Renal oxalate excretion following oral oxalate load in patients with urinary calculus disease and healthy controls

Oral oxalate loading using sodium oxalate or a vegetable juice was done to evaluate the intestinal absorption of exogenous oxalate in 30 patients with renal stones and 13 healthy controls. Fifteen calcium oxalate stone formers, 7 non-oxalate stone formers and 10 healthy volunteers were given an oral loading of sodium oxalate (500 mg). Urinary oxalate increased promptly, reaching a peak value within 4 to 8 hours after administration of a synthetic oxalate orally in a fasting state. In calcium oxalate stone formers, the mean increment of urinary oxalate and the bioavailability following oral sodium oxalate load were significantly higher than in the healthy controls and non-oxalate stone formers. Furthermore, intestinal hyperabsorption of oxalate in our criterion was defined in six patients with calcium oxalate stones (40%). On the other hand, eight calcium oxalate stone formers and three healthy controls were given vegetable juice. Urinary oxalate was increased only slightly after the ingestion, and there was no difference between calcium oxalate stone formers and normal controls. These results suggest that a certain hyperoxaluria might be induced by intestinal absorption of exogenous oxalate, and that the hyperabsorption might indicate a possible risk factor for calcium oxalate stone formation.     

Intestinal Oxalobacter formigenes colonization in calcium oxalate stone formers and its relation to urinary oxalate

BACKGROUND AND PURPOSE: Oxalobacter formigenes is an anaerobic commensal colonic bacterium capable of degrading oxalate through the enzyme oxalyl-CoA decarboxylase. It has been theorized that individuals who lack this bacterium have higher intestinal oxalate absorption, leading to a higher urinary oxalate concentration and an increased risk of calcium oxalate urolithiasis. We performed a prospective, controlled study to evaluate O. formigenes colonization in calcium oxalate stone formers and to correlate colonization with urinary oxalate and other standard urinary stone risk factors. PATIENTS AND METHODS: Thirty-five first-time calcium oxalate stone formers were compared with 10 control subjects having no history of urolithiasis and a normal renal ultrasound scan. All subjects underwent standard metabolic testing by submitting serum and 24-hour urine specimens. In addition, all subjects submitted stool samples for culture and detection of O. formigenes by Xentr(ix) O. formigenes Monitor. RESULTS: Intestinal Oxalobacter was detected in only 26% of the stone formers compared with 60% of the controls (p < 0.05). Overall, the average urinary oxalate excretion by the two groups was similar (38.6 mg/day v 40.8 mg/day). Among stone formers, however, there were statistically higher urinary oxalate concentrations in O. formigenes-negative patients compared with those testing positive (41.7 mg/day v 29.4 mg/day) (p = 0.03). Furthermore, all 10 stone formers with hyperoxaluria (>44 mg/day) tested negative for O. formigenes (p < 0.05). CONCLUSIONS: Calcium oxalate stone formers have a low rate of colonization with O. formigenes. Among stone formers, absence of intestinal Oxalobacter correlates with higher urinary oxalate concentration and an increased risk of hyperoxaluria. Introduction of the Oxalobacter bacterium or an analog of its enzyme oxalyl-CoA decarboxylase into the intestinal tract may be a treatment for calcium oxalate stone disease.     

