In the early 1970s much of the world adopted the System International (SI) approach to scientific measurement. Unfortunately, the remainder of the world ignored it. This means that, today, we have different units presented in the scientific literature depending on the location of the source of the publication.

The USA is the most notable non SI country and this presents a problem in that the majority of English language textbooks and journals in medicine as well as a lot of the international guidelines and clinical pathways are derived in the US. In critical care this is important – as blood gasses are reported in mmHg in the USA (and most of the literature) and in kPa elsewhere – notably in Europe.

In many of my tutorials I have reported clinical “rules” such as the PaO2/FiO2 ratio, the Alveolar Gas Equation and the majority of the calculations in acid base – in mmHg. This series of two tutorials serve to right the balance. However there is a twist.

In this first tutorial I am not just rehashing the approach to oxygenation by swapping out mmHg for kPa. In fact, the use of kPa to measure and monitor oxygenation provides us with a significant helping hand. Effectively, as atmospheric gas is effectively 100kPa and Oxygen exerts 21% of that – Dalton’s law – then it is clear that the partial pressure of inspired oxygen (PiO2) is 21kPa. Oxygen is poorly soluble in blood and water – the solubility co-efficient is 0.225 – meaning that the quantity of oxygen dissolved in blood is the PaO2 x 0.225 kPa. Oxygen follows Henry’s law – meaning that solubility is related to temperature (37 degrees C) and pressure – the PiO2. In the best case scenario the PaO2 – the partial pressure of oxygen in arterial blood is 13kPa. That means that the gradient between PiO2 and PaO2 is, at a minimal, 8kPa. The greater the stretch between the two the larger the lung injury or ventilation perfusion mismatch.

The oxygen content of blood is 1.34 x Hb x SaO2/100 + (PaO2 x 0.225). I explore the impact of different FiO2s and ambient pressure on the blood oxygen content. Although dissolved oxygen is very low breathing air – the use of supplemental oxygen may dramatically increase it – particularly in hyperbaric conditions.

Finally I address the issue of PaO2/FiO2 as a way of quantifying oxygenation. The PF ratio, as we call it, is a significant component of the ARDS definition. A PF ratio of 200 in mmHg is equivalent to 25 in kPa and a ratio of 100 in mmHg is equivalent to 12.5 in kPa. An easier way to look at this, though, is to divide the PiO2 by the PaO2 – the numbers look similar but you now have a proportion in kPa. That PF ratio of 25 in kPa resolves to 0.25 meaning that only 25% of inspired oxygen is reaching the pulmonary veins (PaO2). Likewise a PF ratio of 12.5 in kPa (100 in mmHg) resolves to 0.125 – which means that only 1/8th of the inspired oxygen is delivered to arterial blood. I think that this is a really good way of assessing oxygenation – and a way of clarifying hypoxemia in your brain.