Sialendoscopic removal of fish bone-induced sialoliths in the duct of the submandibular gland.

Obstructive sialadenitis of the submandibular gland is commonly caused by sialoliths, but more rarely by foreign body-induced sialoliths. Here, we report minimally invasive sialendoscopic removal of fish bone-induced sialoliths in the duct of the submandibular gland. A 43-year-old woman presented with recurrent swelling of the right submandibular gland at other hospital. Computed tomography (CT) showed an 8-mm linear calcification in the posterior part of Wharton's duct. The lesion was deemed difficult to remove and she was followed up. However, because the lesion did not resolve spontaneously within 9 months and chronic sialadenitis symptoms persisted, she was referred to our department for endoscopic removal. CT showed a linear calcification (5.6×1.2×0.8mm) connecting 2 spherical calcifications (2.3×2.1×1.9mm; 1.8×1.4×1.1mm) in the anterior part of Wharton's duct. The patient underwent endoscopic removal of the lesion using a 1.6-mm-diameter sialendoscope under local anesthesia. The specimen contained a fish bone connecting 2 sialoliths. The patient was unaware of the fish-bone injury. After removal, there was no recurrence of submandibular gland swelling during 6 months follow-up.

Risk Factors for Complications of Intraoral Removal of Submandibular Sialoliths.

PURPOSE: Intraoral removal of submandibular sialoliths is a surgical technique for the treatment of sialolithiasis and is reported to have excellent outcomes. The aim of this study was to determine the risk factors leading to complications of this procedure. PATIENTS AND METHODS: The medical records of 200 patients who had undergone intraoral removal of sialoliths from January 2006 through June 2015 were retrospectively reviewed. A telephone survey was used to check postoperative symptoms. Dry mouth, wound infection, lingual nerve dysfunction, and recurrence were considered complications. Computed tomograms of the neck were reviewed for location, shape, number, and size of the stone. RESULTS: Forty-four patients reported a complication. The incidence of complications was significantly higher in patients with stones in the proximal region of the salivary duct (proximal group) than in those with middle or distally located stones (middle/distal group; P < .05). The average stone size was larger in the proximal group; the operation time and length of admission also were longer in the proximal group, with a statistically significant difference (P < .05). Complaints of lingual nerve dysfunction were significantly higher in the proximal group than in the middle/distal group (P < .05). CONCLUSION: Patients with proximally located stones had more complications, especially lingual nerve dysfunction, than those with middle or distally located stones. The former group also required a longer operation time and hospital stay.

Evaluation of the prevalence of residual sialolith fragments after transoral approach of Wharton's duct.

Transoral submandibular duct sialolith removal is a simple technique with very few complications. Nevertheless, following this procedure, we have observed long-term calculus recurrence in a number of patients. We therefore elected to evaluate these cases. This was a monocentric prospective study performed between November 2013 and June 2014. All patients received surgery for submandibular gland lithiasis by intraoral removal of submandibular duct calculi. Between the day following the procedure and 3 months postsurgery, these patients systematically underwent an ultrasound examination of the submandibular gland. The study comprised 15 males and 15 females aged between 19 and 87 years, of which one male presented with bilateral calculi (n = 31). Asymptomatic sialolith fragments were found in 16% of patients. A statistically significant risk (p < 0.05) of residual sialolith was demonstrated in cases in which the calculus or multiple calculi fragmented perioperatively. Our aim was to remove the sialolith as non-traumatically as possible and to perform sialendoscopy at the end of the procedure to check the patency of the anterior ductal segment and to ensure that no residual calculus fragments were present despite the loss of fluid tightness subsequent to the opening of the hilum.

Rigid swelling of sublingual caruncle area due to the salivary gland duct obstruction by a sialolith

Sialolithiasis is the presence of calculus within the ductal system of a salivary gland. Among the diagnostic methods are inspection, palpation, checking the amount of saliva secreted and the identification of a sialolith. The authors present the case of a 37-year-old female patient with edema of the submandibular area and a bulging sublingual caruncle due to a calculus that obstructed the salivary gland ostium.

Rigid swelling of sublingual caruncle area due to the salivary gland duct obstruction by a sialolith.

Sialolithiasis is the presence of calculus within the ductal system of a salivary gland. Among the diagnostic methods are inspection, palpation, checking the amount of saliva secreted and the identification of a sialolith. The authors present the case of a 37-year-old female patient with edema of the submandibular area and a bulging sublingual caruncle due to a calculus that obstructed the salivary gland ostium.

Foreign body induced sialolithiasis treated by sialoendoscopic intervention.

