Recent data comparing the prevalence of kidney stone disease in the United States between the National Health and Nutrition Examination Survey (NHANES) III (1988-1994) and NHANES II (1976-1980) show a 37% increase in newonset symptomatic kidney stones. Similar studies in the United Kingdom show a 63% increase. In addition, stone disease is increasingly more common in women. In the past, the male:female ratio was 3:1; currently it is 1.3:1. It is estimated that, by the age of 70 years, as many as 20% of all white men and 7% of all white women will suffer from kidney stone disease. African Americans and Asians are affected less often. The peak incidence occurs between the ages of 20 and 30 years. In the United States, calcium-containing stones make up approximately 90% of all stones; they contain calcium oxalate alone, calcium phosphate alone, or a mixture of both. The remaining 10% are composed of uric acid, struvite-carbonate, and cystine.
Kidney stones are a major cause of morbidity due to associated renal colic, urinary tract obstruction, urinary tract infection (UTI), and renal parenchymal damage. It was recognized that nephrolithiasis may be associated with end-stage renal disease (ESRD) and/or a declining glomerular filtration rate (GFR). According to US Renal Data System reports between 1993 and 1997, stone disease was attributed as the cause of ESRD in 1.2% of patients. In Necker Hospital in France between 1989 and 2000, nephrolithiasis was felt to be the primary cause of ESRD in 3.2% of patients. Struvite stones accounted for 42.2% of these cases. In a case-control study of nephrolithiasis, there was a higher incidence of chronic kidney disease (CKD) noted in patients with kidney stones. This was only observed in those patients who did not report a history of hypertension. Finally, although the effect was small, an analysis of NHANES III data revealed an association between history of kidney stones and estimated GFR that was dependent on body mass index (BMI). Stone formers with a BMI greater than 27 kg/m2 had a mean estimated GFR that was 3.4 mL/minute/1.73 m2 lower than similar nonstone formers.
A kidney stone can form only when urine is supersaturated with respect to a stone-forming salt. Interestingly, urine in many healthy subjects is often supersaturated with respect to calcium oxalate, calcium phosphate, or uric acid and crystalluria was described in as many as 15% to 20% of healthy subjects. However, urine of recurrent stone formers was noted to contain crystals in first morning voided specimens much more frequently than that of stone formers without subsequent recurrence, suggesting that recurrence may depend on the degree and severity of crystalluria.
Several recent studies provided insight into the crystallization process. Calcium oxalate can crystallize as either calcium oxalate monohydrate (COM) or calcium oxalate dihydrate (COD). COM is the predominant species found in calcium oxalate stones and is the more thermodynamically stable of the two species. Macromolecular inhibitors block COM growth and favor COD formation. Using atomic force
microscopy configured with nanoscale tips, which were modified by biologically relevant functional groups, it was shown that COD crystals do not adhere as well to organic compounds and to the surface of renal epithelia in vitro. This suggests that COD crystals in urine might protect against kidney stone formation given their reduced capacity to form stable aggregates and adhere to epithelial cells.
Urine is also often supersaturated with respect to brushite (CaHPO4•2H2O), a calcium phosphate salt, especially after meals. Brushite can act as a nidus upon which calcium oxalate crystals can form. In vitro studies show that COM crystals once formed grow at the expense of brushite.
Another important factor in the pathogenesis of stone formation that is incompletely understood is the presence of crystallization inhibitors in urine. Normal urine contains a variety of inorganic and organic substances that act as crystallization inhibitors. The most clinically important of these are citrate, magnesium, and pyrophosphate.
Sufficient energy must be generated for a crystal to form in solution. Once a crystal forms, it was once thought that it must either grow to sufficient size to occlude the tubular lumen or anchor itself to the urinary epithelium, which in turn provides a surface upon which it can grow. The typical transit time of a crystal through the nephron is on the order of 3 minutes, and this is too short a period for it to nucleate, grow, and occlude the tubular lumen. However, studies by Evan and Coe have shed additional light on how stones form in the kidney. In patients with idiopathic hypercalciuria, the initial site of crystal formation was in the basement membrane of the thin limb of the loop of Henle. The stone core was made up of calcium phosphate alternating with layers of matrix. The crystal deposit then migrates toward the renal pelvis where it acts as a base upon which a plaque forms, which is then bathed in urine supersaturated with stone-forming constituents upon which calcium oxalate is deposited. Why calcium phosphate precipitates at the basolateral surface of the thin limb of the loop of Henle is unclear. Further studies by Worcester and Coe found a postprandial decrease in proximal tubular calcium reabsorption in these patients. In patients with one type of calcium phosphate stone (brushite), mineral is deposited on the luminal membrane of dilated inner medullary collecting duct cells and grows out into the renal pelvis. The dilated inner medullary collecting ducts are surrounded by areas of interstitial fibrosis.
