The sequestrum appears radiographically dense (sclerotic/white) not because it is inherently more mineralized, but because the surrounding viable bone undergoes disuse osteoporosis as a reaction to chronic infection and immobility. The sequestrum itself is dead, avascular bone that has lost its blood supply and cannot remodel; it remains relatively unchanged in mineral content. The surrounding live bone becomes osteoporotic (darker/lucent), making the dead sequestrum appear relatively whiter by contrast. This radiographic appearance is a classic teaching point in chronic osteomyelitis and is fundamental to recognizing the sequestrum on plain films (Campbell's Operative Orthopaedics 14e; IDSA Osteomyelitis Guidelines).
Campbell's Operative Orthopaedics 14e; IDSA Osteomyelitis Guidelines
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