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Description: Condensing osteitis is a reaction to infection. It differs from other periapical inflammatory diseases in that there is a bone production rather than bone destruction. The result is a radiopaque lesion. This sclerotic reaction is apparently brought about by good patient resistance coupled with a low degree of virulence of the offending bacteria. It is more commonly seen in the young and seems to show special predilection for the periapical region of lower molars. The associated tooth is carious or contains a large restoration. Whether or not the pulp is irreversibly diseased is not known. Current level of knowledge suggests that the pulp is irreversibly inflamed. Uncommonly, condensing osteitis occurs as a reaction to periodontal infection rather than dental infection.
# OM032 |
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