Sialolithiasis: an unusually large submandibular salivary stone

Sialolithiasis in the Left Submandibular Gland: A Case

The most common illness affecting the salivary glands is submandibular gland sialoliths. The size of the sialolith and the patient's clinical history mainly influence how this salivary system abnormality is treated. This diagnosis is suggested by a history of salivary gland pain or swelling, particularly during mastication. Palliative therapy combined with conservative therapies, such as the milking of the ducts, can effectively treat small and accessible stones. When a stone or stones are large and inaccessible, surgical therapy should be considered if conservative approaches have not proven to be effective. A case of sialolithiasis affecting the left submandibular salivary gland is described in this article. Under local anesthesia, sialolith was removed following the opening of the duct. The wound was closed with sutures, and the patient was advised to practice tongue exercises and to maintain good oral hygiene.

Sialolithiasis: An Unusually Large Submandibular Salivary Stone

Salivary stones are termed as sialoliths, and the condition is referred to as sialolithiasis. Pain and swelling in the affected area, especially after eating, occur often. Small, easily accessible stones may be managed with conservative methods, such as milking of ducts, along with palliative care, whereas bigger, more difficult-to-reach stones need surgical removal. In this article, we describe a case of sialolithiasis affecting the right submandibular salivary gland, which was treated by removing the gland and stone surgically. When big stones and the gland are removed extra orally, the results are favorable. Submandibular gland sialoliths are the most frequent kind of salivary gland illness. The treatment of this salivary system problem depends on the patient's clinical history, the size of the sialolith, and the degree of cooperation.

Enormous Asymptomatic Intraoral Sialolithiasis: A Case Report

Sialolithiasis is one of the most common diseases of salivary glands. More than 80% of the sialoliths occur in the submandibular gland. While most of the calculi are less than 10 mm in size, 7.6% are larger than 15 mm and are classified as giant sialoliths. We demonstrate a rare case of asymptomatic giant sialolith in the left Wharton's duct with a total atrophy of the left submandibular salivary gland. A 48-year-old female patient presented with lumping sensation for 1 month. A left mouth floor mass was found accidentally during examination and was later revealed to be a painless sialolithiasis. Image study revealed a giant sialolith in the left Wharton's duct with duct dilatation and left submandibular gland total atrophy. She underwent transoral sialolithotomy with removal of a huge stone, measuring 3.5 × 1.4 cm in size. Sialolithiasis usually presents with typical symptoms of the involved salivary gland, and the size of calculi is usually less than 20 mm. This is a rare case report of an asymptomatic giant sialolith in the Wharton's duct, causing left submandibular salivary gland total atrophy, and its diagnosis and management.

Transoral per punctum excision of an impacted parotid duct stone of unfavorable direction: a case report

Background

In the literature, the reported parotid duct stones that did not respond to the conservative measures are few. The present work reported and described the diagnosis and treatment of a case of impacted parotid duct stone that was surgically removed through minimally invasive transoral per punctum approach.

Case presentation

On examination of a 27-year-old male with left intermittent parotid swelling and pain for 1 year, a stone was palpated in the left buccal mucosa region near the orifice of the parotid duct. Ultrasonography (US) showed left Stensen’s duct distal stone. Under general anesthesia and oral intubation, the stone measuring about 1 cm in length was felt transversely located (directed at a right angle with the orifice of the duct). A small mucosal incision was done at the upper lateral part of the punctum; pus came out, and then the stone bulged from the orifice and was pushed outside. Recovery was event-less; postoperative paracetamol was sufficient to relieve pain, and the patient was discharged a few hours after the surgery.

Conclusion

The transoral per punctum excision of an impacted parotid duct stone appears to be a reliable minimally invasive effective and safe procedure. The unfavorable direction of the parotid duct stone might be a cause of failure of the conservative treatment for this stone.

