed.
• A classification system for talocalcaneal coalition based on multi-planar imaging was developed.
• The relative frequencies of different talocalcaneal coalition types were determined.
• Fracture fragments were easily distinguished and frequently originated from the calcaneus.
• Fracture fragments were mostly associated with Type I (linear) with posterior hooking and Type III (calcaneal overgrowth).
Tarsal coalition is defined as an abnormal union between two or more tarsal bones and is recognised as a common cause of rigid flatfeet. Tarsal coalition may be fibrous (synfibrosis or syndesmosis), cartilaginous (synchondrosis) or osseous (synostosis) in nature. The two most common coalitions are talocalcaneal and calcaneonavicular coalitions. The cause of tarsal coalition is reported to be a failure of segmentation of the primitive mesenchyme during development . Tarsal coalitions are clinically significant because they prevent normal joint motion, and they are frequently associated with non-traumatic pain and cavus foot deformity [2–6].
After the anatomical nature of talocalcaneal coalition was reported , its radiographic signs and findings were described in multiple reports [8–10]. The introduction of computed tomography (CT) and magnetic resonance imaging (MRI) improved the understanding of the anatomic properties and characteristics of talocalcaneal coalition [11–19]. Based on three-dimensional (3D) reconstructions, one report classified talocalcaneal coalition of children into five types (linear, linear with a posterior hook, shingled, complete osseous and posterior) and attempted to provide helpful information for surgical planning . However, in our experience with adult patients, there are many cases of talocalcaneal coalition with superiorly overgrown calcanei covering the calcaneal articular facet of the talus that could not be classified into any of these five types. Therefore, in this study, we devised a new radiological classification system for talocalcaneal coalition encompassing cases of talocalcaneal coalition with a superiorly overgrown calcaneus covering the calcaneal articular facet of the talus.
Materials and methods
After obtaining approval from the Institutional Review Board, we retrospectively collected cases by searching the clinical database using the search terms of “coalition”, “tarsal coalition” and “talocalcaneal coalition”. A total of 77 patients were identified from July 2001 to November 2011. All of the patients were soldiers or officers in the Korean military. Of these patients, data from CT or MRI, or both types of imaging, were available on our picture archiving communication system (PACS) for 65 patients. Two experienced radiologists (H.K.L. with 24 years of experience and S.L. with 4 years of experience) reviewed CT and MR images and identified 59 patients with talocalcaneal coalition. The remaining six patients diagnosed with calcaneonavicular coalition were excluded.
As defined by the ankle CT protocol at our institution, all patients were positioned supine on the examination table with the bottom of the affected foot placed against a positioning box. Each affected foot was scanned from the bottom proximally through the ankle joint using one of the following CT machines: MX8000 (Philips Medical Systems, Best, The Netherlands), SOMATOM Sensation 4 (Siemens Healthcare, Forchheim, Germany) or Brilliance 64 (Philips Medical Systems). All examinations were performed without intravenous contrast enhancement. Axial, direct coronal and sagittal reformatted images were obtained in cases before the 64-channel CT machine equipped with volume-rendering software was available. In cases after the 64-channel CT machine became available, the raw axial 2D CT data were uploaded to a workstation, and volume-rendering software was used to reconstruct the sagittal and coronal planes using a standard algorithm.
As defined by the ankle MRI protocol at our institution, all patients were positioned supine on the examination table within the magnetic bore. We obtained five series of MR images, including coronal fast spin echo (FSE) T2-weighted images with fat suppression (TR/TE, 2,816/96 ms), sagittal SE T1-weighted images (TR/TE, 527/20 ms), sagittal FSE T2-weighted images with fat suppression (TR/TE, 2,816/96 ms), axial SE T1-weighted images (TR/TE, 414/40 ms), and axial FSE T2-weighted images with fat suppression (TR/TE, 4,022/96 ms), using MRI machines (MAGNETOM Symphony 1.5 T; Siemens Healthcare/Signa Excite 1.5 T; GE Healthcare, Milwaukee, WI, USA).
After all of the images had been reviewed by two radiologists and a consensus was achieved, the cases were classified as Type I, II, III or IV coalition (Fig. 1) as follows: Type I, linear, parallel, or nearly parallel to the adjacent subtalar joint on the same plane, with or without posterior hooking (Fig. 2); Type II, inferiorly overgrown talus covering the talar articular facet of the calcaneus; Type III, superiorly overgrown calcaneus covering the calcaneal articular facet of the talus; Type IV, complete osseous. We also evaluated the presence of fracture fragments and their origin. The origin of fracture fragments was determined by the surface margin, displacement and signal changes on CT and MRI (Figs. 3 and 4).
To compare fracture sites between the talus and calcaneus, a chi-squared test was used. In statistical comparisons, p values less than 0.05 were considered statistically significant. Statistical analysis was performed using statistical software (Excel; Microsoft Corporation, Redmond, WA, USA).
Among 59 patients diagnosed as talocalcaneal coalition, 11 patients (19 %) had bilateral coalitions. In ten patients, the bilateral coalitions were of the same type, and one patient had Type I and Type III coalitions. Among the remaining 48 patients (71 %) with unilateral involvement, the left and right feet were affected in 26 and 22 patients, respectively. For these 70 feet, 45 (64 %), 10 (14 %), 13 (19 %) and 2 (3 %) coalitions were classified as Type I, II, III and IV coalitions, respectively (Table 1).