I. INITIAL PRESENTATION.
A kidney stone most commonly presents with severe flank pain, sudden in onset, and is often associated with nausea and vomiting. The radiation of the pain may provide some clue as to where in the urinary tract the stone is lodged. Stones in the ureteropelvic junction cause flank pain that may radiate to the groin, whereas those lodged in the narrowest portion of the ureter, where it enters the bladder, are associated with signs of bladder irritation (dysuria, frequency, and urgency). Struvite-carbonate stones are, on occasion, incidentally discovered on abdominal radiograph. A careful abdominal examination and, in women, a pelvic examination are important to rule out other potential causes of abdominal pain.
A. Laboratory evaluation should include a complete blood cell count, serum chemistries, and urinalysis. The white blood cell count may be mildly elevated but is generally less than 15,000/mm
3. A white blood cell count greater than 15,000/mm
3 is suggestive of another intra-abdominal cause or an associated infection behind an obstructing calculus. An elevation of the serum blood urea nitrogen (BUN) and creatinine concentrations indicates prerenal azotemia, parenchymal renal disease, or obstruction of
a solitary functioning kidney. A urinalysis should be performed routinely in any patient with abdominal pain. Microscopic hematuria is observed in approximately 90% of patients with renal colic.
B. Once the diagnosis is suspected based on the history, physical examination, and preliminary laboratory studies, establishing a definitive diagnosis is the focus of the next stage of the evaluation.
1. A flat radiographic plate of the abdomen is often obtained and is capable of identifying radiopaque stones (calcium oxalate, calcium phosphate, struvite-carbonate, and cystine) that are ???2 mm in size. It will miss radiolucent stones, the most common of which are composed of uric acid, and stones that overlie the bony pelvis. For these reasons, an abdominal flat plate is most valuable in ruling out other intra-abdominal processes.
2. An ultrasonographic examination of the genitourinary tract often identifies stones in the renal pelvis; however, most of the stones are lodged in the ureter, and the ultrasonographic examination often misses these.
3. The intravenous pyelogram (IVP) was formerly considered the gold standard for the diagnosis of nephrolithiasis and is still of considerable value in the acute setting. Although the stone itself may not be visualized on IVP, the site of obstruction is regularly identified. Structural or anatomic abnormalities that may be present in the urinary tract and renal or ureteral complications can be recognized. Disadvantages of the IVP include the need for intravenous contrast and the prolonged waiting time often required to visualize the collecting system on the side of the obstruction.
4. Spiral computed tomography (CT) is the test of choice in the patient with suspected renal colic. The advantages of spiral CT include higher sensitivity, faster scan times, and lack of need for contrast.
C. Management. After the diagnosis is established, subsequent management is determined by (a) the presence or absence of associated pyelonephritis; (b) whether parenteral narcotics are required for pain control; and (c) the likelihood of spontaneous stone passage. Obstructing calculi can be managed with observation alone if pain can be controlled with oral analgesics and spontaneous passage is likely. Extracorporeal shock wave lithotripsy or ureteroscopic lithotripsy may need to be employed for stones lodged in the upper ureter. Calculi in the lower ureter can be removed by cystoscopy and ureteroscopy. Hospital admission is necessary if there is evidence of renal parenchymal infection; when nausea, vomiting, or severe pain precludes oral analgesic use; or the stone is unlikely to pass spontaneously. The likelihood of spontaneous passage is determined by stone size and location in the ureter (
Table 6-1). Small stones in the distal ureter will likely pass, whereas large stones in the upper ureter will likely require urologic consultation and intervention. α1-Receptor antagonists, such as tamsulosin, and calcium channel blockers can be used to aid stone passage (medical expulsive therapy).
