| Literature DB >> 29076299 |
Abstract
Prostatic calculi often occur in middle-aged and old men. Prostatic calculi are usually classified as primary/endogenous stones or secondary/extrinsic stones. Endogenous stones are commonly caused by obstruction of the prostatic ducts around the enlarged prostate by benign prostatic hyperplasia (BPH) or by chronic inflammation. Extrinsic stones occur mainly around the urethra, because they are caused by urine reflux. The exact prevalence of prostatic calculi is not known, and it has been reported to vary widely, from 7% to 70%. Most cases of prostatic calculi are not accompanied by symptoms. Therefore, most cases are found incidentally during the diagnosis of BPH using transrectal ultrasonography (TRUS). However, prostatic calculi associated with chronic prostatitis may be accompanied by chronic pelvic pain. Rare cases have been reported in which extrinsic prostatic calculi caused by urine reflux have led to voiding difficulty due to their size. More than 80% of prostatic calculi are composed of calcium phosphate. Prostatic calculi can be easily diagnosed using TRUS or computed tomography. Treatment is often unnecessary, but if an individual experiences difficulty in urination or chronic pain, prostatic calculi can be easily removed using a transurethral electroresection loop or holmium laser.Entities:
Keywords: Calculi; Prostate; Prostatic hyperplasia; Prostatitis
Year: 2017 PMID: 29076299 PMCID: PMC5756803 DOI: 10.5534/wjmh.17018
Source DB: PubMed Journal: World J Mens Health ISSN: 2287-4208 Impact factor: 5.400
Fig. 1Zonal classification of the prostate and prostatic calculi. AFS: anterior fibromuscular stroma, TZ: transitional zone, CZ: central zone, PZ: peripheral zone.
Fig. 2(A) Primary/endogenous prostatic calculi. (B) Secondary/exogenous prostatic calculi. Arrows indicate prostatic calculi.
Fig. 3The solidified dark secretion of the prostate can be seen during holmium laser enucleation of the prostate (arrow).
The main composition of prostatic calculi
| Deposition | Prostatic calculi | Corpora amylacea | ||
|---|---|---|---|---|
| No. of sample | Percent | No. of sample | Percent | |
| Calcium phosphate (hydroxyapatite) | 19/23 | 82.6 | 1/4 | 25.0 |
| Calcium phosphate (hydroxyapatite) Co-deposited with calcium oxalate monohydrate (granular whewellite) | 1/23 | 4.4 | 1/4 | 25.0 |
| Calcium carbonate phosphate (carbonate apatite) | 2/23 | 8.7 | 0/4 | 0 |
| Calcium oxalate monohydrate (whewellite) | 1/23 | 4.4 | 0/4 | 0 |
Data from Sfanos et al. Proc Natl Acad Sci USA 2009;106:3443-8) [9].
The prevalence and location of prostatic calculi
| Reference | Prevalence | Location or type of stone |
|---|---|---|
| Dell'Atti et al (2016) [ | 25.3% (168 of 664 patients) undergoing TRUS and prostate biopsy | 50.6% in TZ, 20.2% in CZ, and 29.2% in PZ |
| Park and Choo (2017) [ | 76.6% (464 of 606) at a HPC | |
| Hong et al (2012) [ | 41.5% (199 of 479), with 36.1% (97 of 268) at a HPC and 48.3% (102 of 211) at a urology outpatient department | 66.3% (132 of 199) in CZ and 33.7% (67 of 199) in PZ |
| Kim et al (2011) [ | 51.1% (799 of 1,563) at a HPC | Small calculi (type A) in 39.4% (615 of 1,563) and large calculi (type B) in 11.8% (184 of 1,563) |
| Shoskes et al (2007) [ | 46.8% (22 of 47 patients) with CPPS | |
| Geramoutsos et al (2004) [ | 7.4% (101 of 1,374) in young adults | Type A in 71.3% and type B in 28.7% |
TRUS: transrectal ultrasonography, HPC: health promotion center, CPPS: chronic pelvic pain syndrome, TZ: transitional zone, CZ: central zone, PZ: peripheral zone.
Fig. 4Transrectal ultrasonography. (A) Transverse view. (B) Sagittal view. Arrows indicate prostatic calculi.
Fig. 5Pelvic computed tomography. Arrows indicate prostatic calculi.