The urinary response to an oral oxalate load in recurrent calcium stone formers

PURPOSE: Dietary oxalate may contribute up to 50% to 80% of the oxalate excreted in urine. We studied the urinary response to an oral oxalate load in male and female idiopathic recurrent calcium oxalate stone formers with and without mild hyperoxaluria to evaluate the potential pathophysiological significance of dietary oxalate. MATERIALS AND METHODS: A total of 60 recurrent calcium stone formers underwent an oral oxalate load test. Urine samples were obtained after an overnight fast. Each patient then received an oral oxalate load (5 mM. sodium oxalate dissolved in 250 ml. distilled water) and 3, 2-hour urine samples were obtained 2, 4 and 6 hours after the oxalate load. We compared the response to the oxalate load in patients with and without mild hyperoxaluria, and in male and female patients without hyperoxaluria. RESULTS: The peak urinary response occurred 4 hours after the oral oxalate load in all patients. Those with mild hyperoxaluria had a mean fasting urinary oxalate-to-creatinine ratio +/- SE of 0.027 +/- 0.003 and a mean peak urinary oxalate-to-creatinine ratio of 0.071 +/- 0.006. In comparison, patients with normal oxalate excretion had a fasting and peak urinary oxalate-to-creatinine ratio of 0.018 +/- 0.001 and 0.056 +/- 0.004, respectively (p <0.05). The mean 6-hour increment for urinary oxalate excretion after the oxalate load for patients with hyperoxaluria versus those with normal urinary oxalate excretion was 17.2 +/- 1.9 versus 12.1 +/- 0.98 mg. (p <0.05). In the subset of patients with normal urinary oxalate excretion mean 6-hour cumulative urinary oxalate excretion was 16.8 +/- 1.3 and 13.3 +/- 1.4 mg. in males and females, respectively (p not significant). CONCLUSIONS: Recurrent calcium stone formers with mild hyperoxaluria have higher fasting urinary oxalate and an exaggerated urinary response to an oral oxalate load compared with recurrent calcium stone formers with normal urinary oxalate excretion. Men and women stone formers without hyperoxaluria excrete similar fractions of an oral oxalate load. Increased gastrointestinal absorption and renal excretion of dietary oxalate may be a significant pathophysiological mechanism of stone formation in patients with mild hyperoxaluria.     

Intestinal absorption of oxalate and calcium in patients with jejunoileal bypass

Jejunoileal bypass (JIB) has been widely performed for treatment of excessive obesity. Formation of calcium oxalate stones is a common side effect. Since, under physiological conditions, the intestinal absorption of calcium and that of oxalate are interrelated, intestinal oxalate and calcium absorption were measured in the present study by isotope techniques in 19 JIB patients and 20 healthy controls. The JIB patients showed pronounced hyperoxaluria and markedly increased absorption of oxalate, with a urinary excretion of 14C-oxalate of 29 +/- 19% (controls 6.2 +/- 3.7%; p less than 0.001). There was a strong correlation between the intestinal absorption and urinary excretion of oxalate in the JIB patients (r = 0.72; p less than 0.001). Furthermore, their oxalate kinetics was altered, with continued urinary excretion of 14C-oxalate for up to 48 hours. The JIB patients also had reduced calcium absorption (36 +/- 9.1% vs. 47 +/- 9.0%; p less than 0.001) and patients with malabsorption of calcium and low urinary calcium had the highest intestinal absorption and urinary excretion of oxalate. It is concluded that hyperoxaluria in JIB patients is due to a significant extent to hyperabsorption of oxalate.     

Role of urinary zinc and copper on calcium oxalate stone formation

INTRODUCTION: It is considered that many factors may play a role in urolithiasis. Experimental and clinical studies have shown that zinc has an inhibitory effect on urolithiasis. MATERIALS AND METHODS: In this study, urinary zinc and copper were measured in 27 healthy controls and 30 calcium oxalate stone formers. RESULTS: Urinary zinc excretion was significantly higher (p < 0.001) in stone formers than healthy controls (2,575 +/- 274 and 960 +/- 80 mg/day, respectively). There was no significant difference in urinary copper excretion between healthy controls and stone formers (32.3 +/- 3.5 and 33.3 +/- 3.2 microg/day, respectively). CONCLUSIONS: According to our results, the potent inhibitory effect of urinary zinc excretion on urolithiasis could be reviewed.     

