Struvite stones are caused by urinary infection with bacteria that split urea in the urine. They can grow rapidly into the branching shape of the kidney's collecting system - a stag-horn stone - and need complete surgical clearance together with eradication of the underlying infection.
Certain bacteria - most commonly Proteus, Klebsiella, Pseudomonas, and Staphylococcus species - produce an enzyme called urease. Urease splits urea in the urine into ammonia and carbon dioxide, driving the urine strongly alkaline (pH often above 7.2) and super-saturating it with magnesium ammonium phosphate crystals - the chemical name for struvite.1
Struvite stones therefore do not form without persistent urinary infection with a urease-producing organism. They are most common in:
Struvite stones often grow silently, detected only when the patient presents with:
CT KUB confirms the size and shape of the stone and defines the branching anatomy of stag-horn stones. A urine culture identifies the offending organism. Because struvite stones form in alkaline urine, a persistently high urine pH in a stone former - particularly a woman with recurrent infections - is a strong clue.
Any fragment of a struvite stone left behind after surgery acts as a reservoir of infection. Antibiotics cannot penetrate into the stone material, and the residual fragment becomes a focus for re-infection and regrowth. International guidelines are clear: the aim of struvite stone surgery is complete stone clearance, not just debulking.1
Most struvite and stag-horn stones are large and branched, which makes them poor candidates for shockwave lithotripsy.
Arrange a consultation or request a second opinion on an acute stone, a recurrent stone problem, or a recommended procedure.