Get Permission Jambhulkar, Palve, Mohite, Udapure, Bodele, and Borkar: Sialadenitis associated with Sialolith- A Case Report


Introduction

Inflammation of the salivary gland is a usual presentation. Most of the conditions of the salivary glands involve predominantly the parotid gland followed by the submandibular and sublingual gland. Inflammation of the salivary glands is termed Sialadenitis. It is an insidious inflammatory disease of the major salivary glands characterized by intermittent swelling of the glands. The most common etiology is thought to be of viral infection including Coxsackie A, ECHO and cytomegalovirus.1 One of the more common causes of sialadenitis is recent surgery, after which acute parotitis may arise. It may be of acute or chronic onset. Most cases of acute bacterial sialadenitis are due to Staphylococcus aureus, other streptococci may also be responsible. Adults and children, both are affected by this condition. Children present it as mumps. In adults, the most frequent cause of chronic sialadenitis is the occurrence of salivary duct calculi with subsequent pyogenic bacterial infection. They are known as sialolith. These are calcified structures that develop within the salivary ductal system which rise from the

deposition of calcium salts around a nidus of debris within the duct lumen in young and middle- aged adults. These most often develop within the ductal system of the submandibular gland due to its long, torturous, upward course. The occlusion of the duct prevents the free flow of saliva, and this stagnation or accumulation of saliva under pressure produces pain and swelling.2 Radiographically, sialoliths appear as radiopaque masses.

Figure 1

The resected submandibular gland.

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Figure 2

Sialolith of size approximately 5mm*10mm

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Figure 3

Concentric laminations seen around a central nidus (10X view)

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Figure 4

Concentric laminations (40 X view)

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Figure 5

Periductal inflammation around salivary gland duct (10X view)

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Case Report

A 56-year old male patient reported in the department with a complaint of pain and swelling in the right lower right back region of the jaw since 15 days. On clinical examination, a diffuse swelling of approximately 25mm*30 mm in size was noticed in the right submandibular region. The swelling extended from 2 cm below the lower border of the mandible to the lower border of the thyroid cartilage. A small swelling was seen in the floor of mouth. The patient also has pain in the right submandibular region before and while eating food. A provisional diagnosis of a sialolith with sialadenitis was made. Radiographic examination revealed a radiopaque mass in the right submandibular region of approximately 5mm*10 mm in size. Oral antibiotics and analgesics were prescribed for 7 days to reduce the pain. On follow-up after 7 days, the swelling had subsided, resection of the submandibular gland was done (Figure 1). A sialolith was observed in the floor of the mouth. The excised sialolith was then sent for histopathological examination to confirm the diagnosis. A cylindrical shaped sialolith was received for grossing, approximately 5mm*10 mm in size of a stony hard consistency. (Figure 2). The sialolith was decalcified first in 5% nitric acid and then sectioned followed by staining with haematoxylin and eosin for histopathological examination.

On the H&E stained section, the calcified mass exhibited concentric laminations around a central nidus of amorphous debris (Figure 3, Figure 4). Periductal inflammation is also seen (Figure 5). The successive deposition of inorganic and organic material lead to the concentric formation.

Discussion

The occurrence of a stone (sialolith) in the salivary gland or ducts is known as sialolithiasis. It is a common cause of salivary gland disease with a prevalence rate of approximately 1.2%. Stones occur as a result of calcification of an intraluminal organic nidus such as dried secretion, bacterial colonies, and cellular debris. Stagnation of salivary flow, high alkalinity, and increased calcium content predispose to sialolith formation.3 Salivary gland calculi are more commonly found in submandibular gland than parotid gland due to factors such as the direction of salivary flow, a tortuous structure of Wharton duct and the high calcium and mucin content of saliva produced in the submandibular gland.4 The size of salivary gland calculi vary from small particles to large concrement formations. The average size of the salivary calculi lies between 3 mm and 17 mm. They are usually located in the ducts of the gland and the hilus, whereas sialolith in the parenchyma occurs in 9-17% of all cases.5 It is the most common cause of acute and chronic infection in the major salivary glands. Sequelae of long-standing calculi include sialadenitis, duct dilation, gland atrophy, and potentially profound cystic dilatation. Other causes of infection in salivary glands are a variety of microbial agents including bacteria, mycobacteria, viruses, fungi, parasites, and protozoa.6

A prompt management is the key. The primary objective of the treatment of sialolithiasis is the restoration of normal salivary secretion. The treatment options for submandibular sialoliths are intraoral removal of stone, interventional sialendescopy and resection of the gland. The appropriate treatment method is chosen according to size, location, and number of sialoliths. Newer treatment modalities such as endoscopic intracorporeal shockwave lithotripsy and extracorpeal shockwave lithotripsy have been introduced as alternatives to conventional submandibular gland surgery. Sialendoscopy has been used as both a diagnostic and an interventional modality in salivary sialolithiasis. Small salivary intraductal calculi may be removed and biopsies may be taken using sialendoscopy systems.4

In this case, a long standing sialolith lead to sialadenitis. The patient presented with typical signs and symptoms of sialadenitis associated with a sialolith and the radiographic and histopathologic findings also confirmed the same. The affected salivary gland was removed and the sialolith extracted from the floor of the mouth. The antibiotic coverage subsided the swelling and then the gland was excised after obtaining the patient’s consent. Post-operative follow-up is important to ensure stone-free salivary glands and fewer chances of infection and inflammation in the salivary glands due to calculi.

Conclusion

Association of the presenting signs and symptoms along with the clinical appearance of hard swelling in the submandibular region should be properly managed and assessed. The presence of a salivary gland calculi must be diagnosed beforehand to decrease the risk of a subsequent salivary gland infection like sialadenitis which may further have detrimental effects.

Source of Funding

None.

Conflict of Interest

None.

References

1 

B Neville D Damm C Allen J Bouquot Oral and Maxillofacial Pathology20153936

2 

R Rajendran Shafer’s Textbook of Oral PathologyNew Delhi2009345

3 

R Chandak S Degwekar M Chandak S Rawlani Acute submandibular sialadenitis- a case report. Case reports in dentistry2012

4 

S Arslan E Vuralkan A Çobanog A Ural Giant sialolith of submandibular gland: report of a caseJ Surgical Case Rep20152015443

5 

J H Jung S O Hong K Noh D W Lee A large sialolith on the parenchyma of the submandibular gland: A case report. Experimental and therapeutic medicineExp Ther Med2014825253110.3892/etm.2014.1730

6 

D Gnepp Diagnostic Surgical Pathology of the Head and Neck200142653



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Article History

Received : 20-08-2021

Accepted : 10-09-2021


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https://doi.org/10.18231/j.adr.2021.023


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