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The Effect of Physical Activity Levels on Hydration Markers in Non-Athletic Free-Living Individuals.

机译:体力活动水平对非运动自由生活个体水合标记的影响。

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摘要

Higher levels of physical activity requires increased fluid intake due to increased water losses via sweating. PURPOSE: To determine the effect of physical activity on hydration status and water intake. METHODS: This study involved 8 visits to the Human Performance Laboratory over 22 days. Body weight and urine measurements were taken every visit. Physical activity was assessed by the International Physical Activity Questionnaire (IPAQ), water intake by the Water Frequency Questionnaire (WFQ), and hydration status by urine osmolality (UOsm), urine specific gravity (USG), and urine color (UC). From the IPAQ subjects were classified as low, moderate and high physical activity levels and the total amount of physical activity was expressed as MET-min·w -1. All values represent means across 22 days of measurements except physical activity and water intake, which was a mean of two measurements. Participants were excluded if they exercised more than 4 hours a week or if they were on medications that effected fluid balance. One-way analysis of variance was computed to determine differences in hydration status between groups. Additionally, 2-tailed Pearson correlations were computed to determine relationships between all measurements while using physical activity as a continuous variable (i.e., MET-min·w-1). RESULTS: 95 participants (45 males, 40+/-13.2 y, 1.76+/-0.07 m, 27.3+/-10.8 %BF 25.9+/-4.6 kg·m2; 50 females, 41.1+/-14.8 y, 1.63+/-.06 m, 35.0+/-11.0 %BF, 26.6+/-6.2 kg·m 2) completed the study; n=39 for low activity (822+/-698 MET-min·w -1), n=48 for moderate activity (1791+/-1195 MET-min·w -1), n=8 for high activity (4,728+/-1150 MET-min·w -1). Hydration status and water intake did not differ across all levels of physical activity; UOsm: 587+/-209, 596+/-223, 562+/-290; and TWI: 2.6+/-.9, 2.9+/-1.4, 3.0+/-1.5 L for low, moderate, and high physical activity levels, respectively (P≤0.05). UOsm (589+/-290) was strongly correlated to Total Water Intake (2.83+/-1.22 L, P=0.000), and weight (76.4+/-17.3 kg, P=0.000) at a significance level of P≤0.01 but not strongly correlated to METmin·w-1 (1640+/-1453). CONCLUSION: No significant differences in hydration or water intake were observed across groups. However, the small numbers of participants in the high physical activity levels may have made this comparison difficult. A wider range of MET-min·w-1 between groups may need to be studied.
机译:较高水平的体育锻炼需要增加出汗量,因为出汗会导致水分流失增加。目的:确定体育锻炼对水合状态和摄水量的影响。方法:本研究涉及22天的8次访问人类绩效实验室。每次访视均进行体重和尿液测量。通过国际体育锻炼问卷(IPAQ)评估体育锻炼,通过水频率问卷(WFQ)评估饮水量,并通过尿渗透压(UOsm),尿比重(USG)和尿色(UC)评估水合状况。从IPAQ中将受试者分为低,中和高体育活动水平,体育活动总量表示为MET-min·w -1。所有值代表22天测量的平均值,但身体活动和摄水量除外,这是两次测量的平均值。如果参与者每周运动超过4小时或正在使用影响体液平衡的药物,则将参与者排除在外。计算方差的单向分析以确定组之间的水合状态差异。另外,在将身体活动作为连​​续变量(即MET-min·w-1)的同时,计算了2尾Pearson相关性以确定所有测量之间的关系。结果:95名参与者(45名男性,40 +/- 13.2岁,1.76 +/- 0.07 m,27.3 +/- 10.8%BF 25.9 +/- 4.6 kg·m2; 50名女性,41.1 +/- 14.8岁,1.63+ /-.06 m,35.0 +/- 11.0%BF,26.6 +/- 6.2 kg·m 2)完成了研究;低活动度n = 39(822 +/- 698 MET-min·w -1),中度活动n = 48(1791 +/- 1195 MET-min·w -1),高活动度n = 8(4,728 +/- 1150 MET-min·w -1)。在所有水平的体育锻炼中,水合状态和摄水量均无差异。 UOsm:587 +/- 209、596 +/- 223、562 +/- 290;和TWI:低,中和高体育活动水平分别为2.6 +/-。9、2.9 +/- 1.4、3.0 +/- 1.5 L(P≤0.05)。 UOsm(589 +/- 290)与总水摄入量(2.83 +/- 1.22 L,P = 0.000)和体重(76.4 +/- 17.3 kg,P = 0.000)和P <0.01的显着水平密切相关但与METmin·w-1(1640 +/- 1453)无关。结论:各组之间的水合作用或摄水量没有显着差异。但是,参加高运动量的参与者数量很少,可能使这种比较变得困难。可能需要研究各组之间更广泛的MET-min·w-1。

著录项

  • 作者

    Hammer, Mikell L.;

  • 作者单位

    University of Arkansas.;

  • 授予单位 University of Arkansas.;
  • 学科 Kinesiology.;Health education.
  • 学位 M.S.
  • 年度 2015
  • 页码 36 p.
  • 总页数 36
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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