An Update and Practical Guide to Renal Stone ManagementJohri N.a · Cooper B.d · Robertson W.a · Choong S.c · Rickards D.b · Unwin R.a
aCentre for Nephrology, UCL Medical School, Royal Free Campus, and Departments of bRadiology and cUrology, University College Hospital, London, UK; dNephrology Department, Royal North Shore Hospital, Sydney, N.S.W., Australia Corresponding Author
Centre for Nephrology, UCL Medical School
Royal Free Campus, Rowland Hill Street
London NW3 2PF (UK)
Tel. +44 207 472 6499, E-Mail firstname.lastname@example.org
Renal stone disease covers kidney and lower urinary tract stones caused by a variety of conditions, including metabolic and inherited disorders, and anatomical defects with or without chronic urinary infection. Most cases are idiopathic, in which there is undoubtedly a genetic predisposition, but where environmental and lifestyle factors play an important role. Indeed, it is becoming apparent that renal stone disease is often part of a larger ‘metabolic picture’ commonly associated with type 2 diabetes, obesity, dyslipidaemia, and hypertension. Renal stone disease is a growing problem in the UK (and other developed and developing populations) with a cross-sectional prevalence of ∼1.2%. This means that there are currently ∼720,000 individuals with a history of kidney stones in the UK. Almost 40% of first-time stone formers will form a second stone within 3 years of the first episode if no prophylactic measures are instituted to prevent stone recurrence, since removal or disintegration of the first stone does not treat the underlying cause of stones in the majority of patients. The age of onset is getting younger and the sex ratio (until recently more men than women) is becoming almost even. Metabolic screening remains an important part of investigating renal stone disease, but to the disappointment and frustration of many doctors, medical treatment is still essentially pragmatic, except perhaps in cystinuria, and to a limited extent in primary hyperoxaluria (if pyridoxine-sensitive); although newer treatments may be emerging. This review summarizes current thinking and provides a practical basis for the management of renal stone disease.
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Renal stone disease is common, with a worldwide prevalence of between 2 and 20% [1,2,3]. Highest lifetime risk of stone formation has been reported in men in the United Arab Emirates (UAE) and Saudi Arabia (KSA) (fig. 1). Prevalence within Europe ranges more narrowly between 2 and 8%; however, a recent study in Greece found prevalence as high as 15% in a rural population in Thebes . Epidemiological studies in the United States show a trend for increasing prevalence in women and those living in more southern latitudes: males in the southeast have a prevalence rate of 12% compared with 7% in the northwest .
Stone recurrence worldwide is also common: it is estimated that almost 50% of stone formers will have a recurrence within 10 years . Recurrent stone disease causes not only pain and distress in those affected, but it also imposes a significant economic burden from lost working days and associated healthcare costs. Minimally invasive surgery has revolutionized acute and complex stone management, but it has not reduced recurrence rates because less invasive therapies, including extracorporeal shock-wave lithotripsy (ESWL), often result in incomplete stone clearance. However, there is evidence that intervention in the form of lifestyle advice  and some forms of medical therapy can reduce the rate of stone recurrence ; thus, metabolic investigation and medical treatment are both important elements in the clinical management of renal stone disease. This review summarizes what we currently know and think about renal stone disease, and it sets out a practical approach to renal stone management, based largely on the authors’ collective experience.
Renal stone disease is not a single disorder, since stone composition varies, which reflects constitutional, environmental, and genetic factors (cystine stones are probably the most common genetic type seen in adult clinical practice). Table 1 lists the main types of renal stone and their relative prevalence.
