BACKGROUND:Collecting a 24-h urine sample is recommended for monitoring the mean population sodium intake, but implementation can be difficult. OBJECTIVE:The objective was to assess the validity of published equations by using spot urinary sodium concentrations to predict 24-h sodium excretion. DESIGN:This was a cross-sectional study, conducted from June to August 2011 in metropolitan Washington, DC, of 407 adults aged 18-39 y, 48% black, who collected each urine void in a separate container for 24 h. Four timed voids (morning, afternoon, evening, and overnight) were selected from each 24-h collection. Published equations were used to predict 24-h sodium excretion with spot urine by specimen timing and race-sex subgroups. We examined mean differences with measured 24-h sodium excretion (bias) and individual differences with the use of Bland-Altman plots. RESULTS:Across equations and specimens, mean bias in predicting 24-h sodium excretion for all participants ranged from -267 to 1300 mg (Kawasaki equation). Bias was least with International Cooperative Study on Salt, Other Factors, and Blood Pressure (INTERSALT) equations with morning (-165 mg; 95% CI: -295, 36 mg), afternoon (-90 mg; -208, 28 mg), and evening (-120 mg; -230, -11 mg) specimens. With overnight specimens, mean bias was least when the Tanaka (-23 mg; 95% CI: -141, 95 mg) or Mage (-145 mg; -314, 25 mg) equations were used but was statistically significant when using the Tanaka equations among females (216 to 243 mg) and the Mage equations among races other than black (-554 to -372 mg). Significant over- and underprediction occurred across individual sodium excretion concentrations. CONCLUSIONS:Using a single spot urine, INTERSALT equations may provide the least biased information about population mean sodium intakes among young US adults. None of the equations evaluated provided unbiased estimates of individual 24-h sodium excretion.

译文

摘要背景:建议收集24小时尿液样本以监测平均人群钠摄入量,但实施起来可能很困难。
目的:目的是通过使用现货尿钠浓度预测24小时钠排泄来评估已发布方程的有效性。
设计:这是一项横断面研究,于2011年6月至8月在华盛顿特区进行,研究对象是407位18-39岁,48%黑色的成年人,他们将每个尿液收集在一个单独的容器中24小时。从每个24小时收集中选择四个定时的空隙(早晨,下午,晚上和过夜)。已发布的方程式用于通过标本计时和不同种族的亚组来预测尿液中24小时钠的排泄。我们通过测量的24小时钠排泄量(偏差)检查了平均差异,并使用Bland-Altman图检查了个体差异。
结果:在方程和样本中,所有参与者预测24小时钠排泄的平均偏差为-267至1300 mg(川崎方程)。对于盐,其他因素和血压(INTERSALT)方程的国际合作研究,使用上午(-165 mg; 95%CI:-295,36 mg),下午(-90 mg; -208,28 mg)的国际合作研究中的偏倚最少。和晚上(-120 mg; -230,-11 mg)标本。对于过夜样本,当使用Tanaka(-23 mg; 95%CI:-141,95 mg)或Mage(-145 mg; -314,25 mg)方程式时,平均偏差最小,但在使用Tanaka时具有统计学意义女性(216至243 mg)之间的方程式和黑人以外的其他种族之间的Mage(-554至-372 mg)方程式。各个钠排泄浓度之间发生明显的高估和低估。
结论:使用单点尿液,INTERSALT方程可提供有关美国年轻成年人中人群平均钠摄入量的偏差最小的信息。所评估的方程式均未提供单个24小时钠排泄的无偏估计。

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