The urinary excretion of oxalic acid and magnesium in oxalate urolithiasis.
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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.
PURPOSE: Oxalate bioavailability is an important determinant of whether the consumption of a particular food is a high risk in individuals predisposed to kidney stones. We estimated and compared oxalate absorption from a high oxalate containing legume (black beans) and a high oxalate containing nut (almonds). We also compared an isotope method using extrinsically labeled oxalate and an oxalate load method to assess oxalate absorption. MATERIALS AND METHODS: Six male and 5 female subjects participated in the 4 oxalate load tests, namely almonds, almonds with 20 mg C2-oxalic acid, black beans and black beans with 20 mg C2-oxalic acid. Each treatment provided a total of 120 mg oxalate, after which timed urine samples were collected for the analysis of oxalate, calcium and creatinine. RESULTS: Average oxalate absorption from the 2 almond treatments (5.9%) using the oxalate load method was significantly higher than that from the 2 black bean treatments (1.8%) during the 24-hour post-oxalate load collection period. In contrast, C2-oxalic acid absorption from the almond (7.9%) and black bean (8.6%) treatments did not significantly differ. CONCLUSIONS: The higher oxalate absorption from almonds than from black beans suggests that the relative amount of soluble and insoluble oxalate in food has an important role in the determination of oxalate absorption. Since extrinsically provided C2-oxalate and oxalate naturally occurring in the high oxalate test foods appeared to be differentially absorbed, the data do not support the use of extrinsically labeled oxalate to assess food oxalate absorption.
In the Gram-negative anaerobe, Oxalobacter formigenes, the generation of metabolic energy depends on the transport and decarboxylation of oxalate. We have now used assays of reconstitution to study the movements of oxalate and to characterize the exchange of oxalate with formate, its immediate metabolic derivative. Membranes of O. formigenes were solubilized with octyl-beta-D-glucopyranoside in the presence of 20% glycerol and Escherichia coli phospholipid, and detergent extracts were reconstituted by detergent dilution. [14C]Oxalate was taken up by proteoliposomes loaded with unlabeled oxalate, but not by similarly loaded liposomes or by proteoliposomes containing sulfate in place of oxalate. Oxalate transport did not depend on the presence of sodium or potassium, nor was it affected by valinomycin (1 microM), nigericin (1 microM), or a proton conductor, carbonylcyanide-p-trifluoromethoxyphenylhydrazone (5 microM) when potassium was at equal concentration on either side of the membrane. Such data suggest the presence of an overall neutral oxalate self-exchange, independent of common cations or anions. Kinetic analysis of the reaction in proteoliposomes gave a Michaelis constant (Kt) for oxalate transport of 0.24 mM and a maximal velocity (Vmax) of 99 mumol/min/mg of protein. A direct exchange of oxalate and formate was indicated by the observations that formate inhibited oxalate transport and that delayed addition of formate released [14C]oxalate accumulated during oxalate exchange. Moreover, [14C]formate was taken up by oxalate-loaded proteoliposomes (but not liposomes), and this heterologous reaction could be blocked by external oxalate. Further studies, using formate-loaded proteoliposomes, suggested that the heterologous exchange was electrogenic. Thus, for assays in which N-methylglucamine served as both internal and external cation, formate-loaded particles took up oxalate at a rate of 2.4 mumol/min/mg of protein. When external or internal N-methylglucamine was replaced by potassium in the presence of valinomycin, there was, respectively, a 7-fold stimulation or an 8-fold inhibition of oxalate accumulation, demonstrating that net negative charge moved in parallel with oxalate during the heterologous exchange. The work summarized here suggests the presence of an unusually rapid and electrogenic oxalate2-:formate1- antiport in membranes of O. formigenes. Since a proton is consumed during the intracellular decarboxylation that converts oxalate into formate plus CO2, antiport of oxalate and formate would play a central role in a biochemical cycle consisting of (a) oxalate influx, (b) oxalate decarboxylation, and (c) formate efflux.(ABSTRACT TRUNCATED AT 400 WORDS)