Plasma oxalate concentration in calcium oxalate stone formers

A sensitive, simplified method for plasma oxalate determination by gas chromatography is described. After deproteinizing the plasma with 3N HC1 and 20% sulfosalicylic acid, the oxalate was methylated, extracted and analysed by gas chromatography. This method has three advantages i.e., smaller sample size (plasma 5.0 ml), rapidity (takes less than 3 hours) and accuracy. The recovery rate of oxalate added to plasma was 91.42 +/- 11.31% (SD) and the coefficient of variation of replicate determinations was 4.18%. The minimum detectable concentration of oxalate was 0.3 micrograms/ml (oxalate peak was higher than 5 mm). The mean oxalate concentration under fasting conditions from 16 healthy subjects was 1.37 +/- 0.39 micrograms/ml (SD), while that from 31 calcium oxalate stone formers was 1.45 +/- 0.39 micrograms/ml (SD). There was no significant difference in plasma oxalate concentration between the two groups. The dietary influence of oxalate on plasma and urinary oxalate was investigated in 5 healthy subjects and 5 calcium oxalate stone formers. When 100 g spinach (total oxalate 545.5 mg, soluble oxalate 381.5 mg) was given, the increase of plasma oxalate concentration was more prominent in stone formers; in stone formers it increased to 142% of control value at 2 hours (p less than 0.05) after spinach loading, to 163% at 4 hour (p less than 0.01) and to 232% at 6 hours (p less than 0.01); while in healthy subjects increased to 119% at 2 hours (ns) after loading, to 144% at 4 hours (p less than 0.05) and only to 167% at 6 hours (p less than 0.01). Urinary oxalate excretion increased promptly between 1 and 2 hours after loading in both groups, reaching peak levels between 2 and 4 hours after loading in healthy subjects and between 4 and 6 hours or later in stone formers. The mean renal clearance of oxalate was 18.0 ml/min in 6 healthy subjects and 19.0 ml/min in 4 calcium oxalate stone formers. There was no significant difference in oxalate clearance between the two groups. The mean ratio of oxalate/creatinine clearance was 0.22 for stone formers, which was equal to that for healthy subjects.     

The relationship of 3' vitamin D receptor haplotypes to urinary supersaturation of calcium oxalate salts and to age at onset and familial prevalence of nephrolithiasis.

BACKGROUND: Idiopathic hypercalciuria (IHc) and idiopathic hypocitraturia are frequently associated with calcium nephrolithiasis. We investigated the relationship of vitamin D receptor (VDR) polymorphisms (BsmI, TaqI and FokI) to urinary supersaturation of calcium oxalate salts in recurrent calcium oxalate stone formers with IHc and the clinical relevance of this relationship. METHODS: The study included 110 Caucasian stone formers with IHc and 127 unrelated healthy controls without history of nephrolithiasis. Age at onset of nephrolithiasis, familial history score (FHS) and the ion activity product of calcium oxalate salts in urine (AP(CaOx)) were tabulated. BsmI, TaqI and FokI VDR polymorphisms were evaluated in all participants. RESULTS: Patients and controls were classified as homozygous (bbTT and BBtt) or heterozygous in relation to BsmI and TaqI polymorphisms. Compared with BBtt patients, bbTT homozygous stone formers showed lower citrate excretion (1.91+/-0.89 vs 3.46+/-1.39 mmol/24 h, P = 0.004) and higher AP(CaOx) (2.02+/-0.51 vs 1.53+/-0.53, P = 0.006). Among controls, there were similar differences in citrate excretion and AP(CaOx) between the two groups, but they were not statistically significant. Compared with BBtt, bbTT patients showed lower mean age at onset of nephrolithiasis (29.7+/-12.1 vs 38.1+/-12.7 years, P = 0.008) and higher values of FHS (2.45+/-1.9 vs 0.83+/-0.7, P = 0.006). Similar results were obtained for individual BsmI and TaqI alleles. The analysis of FokI alleles was not informative. CONCLUSIONS: Recurrent calcium oxalate stone formers with IHc and the bT VDR haplotype have more aggressive kidney stone diseases as indicated by a higher familial incidence and lower mean age at onset. This clinical severity is associated with the higher urinary supersaturation of calcium oxalate salts and abnormalities of renal citrate handling.     

Hypocitraturia as a pathogenic risk factor in the mixed (calcium oxalate/uric acid) renal stones.

A small group of patients with nephrolithiasis who forms mixed (calcium oxalate and uric acid) calculi presents particular problems in their clinical management. In 3,158 stones analyzed in our laboratory, we found 158 mixed calculi in 86 of the patients. In this work, the clinical and biochemical results obtained from 27 patients with mixed stones were compared with those from 27 control patients with calcium oxalate renal lithiasis. A significant difference was found in oxalate and citrate urinary elimination (mean +/- SD) in mixed stone formers versus pure calcium oxalate stone formers: oxaluria (mg/24 h: 38 +/- 15 vs. 28 +/- 12; p less than 0.01) and citraturia (mg/24 h: 214 +/- 139 vs. 437 +/- 303; p less than 0.01). Citraturia was decreased in a high proportion (77%) in mixed stone formers, and only a reduced percentage of them (23%) presented normal values, although in the low limit of normality. As treatment and prophylactic measure, we proposed oral administration of citrates in mixed stone patients because citrate inhibits spontaneous nucleation of calcium salts and crystal growth, and it also increases the urinary pH with a consequent increase in uric acid solubility.     