Removal of Large Wharton's Duct Salivary Stones Using a CO2 Laser: A Report of Two Cases

Introduction: Salivary stones inside the Wharton's duct adjacent to the mylohyoid muscle are often removed by a little incision of the mouth floor under local anesthesia. However, in the case of relatively large salivary stones, a large incision is required, which is commonly accompanied by hemorrhage and the need for surgical hemostasis, resulting in prolonged surgery. Furthermore, troublesome sequelae such as ranula and lingual nerve paralysis can occur after surgical procedures. Methods: Two patients who had relatively large salivary stones (>1 cm diameter) in the Wharton's duct were underwent incision of the mouth floor soft tissues with a CO₂ laser. Results: In both patients, the stone was removed in a few minutes without causing abnormal bleeding, nerve injury, or sublingual gland disorders and was completely healed. Conclusion: We report the usefulness and safety of the CO₂ laser in two patients with relatively large salivary stones, who underwent successful surgical removal.

Painless Giant Submandibular Gland Sialolith: A Case Report

Sialolithiasis is one of the most common diseases involving the salivary glands. It is a condition that occurs due to an obstruction in a salivary gland or its duct due to a calculus. The formation of a salivary stone is believed to be secondary to the deposition of mineral salts around a nidus, which is frequently associated with a recurrent bacterial infection. Patients with submandibular sialolithiasis usually present with acute swelling over the neck associated with pain, fever, and purulent intraoral discharge. The size of the calculus varies from <1 mm to a few centimeters. The frequency of sialolithiasis is relatively common. It is estimated to affect 12 in 1000 of the adult population. However, the occurrence of giant sialoliths, >15 mm in any diameter, is rare. Here, we describe our experience with a case of giant submandibular sialolithiasis measuring 25 mm presenting as a painless submandibular mass. The patient underwent submandibular gland excision followed by a full recovery.

Sialo-cutaneous fistula with ectopic submandibular gland sialolith, revealing a hidden ipsilateral enlarged and elongated styloid process: a consideration based on CT findings

Sialolithiasis is a common salivary pathology, and an uncommon complication of sialadenitis and sialolithiasis is the formation of fistulous tracts to other compartments. Submandibular gland sialo-oral fistulae are not particularly remarkable, given the location of the gland and Wharton's duct, but submandibular sialolith-associated fistulae to other cervico-facial compartments (transcervical sialo-cutaneous and sialo-pharyngeal fistulae) are much less common. We report herein an unusual case of a 49-year-old obese man with sialo-cutaneous fistula containing a large, ectopic sialolith in subcutaneous tissue that was expected to undergo spontaneous elimination, but revealed hidden Eagle syndrome featuring an ipsilateral enlarged, elongated styloid process. Furthermore, we offer a thorough review of the literature regarding sialo-fistulae and highlight the relationship between an abnormal styloid process and submandibular sialadenitis with sialolithiasis and new tract formation based on computed tomography.

Sialolithiasis-Do Early Diagnosis and Removal Minimize Post-Operative Morbidity?

Background and objectives: Sialolithiasis is an inflammation of a salivary gland due to obstruction of salivary flow by a sialolith. We aim to assess potential factors that may predict lower morbidity following endoscopically assisted per-oral sialolith removal. Materials and Methods: Retrospective cohort study. Retrospective review of 100 records of patients with sialolithiasis, following surgical sialolith removal. A single medical center (Department of oral and maxillofacial surgery-Rabin Medical Center, Beilinson & Hasharon-Israel) survey. Data were gleaned from the patient files based on a structured questionnaire. Factors that may predict morbidity were evaluated using linear regression equation. Results: 59 of the subjects were men and 41 were women. The mean age of the patients in the study was 50 ± 17.5 years. Sialolith volume and past antibiotic treatment were positively associated while age was negatively associated with hospitalization duration. Conclusion: Early sialolith diagnosis and removal may lower postoperative morbidity.

Radiographic review of anatomy and pathology of the masticator space: what the emergency radiologist needs to know

The differential diagnosis of a masticator space (MS) lesion is broad, owing in part to the multiple structures contained within such a small region. It is also because the MS is adjacent to many of the other deep spaces within the head and neck, which can act as gateways for disease spread. Therefore, emergency radiologists must be familiar with anatomy of the MS, as well as adjacent spaces in order to provide an accurate diagnosis to the referring clinician. This article illustrates the anatomy and common pathologies within the MS using a case-based multimodality approach. Common masticator space pathologies can be categorized into inflammatory/infectious, neoplastic, and vasoformative lesions. Important imaging features of MS lesions and patterns of disease spread will be discussed, with the aim of making this complex deep space more approachable in the emergent setting.

