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The incidence of urolithiasis in children has increased in recent years (1). The risk factors for urolithiasis commonly observed in children are low urine volume, increased urine calcium excretion, and low normal or decreased urinary citrate level (2). Citrate inhibits the spontaneous nucleation of calcium oxalate, crystal growth of calcium oxalate and calcium phosphate, and the heterogeneous nucleation of calcium oxalate by monosodium urate (38). Bisaz et al. (9) reported that citrate is responsible for 50% of the inhibitory activity against calcium phosphate precipitation in normal urine. The inhibitory effect of citrate on calcium oxalate crystal growth and aggregation is also linked to a direct effect on the crystal surface (3,10). Consequently, and because of lack of significant adverse effects, citrate preparations are widely used in subjects with calcium oxalate nephrolithiasis (2,1113).

In adult studies, Welshman and McGeown (14), Hobarth and Hofbauer (15) and Nikkila et al. (16) observed that urine calcium/citrate ratio was able to discriminate between stone formers and control population; the latter exhibiting a significantly lower calcium/citrate ratio. However, it was the impression in the above studies that the clinical use of urine calcium/citrate ratio was limited because of its wide range of variability and the influence of age and gender on urinary excretion of citrate. There is limited data on urine calcium/citrate ratio in either healthy, hypercalciuric, or stone forming children (17,18). Treatment of stone formers with citrate raises the theoretical concern of increased formation of calcium phosphate crystals in alkaline urine. Currently, no good tools are available to monitor (or target) potassium citrate therapy in children. Furthermore, it is yet unclear why many other symptomatic hypercalciuric children presenting with dysuria-frequency, abdominal/back pain, and microscopic hematuria do not develop kidney stones. Therefore, the objectives of the study were to investigate whether urinary calcium/citrate ratio will be helpful in discriminating between healthy children, hypercalciuric nonstone formers, and hypercalciuric stone formers, and consequently whether it can be used as a tool to target therapy in children with calcium stones. In the textbook of Pediatric Nephrology 5th ed. Milliner (19) indicates the unclarity of normative data of urine citrate by quoting both values of 180 and 400 mg/g. We also thought to use this opportunity to establish normative data of urine citrate/creatinine ratio.

MATERIALS AND METHODS

Random nonfasting urine samples from children between the ages of 5 and 18 y on regular diet were obtained at their initial presentation. They were measured for calcium, citrate, and creatinine in three groups of children: i) healthy control (group C), ii) nonstone forming children with hypercalciuria (group H), and iii) hypercalciuric stone forming children (group SH). The inclusion criteria for group C were children who presented to our clinic with monosymptomatic primary nocturnal enuresis and had a normal physical examination and urinalysis. Group H were children who presented to our clinic with hypercalciuria associated with either voiding symptoms (frequency-dysuria syndrome) or microscopic hematuria, and without clinical symptoms attributable to urolithiasis. Hypercalciuria was defined as urine calcium/creatinine ratio (UCa/Cr) >0.2 mg/mg (20,21). Imaging studies in group H were done at the discretion of the attending physician. Group SH included hypercalciuric children with urolithiasis confirmed by an imaging study (x-ray, CT, or ultrasound) and/or stone analysis. Children with uric acid, cystine, or struvite stones were excluded from the study. Children with primary or secondary hyperoxaluria or hypocitraturia were not included in the study so as to exclude the independent effect of hyperoxaluria or hypocitraturia on hypercalciuric stone formers. Similarly, we excluded all those with anatomical or functional abnormalities of the kidney and urinary tract, and gastrointestinal tract.

In each participant, we recorded the ethnicity, gender, age, results of the imaging studies, and/or stone analysis when applicable. At the initial clinic visit, urine creatinine (UCr), citrate (UCit), and calcium (UCa) were measured on the Roche Cobas Mira Classic by kinetic Jaffe, enzymatic (citrate lyase), and cresolphthalein complexone methods, respectively. The UCa/Cr and urine calcium/citrate ratio (UCa/Cit) ratio were expressed as mg/mg, and urine citrate/creatinine ratio (UCit/Cr) as mg/g. Once the raw data were available, the normal percentile distribution of UCit/Cr in group C was calculated. Subsequently, children with documented hypocitraturia (UCit/Cr <180 mg/g) were excluded from further analysis to ensure that the analysis includes only children with isolated hypercalciuria.

