Hypoxia (medical)

Hypoxia
ICD-10
ICD-9 799.02
MeSH D000860

Hypoxia is a pathological condition in which the body as a whole (generalized hypoxia) or region of the body (tissue hypoxia) is deprived of adequate oxygen supply. However variations in arterial oxygen concentration can be part of normal physiology, e.g. during strenuous physical exercise due to mismatch between supply and demand for oxygen at the cellular level. Hypoxia in which there is complete deprivation of oxygen supply is referred to as anoxia.

Hypoxia differs from apoxemia, which is an abnormally low concentration of oxygen in arterial blood.[1] A frequent error is to use the term hypoxia to mean a low oxygen content in arterial blood. A correct term for low oxygen content in arterial blood is hypoxemia. It is possible to have a low oxygen content (e.g., due to anemia) but a high PO2. Incorrect use of these terms can lead to confusion.

Generalized hypoxia occurs in healthy people when they ascend to high altitude, where it causes altitude sickness leading to potentially fatal complications: high altitude pulmonary edema (HAPE) and high altitude cerebral edema (HACE). Hypoxia also occurs in healthy individuals when breathing mixtures of gases with a low oxygen content, e.g. while diving underwater especially when using closed-circuit rebreather systems that control the amount of oxygen in the supplied air. A mild and non-damaging intermittent hypoxia is used intentionally duringaltitude trainings to develop an athletic performance adaptation evident in beneficial effects that are at both systemic and cellular level.[2]

Contents

Symptoms

Symptoms of generalized hypoxia depend on its severity and acceleration of onset. In the case of altitude sickness, where hypoxia develops gradually, the symptoms include headaches, fatigue, shortness of breath, a feeling of euphoria and nausea. In severe hypoxia, or hypoxia of very rapid onset, changes in levels of consciousness, seizures, coma, priapism, and death occur. Severe hypoxia induces a blue discolouration of the skin, called cyanosis. Because haemoglobin is a darker red when it is not bound to oxygen (deoxyhemoglobin), as opposed to the rich red colour that it has when bound to oxygen (oxyhaemoglobin), when seen through the skin it has an increased tendency to reflect blue light back to the eye. In cases where the oxygen is displaced by another molecule, such as carbon monoxide, the skin may appear 'cherry red' instead of cyanotic.

Types of hypoxia

Pathophysiology

After mixing with water vapour and expired CO2 in the lungs, oxygen diffuses down a pressure gradient to enter arterial blood around where its partial pressure is 100mmHg (13.3kPa).[3] Arterial blood flow delivers oxygen to the peripheral tissues, where it again diffuses down a pressure gradient into the cells and into their mitochondria. These bacteria-like cytoplasmic structures strip hydrogen from fuels (glucose, fats and some amino acids) to burn with oxygen to form water. Released energy (originally from the sun and photosynthesis) is stored as ATP, to be later used for energy requiring metabolism. The fuel's carbon is oxidized to CO2, which diffuses down its partial pressure gradient out of the cells into venous blood to finally be exhaled by the lungs. Experimentally, oxygen diffusion becomes rate limiting (and lethal) when arterial oxygen partial pressure falls to 40mmHg or below.

If oxygen delivery to cells is insufficient for the demand (hypoxia), hydrogen will be shifted to pyruvic acid converting it to lactic acid. This temporary measure (anaerobic metabolism) allows small amounts of energy to be produced. Lactic acid build up in tissues and blood is a sign of inadequate mitochondrial oxygenation, which may be due to hypoxemia, poor blood flow (e.g., shock) or a combination of both.[5] If severe or prolonged it could lead to cell death.

Vasoconstriction and vasodilation

In most tissues of the body, the response to hypoxia is vasodilation. By widening the blood vessels, the tissue allows greater perfusion.

By contrast, in the lungs, the response to hypoxia is vasoconstriction. This is known as "Hypoxic pulmonary vasoconstriction", or "HPV".

Treatment

To counter the effects of high-altitude diseases, the body must return arterial PO2 toward normal. Acclimatization, the means by which the body adapts to higher altitudes, only partially restores PO2 to standard levels. Hyperventilation, the body’s most common response to high-altitude conditions, increases alveolar PO2 by raising the depth and rate of breathing. However, while PO2 does improve with hyperventilation, it does not return to normal. Studies of miners and astronomers working at 3000 meters and above show improved alveolar PO2 with full acclimatization, yet the PO2 level remains equal to or even below the threshold for continuous oxygen therapy for patients with chronic obstructive pulmonary disease (COPD).[6] In addition, there are complications involved with acclimatization. Polycythemia, in which the body increases the number of red blood cells in circulation, thickens the blood, raising the danger that the heart can’t pump it.

In high-altitude conditions, only oxygen enrichment can counteract the effects of hypoxia. By increasing the concentration of oxygen in the air, the effects of lower barometric pressure are countered and the level of arterial PO2 is restored toward normal capacity. A small amount of supplemental oxygen reduces the equivalent altitude in climate-controlled rooms. At 4000 m, raising the oxygen concentration level by 5 percent via an oxygen concentrator and an existing ventilation system provides an altitude equivalent of 3000 m, which is much more tolerable for the increasing number of low-landers who work in high altitude.[7] In a study of astronomers working in Chile at 5050 m, oxygen concentrators increased the level of oxygen concentration by 6 percent (that is, from 21 percent to 27 percent). This resulted in increased worker productivity, less fatigue, and improved sleep.[8]

Oxygen concentrators are uniquely suited for this purpose. They require little maintenance and electricity, provide a constant source of oxygen, and eliminate the expensive, and often dangerous, task of transporting oxygen cylinders to remote areas. Offices and housing already have climate-controlled rooms, in which temperature and humidity are kept at a constant level. Oxygen can be added to this system easily and relatively cheaply.

See also

For aircraft decompression incidents at altitude see:

Footnotes

  1. West, John B. (1977). Pulmonary Pathophysiology: The Essentials. Williams & Wilkins. pp. 22. 
  2. *Nonhematological mechanisms of improved sea-level ... - PubMed Med Sci Sports Exerc. 2007 Sep;39(9):1600-9.
  3. 3.0 3.1 Kenneth Baillie and Alistair Simpson. "Altitude oxygen calculator". Apex (Altitude Physiology Expeditions). Retrieved on 2006-08-10. - Online interactive oxygen delivery calculator
  4. Kenneth Baillie and Alistair Simpson. "Oxygen content calculator". Apex (Altitude Physiology Expeditions). Retrieved on 2006-08-10. - A demonstration of the effect of anaemia on oxygen content
  5. Hobler, K.E.; L.C. Carey (1973). "Effect of acute progressive hypoxemia on cardiac output and plasma excess lactate" (scanned copy). Ann Surg 177 (2): 199–202. doi:10.1097/00000658-197302000-00013. PMID 4572785. http://www.pubmedcentral.gov/articlerender.fcgi?tool=pubmed&pubmedid=4572785. 
  6. West, John B. (2004). "The Physiologic Basis of High-Altitude Diseases". Annals of Internal Medicine 141 (10): 791. 
  7. West, John B. (1995). "Oxygen Enrichment of Room Air to Relieve the Hypoxia of High Altitude". Respiration Physiology 99 (2): 230. doi:10.1016/0034-5687(94)00094-G. 
  8. West, John B. (2004). "The Physiologic Basis of High-Altitude Diseases". Annals of Internal Medicine 141 (10): 793. 

Bibliography