The influence of diet on urinary risk factors for stones in healthy subjects and idiopathic renal calcium stone formers

The daily intake of 103 recurrent idiopathic calcium stone formers and 146 controls was assessed by means of a computer-assisted 24-h dietary record. Timed 24-h urine samples were collected over the same period to assess the relationship between dietary intake of nutrients and urinary risk factors for calcium stones. After standardisation for sex, age and social status a total of 128 subjects underwent final statistical analysis; 64 renal stone formers and 64 controls. Significant increases in the consumption of animal and vegetable protein and purine were identified as the nutritional factors that distinguished renal stone formers from controls. As expected, the daily urinary excretion of calcium and oxalate was higher and the daily urinary excretion of citrate was lower in stone formers than in controls. No difference with respect to daily urinary uric acid excretion was recorded. Daily urinary excretion of calcium was correlated to dietary protein intake while daily urinary oxalate was correlated to dietary vitamin C intake. It was concluded that renal stone formers could be predisposed to stones because of their dietary patterns. A link between the protein content of the diet and urinary calcium was confirmed, but dietary animal protein had a minimal effect on oxalate excretion.     

Intestinal oxalate absorption is higher in idiopathic calcium oxalate stone formers than in healthy controls: measurements with the [(13)C2]oxalate absorption test

PURPOSE: We assessed the importance of oxalate hyperabsorption for idiopathic calcium oxalate urolithiasis, oxalate absorption in healthy volunteers and recurrent calcium oxalate stone formers was compared. MATERIALS AND METHODS: The [(13)C2]oxalate absorption test, a standardized, radioactivity-free test, was performed. On 2 days 24-hour urine was collected and an identical standard diet containing 800 mg Ca daily was maintained. On the morning of day 2 a capsule containing 0.37 mmol sodium [(13)C2]oxalate was ingested. A total of 120 healthy volunteers (60 women and 60 men) and 120 patients (30 women and 90 men) with idiopathic CaOx urolithiasis (60% or greater CaOx) were tested. RESULTS: Mean intestinal oxalate absorption in the volunteers was 8.0 +/- 4.4%, and in the patients was 10.2 +/- 5.2% (p <0.001). There was no significant difference in mean absorption values between men and women within both groups. A high overlap between the absorption values of volunteers and patients was found. Only in the patient group did absorption values greater than 20% occur. Oxalate absorption correlated with oxalate excretion in the patients, r = 0.529 (p <0.01) and in the volunteers, r = 0.307 (p <0.01). CONCLUSIONS: In high oxalate absorbers dietary oxalate has a significant role in oxalate excretion and, therefore, increases the risk of calcium oxalate stone formation.     

Physicochemical metabolic characteristics for calcium oxalate stone formation in patients with gouty diathesis

PURPOSE: We determined why calcium oxalate stones instead of uric acid stones form in some patients with gouty diathesis. MATERIALS AND METHODS: Gouty diathesis was diagnosed from absence of secondary causes of uric acid stones or low urinary pH, and reduced fractional excretion of urate with discriminant score of the relationship between urinary pH and fractional excretion of urate less than 80. From the stone registry 163 patients with gouty diathesis were identified, including 62 with uric acid stones (GD + UA) and 101 patients with calcium oxalate stones (GD + Ca). Metabolic data and 24-hour urinary chemistry study were compared between the 2 groups. RESULTS: Compared with GD + UA, GD + Ca had significantly greater urinary calcium (196 +/- 96 mg per day vs 162 +/- 82 mg per day, p <0.05) and significantly lower urinary citrate (430 +/- 228 vs 519 +/- 288 mg per day, p <0.05), resulting in higher urinary saturation of calcium oxalate. Both groups had low urinary pH (less than 5.5) and high urinary undissociated uric acid (greater than 100 mg/dl). Urinary calcium post-oral calcium load was significantly higher in GD + Ca than in GD + UA (0.227 vs 0.168 mg/dl glomerular filtrate, p <0.001). CONCLUSIONS: Calcium oxalate stones may form in some patients with gouty diathesis due to increased urinary excretion of calcium and reduced excretion of citrate. Relative hypercalciuria in GD + Ca may be due to intestinal hyperabsorption of calcium.     