As children in all groups were predominantly (>95%) White, we did not analyze the effect of ethnicity. To evaluate the possible impact of age and gender, the data were analyzed twice; with and without adjustment for age and gender. For statistical analysis, analysis of covariance with Bonferroni correction was used to compare multiple groups. In addition, we compared the predictive power of urinary ratios for identifying stone risk using receiver operating characteristic curves (ROC) and multilevel likelihood ratios. The data were analyzed using SPSS version 15.0 statistical software. A p value <0.05 was regarded as statistically significant. The study was approved as an exempt study by the Institutional Review Board of Children's Mercy Hospital of Kansas City (No 05 10-138E) and thus the need to obtain informed consent was waived.

RESULTS

There were 158 children in group C, 78 in group H, and 37 in group SH. Figure 1 depicts the normal percentile distribution of UCit/Cr in group C, establishing the 5th percentile at 176 mg/g. Nine children in group C (4.4%) and three in group SH (8.1%) who met the literature criterion of hypocitraturia (UCit/Cr <180 mg/g), compatible with the 5th percentile of our normal population, were deleted from further analysis (22). Thus, leaving 149 children in group C (89 boys/60 girls, 10.02 ± 2.82 y), 78 children in group H (26 boys/52 girls, 7.83 ± 2.25 y, p = <0.001 compared with C) and 34 children in group SH (15 boys/19 girls, 10.66 ± 3.22 y, p = 0.65 compared with C and p = <0.001 compared with H). In group H, 35 children (45%) had imaging studies that confirmed the absence of urolithiasis. In group SH stone analysis was available in 20 of 34 children who were composed of either pure calcium oxalate dihydrate (7/20), calcium oxalate monohydrate (1/20) or calcium phosphate (1/20), or a mixture (11/20) of these calcium salts.

Figure 1
figure 1

The Gaussian distribution of urine citrate/creatinine from random urine specimen in 158 healthy school-age children with monosymptomatic nocturnal enuresis. The 5th percentile is at 176, 25th percentile at 419, 50th percentile at 638, 75th percentile at 880, and 95th percentile at 1311 mg/g.

Comparison of urine biochemistry among controls (C), hypercalciuric without stone (H), and hypercalciuric with stone (SH).

Table 1 shows the comparison of UCa/Cr, UCit/Cr, and UCa/Cit among the three groups. As shown in Table 1 and Figure 2, and by definition, UCa/Cr was significantly lower in group C compared with groups H and SH, with no difference between the latter two. The UCit/Cr value was significantly higher in group H, compared with C and SH; which had no difference between themselves. The UCa/Cit ratio increased significantly from group C to group H to group SH. Gender had no effect on these ratios but Pearson's correlation found UCa/Cr to decrease with age (r = −0.21, p = 0.001), UCit/Cr to decrease with age as well (r = −0.32, p < 0.001), and UCa/Cit to be unaffected by age (r = 0.06, p = 0.35). As shown in panel II, data analysis after adjustment for both age and gender, showed the same significant differences among the three groups.

Table 1 UCa/Cr, UCit/Cr, and UCa/Cit in group C, group H, and group SH
Figure 2
figure 2

Box plot distribution of (A) urine calcium/creatinine, (B) citrate/creatinine and (C) calcium/citrate ratios in groups C (controls), H (hypercalciuric without stone), and SH (hypercalciuric stone formers).

Figure 3 shows the distribution of UCit/Cr against UCa/Cr as an ellipse in children from all three groups. It shows that for every degree of hypercalciuria nonstone formers had higher urinary citrate excretion compared with stone formers.

Figure 3
figure 3

Distribution of urine citrate/creatinine against calcium/creatinine ratio in groups C (control children represented by 224 and surrounded by — ellipse), H (hypercalciuric without stone represented by * and surrounded by … ellipse), and SH (hypercalciuric stone formers represented by ♦ and surrounded by - - - ellipse).

Receiver operating characteristic curves.