Sialolithiasis: An Unusually Large Salivary Stone

Sialolithiasis is characterized by obstruction of a salivary gland or its duct due to the formation of calcareous concretions, leading to recurrent painful swelling of the involved gland. It is aggravated while eating. Submandibular gland is the most commonly affected gland. The size of the sialolith may range from 1 to 10 mm. Sometimes, the formation of sialo-oral or sialo-cutaneous fistula may promote the growth of the sialolith to a giant size of 15 to 20 mm. Giant sialolith of size greater than 20 mm is sparse in the literature. The purpose of this presentation is to report a case of an unusually large sialolith measuring 28 mm located in the left submandibular salivary gland of a 29-year-old male patient.

Management of anterior submandibular sialolithiasis

Introduction: Sialolithiasis is defined by the presence of a calculus within the salivary gland or its excretory system. It primarily affects the submandibular gland at a frequency of 80%. Involving many factors, the exact aetiology and pathogenesis of salivary calculi remain to be discussed. Body: The purpose of this article is to expose the different aspects of the pathology. Aetiological factors, the diagnostic approach which requires the use of imaging tests as well as the medical and surgical management of anterior submandibular sialolithiasis, will be described. A decision tree regarding the type of management and a table summarizing the main differential diagnoses will be proposed. Conclusion: Submandibular sialolithiases are a common salivary gland disorder. The treatment of sialolithiasis must be early and remains mainly surgical. The level of cooperation as well as the patient's medical and surgical history should guide the management of this type of disorder of the salivary system.

Incidental Findings in TMJ Imaging

For years, the conventional imaging modalities are generally used in dental practice routine. They provide precious information about dentomaxillofacial region; they also have some limitations such as superimpositions, magnifications, distortions, and low-image quality. Because of these limitations, some pathologies, calcifications, and anatomical variations may be missed. Any findings on a radiographic image which are not related to the research areas of interest could be a description of “incidental findings.” Calcifications are one of these incidental findings. They are asymptomatic and also common in TMJ images. Although most of the calcifications require no treatment, correct identification will reduce further diagnostic assessments. Incidental findings on TMJ images were rare, while examining images for temporomandibular disorders and associated issues, it is important not only to examine the TMJ structures but also to look at the nearby anatomical features to check for evidence of incidental findings pathologies that may have mimicked signs and symptoms of TMJ disorders.

Submandibular sialolithiasis: The roles of radiology in its diagnosis and treatment

E. N was a 48-year-old man referred from a peripheral hospital to the Maxillofacial unit of Ahmadu Bello University Teaching Hospital, Zaria, on account of 1-year history of left-sided jaw pain and swelling, particularly after meal. The conventional plain radiograph of the jaws appeared normal as there was no opacity of soft tissue or calcific density visualized. Sialography revealed an oval-shaped filling defect in the dilated left Wharton's duct, which could suggest radiolucent calculus. Ultrasound scan showed the lesion as a brightly echogenic mass surrounded by anechoic clear fluid (saliva), casting posterior acoustic shadow. A diagnosis of left submandibular sialolithiasis was made. The maxillofacial surgeons decided to remove the calculus surgically, but the patient refused surgery and then defaulted from subsequent follow-up visits.

Multiple microlithiasis in bilateral parotid glands as the initial clinical manifestation of primary Sjögren's syndrome

We report a rare case of Sjögren's syndrome (SS) with multiple microliths in the bilateral parotid glands. A 41-year-old man presented to our department with mild pain in the region of the right parotid gland. The dental examination was negative except for the parotid regions. The right region was moderately swollen and the left mildly swollen. Plain radiography revealed multiple calculi in the bilateral parotid glands. Ultrasonography showed heterogenic parenchyma, with microliths and cystic lesions in the parotid glands and heterogenic echotexture in the submandibular glands. Immunologic tests and the Schirmer test confirmed the diagnosis of SS. As the patient had no classic symptoms of SS, the bilateral multiple microliths were the first sign, facilitating the final diagnosis. Early diagnosis of SS is highly relevant because the proper therapy can be initiated. Adequate follow-up and, especially, control of the disease activity by identifying the predictive factors, are the primary objectives of SS management, enabling personalized treatment of this malignant disease. This case is a good example of how detection of calcifications in the bilateral parotid glands by plain radiography can help diagnose SS at an early stage.

