Struvite Nephrolithiasis
Also known as: Infection Stones, Struvite Stones
Struvite (infection) stones are composed of magnesium ammonium phosphate hexahydrate (struvite) and carbonate apatite. They form only when urine is persistently alkaline (pH above 7.2) and rich in ammonium. This occurs in infection with urease producing bacteria.
Urease producers include Proteus (most common), Klebsiella, Pseudomonas, Providencia, Serratia, Enterobacter, Staphylococcus, Ureaplasma urealyticum, Corynebacterium urealyticum and Mycoplasma hominis.
Urease hydrolyses urea into two molecules of ammonia and carbon dioxide. This raises pH and increases ammonium and carbonate, which supersaturates urine with struvite.
Struvite stones account for 10 to 15 percent of all stones. They are more frequent in:
- Women (2 to 3:1).
- The elderly.
- Patients with neurogenic bladder, urinary diversion or spinal injury.
- Chronic catheterisation and indwelling stents.
- Urinary stasis and anatomic abnormalities.
They grow rapidly (weeks to months) and fill the collecting system as staghorn calculi. They incorporate bacteria within the matrix, which protects them from antibiotics, so cure requires complete stone removal. Untreated, they lead to chronic pyelonephritis, renal scarring, abscess and loss of renal function.