To establish potential “cut-off” values to discriminate between groups, ROC were constructed for UCa/Cr, UCit/Cr, and UCa/Cit ratios (Fig. 4). Assessing the stone risk between groups C and SH, the area under ROC (AUC) was 0.939, 0.399, and 0.933 for UCa/Cr, UCit/cr, and UCa/Cit, respectively. Between groups H and SH, AUC was 0.484, 0.747, and 0.733 for UCa/Cr, UCit/cr, and UCa/Cit, respectively, to assess the stone risk in hypercalciuric children. Between groups C and H, the AUC was 0.945, 0.660, and 0.858 for UCa/Cr, UCit/cr, and UCa/Cit, respectively, for the development of symptoms related to hypercalciuria. Thus, UCa/Cit ratio showed a good discriminatory potential to differentiate across all the three groups. Based on the above analysis, combined with multilevel likelihood analyses, a UCa/Cit value of 0.326 was found to be a good cut-off point that produced equal sensitivity and specificity in differentiating between group C and group SH (Table 2, Fig. 4). A UCa/Cit value of 0.199 was a good cut-off point between groups C and H (Table 2, Fig. 4), and a value of 0.336 between groups H and SH (Table 2, ROC data not shown).

Figure 4
figure 4

The figure shows the ROC for urine calcium/citrate ratio between groups C and H (A) and groups C and SH (C). A urine calcium/citrate ratio of 0.199 gave the best discriminatory ratio between groups C and H and 0.326 between groups C and SH. (B) Box plot distribution of urine calcium/citrate ratio in groups C, H, and SH, with the lower broken line at 0.199 and the upper broken line at 0.326 mg/g.

Table 2 Multilevel likelihood ratios with sensitivities and specificities at different urine calcium/citrate(UCa/Cit) ratios for risk of development of stone (groups C vs. SH and groups H vs. SH), and development of symptomatic hypercalciuria without stone formation (groups C vs. H)

DISCUSSION

The normal urinary citrate excretion in children has been reported to range from >180 to >408 mg/g based on citrate lyase assay (1,22). Indeed, in the textbook of Pediatric Nephrology 5th ed. Milliner (19) indicates the unclarity of normative data of urine citrate by quoting both values of 180 and 400 mg/g. In this study, urinary citrate excretion of 180 and 408 mg/g equal approximately the 5th and 25th percentiles, respectively, in our healthy controls (Fig. 1). Assuming that nowadays, the methodology to analyze urine citrate is standardized, it is unacceptable to have such different values. Our laboratory uses the citrate lyase assay, as do other major reference laboratories. When compared with Mayo Clinic methodology, which regards hypocitraturia as <180 mg/g creatinine, our laboratory shows excellent mean bias, slope, intercept, and R2 values of 0.7, 0.998, 0.801, and 0.996, respectively (data not shown). In the past, Miller and Stapleton (22) found the threshold of 2SD below the mean for urine citrate/creatinine in children to be 182 mg/g. These values are consistent with our finding of the 5th percentile in controls of 176 mg/g (Fig. 1). Because of the fact that we found a weak inverse correlation between UCit/Cr and age, we further analyzed the data dividing controls into two groups based on median age of 9.75; the 5th percentile of UCit/Cr in those younger than 9.75 was 178.6 mg/g while in the older subjects it was 145.8 mg/g indicating that in pediatric age groups UCit/Cr >180 mg/g can be regarded as normal. Indeed, Norman et al. (23) found urine citrate/creatinine to be <75 mg/g in nine children with complete and incomplete distal renal tubular acidosis. On the other hand, using the reference value of 400 mg/g as was recently done by VanDervoort et al. (1) would have rendered 25% of our control population and 44.3% of our stone formers as hypocitraturic. Their study, however, which not surprisingly defined 52% of their pediatric stone formers to be hypocitraturic, did not use a control group to support the high cut-off value (1). It is important to note that our data were based on random urine sample. However, as aforementioned the value of 180 mg/g is also used for 24-h urine collection at the Mayo Clinic. Furthermore, we have shown in the past a correlation coefficient value of 0.96 between our random mid-day urine chemistries and 24-h collection (24). Thus, combining the findings in our study, previous studies and reference values used in other laboratories, and for the maintenance of consistency we recommend using urine citrate/creatinine ratio of 180 mg/g as the lower limit of normal in school-age children.