Frequency of renal phosphate leak among patients with calcium nephrolithiasis.

BACKGROUND: Nephrolithiasis is a frequent disorder affecting 10 to 15% of the population in Europe and the United States. More than 80% of renal stones are made of calcium oxalate and calcium phosphate. The main identified risks for calcium renal stone formation are hypercalciuria and urinary saturation. A urine phosphate (Pi) loss is often associated with hypercalciuria; furthermore, hyperphosphaturia increases urinary saturation. METHODS: To determine whether urinary phosphate loss is associated with calcium urolithiasis, we measured renal Pi threshold (TmPi) in 207 stone formers with normal parathyroid hormone (PTH) serum concentration and in 105 control subjects. RESULTS: The TmPi followed a normal distribution in both groups. The mean TmPi was significantly lower in stone formers versus controls (0.72 +/- 0.13 vs. 0.87 +/- 0.18 mmol/L, P < 0.0001) because of a shift to the left of the TmPi distribution curve in the stone former population, with no evidence for bimodal distribution. Five percent of the controls had a TmPi <0.63 versus 19% of the stone formers. Daily urinary calcium excretion was significantly higher in stone formers than in controls. Calcium excretion was also significantly higher in stone formers with TmPi <0.63 mmol/L compared with those with TmPi > or =0.63. Serum PTH and ionized calcium concentrations were not different in stone formers and in control subjects, whatever the TmPi value. CONCLUSIONS:: A low TmPi is more frequently encountered in stone formers with a normal PTH concentration than in control subjects and is associated with a high urinary Ca excretion. The hypophosphatemia induced by a renal phosphate leak may predispose the subject to calcium stone formation by increasing the serum calcitriol level, calcium excretion, and urinary saturation.     

13C2]oxalate absorption in children with idiopathic calcium oxalate urolithiasis or primary hyperoxaluria

Intestinal oxalate absorption is an important part of oxalate metabolism influencing its urinary excretion and its measurement can be a valuable diagnostic tool in hyperoxaluric disorders. In this study, we use [(13)C(2)]oxalate absorption under standardized dietary conditions to assess intestinal oxalate absorption and its impact on urinary oxalate excretion. Tests were conducted in age-matched pediatric patients that included 60 with idiopathic calcium oxalate urolithiasis, 13 with primary hyperoxaluria, and 35 healthy children. In the idiopathic stone formers, median oxalate absorption was significantly higher than that in the controls or in patients with primary disease. From standardized values obtained in control patients, oxalate hyperabsorption was detected in 23 patients with idiopathic disease but not in any patients with primary hyperoxaluria; therefore, a significant correlation between intestinal absorption and urinary excretion was found only in those with the idiopathic disease. We have shown that increased intestinal oxalate absorption is an important risk factor of idiopathic calcium oxalate urolithiasis. In contrast, low intestinal oxalate absorption in patients with primary hyperoxaluria indicates that only foods with excessive oxalate content be restricted from their diet.     

Hyperoxaluria in idiopathic calcium nephrolithiasis--what are the limits?

OBJECTIVE: The object of this study was to investigate the role for measurement of 24-h renal oxalate excretion in the evaluation of idiopathic calcium stone formers. MATERIALS AND METHODS: Renal excretion rates of oxalate and creatinine were measured in 24-h urines in 46 consecutive male recurrent idiopathic calcium stone formers and 61 healthy males. Furthermore, day-to-day variation in renal oxalate excretion in 10 male recurrent stone formers and 10 healthy males were evaluated by measuring 24-h oxalate excretion on 5 different days in each individual. Concentrations of oxalate in urine were measured using an enzymatic method without ascorbate interference. RESULTS: The cumulative frequency distribution curves of 24-h renal oxalate excretion rates of stone formers and controls were congruent, and there were no statistically significant differences in oxalate excretion rates between stone formers and controls. Mean 24-h oxalate excretion (95%-confidence intervals) was 0.22 (0.18-0.25) mmol and 0.21 (0.18-0.24) mmol in stone formers and controls, respectively (p = 0.9). The day-to-day variation study did not reveal any differences in renal oxalate excretion pattern between stone formers and controls, and the presence of intermittent hyperoxaluria could not be confirmed. The oxalate excretion rates were generally low. CONCLUSION: In our region, there appear to be no differences in 24-h renal excretion rates of oxalate between male recurrent idiopathic calcium stone formers and healthy males, and the syndrome of mild hyperoxaluric calcium nephrolithiasis could not be identified in our population of idiopathic stone formers. Hence, a limit of abnormal oxalate excretion that distinguishes an idiopathic stone former from a non-stone former could not be defined in our population. Therefore, the value of routine measurement of urinary oxalate in idiopathic urolithiasis is difficult to accept, and cannot be recommended.     

