Revision 7 for 'Calyceal diverticulum'All Revisions
Calyceal diverticula, also known as pyelocalyceal diverticula are congenital outpouchings from the renal calyx or pelvis into the renal cortex. These diverticula are lined with transitional/urothelial epithelium.
Relatively uncommon, seen in 0.21% to 0.60% of intravenous urograms (IVU).
- gender: females are more commonly affect than men by a ratio of 2:1
- high incidence of stone formation due to urine stagnation
The majority of the time this is an asymptomatic congenital variant and discovered when patients present for other complications such as hematuria, calculi, or repeated infections.
The most common theory for the origin of calyceal diverticula is a failure of regression of the third and fourth-generation ureteric buds, as a result of obstructing stones or infection.
There are two categories of calyceal diverticula. The first and more common type communicates with a minor calyx. The second communicates with a major calyx or the renal pelvis.
Plain abdominal radiographers will rarely show a crescent-shaped meniscus calcification of radio-opaque milk of calcium within a diverticulum.
A calyceal diverticulum complicated by calculi or layered dependent milk of calcium appears echogenic on ultrasound
Nephrographic phase contrast-enhanced CT will have an appearance similar to that of a simple cyst. The diagnosis is made with certainty in the excretory phase of imaging, the cystic structure fills with contrast material due to communication with the collecting systeem, and layering of contrast material is seen within. This helps differentiate it from a renal cyst, which does not connect with the collecting system.
A calyceal diverticulum complicated by calculi or layered dependent milk of calcium will be a high-attenuating material on an unenhanced CT.
General imaging differential considerations include: