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将用于从高空或栖息地进行免停留潜水的标准空气减压表进行转换。

Converting standard air decompression tables for no-stop diving from altitude or habitat.

作者信息

Hennessy T R

出版信息

Undersea Biomed Res. 1977 Mar;4(1):39-53.

PMID:857357
Abstract

Using the phase equilibration theory of Hills (1966), as modified by Hennessy and Hempleman (1977), it is possible to predict formulas for converting standard air decompression tables for no-stop diving at altitude or from a normoxic habitat, breathing air. For diving following equilibration at altitude, the Royal Navy, Royal Naval Physiological Laboratory, and Haldane-type rules appear to be too conservative, with the opposite result for diving after excursion to altitude. Predictions in the latter case are in fair agreement with the Swiss (Boni, Schibli, Nussberger, and Bühlmann 1976) no-stop altitude tables. In the case of habitats, close agreement is found between the Hamilton, Kenyon, Freitag, and Schreiner (1973) normoxic tables for no-stop downward excursions and indefinite dive upward-excursions on air. In the case of flying directly after no-stop diving, the US Navy rule of using repetitive group D appears to be conservative for dives less than 50 fsw, and possibly unsafe for dives over 50 fsw. It is concluded that for no-stop diving a single tissue and single safe ascent pressure formula are all that is necessary to generate equivalent air dives. This enforces the hypothesis that it is the volume of gas released on ascent that governs marginal type I bends, and that in a no-stop ascent, all excess dissolved gas is released in the worst case.

摘要

运用经亨尼西和亨普尔曼(1977年)修正的希尔斯(1966年)相平衡理论,可以预测用于将高空或常氧栖息地无减压潜水的标准空气减压表进行转换的公式,潜水时呼吸空气。对于在高空达到平衡后的潜水,皇家海军、皇家海军生理实验室以及霍尔丹型规则似乎过于保守,而对于前往高空后进行的潜水则结果相反。后一种情况下的预测与瑞士(博尼、施布利、努斯贝格尔和比尔曼,1976年)的无减压高空表相当吻合。对于栖息地的情况,汉密尔顿、凯尼恩、弗赖塔格和施赖纳(1973年)的常氧无减压下潜表与在空气中进行的无限制潜水上升表之间达成了密切一致。在无减压潜水后直接飞行的情况下,美国海军使用重复组D的规则对于深度小于50英尺海水的潜水似乎过于保守,而对于深度超过50英尺海水的潜水可能不安全。得出的结论是,对于无减压潜水,生成等效空气潜水所需的全部内容是一个单一组织和单一安全上升压力公式。这强化了这样一种假设,即上升时释放的气体体积决定了边缘性I型减压病,并且在无减压上升过程中,在最坏的情况下所有多余的溶解气体都会被释放出来。

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