Bladder calculus

Last revised by Dr Ian Bickle on 05 Aug 2022

Bladder calculi, commonly referred to as bladder stones, are urinary stones that are found primarily in the urinary bladder and comprise only 5% of all urinary tract stones. They can be divided into primary, secondary, and migratory stones:

  • primary: bladder stones form in the absence of other urinary tract abnormality, typically seen in children in endemic areas
  • secondary: stones form in an abnormal bladder or from concretions on foreign material (e.g. urinary catheters)
  • migratory: usually renal calculi which have migrated down into the bladder; uncommon

Primary bladder stones are now uncommon in developed countries and incidence is ever on the decline. In developing countries, however, incidence is still quite high, especially in endemic areas in North Africa, the Middle East, and Southeast Asia. This is has been found to occur due to poor hydration, recurrent diarrhea, and a diet deficient in animal protein.
Family history is found in up to a third of idiopathic cases 2.

Secondary bladder stones are due to urinary stasis, including from:

Migratory stones are either a renal stone or a sloughed renal papilla that serves as a nidus for formation of a bladder stone. This type of stone is uncommon, as virtually any stone that can pass though the ureter, can also pass on through the urethra. A stone will stay stuck in the urinary bladder due to bladder outlet obstruction or bladder dysfunction (similarly to secondary stones), and may be laminated by material other than that of the original stone.

Bladder calculi may present with pain, infection or hematuria or may be asymptomatic.

Usually densely radiopaque, calculi may be single or multiple and are often large. Frequently lamination is observed internally, like the skin of an onion.

Sonographically they are mobile, echogenic, and shadow posteriorly. They may be associated with bladder wall thickening due to inflammation.

The earliest method of operative removal of bladder calculus was performed via the perineal route with the patient in a supine position and the legs elevated, hence the term lithotomy position.

  • occasionally a calculus which appears to be in the bladder is actually in the distalmost part of the ureterovesical junction: rescanning the patient in the prone position can help to distinguish these from true bladder calculi
  • for a tiny calculus abutting the anterior margin of the bladder at supine CT, consider a calcification at the insertion of a urachal remnant into the urinary bladder 4
  • for other pelvic calcifications on plain film just outside the outline of the bladder, consider entities such as vascular calcification, most commonly phleboliths

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Cases and figures

  • Figure 1: bladder calculi
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  • Case 1
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  • Figure 2: bladder calculi
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  • Case 2: laminated calculus
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  • Figure 3: photograph - toy jacks
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  • Case 3
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  • Figure 4: urinary bladder stones
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  • Case 4
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  • Case 5
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  • Case 6: ultrasound
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  •  Case 7
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  • Case 8
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  • Case 9: huge calculus with lamination
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  •  Case 10
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  • Case 11: jackstone
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  • Case 12: multiple
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  • Case 13: extensive
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  • Case 14: laminated
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  • Case 15
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  • Case 16: 3D VR CT
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  • Case 18
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  • Case 17
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