Hilgenfeld Michelle Stuart, Simon Stephen, Blowey Douglas, Richmond Wendy, Alon Uri S
Section of Nephrology, Children's Mercy Hospital, Kansas City, Missouri 64108, USA.
Pediatr Nephrol. 2004 Oct;19(10):1153-5. doi: 10.1007/s00467-004-1568-z. Epub 2004 Aug 7.
Seasonal variations in urinary calcium excretion have been observed in adults and are thought to be due to seasonal changes in sunlight exposure, which results in fluctuation of blood levels of 25-hydroxyvitamin D. The goal of the present study was to explore the possible effect of season on urinary calcium/creatinine ratio (UCa/Cr) in healthy school children. We studied 65 healthy Caucasian children aged 5.1-14.6 years (mean+/-SD 9.6+/-2.0, median 9.7 years). Random, non-fasting urine samples were collected from each participant between the 1st and 5th days of the month for 16 successive months and analyzed for UCa/Cr. In parallel, meteorological data, which included average monthly temperature and average monthly UV index, were collected for the whole study period. A mathematical model describing the monthly mean values of UCa/Cr as a sine function was used to determine the presence of seasonal variation. The observed maximum mean UCa/Cr, 0.092 mg/mg (0.260 mmol/mmol), occurred in the late summer months (August/September) and minimum mean UCa/Cr, 0.083 mg/mg (0.235 mmol/mmol), occurred in mid-winter (January/February), reflecting an infinitesimal and statistically insignificant change. Moreover, both values were well within the previously established normal range for UCa/Cr of </=0.20 mg/mg (0.566 mmol/mmol). The pattern seen in the last 4 months of the study repeated that seen in the first 4 months. The mean temperature in July of the 1st year was 27.1+/-2.6, January 1.8+/-5.4, and July of the 2nd year 27.0+/-2.2 degrees C. The mean UV index in July of the 1st year (7.61+/-1.01) was not different from that in July of the 2nd year (7.73+/-0.86), and both were statistically much higher than that in January (1.37+/-0.44) ( P<0.001). Evidently, in spite of significant changes in seasonal meteorological indices of sunlight, no significant seasonal variations in UCa/Cr were observed in a cohort of healthy school children. Thus the current UCa/Cr value used to diagnose hypercalciuria does not require a seasonal adjustment.
在成年人中已观察到尿钙排泄的季节性变化,据认为这是由于阳光照射的季节性变化所致,而阳光照射的变化会导致血液中25-羟基维生素D水平的波动。本研究的目的是探讨季节对健康学龄儿童尿钙/肌酐比值(UCa/Cr)的可能影响。我们研究了65名年龄在5.1至14.6岁之间的健康白种儿童(平均±标准差9.6±2.0,中位数9.7岁)。在连续16个月中,于每月的第1天至第5天从每位参与者收集随机、非空腹的尿液样本,并分析其UCa/Cr。同时,收集了整个研究期间的气象数据,包括月平均温度和月平均紫外线指数。使用一个将UCa/Cr的月均值描述为正弦函数的数学模型来确定是否存在季节性变化。观察到的UCa/Cr最大平均值得出,在夏末月份(8月/9月)为0.092mg/mg(0.260mmol/mmol),而在冬季中期(1月/2月)最小平均值得出为0.083mg/mg(0.235mmol/mmol),反映出变化极小且在统计学上无显著意义。此外,这两个值均完全在先前确定的UCa/Cr正常范围(≤0.20mg/mg,即0.566mmol/mmol)之内。研究最后4个月观察到的模式与最初4个月观察到的模式重复。第一年7月的平均温度为27.1±2.6,1月为1.8±5.4,第二年7月为27.0±2.2℃。第一年7月的平均紫外线指数(7.61±1.01)与第二年7月的平均紫外线指数(7.73±0.86)无差异,且两者在统计学上均显著高于1月的平均紫外线指数(1.37±0.44)(P<0.001)。显然,尽管阳光的季节性气象指标有显著变化,但在一组健康学龄儿童中未观察到UCa/Cr有显著的季节性变化。因此,目前用于诊断高钙尿症的UCa/Cr值不需要进行季节调整。