Sialolith removal in the submandibular region using surgical diode laser: report of two cases and literature review

PURPOSE

Sialolithiasis is defined as the presence of one or more calcified structures within the duct of a major or minor salivary gland. It occurs as a result of deposition of calcium salts around an accumulation of organic debris in the duct lumen. The main signs and symptoms are edema and bacterial infection with abscess formation.

METHODS

This study aimed to report two cases of submandibular sialolithiasis treated surgically with diode laser and conduct a review of the literature by means of a systematic search. In the two cases, the calculi were located in the distal part of the submandibular duct and could be palpated intraorally. Surgery was performed in an outpatient setting under local anesthesia. A linear incision was made in the floor of the mouth, in the region of the opening of Wharton's duct, to expose and remove the calculi. Laser cutting was performed using a diode laser module coupled to a 400-μm optical fiber emitting at a wavelength of 980 nm (infrared), 2.5 W output power, and in continuous pulse mode.

RESULTS

The use of diode laser is a safe and minimally invasive option for this type of procedure.

CONCLUSION

Offering advantages such as enhanced coagulation properties and high-quality incision, absence of bleeding, low risk of nerve damage, and few comorbidities.

Chronic sialadenitis with sialolithiasis associated with parapharyngeal fistula and tonsillolith

Sialolithiasis is a common salivary pathology, suggested to affect over 1% of the population by postmortem studies. An uncommon complication of sialadenitis and sialolithiasis is the formation of fistulous tracts to other cervicofacial compartments. Submandibular gland sialocutaneous and sialo-oral fistulae have been sparsely described, but a sialo-pharyngeal fistula manifesting as a tonsillolith has yet to be described. We present an unusual case of a 35-year-old male presenting with recalcitrant neck pain and a presumed tonsillolith in the background of chronic submandibular sialadenitis, subsequently demonstrating a salivary fistula through the parapharyngeal space. We offer a thorough review of the literature to highlight the possibility of migratory sialolithiasis and its complications.

Removal of submandibular calculi by surgical method and hydraulic power with curved needle: a case report

Sialolithiasis, the most common salivary gland pathology, is caused by calculi in the gland itself and its duct. While patients with small sialoliths can undergo conservative treatment, those with standard-size or larger sialoliths require sialolithotomy. In the present case study, we removed two sialoliths located beneath the mucosa in the posterior and anterior regions of Wharton's duct, respectively. For the posterior calculus, we performed sialolithotomy via an intra-oral approach; thereafter, the small anterior calculus near the duct orifice was removed by hydraulic power. This method has not previously been reported. There were no complications either during the operation or postoperatively, and the salivary function of the gland remained normal.

Unusual giant sialolith of Wharton's duct

Salivary gland calculi account for the most common disease of the salivary glands. Most of the salivary calculi are small in size. Some calculi that reach several centimeters are reported as megaliths or giant calculi in the literature. They may occur in any of the salivary gland ducts but are most common in Wharton's duct and in the submandibular gland. This report presents clinical and radiographical sign of an unusually large sialolith. A patient came with pain in the floor of mouth. There was a swelling on floor of mouth on the left side. Radiographical examination revealed large irregular radio-opaque mass superimposed on left lateral incisor to molar areas. This case report describes a patient presenting with an unusually large submandibular gland duct sialolith, the subsequent patient management, the etiology, diagnosis, and its treatment.

Transcervical approach to the removal of a deep-seated giant submandibular calculus and the submandibular gland

Sialolithiasis is among the most common disease affecting the major salivary glands whereby the submandibular gland or its duct is affected in the majority of cases. We report a case of the surgical removal of a giant sialolith along with the submandibular gland using the transcervical approach and its clinical outcome.