The physico-chemical theory of stone formation considers urine as a supersaturated solution in which homogeneous or heterogeneous nucleation can lead to initiation of crystal formation, which can then aggregate and grow. However, incompletely understood biological processes can anchor these crystals to the urothelium. A widely held theory is that of Randall’s plaques, which proposes that subepithelial interstitial calcium-based deposits (the originally described ‘Randall’s plaques’) act as nuclei for stone formation. These plaques, which are composed of apatite (calcium phosphate and not calcium oxalate), originate adjacent to the thin limbs of loops of Henle (which could be related to the high local ion concentrations at this site). As they grow in size, they erode through the renal papillary duct epithelium to provide sites for intratubular calcium oxalate crystal adhesion and growth. Radiological and endoscopic studies have shown that many, but not all, stone formers have Randall’s plaques [8,9]. While this theory might explain the origin of many calcium oxalate stones, the plaques are not evident in non-calcium stones or in all calcium oxalate stone formers, for example, post-gastric bypass surgery. A more recent theory is that surface molecules such as phosphatidylserine, sialic acid, hyaluronan, osteopontin, or the glycoprotein receptor CD44 (involved in cell adhesion), expressed on the luminal membrane of collecting duct epithelial cells, may promote or retard cell membrane-crystal interactions [10,11,12]. In the presence of these molecules, crystals adhere to the luminal membrane, where they are normally taken up into the cell by endocytosis and degraded or transported into the interstitium (perhaps to form Randall’s plaques) . Several in vitro studies have shown that cell injury and repair, or regeneration, increase the surface expression of these molecules, resulting in more crystal adhesion , which may form the nidus for eventual stone formation; defective endocytosis may also be a causal factor (e.g. in Dent’s disease) .
Certain environmental and lifestyle factors can increase stone risk. A higher risk is found in professional chefs or others working in hot environments, as well as in taxi drivers who often try to minimize their fluid intake to avoid too many ‘toilet stops’.
Diet-related factors that are known to increase stone risk are listed in table 2. Tea or coffee (particularly instant coffee) without milk has been shown to increase oxalate excretion, although this effect is probably offset by their diuretic action . Dietary calcium has a biphasic risk curve: stone risk is greater in those on a high or low calcium diet . The link between vitamin D intake and renal stones is less clear: while excessive active (1,25-OH) vitamin D supplementation, by increasing intestinal calcium absorption, increases the risk of stone formation, there is no evidence that correction of native (25-OH) vitamin D deficiency has the same effect; moreover, correction, especially if there is secondary hyperparathyroidism, is likely to be a health benefit. Vitamin C excess could also increase the risk of calcium oxalate stone formation, but in practice this is rarely encountered. High dietary intake of potassium or magnesium is inversely related to stone formation because potassium promotes urinary citrate excretion, and both citrate and magnesium inhibit crystal formation. However, the impact of low urinary magnesium on stone risk is at best modest. Other factors associated with increased stone risk are chronic laxative abuse, antacid excess or betel nut chewing (both forms of ‘milk-alkali syndrome’), tropical holidays, regular strenuous exercise, and even psychological stress (although how is unclear).
Several non-lifestyle factors can increase the risk of stone formation and recurrence; these, along with the underlying mechanisms, are listed in table 3. Conditions in which there is insulin resistance, such as obesity, the metabolic syndrome , and type 2 diabetes mellitus [19,20], are now known to be associated with increased stone risk. Insulin resistance may be the underlying cause, as it is linked to reduced renal ammoniagenesis and decreased urinary ammonium excretion relative to net acid excretion, resulting in a more acid urine pH, which favours uric acid and mixed urate-calcium oxalate stone formation .
Congenital, surgical and anatomical defects causing localized urine stasis and renal stones include medullary sponge kidney, horseshoe kidney, enterocystoplasty, and pelviureteric junction obstruction.
Colonization of the gut by an oxalate degrading anaerobe, Oxalobacter formigenes, has been linked to reduced oxalate stone risk . It has been shown that these bacteria not only degrade oxalate, but that they also interact (in an as yet unspecified way) with the chloride/oxalate anion exchanger (CFEX, SLC26A6) present in intestinal epithelial cells to increase oxalate secretion and reduce its net absorption .
Gastric bypass surgery (Roux-en-Y) is increasingly used to treat widespread obesity (which itself is a risk factor for renal stones). Recent studies have shown increased stone risk following this form of surgery , which is due to ‘enteric hyperoxaluria’ from a combination of disturbed enterohepatic bile circulation and loss of calcium (that normally binds dietary oxalate) through binding to fatty acids, and changes in the gut microflora affecting oxalate absorption.