A study of the etiology of idiopathic calcium urolithiasis in children: hypocitruria is the most important risk factor

PURPOSE: To determine the association of metabolic risk factors with pediatric calcium urolithiasis we compared metabolic evaluation data on children with idiopathic calcium stones and those on healthy children. MATERIALS AND METHODS: Metabolic evaluation was done in 78 calcium stone formers 1 to 15 years old (mean age 7.2) who were free of urinary tract infection, anatomical abnormalities, and metabolic, endocrinological and intestinal disorders, and in 24 healthy children. Evaluation included serum biochemistry, and measurement of daily excretion of urinary calcium, oxalate, urate, phosphorus, citrate and magnesium. RESULTS: Demographic characteristics, serum parameters, and daily excretion of calcium, urate, phosphorus and magnesium did not differ statistically in the 2 groups. However, urinary oxalate was significantly higher and urinary citrate was significantly lower in stone formers than in controls (p = 0.002 and 0.028, respectively). Hypocitruria and hyperoxaluria were 4.3 and 3-fold more common in stone formers than in controls, respectively. Multivariate analysis using logistic regression showed that hypocitruria was the only significant risk factor for idiopathic calcium stones (p = 0.008). CONCLUSIONS: Hypocitruria was the most important risk factor in our patients. Hyperoxaluria was also common and accompanied hypocitruria in many stone formers. In contrast to many previous reports, we failed to show that hypercalciuria is an important metabolic defect for idiopathic calcium stones, possibly because our study evaluated a different population.     

Low urine citrate excretion as main risk factor for recurrent calcium oxalate nephrolithiasis in males.

To better define the relative role of metabolic factors in the recurrence of stone formation, we studied the 24-hour urinary excretion of calcium (uCa), citrate (uCit), oxalic acid (uOx) and uric acid (uUa) in 73 male patients with primary calcium oxalate urolithiasis. According to the episodes of stone formation per year, we identified 51 recurrent stone formers (RSF) and 22 single stone formers (SSF). 20 normal adult males constituted the control group (C). uCa and uOx were higher in RSF than in C, but quite similar in SSF and RSF. The only difference between RSF and SSF was uCit, significantly lower (2.06 +/- 1.04 mmol/24 h) in RSF than in SSF (3.22 +/- 1.18 mmol/24 h, p less than 0.001) and in C (3.42 +/- 1.33 mmol/24 h, p less than 0.001). Hypocitraturia (uCit less than 1.5 mmol/24 h) was found in 16 of 51 RSF (31.4%) and in 1 of 22 SSF (4.5%). These data confirm that high levels of uCa and uOx represent a risk factor for lithogenesis, but also strongly indicate the low uCit excretion as the most important urinary abnormality accounting for the recurrence of calcium oxalate stones.     

Comparative study of 24-hour urinary excretion of glycosaminoglycans by renal stone formers and healthy adults

In order to find out the possible aetiological factors for urolithiasis in North-Western India, an endemic region for urinary calculi, we studied the 24-hour urinary excretion of glycosaminoglycans (GAGs), inhibitors of calcium oxalate crystallisation and/or crystal aggregation, in 58 healthy adults and in 100 stone formers. GAGs were colorimetrically estimated in urine in terms of glucuronic acid content after precipitation of GAGs by cetyl pyridinium chloride. The 24-hour urinary excretion of GAGs was significantly less in stone formers as compared to healthy adults (15.32 +/- 6.94 vs. 22.44 +/- 5.54 mumol/day; p less than 0.001). There was no significant difference in the 24-hour urinary excretion of GAGs between male and female stone formers, or between male and female healthy adults. There was no correlation between age and 24-hour urinary excretion of GAGs in any of the groups. In conclusion, 24-hour urinary excretion of GAGs is significantly less both in male and in female stone formers. The 24-hour urinary excretion of GAGs is not related to age or sex in both healthy adults as well as in stone formers.     

