The most common cause of obstructive sialadenitis of the major salivary glands is sialolithiasis [
1]. This disease is characterized by formation of calcified stones (sialoliths) within the gland’s ductal system that hinder saliva outflow into the oral cavity. Etiologically, changes in ion composition, quantity and flow rate as well as pH changes of the saliva, nicotine abuse and dehydration are currently being discussed [
2,
3]. The incidence of sialolithiasis within the general population is estimated to be between 28 and 59 cases per million and year [
2]. The mean age for onset of symptoms due to sialolithiasis is approximately 45 years [
4]. Of all major salivary glands the submandibular gland (SMG) is specifically prone to sialolith formation due to its seromucous saliva content as well as a long and curved duct (Wharton’s duct) both of which facilitate calcification [
5]. The parotid gland (PG) is the second most affected gland followed by the sublingual gland (SLG) which rarely is affected [
6]. The average time between the occurrence of symptoms like recurrent colicky pain and swelling of the affected gland and final diagnosis is 2.4 years [
7]. Without removal of the obstructive sialolith complications like abscesses, fistulas and phlegmonous inflammations have been reported [
8]. Cervical sonography is the gold-standard modality for diagnosis of sialolithiasis due to its ubiquitous availability, low cost and non-invasiveness [
9]. The specificity and sensitivity of sonography in sialolith detection is reported to be 94 and 86%, respectively [
10]. In the 1990s the procedure of diagnostic sialendoscopy was introduced as a method to directly visualize sialoliths by insertion of a semi-rigid endoscope with a diameter of no more than 1.7 mm into the gland’s excretory duct [
11]. Additionally, sialography, computer tomography (CT), cone-beam computer tomography (CBCT) as well as magnetic resonance sialography (MRS) can be conducted to diagnose sialolithiasis [
12]. The line of therapy follows an escalating treatment algorithm depending on the type of affected gland as well as the position and number of sialoliths [
13,
14]. Due to the deep position within the ductal system sialolith formation in the hilus and the parenchyma is most difficult to treat [
4]. Whereas sialadenectomy was often conducted in these cases the innovative guidance of the developed treatment algorithm nowadays allows gland preservation in > 90% of cases leading to lower postoperative complication rates such as wound infection and injuries to the lingual and facial nerve [
4,
15]. According to the treatment algorithm initial prescription of antibiotics in combination with analgesics, sialogogues and massage of the affected gland should be attempted to enable spontaneous sialolith discharge [
12,
13]. Sialoliths of the SMG and PG with a diameter of no more than 3 mm can usually be removed with sialendoscopy with success rates of > 90% [
10,
16]. Larger sialoliths within the distal third of Wharton’s duct can be removed by papillotomy, whereas sialoliths within the middle third are commonly extracted by sialendoscopy [
17]. Sialoliths within the parenchyma of SMG and PG that cannot be removed by interventional sialendoscopy (ISE) or extracorporeal shockwave lithotripsy (ESWT) alone may be removed by an intraoral (SMG) or extraoral (PG) endoscopy-assisted sialolithotomy (IEAS) with success rates of > 90% [
18,
19]. As a last resort in rare cases with inaccessible symptomatic sialoliths sialadenectomy has to be performed.
The aim of the present study was to retrospectively analyze and evaluate the therapeutic success rates of an escalating treatment algorithm in sialolithiasis. The novelty in this study is the special emphasis on the patient perceived physical and psychological strain throughout therapy.