Does gallbladder angle affect gallstone formation?

INTRODUCTION

Morphology of gallbladder varies considerably from person to person. We believe that one of the morphological variations of gallbladder is the "gallbladder angle". Gallbladder varies also in "angle", which, to the best of our knowledge, has never been investigated before. The purpose of this study was to investigate the impact of gallbladder angle on gallstone formation.

METHODS

in this study, 1075 abdominal computed tomography (CT) images were retrospectively examined. Patients with completely normal gallbladders were selected. Among these patients, those with both abdominal ultrasound and blood tests were identified in the hospital records and included in the study. Based on the findings of the ultrasound scans, patients were divided into two groups as patients with gallstones and patients without gallstones. Following the measurement of gallbladder angles on the CT images, the groups were statistically evaluated.

RESULTS

The gallbladder angle was smaller in patients with gallstones (49 ± 21 degrees and 53 ± 19 degrees) and the gallbladder with larger angle was 1.015 (1/0.985) times lower the risk of gallstone formation. However, these were not statistically significant (p>0,05).

CONCLUSION

A more vertically positioned gallbladder does not affect gallstone formation. However, a smaller gallbladder angle may facilitate gallstone formation in patients with the risk factors. Gallstones perhaps more easily and earlier develop in gallbladders with a smaller angle.

Association of serum electrolytes and smoking with salivary gland stone formation

To further define potential factors that may contribute to stone formation in salivary glands (sialolithiasis), a retrospective chart review was performed of patients diagnosed with sialolithiasis between March 1, 1998 and February 29, 2012. Information on salivary gland stone number, location and size, medical history, medications, and serum electrolyte levels were collected. Associations between electrolyte levels and stone characteristics (such as stone number and size) were examined. Fifty-nine patients were identified; their median age was 58 years (range 25-89 years) and most were male (95%). Salivary stones were most commonly located in the submandibular glands (83%). Thirty-five patients (59%) had a smoking history, with 16 (27%) reported as current smokers. There was a significant association between current smoker status and stone size (mean largest stone size 12.4±8.8mm vs. 7.5±4.8mm in current smokers vs. non-smokers; P=0.03). Serum sodium levels (r=0.32, P=0.014) and serum potassium levels (r=0.31, P=0.017) showed significant positive correlations with stone size. While the aetiology of sialolithiasis remains unclear, smoking (which can contribute to reduced saliva flow) and higher serum sodium levels (which can reflect volume depletion) are associated with larger salivary stones.

CT Scan as an Essential Tool in Diagnosis of Non-radiopaque Sialoliths

Sialolithiasis is the second most common disease of the salivary glands and the main cause of salivary gland obstruction. Diagnosis of calculi/sialoliths can be made by means of an elaborate history, precise clinical examination and radiographic support. But all sialoliths do not present with predictable signs and symptoms and radiographic appearance. Sialoliths have a variety of manifestations and they may or may not be radiopaque. Non-radiopaque sialoliths are difficult to diagnose radiographically. Although newer techniques like CBCT, CT virtual sialandoscopy and established techniques like sialography, xeroradiography can be useful in selected cases. A regular CT scan is an excellent tool in the diagnosis of a non-radiopaque sialolith and associated salivary gland changes. CT scan should be considered as an important tool of imaging for diagnosis, treatment planning and follow-up of all cases of sialoliths and associated pathologies of the salivary gland.

Submandibular Sialolithiasis Perforating the Floor of Mouth: A Case Report

Calculus formation in salivary glands (sialolithiasis) is one of the most common diseases of the salivary glands and is most commonly seen in the submandibular gland. Not only can the stones be small and inside the duct, they may also get larger and reside inside the gland. We can easily see submandibular sialolithiasis perforating the floor of the mouth in cases having sialolithiasis for decades and not having any treatment and its transoral removal as we look in the medical literature. A 52-year-old lady who had rejected surgical treatment for submandibular sialolithiasis for 25 years is presented as a case in this study. Treatment of the case was performed effectively by taking out the calculus transorally with a simple intervention whose examination revealed that the calculus was seen to perforate the floor of the mouth. It is aimed to stress with this case that transoral removal of submandibular sialolithiasis that perforates the floor of the mouth without performing external approaches is a method that has to be thought in the first step.