A positive family history of kidney stones is strongly associated with increased stone risk. Relative risk in those with a positive family history is 2–3 times higher, and several genetic factors have been proposed that may explain some of this association. Alanine:glyoxylate aminotransferase (AGT) is a key vitamin B6 (pyridoxine)-dependent enzyme found predominantly in liver peroxisomes, where it converts glyoxylate to glycine, reducing the formation of oxalate from glyoxylate. A polymorphism of this enzyme (Pro11Leu) has been identified that mistargets some AGT to mitochondria rather than peroxisomes. Peroxisomes deal more effectively with plant-derived glycolate, whereas mitochondria handle meat-derived hydroxyproline, both sources of glyoxylate production. Thus, the Pro11Leu AGT polymorphism may be an advantage to those consuming a high animal protein diet, but a disadvantage for those on a more vegetarian diet ; as yet this hypothesis remains untested. The already mentioned novel oxalate transporter CFEX is present in renal and intestinal epithelia, and CFEX null mice have a high incidence of calcium oxalate stones, primarily due to increased oxalate absorption in their small intestine . It is possible that polymorphisms of this transporter may affect oxalate absorption in humans and thereby calcium oxalate stone risk. Other gene polymorphisms that have been linked to increased renal stone risk include the renal sodium-phosphate co-transporters NaPT2a and NaPT2c, the sodium-proton exchanger regulatory factor NHERF1 , as well as the renal calcium-sensing receptor , and some monogenic disorders such as primary hyperoxaluria (types I and II), Dent’s disease, Bartter’s syndrome (types I and II), inherited forms of distal renal tubular acidosis (dRTA), and cystinuria.
Metabolic investigations are important in predicting the likely stone type (if stone material is not available for analysis), in identifying secondary causes and metabolic risk factors, in assessing prognosis, and as a guide to therapy. Ideally, a complete metabolic workup should include fasting blood and spot urine samples, along with non-fasted 24-hour urine collections for analysis. Contemporaneous dietary assessment is useful in interpreting the results of blood and urine analyses and to give tailored dietary advice on how to minimize future stone risk. A 1-week diet diary gives a reasonable average, although a shorter period can still be useful. While a detailed metabolic screen may not be necessary in cases of first presentation with a single stone, it should be considered in those with multiple stones, bilateral stones, uric acid stones, staghorn calculi, nephrocalcinosis, a single kidney, a history of recurrent stones, or in those undergoing workup as prospective live kidney transplant donors and found to have an incidental renal stone1. Those with their first kidney stone at an early age (<25 years), or those found to have renal impairment with stones, should also be investigated further. Figure 2 is the clinical management algorithm that we currently use in renal stone disease. Ideally, metabolic screening should be postponed until at least 6 weeks after a stone episode or intervention such as ESWL, percutaneous nephrolithotomy (PCNL) or uretero-renoscopy (URS), since initial compliance with more general measures like increased fluid intake is usually good for the first few weeks after an episode of painful renal colic.
The value of chemical stone analysis (usually carried out by infra-red spectroscopy and/or quantitative wet analysis) cannot be overemphasized; although it does not replace metabolic investigations, it can add to or confirm any findings and help in their interpretation. Unfortunately, in most stone clinics, renal stone analysis is available in only 30 or 40% of cases. This is because small stones are often passed without the patient realizing it, or because of the difficulties in trying to collect stone material after lithotripsy.
Routine blood tests should include urea, creatinine, electrolytes, glucose, chloride, bicarbonate, uric acid, calcium, phosphate, magnesium, parathyroid hormone and vitamin D. These blood values help to establish baseline renal function and can detect primary or secondary hyperparathyroidism, hyperchloraemic metabolic acidosis, and features of the metabolic syndrome, including impaired glucose tolerance. Spot fasting urine testing should include pH, electrolytes, protein, and a qualitative cystine screen. Screening urine for retinol-binding protein and N-acetylglucosamine are useful in patients with a suspected underlying proximal tubulopathy (e.g. Fanconi syndrome or Dent’s disease). Urine dipstick testing is helpful in detecting blood, protein, leukocyte esterase and nitrites2. If positive, microscopy and urine culture screening for infection should be considered; however, in patients with kidney stones or fragments still in situ, dipstick testing is often positive for blood, protein and esterase without infection.
Urine pH is a key determinant of stone formation, but it can vary widely before and after meals; measurement on a fasting early-morning (second void) sample reduces variability. Urinary infection with urea-splitting organisms like Proteus, Klebsiella or Pseudomonas species can increase urine pH by generating ammonium to produce stones composed of ammonium-magnesium-phosphate; these stones are also found in chronic laxative abuse (sometimes a clue to an underlying eating disorder), which causes potassium depletion that stimulates ammoniagenesis and reduces citrate excretion. When adjusted for diet, which can be used to calculate a predicted urine pH , an ‘inappropriately’ acid urine pH is often found in uric acid and calcium oxalate stone formers with underlying metabolic syndrome or type 2 diabetes mellitus (see fig. 3).