OBJECTIVE: The study aims to identify the impact of sialolith formation by reviewing the foreign body induced sialolithiasis treated by sialoendoscopic intervention. METHODS: The study group included 13 patients whose sialolithiasis was induced by foreign body. After the routine radiographic examination, sialoendoscopic procedures were performed. Then, the treatment protocol was designed. RESULTS: The occupations of the 13 patients included 5 fishermen, 3 office workers, 2 workers, 1 teacher, 1 farmer, and 1 retired police officer. All patients had a unique diet habit-seafood. Eleven patients had a remembered incident of implanted fish bone and the following symptoms, with either obstructions or infections. Only 2 of the 13 had no memory of such an injury. All the stones were in the ducts of submandibular glands. In 10 procedures, there was 1 solitary stone, whereas 2 stones were encountered in 3 procedures. After being removed, 16 stones were crushed to expose the fish bone nidus of the stone. There was relief of symptoms after the procedures. CONCLUSIONS: This study supported the possibility that some sialoliths resulted from a retrograde migration within the salivary ducts. In our study, the occupations (fisherman), the diet habit (seafood), and the injury history (a remembered incident of implanted fish bone and the following symptoms) were obviously related to the stone formation that was induced by the fish bone.

[The new S2k AWMF guideline for the treatment of obstructive sialadenitis in commented short form]. / Die neue S2k AWMF Leitlinie zur Behandlung der obstruktiven Sialadenitis in kommentierter Kurzform.

A new and interdisciplinary S2k AWMF guideline for the treatment of obstructive sialadenitis has been published. There have been several technical achievements, for instance in the field of ultrasonography, via sialendoscopy, or by MR-sialography, that have increased the possibilities for diagnosis and treatment of patients with obstructive sialadenitis. In the past, the treatment of choice in case of unsuccessful medical treatment was a complete extirpation of the affected salivary gland. Nowadays, using a variety of modern treatment options (like sialendoscopy, or extracorporeal shock-waves lithotripsy sometimes combined with salivary duct incision), it is possible in most patients, especially in cases of sialolithiasis, to preserve the affected gland. A functional recovery after gland-sparing surgery is described but more data is needed to finally evaluate the long-time results. The new guideline describes all relevant steps to diagnose an obstructive sialadenitis and values all diagnostic tools critically. Finally, all recommendable therapy options are described and valued, too.

Computational fluid dynamics analysis of salivary flow and its effect on sialolithogenesis.

OBJECTIVE: Sialolithiasis is a common disease caused by intraductal stones, formed by reduction in salivary flow, salivary stagnation, and metabolic events. We used computational fluid dynamics to investigate changes in salivary flow field around parotid stones of different shapes. MATERIALS AND METHODS: Three-dimensional configurations of the Stensen's duct were reconstructed from computed tomography sialographic images. Fluid dynamics modeling was used to analyze the salivary flow field around stones under unstimulated and stimulated conditions. RESULTS: The majority of sialoliths were oval-shaped (59/98), followed by irregular (24/98) and round (15/98). Salivary velocity was significantly higher around streamlined stones, compared with round (P = 0.013) and oval (P = 0.025) types. Changes in salivary flow field around sialoliths were found to affect the pattern of mineral deposition in saliva. The area of low velocity around the round stone was double the size observed around the streamlined stone during the unstimulated state, whereas in the stimulated state, local vortexes were formed on the downstream side of round and oval stones. CONCLUSIONS: Salivary flow field around sialoliths plays an important role in the progression of multicentric stones, and analysis of the salivary dynamics during sialolithiasis may provide deeper understandings of the condition and aid in developing successful treatment strategies.

A retrospective case series illustrating a possible association between a widened hilum and sialolith formation in the submandibular gland.

OBJECTIVE: The purpose of this study was to explore any association between anatomical variances in the ductal system and sialolith formation using sialoendoscopy and acrylic resin replication of the ductal system. METHODS: A retrospective study of 372 submandibular gland sialoendoscopies was performed to review the findings of the submandibular gland duct anatomy. Using sialoendoscopy and replicated casts, a high rate of hilar widening was noted in patients with submandibular sialolithiasis. RESULTS: Sialolithiasis was detected in 326 of the patients who presented with obstructive symptoms. Around 67% (285/426) of the stones were located in the distal third of the ducts or at the hilum of the submandibular gland. During the sialoendoscopic procedure, the anatomy of the ductal system was examined and 285/326 (87.4%) of the hilums were noted to be widened like a basin. The anatomy of the duct from the replicated casts demonstrated a treelike structure and the basin-like widening of the hilum was found in all the excised submandibular glands. CONCLUSION: Using sialoendoscopy, a high number of patients presenting with sialolithiasis in the submandibular gland seem to have an anatomical variance in the hilar region. The reproduced ductal system from excised glands also demonstrated this abnormal widening of the hilum. Although further studies need to be performed, we try and explain why there is such a high prevalence of hilar widening in patients with submandibular sialolithiasis.

Postenucleation orbital sialocele in a dog associated with prior parotid duct transposition.