Parks and Coe (25) found that compared with normal people, adults with urolithiasis had a high level of urine calcium for any given level of urine citrate, and no other urinary constituent could improve on this relationship. Thus, it may not be the absolute urinary calcium or citrate concentrations that determine the risk of stone formation but rather the relative excess of calcium over citrate. Similarly, Cupisti et al. (26) found that stone formers had higher urinary calcium excretion and low citrate excretion, which was more marked in recurrent stone formers. As early as 1976, Welshman and McGeown (14) had found urinary calcium/citrate ratio to be different in normal adult subjects and stone formers but found a difference between the two genders. Subsequently, Nikkila et al. (16) documented urinary citrate/calcium excretion to be significantly higher in stone-formers (0.25 ± 0.03 mmol/mmol) than in control subjects (1.25 ± 0.31 mmol/mmol). This remained true for both genders separately but the absolute values were lower in females. In the study by Hobarth and Hofbauer (15), urinary calcium/citrate (mmol/mmol) ratio increased from 1.7 ± 0.45 in normal adults to 3.1 ± 0.49 in single stone formers and to 5.3 ± 1.1 in recurrent stone formers, and in contrast to the above two studies no gender difference was observed.

Therefore, because of the inconsistencies in the adult studies regarding the effects of age and gender on urinary excretion of citrate it was felt that the clinical use of urine calcium/citrate ratio is of limited value (27). In contrast, in our study UCa/Cit ratio was not influenced by either age or gender in children when analyzed with and without adjustment for these factors (Table 1). Gender by itself had no influence on either urinary calcium/creatinine, citrate/creatinine, or calcium/citrate ratios as was found in other pediatric studies (17,21,28). Indeed, in contrast to the adult population, the absence of preponderance of urolithiasis in boys in our study and others indirectly further supports the lack of gender influence in the pediatric population (29,30). Similar to previous studies, we found age to have an effect on UCa/Cr and UCit/Cr; however, because both were in the same direction, namely decreasing as age advanced, they ended up having no effect on UCa/Cit ratio (20,21,31,32). In summary, we found that UCa/Cit ratio could discriminate between normal children and stone formers, and in contrast to adults was not affected by either age or gender, which simplifies its use as a clinical parameter in children. These results are consistent with the recent findings by DeFoor et al. (18) that urine calcium/citrate ratio in children is the best parameter to assess the risk for recurrent calcium stone formation.

As often happens in clinical practice, not all stones were captured, hence no stone analysis was available in 14 of the 34 stone forming children (33). However, when the group of 20 children with known stone composition was compared with control children, the findings were the same as for the whole stone group (data not shown). Indeed, calcium stone has become the most common form of stone in developed countries (33,34). The likelihood of the remaining 14 hypercalciuric stone-forming children as not to have a calcium-based stone is low as we had included only children with hypercalciuria with radiologically documented stone and had excluded children with cystine, uric acid, and struvite stones, and those with hyperoxaluria or hypocitraturia, and children with history of UTI, or anatomic and functional abnormalities in the urinary and gastro intestinal tracts. Thus, we believe that it was acceptable to use all 34 children in the stone group under the pathophysiologic umbrella of hypercalciuric stone formers.

The hypercalciuric nonstone formers presented with either voiding symptoms or microscopic hematuria but did not have symptoms attributable to urolithiasis. Imaging studies confirming the absence of stone were available in only 45% of them. We believe that the possibility of having a stone in some of the other 55% is low due to the observation that the incidence of stone formation in hypercalciuric children is low (5%) in the absence of gross hematuria, severe lower abdominal, or flank pain (35). There was no difference in hypercalciuric nonstone formers for gender, age, UCa/Cr and UCit/Cr between children who had the imaging study vs. no imaging study (data not shown).

