sylkirauhaskivet

Sylkirauhaskivet, also known as salivary stones or sialoliths, are calcified deposits that form within the salivary glands or their ducts. These stones are composed primarily of calcium salts, although other organic materials can also be present. The exact cause of sylkirauhaskivien formation is not fully understood, but factors such as dehydration, certain medications that reduce saliva flow, and trauma to the salivary glands are thought to contribute.

The most common symptom of sylkirauhaskivi is pain and swelling in the affected salivary gland, particularly during or after eating. This is because the stone obstructs the normal flow of saliva, leading to a backup and pressure buildup. The gland may feel hard and tender to the touch. In some cases, an infection may develop secondary to the blockage, causing fever and pus discharge.

Diagnosis of sylkirauhaskivien typically involves a physical examination, a review of symptoms, and imaging techniques. X-rays, ultrasound, or CT scans can help visualize the stones. Treatment depends on the size and location of the stone, as well as the severity of symptoms. Small stones may pass on their own or can be encouraged to pass with increased fluid intake and by stimulating saliva production through chewing gum or sour candies. Larger or persistent stones may require medical intervention, such as manual removal by a physician, or in some cases, surgical removal of the stone or even the affected salivary gland. Prevention strategies include maintaining good oral hygiene and adequate hydration.