ABSTRACT
Background: The Schatzker classification system for tibial plateau fractures is one of the most commonly used systems. However, there has been controversy if a Schatzker III type fracture truly exists by their original definition. We aimed to correlate the radiographic and CT images of type III fractures, describe the additional propagating fracture patterns and determine if these fractures do exist by their original description. Methods: This multicenter retrospective cohort observational study included patients with tibial plateau fractures across five trauma centers over 9 years were identified. All X-rays and CT scans were assessed. Two independent fellowship trained, Orthopaedic trauma surgeons reviewed all knee X-rays and classified them according to the Schatzker system. The CTs were subsequently reviewed and the fractures were reclassified based on CT findings. Results: 569 Tibial plateau fractures in 566 patients were analyzed. All X-ray classified Schatzker III fractures were reclassified to a Schatzker II type after review of CT scans by both assessors independently as there were always at least two or more fracture lines propagating from the depressed fragment to the lateral cortex in all cases. The interobserver variability as assessed by the kappa correlation coefficient (κ) for X-rays and CT-based classifications were κ = 0.274 and κ = 0.906, respectively. The majority of cases had two lateral cortical breaks (83.8%). In addition, the depression occurred mostly in the anterolateral and posterolateral positions (60.3%) of the lateral tibial plateau. Conclusion: This study did not support the existence of true Schatzker Type III fractures.