Deep and unusual sialolithiasis of submandibular duct and gland: a surgical dilemma

Giant solitary submandibular duct calculus and multiple calculi of the gland are extremely rare. This occurrence along with more deep and proximally placed common calculi in submandibular gland may occasionally cause a dilemma in selection of the appropriate surgical approach in the present era of sialoendoscopic surgery. There is a high chance of fracture of the stone in a proximally placed stone in the gland followed by likely dissemination of fragments of the stone into the gland parenchyma during the procedure of sialoendoscopy which is a matter of grave concern. We authors believe that excision of the submandibular gland with the stone in such a situation should still be preferred as the gold standard of treatment leaving the ductal stone for endoscopic removal.

Structure and growth of sialoliths: computed microtomography and electron microscopy investigation of 30 specimens

Theories have been put forward on the etiology of sialoliths; however, a comprehensive understanding of their growth mechanisms is lacking. In an attempt to fill this gap, the current study has evaluated the internal architecture and growth patterns of a set of 30 independent specimens of sialoliths characterized at different scales by computed microtomography and electron microscopy. Tomography reconstructions showed cores in most of the sialoliths. The cores were surrounded by concentric or irregular patterns with variable degrees of mineralization. Regardless of the patterns, at finer scales the sialoliths consisted of banded and globular structures. The distribution of precipitates in the banded structures is compatible with a Liesegang-Ostwald phenomenon. On the other hand, the globular structures appear to arise from surface tension effects and to develop self-similar features as a result of a viscous fingering process. Electron diffraction patterns demonstrated that Ca- and P-based electrolytes crystallize in a structure close to that of hydroxyapatite. The organic matter contained sulfur with apparent origin from sulfated components of secretory material. These results cast new light on the mechanisms involved in the formation of sialoliths.

Advances in imaging of obstructed salivary glands can improve diagnostic outcomes

INTRODUCTION

Obstruction of the major salivary glands is a relatively common condition defined as the blockage of the salivary outflow in the glandular ductal system. It can however mimic more aggressive pathology.

METHODS

The most common cause of salivary obstruction is sialolithiasis, followed by ductal strictures. Salivary obstruction is clinically characterized by a food-related painful swelling of the affected gland, known as 'mealtime syndrome'.

RESULTS

When obstruction is clinically suspected, the role of imaging consists of confirming the obstruction, identifying its cause, evaluating the position and extent of the obstruction and evaluating for associated complications. However, if imaging shows up signs of a tumour or other pathology which can mimic an obstructed gland clinically instead, the radiologist can alert the clinician accordingly to change the course and plan of treatment. Several imaging techniques are available for investigating the obstructed salivary glands.

CONCLUSIONS

This review looks at the causes of obstruction and the use, diagnostic performance and practicality of the various imaging modalities. Importantly, an imaging approach algorithm for the evaluation of the obstructed salivary gland is also proposed.

Parotid sialolithiasis

Salivary dysfunction may be due to systemic diseases and medications. The development of sialoliths is a multifactorial event in which disturbance in secretion, microliths and bacteria may play a major role. A case of sialolith in the parotid gland of a 25-year-old man, with no relevant medical history is reported here.

Self-exfoliation of large submandibular stone-report of two cases

Sialoliths are the most common diseases of the salivary glands. They may occur in any of the salivary gland ducts but are most common in Wharton's duct and the submandibular gland. This report presents clinical and radio graphical signs of two unusually large sialoliths which exfoliated by itself. There were painless swellings on the floor of the mouth in both cases. Radiographical examination revealed large irregular radioopaque mass superimposed right canine and premolar areas. Sialoliths were yellow in color and approximately 1.8 cm and 2.1 cm in size.

An unusual sequel of submandibular gland calculus-A case report

Sialolithiasis in sub-mandibular gland is a common condition. Sub-mandibular fistula as a sequel of sub-mandibular sialolithiasis is a rare entity. We report a case of an unusually large sub-mandibular gland calculus causing a cutaneous fistula.