II. TYPES OF STONES
A. Calcium-containing stones make up 90% of all stones and are generally composed of a mixture of calcium oxalate and calcium phosphate. In mixed stones, calcium oxalate usually predominates, and pure calcium oxalate
stones are more common than pure calcium phosphate stones. Calcium phosphate tends to precipitate in alkaline urine, as occurs with renal tubular acidosis (RTA), whereas the precipitation of calcium oxalate does not vary with pH. Because urine is acidic in most patients, calcium oxalate stones are more common. The major risk factors for the formation of calciumcontaining stones include hypercalciuria, hypocitraturia, hyperuricosuria, hyperoxaluria, low urine volume, and medullary sponge kidney. These risk factors can occur either alone or in combination. Their relative frequency is shown in
Table 6-2.
1. Hypercalciuria is often defined as urinary calcium excretion greater than 250 mg/24 hours in women and greater than 300 mg/24 hours in men. Hypercalciuria is present in approximately two-thirds of patients with calcium-containing stones and may result from an increased filtered load, decreased proximal reabsorption, or decreased distal reabsorption. Proximal calcium reabsorption parallels sodium. Any situation that decreases proximal sodium reabsorption such as extracellular fluid (ECF) volume expansion also decreases proximal calcium reabsorption. Distal tubular calcium reabsorption is stimulated by parathyroid hormone (PTH), thiazides, and amiloride and inhibited by acidosis and phosphate depletion.
Hypercalciuria may be idiopathic or secondary to primary hyperparathyroidism, RTA, sarcoidosis, immobilization, Paget’s disease, hyperthyroidism, milk-alkali syndrome, and vitamin D intoxication. The idiopathic group makes up 90% of all hypercalciuria. This category of patients is characterized by increased 1,25(OH)
2 vitamin D
3 concentration, suppressed PTH, and reduced bone mineral density. Three potential pathophysiologic mechanisms are postulated: increased intestinal calcium absorption; decreased renal calcium or phosphorus reabsorption; and enhanced bone demineralization. On the basis of a fast-and-calcium-load study, some authors advocate subdividing idiopathic hypercalciuria into
absorptive hypercalciuria type I (due to primary intestinal calcium hyperabsorption with low-normal PTH), type II (dietary calcium-dependent hypercalciuria), type III (intestinal calcium hyperabsorption induced by elevated calcitriol levels secondary to renal phosphate leak), and renal leak hypercalciuria. Patients with absorptive hypercalciuria have exaggerated intestinal calcium reabsorption, which can be reduced in some by dietary calcium restriction. Some authors have expressed concern over the potential long-term effects of dietary calcium restriction. Patients with idiopathic hypercalciuria often have reduced bone mass and are in negative calcium balance, which may be further exacerbated by a low-calcium diet. In addition, a reciprocal relationship exists between free calcium and free oxalate in the intestinal lumen. Calcium acts to bind oxalate in the intestine and reduce absorption. If oral calcium intake is reduced, oxalate remains free in the intestinal lumen and its absorption increases. However, this may be reduced by concomitant oxalate restriction. Finally, as shown in
Table 6-3, most randomized controlled trials demonstrating that a given pharmacologic intervention reduces the risk of calcium-containing stones did not subdivide patients based on results of a calcium load study. Whether patients with recurrent calcium oxalate stone formation should ingest a diet that is either liberal or restricted in calcium remains controversial and will be further discussed in the section on therapy.
In primary hyperparathyroidism, filtered calcium load is increased as a result of bone calcium release and increased intestinal calcium absorption mediated by 1,25(OH)2 vitamin D3. In those patients with hypercalciuria, the increase in filtered calcium load overcomes distal PTH action to increase tubular calcium reabsorption. In RTA, the decreased systemic pH results in increased calcium release from bone. In addition, acidosis directly inhibits distal nephron calcium reabsorption.
Macrophages in sarcoidosis produce 1,25(OH)2 vitamin D3, which leads to increased intestinal calcium absorption. Immobilization, Paget’s disease, and hyperthyroidism cause hypercalciuria by releasing calcium from bone and increasing filtered calcium load.
2. Hypocitraturia. It is defined as less than 320 mg citrate excretion/day. Citrate combines with calcium in the tubular lumen to form a nondissociable but soluble complex. As a result, less free calcium is available to combine with oxalate. Citrate also prevents nucleation and aggregation of calcium oxalate. Chronic metabolic acidosis from any cause enhances proximal tubular citrate reabsorption and decreases urinary citrate concentration; this is the mechanism whereby chronic diarrhea, RTA, and increased dietary protein load result in hypocitraturia. Another important cause of hypocitraturia is hypokalemia, which increases expression of the sodium-citrate cotransporter present in the proximal tubular luminal membrane.