I n urolithiasis, stones are formed in the urethra, kidney, or bladder. Kidney stones cause severe pain in the abdomen and flank [1]. Supersaturation of urine leads to the formation of kidney stones, and their formation is dependent on the pH, ionic strength, specific gravity, and solute concentration of urine [2]. Five types of urinary stones are primarily encountered: calcium oxalate, calcium phosphate, urates, cysteines, and magnesium ammonium phosphate hexahydrate (MgNH 4 PO 4 .6H 2 O, struvite) [3,4]. Of these types of stone, struvite is unique owing to its association with the presence of infection in the urinary tract and thus struvite stones are also called infection stones [1,4]. The main cause of the infection is urease-producing organisms, such as Proteus spp., Klebsiella pneumoniae spp., and Providencia spp [5,6]. Urease is a characteristic bacterial enzyme that hydrolyzes the urea (H 2 N-CO-NH 2 ) in urine to form ammonia [1,5]. As a result of this hydrolysis reaction, the pH of the urine and then the concentration of ammonia (NH 4 +