Samples from 24-hour urine collections should be analyzed for volume, pH, calcium, phosphate, magnesium, oxalate, citrate, urate and electrolytes (Na+, K+ and Cl–), creatinine and urea (a useful index of dietary protein intake). Urinary electrolytes can be used to calculate the urine anion gap to estimate urinary ammonium (NH4+), which is often reduced in renal tubular acidosis (RTA) or type 2 diabetes (‘metabolic syndrome’). Two or more 24-hour collections on consecutive days help to achieve better averaging, since analyte concentrations tend to vary from day to day. The first 24-hour collection is made in an acid-containing bottle (pH <2) for a more accurate estimate of urinary oxalate. Urine acidification prevents precipitation of calcium oxalate crystals and interference from vitamin C in colorimetric-enzymatic assays. The second collection is made in a plain container to measure average 24-hour pH, uric acid and protein concentrations.
Urinary citrate is an inhibitor of crystallization of calcium salts in urine, and studies have linked lower levels of urinary citrate excretion to increased calcium oxalate stone risk . Urinary citrate levels of <2.0 mmol/day in males and <2.5 mmol/day in females are considered abnormal. A low urinary citrate occurs with metabolic acidosis (e.g. in distal or type 1 RTA3) and with chronic potassium depletion. Low urinary citrate excretion is also commonly found in those with a high dietary intake of animal protein (a high acid-ash diet), whereas vegetarians (a high alkaline-ash diet) tend to have higher levels of citrate excretion.
In idiopathic calcium oxalate stone formers, hypercalciuria is the commonest metabolic abnormality . Stone risk is a continuum that increases with increasing concentrations of urinary calcium and oxalate. Any cut-offs are largely dependent on the reference population and analytical methods used, but urinary calcium excretion >6.0 mmol/24 h is considered abnormal in stone formers, and a reduction can reduce rates of stone recurrence. Before diagnosing ‘idiopathic hypercalciuria’, primary hyperparathyroidism, vitamin D excess, milk-alkali syndrome, multiple myeloma and malignancy should be excluded; high dietary sodium also increases urinary calcium excretion. Hypercalciuria in dRTA is really only seen in those patients who are acidotic (so-called ‘complete’ dRTA) with serum bicarbonate concentrations <20 mmol/l.
Idiopathic hypercalciuria patients have been subdivided into those who have increased intestinal absorption (‘hyperabsorptive hypercalciuria’) and those who have increased renal losses (‘renal hypercalciuria’); however, this classification provides no insights into the underlying mechanisms, or helps in the management, of idiopathic hypercalciuria. Moreover, urinary oxalate is the critical factor in calcium oxalate stone formation because its concentration is much less than that of urinary calcium. This means that a small decrease in urinary oxalate will have a much greater impact on the reduction in stone risk than a decrease in urinary calcium. Urinary oxalate levels of >450 µmol/day are considered abnormal. A variable amount of urinary oxalate is derived from the diet (10–20%), which depends on oxalate intake, intestinal absorption (and excretion), and concomitant dietary calcium. Oxalate absorption is increased in inflammatory bowel disease (Crohn’s disease or ulcerative colitis affecting the small intestine), following small bowel resection, and after gastric bypass surgery (see earlier). However, most urinary oxalate is endogenous in origin and the metabolic end-product of glyoxylate. Very high levels of urinary oxalate (>800 µmol/day) occur in primary hyperoxaluria (types I and II), which does not always present in early childhood; high levels (>450 and <800 µmol/day) are seen more commonly in idiopathic hyperoxaluria.
Hyperuricosuria and hyperuricaemia are positively linked to both uric acid and calcium oxalate stone formation (through heterogeneous nucleation) . Hyperuricosuria is most commonly associated with a high purine-containing (animal protein and beer) diet, uricosuric drugs, increased protein catabolism, and, more recently, the metabolic syndrome. Ten percent of patients with gout have associated hyperuricosuria, and the risk of uric acid stones is proportional to uric acid excretion: only 11% of patients with uric acid excretion <1.8 mmol/day have uric acid stones , whereas 23% of those excreting >3.6 mmol/day, and 50% of those excreting >6 mmol/day, have stones .