An orbital sialocele developed in a dog following enucleation for protracted glaucoma. This eye had historically been treated for keratoconjunctivitis sicca by parotid duct transposition approximately 5 years previously, and the duct was ligated distally at the time of enucleation. One month following enucleation, the dog presented with a fluctuant conical-shaped swelling ventrolateral to the orbital socket. Surgical exploration revealed a dilated, fibrotic distal portion of the previously transposed parotid duct, and saliva, within the enucleated orbit. The distal portion of the duct and saliva-containing tissues from within the orbit were excised. The remaining proximal normal portion of the parotid duct was re-routed into the oral cavity. Clinicopathologic and histologic examination of the excised orbital contents and dilated portion of duct revealed a sterile sample of saliva and moderate chronic periductal fibrosis. At a 6-month re-evaluation there was no evidence of recurrence of the sialocele, and the parotid duct was functional.

Possible etiology of calculi formation in salivary glands: biophysical analysis of calculus.

Sialolithiasis is one of the common diseases of the salivary glands. It was speculated that, in the process of calculi formation, degenerative substances are emitted by saliva and calcification then occurs around these substances, and finally calculi are formed. However, the exact mechanism of the formation of calculi is still unclear. In this study, we identify some possible etiologies of calculi formation in salivary glands through biophysical analysis. Calculi from 13 patients with submandibular sialolithiasis were investigated by transmission electron microscopy, scanning electron microscopy, X-ray microanalyzer, and electron diffraction. Transmission electron microscopic observation of calculi was performed in the submandibular gland (n = 13). In 3 of the 13 cases, a number of mitochondria-like structures and lysosomes were found near calcified materials. Scanning electron microscopic examination of these materials revealed that there were lamellar and concentric structures and that the degree of calcification was different among the calculi. X-ray microanalysis disclosed the component elements in the calculi to be Ca, P, S, Na, etc., and the main constituents were Ca and P. The calcium-to-phosphorus ratio was 1.60-1.89. Analysis of the area including mitochondria-like structures, lysosomes, and the fibrous structures by electron diffraction revealed the presence of hydroxyapatite and calcified materials. It is speculated that mitochondria and lysosomal bodies from the ductal system of the submandibular gland are an etiological source for calcification in the salivary gland.

[A new method for treating chronic sialodochitis and sialolithiasis in dilatation of the intraglandular portion of the parotid duct]. / Novyi sposob lecheniia khronicheskogo sialodokhita i sliunnokamennoi bolezni pri rasshirenii vnutrizhelezistoi chasti okoloushnogo protoka.

A new method for the treatment of chronic sialodochitis and sialolithiasis is suggested for cases with essential dilatation of the duct in the intraglandular compartment of the parotid gland: the external wall of dilated duct is dissected and the two resultant parts are twisted inside and sutured to the internal wall of the dilated duct; the parotid duct is ligated at the site of its exit from the gland.

Parotid salivary duct mucocoele and sialolithiasis following parotid duct transposition.

An 11-year-old, female neutered English springer spaniel presented with recurrent episodes of mucopurulent discharge from the right eye, 17 months after parotid duct transposition, culminating in the development of a swelling over the infraorbital area. A diagnosis of parotid duct obstruction with resulting rupture of the duct and sialocele was made. On exploratory surgery, three sialoliths were removed from various sites within the duct. Surgical repair of the duct restored normal saliva flow.

Salivary calculus: an insight into its pathogenesis--a case report of parotid sialolith in a 9 year old child.

The occurrence of sialolithiasis in children is uncommon, while parotid sialoliths are rare. A case of parotid sialolith in a 9 year old child is reported.

[Lithiasis in small salivary ducts. Report of 3 cases]. / Lithiasis der kleinen Speicheldrüsen. Bericht über drei Fälle.

Three cases with sialolithiasis of minor salivary gland are presented. The sialoliths were found on the left side of the upper lip (two patients) with local infection and on the right side of buccal mucosa (one patient) without any symptom. The histologic findings resulted from our own cases and the etiology are discussed extensively and a literature review is made as well.

Giant salivary calculi: an orocervical fistula caused by a submandibular gland calculus.

Large calculi of the salivary glands are rare. They may go undetected for many years. The authors report three cases of giant submandibular gland calculi. In one patient, the calculus was an incidental finding. In all patients, the mass was in the substance of the gland; in one, the configuration of the mass was unusual and it had eroded through the floor of the buccal cavity forming an orocervical fistula (the first such report) and in another the mass occupied a small portion of Wharton's duct. The histopathologic findings in all three cases were of nonspecific chronic inflammation. All the patients made a smooth recovery and had no complaints at follow-up.

Structural analysis of phleboliths and salivary calculi.

Three phleboliths and ten salivary calculi in the submandibular duct were studied with scanning electron microscopy (SEM) and computer aided microanalyser (CMA). The surface of the phleboliths was rather even with some irregularity. According to their surface structure the salivary calculi were divided into three types: the rock-like type, the granular type, and the globular type. The phleboliths were classified into two types according to their cut surface: the calcified-core type, and the uncalcified-core type. The core structure was similar to the surface structure in the calcified-core type of phleboliths, but in the salivary calculi the core structure was different from the surface structure in that the cut surface of the core was an accumulation of circular or polygonal structures forming a honey-comb pattern which was surrounded by small projections distributed radially. On the basis of these results some etiological factors of phleboliths and salivary calculi are discussed.