25.2
The pathophysiology of kidney stones involves several key factors.
Initially, urine volume increases the concentration of minerals, promoting crystal formation.
The urine's pH level influences stone formation as the solubility of stone-forming substances varies with pH levels.
Additionally, supersaturation occurs when excess stone-forming substances like calcium, oxalate, and uric acid exceed the urine's ability to dissolve them, leading to nucleation and crystal formation, which can grow into larger stones.
Next, the clinical manifestations of renal calculi vary by location.
Stones in the renal pelvis cause deep, aching pain in the costovertebral area, often with hematuria and pyuria.
Renal colic presents as acute pain with costovertebral tenderness, nausea, and vomiting.
Ureteral stones obstruct urine flow, causing severe, colicky pain that radiates to the thigh and genital area, with a strong urge to void and passage of small amounts of blood-stained urine.
Finally, bladder stones may cause irritation, hematuria, and urinary retention by obstructing the bladder neck.
Renal calculi, commonly termed kidney stones, are crystalline solid masses that form in the kidneys but can occur at any point within the urinary syst…
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