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The subtalar joint has a possible compensatory mechanism for supramalleolar deformities; the failure of this mechanism causes the progression of ankle osteoarthritis. However, the reason for this failure has not been fully elucidated. This study aimed to evaluate the characteristics of the morphologic changes in the subtalar joint in varus ankle osteoarthritis using computed tomography. The study included 30 patients with severe osteoarthritis (modified Kellgren-Lawrence classification grade ≥ 3; mean age: 68.5 years) and 30 patients without- or with early osteoarthritis (grade 0-1; mean age: 43.0 years) as the control group. The location of cysts, osteophyte formation in the subtalar joint, and thickness of the subchondral bone plate were evaluated. In the osteoarthritis group, cyst formation was observed on the posterolateral side of the posterior facet of the calcaneus in 6 cases (20%) and of the talus in 7 cases (23.3%). Osteophyte formation was observed in the talus in 21 cases (70.0%) and in the calcaneus in 29 cases (96.6%). Osteophyte formation was observed on the posterior or lateral side of the posterior facet, and osteophyte contact between the talus and calcaneus was observed. The subchondral bone plate of the posterior medial side of the posterior facet of the talus was significantly thicker in the osteoarthritis group. The subtalar joint is less affected in severe varus ankle osteoarthritis containing a thickened subchondral bone plate in the posteromedial aspect of the posterior talar facet.

Arthroscopic ankle arthrodesis (AAA) has advantages of being less invasive and achieving a high bone union rate. However, there are still some nonunion or delayed union cases, especially those of high-grade deformity. During AAA, curettage of the subchondral bone using an abrader burr provides bone debris, and there is the possibility of bone debris being used as autograft to improve bone union. The purpose of this study is to analyze bone debris histologically, and the effect of its implantation on bone union of AAA. Bone debris from 6 patients was collected during AAA. Bone debris/atelocollagen composite was made and cultured for 4 weeks. Histological analyses were performed before and after culture. Twenty-six patients with AAA were divided into 2 groups with or without bone debris implantation, and the time to union after surgery was evaluated. In histological analysis of bone debris/atelocollagen composite, bone debris contained bone, cartilage and synovium fragment at time 0. After 4 weeks of culture, osteocalcin positive cells migrated and proliferated in the gel. Ki67 positive cells significantly increased after culture. In clinical cases, time to union was significantly shorter in the bone debris group (9.3 ± 1.3 weeks) than that in the control (12.4 ± 3.1 weeks). This study showed that bone debris contained the osteochonductive and osteoinductive properties, and there is the potential for its implantation into the ankle joint to improve bone union in ankle arthrodesis.

Recent reports have described midterm natural courses of osteochondral lesion of the talus (OLT) and lack of progression of ankle osteoarthritis (OA) in adult patients. The relationship between the OLT managed with nonoperative treatment and development of OA in children remains unknown. We report the long-term course of medial OLT in a 12-year-old female who was treated nonoperatively for 10 years. Radiographically, no osteoarthritic changes were observed at the first examination. She initially returned to her basketball club after nonoperative treatment. Although daily activities were not restricted, limitation of recreational activities began to appear at 4 years of follow-up. Subsequently, plain radiographs revealed bone absorption around the osteochondral fragment and osteophyte formation at the medial gutter, then ankle OA was advanced at the final follow-up.