Since stone risk is a composite of several risk factors, use of risk indices that combine these risk factors to give a single and predictive score has always been a goal, especially since any intervention can only be judged by rates of stone recurrence. Several risk indices have been proposed : Tiselius risk index, Bonn Risk Index, and calcium oxalate risk index, EQUIL, SEQUIL, and Psf. All, except for Psf, have a physico-chemical basis, treating urine as a supersaturated solution with citrate as the main stabilizer or inhibitor. In contrast, Psf is based on retrospective observational metabolic data comparing non-stone formers with stone formers. Figures 4 and 5 summarize SEQUIL and Psf, respectively. These scores (which can be combined) can be used to determine the most significant risk factors in an individual patient and as a guide to medical therapy, including the use and balance of fluid intake and citrate supplements.
Previously, those presenting with renal colic had an emergency plain X-ray or KUB (kidneys, ureters and bladder). If a stone was identified in the line of the ureters, no further investigation was considered necessary, and appropriate urological treatment was carried out. When there was any doubt about a radio-opacity or none was detected, an intravenous contrast study (pyelography or urography, IVP/IVU) was performed. The classic triad of a delayed pyelogram, dense and persistent nephrogram, and dilatation of parts, or all, of the upper urinary tract indicated a ureteric obstruction, usually requiring prompt surgical intervention. However, since the advent of computerized tomography (CT), the non-contrast or unenhanced CT-KUB has rendered IVU obsolete and it is rarely used today. Why is CT-KUB so much better? It can detect and localize almost 100% of stones, whatever their composition (except some drug-containing stones, e.g. indinavir) or radio-opaqueness on KUB; small stones overlying bony structures can also be missed on KUB. The degree and duration of obstruction can be diagnosed with CT-KUB, as well as abnormally sited stones, and stones in post-operative urinary tracts. Moreover, CT-KUB does not usually require use of contrast, thus avoiding the risk of allergic reactions or an acute deterioration in renal function in those with renal impairment. In addition, using the Hounsfield units of image opacity on CT, an estimate of stone composition and ‘hardness’ can also be made and thus the likelihood of successful fragmentation by lithotripsy.
Ultrasound scanning (USS) is of limited value in the initial investigation and management of renal stones because of its low sensitivity compared with CT-KUB (<25 vs. >95%) , although it does have a place in following up any identified stones. Recurrent and frequent stone formers usually require periodic radiological surveillance, since there is evidence that asymptomatic stones may dislodge and cause ureteric obstruction; combined USS with KUB is the most convenient way of doing this. Although more sensitive than KUB or USS, CT-KUB has the major disadvantage of its cumulative radiation dose and it should not be repeated too often. The choice and frequency of imaging ought to be guided by the clinical features in consultation with colleagues in radiology and urology.
Surgical management of urinary tract stones depends on their size and site, and on any symptoms and signs, particularly of obstruction. Stones can lodge in the proximal, mid- (overlying the sacroiliac joint) or distal ureter. Approximately 70% of small (≤5 mm) ureteric stones and 50% of stones >5 and ≤10 mm should pass spontaneously; α- blocker therapy can increase the rate of stone passage by up to 30% . With a ureteric stone >10 mm, and when pain persists despite intramuscular diclofenac or pethidine, and/or if there is renal obstruction, treatment is by endoscopic removal (URS). However, if this is not possible, a ureteric stent or nephrostomy tube is inserted until URS can be carried out. In a patient with an obstructed kidney and signs of infection, relief of obstruction is an emergency. With small ureteric stones and satisfactory pain control with analgesia, patients can be given a supply of an α-blocker and reviewed within 2 weeks. Stones <10 mm in the proximal and mid-ureter can also be managed by lithotripsy, but distal ureteric stones of whatever size are better treated by URS .
Calyceal and pelvic stones can be managed by lithotripsy, flexible URS and laser removal, or PCNL. As with ureteric stones, the choice depends on size and site, hardness (assessed by CT – see above), intrarenal anatomy, and the patient’s symptoms and preference. Patients with asymptomatic stones are usually offered treatment, since if left untreated, over 70% of stones are likely to increase in size, dislodge and cause symptoms . Lithotripsy can be recommended for stones <20 mm in size; a course of treatment involves two or more 30-min sessions. Contraindications to lithotripsy are pregnancy or taking anticoagulants such as warfarin and clopidogrel (aspirin should be stopped 10 days before treatment). Reported success rates for lithotripsy vary from 30 to 100%, depending on how patients are selected, how hard the stone is, and the type of lithotripter used [39,40]. Complications of lithotripsy are rare , although there have been unusual case reports of post-treatment anti-GBM antibody-positive glomerulonephritis [42,43], and even a later increase in the incidence of hypertension and diabetes . A stone in a calyceal diverticulum, or a dependent lower pole calyx, can break up, but may not pass. Treating large stones with lithotripsy risks producing multiple stone fragments that can cause ureteric obstruction (so-called ‘steinstrasse’), unless a ureteric stent is in place. It can take several weeks to determine if lithotripsy will be successful. Renal stones that do not respond to lithotripsy can be treated by flexible URS if they are small (∼3 mm), but larger stones ≥20 mm, or those in a calyceal diverticulum or lower pole calyx, are better treated by PCNL. Surgical treatment depends on available local expertise and facilities, as well as a patient’s preference.