Intra-oral surgical access for the treatment of bilateral submandibular sialolithiasis: case report

Sialolithiasis is a disease that affects the salivary glands. It is characterized by the presence of calcified structures within the duct system or within the glandular parenchyma. Those calculi, or sialoliths, can obstruct normal salivary flow, potentially leading to infectious sialadenitis, with pain, local swelling, and purulent discharge. Treatment typically consists of the surgical removal of the calculus, often in conjunction with sialoadenectomy. The authors report an atypical case of bilateral submandibular gland sialolithiasis treated conservatively, using intra-oral access to remove the calculi.

Sialolithiasis of the submandibular gland

Sialolithiasis of the salivary gland is a benign pathology that occurs most frequently in the submandibular gland because of its anatomic features. Depending on the sialolith size and calcification degree, it can be visible in radiographic examinations. Commonly, patients may experience pain and/or edema, when the ducts are obstructed. The authors report the case of sialolithiasis of the submandibular gland in a 42-year-old, female, white-skinned patient, noticed during routine dental examination. Following diagnosis confirmed by clinical and radiographic examinations, the treatment plan consisted of surgery for removal of the calcified mass. The prognosis is often good, and generally there is no recurrence.

Lithotripsy

Shock wave lithotripsy (SWL) is the process of fragmentation of renal or ureteric stones by the use of repetitive shock waves generated outside the body and focused onto the stone. Following its introduction in 1980, SWL revolutionized the treatment of kidney stones by offering patients a non-invasive procedure. It is now seen as a mature technology and its use is perceived to be routine. It is noteworthy that, at the time of its introduction, there was a great effort to discover the mechanism(s) by which it works, and the type of sound field that is optimal. Although nearly three decades of subsequent research have increased the knowledge base significantly, the mechanisms are still controversial. Furthermore there is a growing body of evidence that SWL results in injury to the kidney which may have long-term side effects, such as new onset hypertension, although again there is much controversy within the field. Currently, use of lithotripsy is waning, particularly with the advent of minimally invasive ureteroscopic approaches. The goal here is to review the state of the art in SWL and to present the barriers and challenges that need to be addressed for SWL to deliver on its initial promise of a safe, effective, non-invasive treatment for kidney stones.

Multiple, large sialoliths of the submandibular gland duct: a case report

This paper reviews the major clinical and radiographic features of sialoliths and illustrates these with an unusual case of multiple sialoliths within the submandibular gland duct. The differential diagnosis of other calcific structures both within and outside the salivary gland that may mimic a sialolith is also presented.

Giant Sialolith of the Submandibular Salivary Gland

We report the case of a 48-year-old man who had an unusually large submandibular gland sialolith (2.6 cm in greatest dimension), which led to sialadenitis and subsequent abscess formation. We describe the management of this patient and review the literature with emphasis on the various modalities available for diagnostic imaging.

Spectroscopic and thermal analysis of a submandibular sialolith of Wharton’s duct resected using Nd:YAG laser

A sialolith observed in the Wharton's duct of a male patient was resected using an Nd:YAG laser. This is the first report on the resection of sialolith using laser. The resected sample was analyzed for structural details using Fourier transform infrared (FTIR), FT-Raman, and fluorescence spectroscopic techniques. Other techniques like energy dispersive X-ray analysis, scanning electron microscopy, and thermal analysis were also used for the analysis of structural details. The major peaks of the vibrational spectra are observed to be due to the vibrations of the phosphate and hydroxyl groups of the inorganic part of the sample and the proteinaceous component of the organic part. The major elements in the sample are identified as calcium and phosphorous in the ratio 7:3. The fluorescence spectra recorded at excitation wavelengths 280, 325, and 410 nm showed emission maxima corresponding to the endogenous fluorescence of structural proteins and amino acids. The inorganic part of the sialolith remained stable even at temperatures up to 1,673 K. The spectroscopic studies indicated that the structure of the sialolith is similar to that of the dentine part of the human teeth. In situ disintegration of the sialolith involves very high temperature. High calcium and phosphorous content in the food may be attributed to one of the reasons for the formation of sialoliths.