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[患有结石形成疾病儿童的钠排泄]

[Sodium excretion in children with lithogenic disorders].

作者信息

Kovacević L, Kovacević S, Smoljanić Z, Peco-Antić A, Kostić N, Gajić M, Kovacević N, Jovanović O

机构信息

University Children's Hospital, Belgrade.

出版信息

Srp Arh Celok Lek. 1998 Sep-Oct;126(9-10):321-6.

PMID:9863402
Abstract

INTRODUCTION

The causes of nephrolithisis are multifactorial and have not yet been enough investigated [1]. Hypercalciuria is the most common cause of metabolic nephrolithiasis [2-4]. Close relationship between urinary calcium and urinary sodium has been a subject of reported observations in the past, showing that high urinary sodium is associated with high urinary calcium [5-7]. Hyperoxaluria, hyperuricosuria and cystinuria are also metabolic disorders that can lead to nephrolithiasis. Recent studies have indicated that urinary elimination of cystine is influenced by urinary sodium excretion. Based on these observations it has been hypothesised that patients with high urinary sodium excretion are at high risk of urinary stone disease. The purpose of the study was to investigate sodium excretion in a 24-hour urine and first morning urine collected from children with lithogenic metabolic abnormalities (hypercalciuria, hyperoxaluria, hyperuricosuria, cystinuria), both with nephrolithiasis and without it, in order to determine its significance in urinary calculi formation.

PATIENTS AND METHODS

Urinary sodium excretion was investigated in 2 groups of children: patients with lithogenic metabolic abnormalities, but without urinary stone disease (L group) and patients with nephrolithiasis (C group). Both groups were divided into 2 subgroups: patients with hypercalciuria and without it. There were 22 patients in group L (mean age 11.97 +/- 4.13 years), of whom 17 formed a hypercalciuric subgroup and 5 formed a non-hypercalciuric subgroup (3 patients with hyperuricosuria and 2 patients with hyperoxaluria). Group C consisted of 21 patients with nephrolithiasis (mean age 12.67 +/- 3.44 years), of whom 6 formed a hypercalciuric subgroup and 15 formed a non-hypercalciuric group (2 patients with cystinuria and 13 patients without lithogenic metabolic abnormalities). Control group consisted of 42 healthy age-matched children. All subjects had a normal renal function. A detailed history and clinical examination were done, and ultrasonography was performed in all patients. A 24-hour urine, first morning urine and serum specimen were analysed for sodium, potassium, calcium, uric acid, urea and creatinine. Fractional excretion of sodium, as well as urinary sodium to creatinin ratio and urinary sodium to potassium ratio, were calculated from the findings. Sodium and potassium levels were determined by flame photometry, calcium was measured by atomic absorption technique (Beckman Atomic Spectrophotometer, Synchron CX-5 model, USA), uric acid by carbonate method and creatinine by Jaffe technique. Cystine and dibasic amino acids were quantified by ion chromatography. Urinary oxalate excretion was determined by enzyme spectrophotometry. Hypercalciuria was defined by 24-hour calcium excretion greater than 3.5 mg/kg per day and/or calcium to creatinine ratio greater than 0.20 [8]. Uric acid excretion was expressed as uric acid excretion factored for glomerular filtration, according to Stapleton's and Nash's formula [9]. Normal values were lower than 0.57 mg/dl of glomerular filtration rate in 24-hour samples. Mean values were statistically analyzed by Pearson's linear correlation and analysis of variance (ANOVA).

RESULTS

Urinary sodium concentration values including urinary sodium to potassium ratios, are shown in Table 1. We found that urinary sodium excretion was significantly increased in patients of both L and C groups when compared with controls (p < 0.05). Further analysis of the subgroups showed that urinary sodium excretion was significantly higher only in patients with hypercalciuria of both L and C groups in comparison to controls (p < 0.05) (Table 2). A significant positive correlation was found between 24-hour urinary sodium to creatinine ratio and urinary calcium to creatinine ratio (r = 0.31; p < 0.001) (Graph 1), as well as between urinary sodium to potassium ratio in 24-hour and first morning urine (r = 0.69; p < 0.001) (Graph 2). (A

摘要

引言

肾结石的病因是多因素的,尚未得到充分研究[1]。高钙尿症是代谢性肾结石最常见的病因[2-4]。尿钙与尿钠之间的密切关系过去已有相关观察报道,表明高尿钠与高尿钙有关[5-7]。高草酸尿症、高尿酸尿症和胱氨酸尿症也是可导致肾结石的代谢紊乱疾病。最近的研究表明,胱氨酸的尿排泄受尿钠排泄的影响。基于这些观察结果,有人提出尿钠排泄高的患者患尿路结石病的风险较高。本研究的目的是调查从患有致石性代谢异常(高钙尿症、高草酸尿症、高尿酸尿症、胱氨酸尿症)的儿童中收集的24小时尿液和晨尿中的钠排泄情况,这些儿童既有肾结石患者,也有未患肾结石的患者,以确定其在尿路结石形成中的意义。

患者与方法

对两组儿童的尿钠排泄情况进行了调查:患有致石性代谢异常但无尿路结石病的患者(L组)和患有肾结石的患者(C组)。两组均分为两个亚组:高钙尿症患者和非高钙尿症患者。L组有22例患者(平均年龄11.97±4.13岁),其中17例组成高钙尿症亚组,5例组成非高钙尿症亚组(3例高尿酸尿症患者和2例高草酸尿症患者)。C组由21例肾结石患者(平均年龄12.67±3.44岁)组成,其中6例组成高钙尿症亚组,15例组成非高钙尿症组(2例胱氨酸尿症患者和13例无致石性代谢异常的患者)。对照组由42名年龄匹配的健康儿童组成。所有受试者肾功能正常。进行了详细的病史询问和临床检查,并对所有患者进行了超声检查。对24小时尿液、晨尿和血清样本进行钠、钾、钙、尿酸、尿素和肌酐分析。根据检测结果计算钠的分数排泄率,以及尿钠与肌酐比值和尿钠与钾比值。钠和钾水平通过火焰光度法测定,钙通过原子吸收技术(美国贝克曼原子分光光度计,Synchron CX-5型号)测定,尿酸通过碳酸盐法测定,肌酐通过杰氏法测定。胱氨酸和二元氨基酸通过离子色谱法定量。尿草酸排泄通过酶分光光度法测定。高钙尿症的定义为24小时钙排泄量大于3.5mg/kg/天和/或钙与肌酐比值大于0.20[8]。尿酸排泄根据斯台普顿和纳什公式[9]表示为经肾小球滤过校正的尿酸排泄量。24小时样本中正常数值低于0.57mg/dl肾小球滤过率。平均值通过皮尔逊线性相关和方差分析(ANOVA)进行统计学分析。

结果

尿钠浓度值包括尿钠与钾比值见表1。我们发现,与对照组相比,L组和C组患者的尿钠排泄均显著增加(p<0.05)。对亚组的进一步分析表明,与对照组相比,仅L组和C组高钙尿症患者的尿钠排泄显著更高(p<0.05)(表2)。发现24小时尿钠与肌酐比值与尿钙与肌酐比值之间存在显著正相关(r = 0.31;p<0.001)(图1),以及24小时和晨尿中的尿钠与钾比值之间存在显著正相关(r = 0.69;p<0.001)(图2)。(A

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