Fluid intake and dietary advice are important interventions in all stone formers and remain first-line in stone management. Controlled trials have shown that increasing urine volume to at least 2 litres a day can reduce recurrence rates by 40–50% . Fluid intake should include mainly water, and tea or coffee should be taken with some milk (which binds free oxalate). Bear in mind that increasing fluid intake, and thus urine volume, may critically lower urinary citrate concentration, especially if it is already low. Citrus fruits, particularly lemons and limes, may be of some benefit, but the sugar content of many fruit juices is a disadvantage. A calcium intake of ∼25 mmol/day is the estimated mean on a typical Western diet, whereas oxalate intake is ∼1.5 mmol/day. The ratio of dietary oxalate/total calcium is a guide to dietary modifications; in the general population this is around 0.05. Several studies have shown that low dietary calcium increases the risk of calcium oxalate stones, and stone formers should generally be advised to maintain a normal, and not to reduce, calcium intake. A small reduction in urinary oxalate can significantly reduce the risk of forming calcium oxalate stones (see earlier), therefore, avoiding oxalate-rich foods (spinach, rhubarb, beetroot, soya beans and tofu, nuts, peanut butter, okra, yams, sesame seeds, tahini and chocolate) is justified, even if the contribution of dietary oxalate to urinary oxalate excretion is limited . A reduction in dietary fat intake can decrease urinary oxalate excretion: in 13 patients with disease of the ileum (mainly due to Crohn’s disease) who switched from a 100- to a 40-gram fat diet, oxalate excretion decreased slowly, but significantly, up to 50%, if faecal fat excretion fell to <15 g/day . In patients with significant hypercalciuria and a high calcium intake (particularly if derived from dairy produce, the more absorbable form), some reduction in dietary calcium with oxalate may be justified. Reducing daily animal protein intake, including fish, red meat and poultry (there is no distinction for stone risk), to 40–50 g (140–160 g of animal flesh) per day is recommended in both calcium oxalate and uric acid stone formers, although a low protein diet is not advisable. Replacing animal protein with fresh fruit and vegetables should be encouraged, as this not only reduces urate excretion, but it also alkalinizes the urine; increased potassium intake can also increase urinary citrate excretion. Beer increases urate excretion due to its high content of the purine guanosine, and it should be restricted in uric acid stone formers; non-fortified wines, though uricosuric, have a much smaller effect on urate production and excretion. Increasing dietary potassium and magnesium, if urinary levels are low, and reducing dietary sodium, if intake and excretion are high, are also worthwhile measures and can be achieved by eating a more Mediterranean-style diet, such as the widely publicized DASH (Dietary Approaches to Stop Hypertension) diet .