Clinical studies on the recurrence of urolithiasis: (1). Influence of diet on urinary excretion of the stone forming constituents

Twenty-four hour urinary excretion of the stone forming constituents, calcium, oxalate, uric acid, phosphate and magnesium were assayed either under the restricted diet (190 stone formers and 52 non-stone formers) or under the ambulatory free diet (93 stone formers and 14 non-stone formers). Under the ambulatory free diet, urinary excretion of calcium, uric acid and magnesium in the male stone formers, and urinary excretion of calcium and magnesium in the female stone formers was significantly higher than that under the restricted diet. Under the restricted diet, no difference in urinary excretion of calcium, oxalate, uric acid or phosphate was noted between the stone formers and non-stone formers. However, urinary magnesium excretion of the stone formers under the restricted diet was significantly lower than that of the non-stone formers. Under the free diet, no difference in urinary excretion of calcium, oxalate, uric acid, phosphate or magnesium was observed between the stone formers and non-stone formers. Also, there was no significant difference in urinary excretion of calcium, oxalate, uric acid, phosphate or magnesium between the unilateral urolithiasis patients without previous stone history and that of the bilateral or recurrent stone formers. We conclude that urinary excretion of calcium, oxalate, uric acid, phosphate and magnesium have no major role in the stone producing mechanism. However, reduction of urinary excretion of calcium, oxalate, uric acid and phosphate and augmentation of urinary excretion of magnesium are mandatory in preventing stone recurrence until a better understanding of the cause of urolithiasis is obtained.     

Value of routine citrate analysis and calcium/citrate ratio in calcium urolithiasis

24-hour urinary citrate excretion was measured in 176 calcium oxalate stone formers and 100 normal controls. A statistically significant difference (p less than 0.03) could be found between the two groups. When stone formers were divided into a group of 69 patients with recurrent calcium urolithiasis (RCU) and a group of 106 patients with a single stone episode, the latter did not differ from the control group, while in RCU a significantly lower citrate excretion compared with controls (p less than 0.005) could be found. Thus, patients with RCU could benefit from alkali citrate prophylaxis. A female-male difference in citrate excretion could not be found in either the control group or stone formers. Recurrent stone formers presented a significantly higher calcium/citrate ratio compared with controls, which would indicate an increased risk for stone formation. The value of routine citrate analysis is limited, however, by the great, variability of citrate levels in stone formers and controls.     

Influence of the calcium content of the diet on the incidence of mild hyperoxaluria in idiopathic renal stone formers

Urinary oxalate excretion was measured in 101 male idiopathic calcium (Ca) stone formers studied on 3 dietary conditions (free-choice, Ca-enriched, and low-Ca diet). The population consisted of 38 normocalciuric and 63 hypercalciuric patients. Mean oxalate excretion was similar in normocalciuric and in hypercalciuric patients, on free-choice as well as on Ca-enriched diet. In both conditions the incidence of hyperoxaluria (greater than or equal to 435 mumol/24 h) within each group of stone formers was also similar, ranging from 11 to 22%. On low-Ca diet, however, mean oxalate excretion increased significantly (p less than 0.01) in hypercalciurics but not in normocalciurics; on this diet, the incidence of hyperoxaluria was particularly high in the hypercalciurics (33%), compared with the normocalciurics (13%). On low-Ca diet, oxalate excretion was positively correlated with the estimated degree of intestinal absorption of calcium (p = 0.01). These results show that among idiopathic stone formers, mild hyperoxaluria is not a rare finding and that this disorder can be encountered in each group of patients; its incidence, however, is influenced by the calcium content of the diet. On a low-Ca diet, patients with intestinal Ca hyperabsorption are particularly prone to develop hyperoxaluria, an observation which leads to question the relevance of such a dietary advice unless oxalate intake is simultaneously reduced.