OBJECTIVE: To study urinary oxalate excretion in infants fed human milk versus formula, and to compare urinary calcium oxalate and calcium phosphate saturation in premature infants with term infants and adults. METHODOLOGY: We measured urinary oxalate-to-creatinine ratio and urinary oxalate concentration in 15 premature infants fed human milk compared to 16 formula-fed premature infants, and in eight human milk-fed term infants compared to 17 formula-fed term infants. We then studied urinary calcium oxalate and calcium phosphate saturations based on our observations of elevated urinary oxalate excretion in premature infants. Urinary calcium oxalate and calcium phosphate saturations were calculated from urinary concentrations of oxalate, calcium, sodium, potassium, chloride, uric acid, magnesium, phosphorus, and urinary pH. We calculated urinary calcium oxalate and calcium phosphate saturations in nine healthy adults and nine formula-fed term infants to establish control values for urinary saturation. Urinary calcium oxalate and calcium phosphate saturations were determined in nine premature infants receiving a glucose and electrolyte solution, 11 premature infants receiving parenteral nutrition, nine formula-fed premature infants, and 11 human milk-fed premature infants. RESULTS: Urinary oxalate excretion was higher in formula-fed compared to human milk-fed premature infants whether expressed as oxalate-to-creatinine ratio (0.32 +/- 0.04 versus 0.18 +/- 0.03, P < .01) or urinary oxalate concentration (0.047 +/- 0.007 versus 0.022 +/- 0.002 mg/mL, P < .01). Urinary oxalate excretion was higher in formula-fed term infants than in human milk-fed term infants whether expressed as oxalate-to-creatinine ratio (0.14 +/- 0.01 versus 0.07 +/- 0.01, P < .01) or urinary oxalate concentration (0.022 +/- 0.002 versus 0.012 +/- 0.002 mg/mL, P < .01). The urinary calcium oxalate saturation in healthy adults was 2.84 +/- 0.79; the value in formula-fed term infants was 2.12 +/- 0.31. The urinary calcium oxalate saturation was significantly higher in premature infants receiving formula (15.68 +/- 3.15), human milk (15.02 +/- 2.27), or parenteral nutrition (11.38 +/- 2.56) compared to adults or term infants (P < .01). Urinary calcium oxalate saturation in premature infants receiving a glucose and electrolyte solution (2.45 +/- 0.36) was not significantly different from that in adults or term infants. In contrast, urinary calcium phosphate saturation in premature infants as well as term infants and adults was less than 1; precipitation of calcium phosphate is not likely to occur under these conditions. CONCLUSION: Formula-fed infants have higher urinary oxalate excretion than human milk-fed infants. Premature infants receiving standard nutritional regimens may have urinary calcium oxalate saturation levels at which dissolved calcium oxalate may form nuclei of its solid phase.
Dietary oxalate is currently believed to make only a minor contribution (< 20%) to urinary oxalate excretion. A recent prospective study of stone disease suggested that dietary oxalate may be a significant risk factor. This observation led us to re-evaluate the contribution of dietary oxalate to urinary oxalate excretion. Previous studies have been hampered by inaccurate food composition tables for oxalate and inadequate methods for studying intestinal oxalate absorption. This evidence as well as factors that modify oxalate absorption are reviewed. New approaches to measure food oxalate and intestinal oxalate absorption have been examined. Capillary electrophoresis appears to be well suited for the analysis of the oxalate content of food. Two individuals consumed an oxalate-free formula diet for 7 days. This diet decreased urinary oxalate excretion by an average of 67% (18.6 mg per 24 hours) compared to oxalate excretion on self-selected diets. The absence of detectable oxalate in feces by day 6 of the diet suggested that the intestinal absorption was minimal. However, an effect of the formula diet on endogenous oxalate synthesis cannot be excluded. Restoring oxalate to the formula diet increased urinary oxalate excretion and illustrates that this experimental protocol may be well-suited for studying oxalate absorption and factors that modify it. Our results suggest that the intestinal absorption of dietary oxalate makes a substantial contribution to urinary oxalate excretion and that this absorption can be modified by decreasing oxalate intake or increasing the intakes of calcium, magnesium, and fiber.