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Changes in blood gas transport of altitude native soccer players near sea-level and sea-level native soccer players at altitude (ISA3600)

机译:海拔附近的海拔高度本地足球运动员和海拔高度处的海拔水平本地足球运动员的血液气体传输变化(ISA3600)

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摘要

Objectives: The optimal strategy for soccer teams playing at altitude is not known, that is, ‘fly-in, fly-out’ versus short-term acclimatisation. Here, we document changes in blood gas and vascular volumes of sea-level (Australian, n=20) and altitude (Bolivian, n=19) native soccer players at 3600 m. Methods: Haemoglobin-oxygen saturation (Hb-sO2), arterial oxygen content (CaO2), haemoglobin mass (Hbmass), blood volume (BV) and blood gas concentrations were measured before descent (Bolivians only), together with aerobic fitness (via Yo-YoIR1), near sea-level, after ascent and during 13 days at 3600 m. Results: At baseline, haemoglobin concentration [Hb] and Hbmass were higher in Bolivians (mean±SD; 18.2±1.0 g/dL, 12.8±0.8 g/kg) than Australians (15.0±0.9 g/dL, 11.6±0.7 g/kg; both p≤0.001). Near sea-level, [Hb] of Bolivians decreased to 16.6±0.9 g/dL, but normalised upon return to 3600 m; Hbmass was constant regardless of altitude. In Australians, [Hb] increased after 12 days at 3600 m to 17.3±1.0 g/dL; Hbmass increased by 3.0 ±2.7% (p≤0.01). BV decreased in both teams at altitude by ∼400 mL. Arterial partial pressure for oxygen (PaO2), Hb-sO2 and CaO2 of both teams decreased within 2 h of arrival at 3600 m (p≤0.001) but increased over the following days, with CaO2 overcompensated in Australians (+1.7±1.2 mL/100 mL; p≤0.001). Yo-YoIR1 was lower on the 3rd versus 10th day at altitude and was significantly related to CaO2. Conclusions: The marked drop in PaO2 and CaO2 observed after ascent does not support the ‘fly-in, fly-out’ approach for soccer teams to play immediately after arrival at altitude. Although short-term acclimatisation was sufficient for Australians to stabilise their CaO2 (mostly due to loss of plasma volume), 12 days appears insufficient to reach chronic levels of adaption.
机译:目标:尚不清楚足球运动员在高空比赛的最佳策略,即“飞入,飞出”与短期适应。在这里,我们记录了在3600 m处的本地足球运动员的海平面(Australian,n = 20)和海拔(Bolivian,n = 19)的血气和血管体积的变化。方法:血红蛋白氧饱和度(Hb-sO2),动脉血氧含量(CaO2),血红蛋白质量(Hbmass),血容量(BV)和血气浓度在下降之前(仅玻利维亚人)进行测量,并进行有氧适应性测定(通过Yo -YoIR1),靠近海平面,上升后以及3600 m的13天中。结果:基线时,玻利维亚人的血红蛋白浓度[Hb]和Hbmass(平均值±SD; 18.2±1.0 g / dL,12.8±0.8 g / kg)高于澳大利亚人(15.0±0.9 g / dL,11.6±0.7 g / kg)。 ; p均≤0.001)。在海平面附近,玻利维亚人的[Hb]下降至16.6±0.9 g / dL,但在返回3600 m后恢复正常;无论海拔高低,Hbmass都是恒定的。在澳大利亚人中,[Hb]在3600 m下停留12天后增加至17.3±1.0 g / dL;体重增加3.0±2.7%(p≤0.01)。两支球队的BV在海拔高度均下降了约400 mL。两组的氧气(PaO2),Hb-sO2和CaO2的动脉分压在3600 m到达后的2小时内下降(p≤0.001),但随后几天有所增加,其中CaO2在澳大利亚人中被过度补偿(+ 1.7±1.2 mL / 100mL;p≤0.001)。在海拔第3天和第10天,Yo-YoIR1较低,并且与CaO2显着相关。结论:上升后观察到的PaO2和CaO2明显下降,不支持足球队到达高空后立即比赛的“飞入,飞出”方法。尽管短期适应足以使澳大利亚人稳定其CaO2(主要是由于血浆量减少),但12天似乎不足以达到慢性适应水平。

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