Fracture mapping of adult femoral neck fractures with three dimensional computed tomography

Purpose Femoral neck fractures (FNFs) are a commonly encountered injury in orthopaedic practice. It is essential that surgeons recognize specific fracture patterns to effectively manage these fractures. The purpose of this study was to analyze the fracture morphology of FNFs by three-dimensional (3D...

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Veröffentlicht in:International orthopaedics 2023-05, Vol.47 (5), p.1323-1330
Hauptverfasser: Öğümsöğütlü, Erman, Kılınçoğlu, Volkan
Format: Artikel
Sprache:eng
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Zusammenfassung:Purpose Femoral neck fractures (FNFs) are a commonly encountered injury in orthopaedic practice. It is essential that surgeons recognize specific fracture patterns to effectively manage these fractures. The purpose of this study was to analyze the fracture morphology of FNFs by three-dimensional (3D) mapping of the fracture. Methods The fracture line location and distribution of 120 FNFs were identified using computed tomography reconstructions. After segmentation and virtual reduction, the fracture line was revealed. The femoral neck region was divided into zones according to anatomical localization, and the zones through which the fracture lines passed were recorded. All fracture lines are superimposed on the standard model to create fracture mapping. Results A total of 120 patients with FNFs were analyzed. The mean age of the patients was 67 (18–96) years. Of all patients, 59 were male, and 61 were female. The most affected region was Zone 4. The least affected region was Zone 6. The displacement in Zone 1 and Zone 4 was found to be significantly higher. The displacement in patients under 65 years was found to be significantly higher. Zone 2 and Zone 5 involvement was significantly higher in patients under 65 years. Conclusion The fracture map showed fracture patterns of FNFs. It was found that fracture displacement and transcervical region involvement were more common in patients under 65 years. It was also found that the displacement rate was high in fractures of the subcapital region.
ISSN:0341-2695
1432-5195
DOI:10.1007/s00264-023-05742-9