As expected, compared with normal, hypercalciuric children had higher urinary UCa/Cr ratio but quite interestingly there was no difference in UCa/Cr between hypercalciuric stone formers and nonstone formers (Table 1, Fig. 2). On the other hand, mean UCit/Cr in group H was 34% higher than in hypercalciuric stone formers (Table 1). Consequently, compared with controls UCa/Cit ratio was 2.5 times higher in the hypercalciuric children without stones and 4 times higher in the stone formers (Table 1, Fig. 2). Furthermore, as shown in Fig. 3, compared with hypercalciuric stone formers urine citrate excretion in hypercalciuric children without stone was much higher at any given value of calcium excretion. Thus, our data suggest that a high urinary citrate excretion in hypercalciuric children has a protective role against stone formation. Citrate in urine is well known to have an inhibitory role in calcium stone formation, and citrate preparations are currently used routinely in the treatment of patients with calcium stones (9,27,36). This finding may have an importance in both estimating the risk of the hypercalciuric child to develop stones, and possibly as a guideline for treatment (vide infra). An important question is whether the relative hypocitraturia in stone formers, compared with nonstone formers, was the cause or the effect of hypercalciuria. Multiple studies showed acidification defect in hypercalciuric stone formers, which in some may result in hypocitraturia (3739). Bonilla-Felix et al. (37) found that among hypercalciuric children only those with stones had an acidification defect. However, not all stone formers had an acidification defect and no correlation was found between the latter and urine citrate. In adult studies, Wikström et al. (38) found 22% of 389 stone formers to have an acidification defect; however, in the majority of them another etiology rather than primary hypercalciuria was observed. In another study based on ammonium chloride loading test, Osther et al. (39) found an acidification defect in only 12.7% of stone formers, the majority of whom had bilateral stone disease. Nevertheless, as stated by the latter group “regardless of whether the acidification defect is primary or secondary to stone formation, all renal stone formers with an acidification defect can benefit from prophylactic alkali therapy” (39). We also agree that even if the diagnostic value of UCa/Cit is questioned, it can still serve as a therapeutic yardstick.

The beneficial effect of treatment with potassium citrate in decreasing recurrence of new stones, growth of residual stone fragments after lithotripsy and in stone-forming children with hypocitraturia is well established (4044). In a preliminary study in nine healthy children, treatment with potassium citrate at 0.5 or 1 mEq K/kg/d resulted in an increase in urinary citrate excretion, but the higher dose also caused a significant increase in urine pH (Auron A et al. Effects of low vs. high dose potassium citrate on urine chemistry and acid-base status. 40th Annual Renal Meeting of American Society of Nephrology, November 2–5, 2007 in San Francisco, SU-FC026). Indeed, there is a concern that the increase in urine pH observed with citrate therapy may promote urinary supersaturation and activity product of calcium phosphate, thus defeating the purpose of treatment (45). Although as aforementioned potassium citrate is being used effectively in the prevention of urolithiasis, there is no data on how to titrate its dose (46). Our ROC data and multilevel likelihood table (Fig. 4, Table 2) show that a UCa/Cit ratio of 0.326 gives a good discrimination point between normal and stone formers and a UCa/Cit ratio of 0.199 between hypercalciuric children and control children. Thus UCa/Cit ratio of <0.326 could be a target goal for hypercalciuric stone formers receiving potassium citrate or other therapy. Providing support for this cut-off value is the very similar value of 0.336 differentiating hypercalciuric stone formers from nonstone formers (Table 2). However, as shown in Table 2, in reality there is a continuum effect that suggests that the lower the UCa/Cit value the lower is the stone risk. Another conclusion from the above data are that it might not be needed to fully correct hypercalciuria in stone formers if one can maintain satisfactory urine citrate concentration, thus keeping the ratio of UCa/Cit low enough to protect from stone formation. As our proposed UCa/Cit cut-off values are based on retrospective data, there will be a need to validate them in prospective studies, taking into consideration also urine pH, which was not available for analysis in this study.

In summary, this study provides the normal urine citrate/creatinine percentile distribution in children 5–18 y old, and the establishment of the 5th percentile at 180 mg/g. We found urinary citrate to be important in protecting hypercalciuric children form stone formation, and UCa/Cit ratio to be helpful in discriminating between healthy and stone forming children. Given its advantage of not being influenced by gender, age, or muscle mass (due to absence of creatinine in the equation) UCa/Cit has the potential to be used as a clinical tool to assess the risk of urolithiasis in children and as a therapeutic target. The latter may provide a better guidance for potassium citrate therapy, where unnecessarily high doses that might lead to alkaline urine should be avoided. Further prospective studies in children with urolithiasis using the recommended cut-off values will be required to confirm our findings.