Most of the coalitions (90 %, 63/70 feet) involved the middle talocalcaneal joint. Four and two feet displayed coalition at the middle/posterior and posterior joints, respectively, and all of these coalitions were Type I coalitions. A Type IV coalition involving the anterior/middle joint was detected in one foot.
Fracture fragments were found in 17 feet (24 %, 17/70 feet); eight Type I and nine Type III coalitions. The fragments more frequently originated from the calcaneus (16 feet; p < 0.05). All of the fractures appeared to occur in overgrown or hooked bone. A fragment in one foot that originated from the talus was classified as Type I.
Bone marrow oedema at both bones was evident in 37 (86 %) of 43 feet with MRI data. In five feet (12 %, 5/45 feet) of three Type I and two Type III coalitions, bone marrow oedema was equivocal at both bones; in one type I foot (2 %, 1/45 feet), bone marrow oedema was evident in the calcaneus but equivocal in the talus. Clinically, pain at rest that increased with athletic activity was the major symptom and was reported in 60 (86 %) of 70 feet. Among the ten feet without clinical symptoms, seven Type I, one Type II and two Type III coalitions were observed.
Posterior talar hooking and posterior calcaneal hooking were detected in 25 and 5 feet with Type I coalitions, respectively. All five feet with posterior calcaneal hooking involved the posterior talocalcaneal joint, and the middle joint was also involved in three of these feet.
Until the early 1980s, talocalcaneal coalition was diagnosed using standard X-ray, which is still commonly used for screening purposes. However, radiographic confirmation of talocalcaneal coalition was more difficult than for fusion at other locations . Additionally, in the present study, only 23 % of the coalitions could be diagnosed by X-ray. Even in those cases, either subtyping or detection of fracture was not possible.
Since the introduction of CT and MRI, both imaging modalities have been used to differentiate osseous from non-osseous coalition and depict the extent of joint involvement and secondary degenerative changes, which are vitally important for surgical planning. Short inversion time recovery MRI may reveal bone marrow oedema along the margins of abnormal articulation, an important clue for the diagnosis [17, 21, 22]. Frequently, CT or MRI is required to confirm the diagnosis of talocalcaneal coalition when radiographic findings are equivocal. Occasionally, tarsal coalition may be encountered incidentally during the evaluation of adolescent feet for other indications .
In this study, we analysed the characteristics of talocalcaneal coalition among 70 feet, which is the largest collection to our knowledge. The frequency of complete osseous coalition was lower than expected, particularly in comparison with a previous report based on adolescent patients . In addition, we did not find the peripheral posterior coalition reported previously . We suggest two reasons for these discrepancies. First, during the health-screening process for military recruitment, subjects with complete osseous coalition are more likely to have been excluded because it is a disadvantageous factor. Second, in adults, complete or peripheral posterior osseous coalition is typically asymptomatic. Thus, a subject with complete osseous coalition would be less likely to visit a hospital.
It is worth noting that most of the cases involved the middle talocalcaneal joint. Only two cases involved the posterior joint instead of the middle talocalcaneal joint, and both of these cases involved Type I coalitions. Four additional Type I cases exhibited coalition with middle/posterior involvement. All Type II and III coalitions involved only the middle talocalcaneal joint.
The probability of associated fractures in talocalcaneal coalition has not been reported previously. In this study, fracture fragments were detected at a frequency of one out of four cases. Most of these originated from the calcaneus, and all of these cases involved either Type I coalitions with posterior calcaneal hooking or Type III coalitions. A fragment originating from the talus was detected in one Type I coalition with posterior talar hooking. Fracture fragments were significantly more likely to originate from the calcaneus than from the talus (p < 0.05). In most cases, the origins of fracture fragments were easily distinguished by evaluating either CT or MRI findings. In particular, the margin changes, direction of displacement and/or signal changes on MRI were extremely helpful (Fig. 4). Because there is a chance that the fracture fragments cause symptoms, it is advantageous to report their presence so that surgeons can consider their removal. In addition, in Type I with posterior calcaneal hooking or a Type III coalition, the presence of fracture fragments should be monitored more carefully.
Bilateral coalitions were found only in 11 of 59 patients (19 %), which was much lower than the findings of a previous report (63 %) . This likely originated from the selection bias of our study. This study only included members of the Korean military, which has a pre-screening system for the recruitment of candidates for officers and soldiers.
While evaluating the cases enrolled in this study, we developed an efficient scheme for classifying and describing talocalcaneal coalition. With coronal images, the type of coalition can be determined. Then, the presence of talar or calcaneal hooking can be detected on sagittal images. The presence of fractures and their origin can be detected using either CT or MRI. This classification system provides information regarding the incision site and approach of resection to surgeons. Additionally, fracture fragments would be more thoroughly searched in Type I with posterior calcaneal hooking and Type III coalitions. The limitation of the present study lies in its retrospective nature. Moreover, the present study is a single-centre study including only male soldiers and officers.
In conclusion, we established a classification system for talocalcaneal coalition suitable for adult patients and report that the probability of associated fractures is 24 %. The fractures mostly originated from the calcaneus and were associated with Type I coalition with posterior hooking or Type III.
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Lim, S., Lee, H.K., Bae, S. et al. A radiological classification system for talocalcaneal coalition based on a multi-planar imaging study using CT and MRI. Insights Imaging 4, 563–567 (2013). https://doi.org/10.1007/s13244-013-0267-3
- Talocalcaneal coalition syndrome
- X-ray computed tomography
- Magnetic resonance imaging