Thiazide diuretics can be tried in recurrent calcium oxalate stone formers with idiopathic hypercalciuria. Randomized-controlled trials have shown reductions in stone recurrence rates of up to 70% with thiazide diuretics . Adverse effects that may offset any benefit are hypokalaemia (associated with reduced citrate excretion), hyperuricaemia, and hyperglycaemia. Use of thiazides in calcium oxalate stone formers without hypercalciuria is unlikely to be beneficial . Citrate supplements have been shown to reduce stone recurrence in idiopathic calcium oxalate stone formers with hypocitraturia and also in those with normal urinary citrate levels [51,52]. Alkali therapy in the form of potassium or magnesium citrate (40–120 mmol/day in 2–3 divided doses) can be used to try to boost citrate excretion (to >3 mmol/day) in stone formers with hypocitraturia, but these salts are not always well tolerated. Although sodium citrate is better tolerated, like sodium bicarbonate, it has the disadvantage of an additional sodium load, which may tend to increase calcium excretion. However, by raising urine pH, all alkalis can increase the risk of forming calcium phosphate stones, but less so if given as the potassium salt (see fig. 6). Allopurinol has been shown to benefit recurrent calcium oxalate stone formers who have hyperuricaemia or hyperuricosuria , but not those who have normal urate excretion. Allopurinol in doses of 50 or 100 mg daily can be prescribed if dietary recommendations do not reduce urinary urate excretion; doses of 300 mg or more daily are usually required in hyperuricaemic patients. Calcium supplements may be necessary in those with a low calcium intake (<15 mmol/day) and high oxalate/total calcium ratio (>0.05 – see earlier); calcium supplements taken with meals may also be helpful in those with enteric hyperoxaluria. Pyridoxine can sometimes reduce oxalate excretion in primary hyperoxaluria (PH1, but not PH2), but not in idiopathic hyperoxaluria. Finally, because of the underlying hypothesis that stone formation is the result of initial renal tubular cell injury, which may involve oxidative damage, especially from oxalate, antioxidants such as vitamin E, catechin in green tea, and some flavenoids like quercetin, have been proposed as adjunctive therapy , although there is little supporting data in humans.
Unlike the other main stone types, uric acid stones can be managed medically. The aim of treatment is to increase the solubility of uric acid in urine and to reduce its concentration. Increasing urine volume to >2.5–3.0 l/day is essential and should be emphasized. Alkalinization of urine may be carried out using citrate or bicarbonate salts given in 2 or 3 daily divided doses. Alkali treatment can be guided by urine pH to achieve a fasting urine pH >6.0 (a fasting urine pH of >7 can increase the risk of forming calcium phosphate stones). As already mentioned, allopurinol is a useful adjunct in reducing urate excretion. A focus on long-term weight reduction and a low animal protein diet is also worthwhile.
Struvite, or triple phosphate (calcium, magnesium, ammonium phosphate), stones form in alkaline urine from infection with a urea-splitting organism. Treatment is with antibiotics and sometimes the urease inhibitor acetohydroxamic acid. Pure calcium phosphate stones should always raise the possibility of an underlying defect in renal acid excretion, more specifically dRTA, especially if nephrocalcinosis is also present. This can be detected by acid loading with oral ammonium chloride, or the more convenient furosemide plus fludrocortisone urinary acidification test .
Cystine stones are rare but require intensive management to prevent complications and recurrence. Treatment is aimed at reducing the concentration of free cystine (formed from oxidation of the amino acid cysteine) in urine and increasing its solubility. A high fluid intake of around 4–5 litres a day is required, and to drink before going to bed and during the night to maintain a dilute urine overnight. Alkalinization of urine with citrate or bicarbonate will increase cystine solubility, but fasting urine pH needs to be >7, with the attendant risk of calcium phosphate precipitation, unless urine is sufficiently dilute. Twenty-four-hour urine cystine measurements are used to guide therapy: if 24-hour urine cystine concentration remains >2,000 µmol/l, chelation therapy is usually necessary, given as D-penicillamine or Tiopronin (α-mercaptopropionylglycine), to reduce free cystine concentration to <1,000 µmol/l (ideally <500 µmol/l). These compounds bind cysteine and prevent formation of less soluble cystine. D-penicillamine is more easily available, but can have serious side effects (agranulocytosis and proteinuria), and it needs close monitoring and careful dose titration.
Apart from some rare drug-related causes of renal stones, such as triamterene, indinavir and, more recently, lopinavir, investigation and practical management of renal stone disease require a holistic approach. Renal stones do occur more commonly in patients with hypertension, diabetes, and the metabolic syndrome, and their presence could be viewed as yet another cardiovascular risk factor . In fact, the advice that we give and the treatments we recommend are of wider cardiovascular benefit, which is worth reinforcing in our patients.
Whether the finding of an incidental and asymptomatic renal stone should exclude kidney donation is debatable and must depend on the individual circumstances. If the stone is small, single, and unilateral, and/or can be easily treated by lithotripsy, and the estimated future stone risk is low (see later), then the affected kidney is the one that can be donated; however, all such donors should be monitored indefinitely because of the still finite risk of stone formation in a single kidney.
Use of a routine clinic urine dipstick to measure urine pH is inaccurate and should not be used for reliable urine pH measurements.
In proximal or type 2 RTA, citrate excretion may be normal or increased.
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