RESPIRATION   

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Respiration can be broken up conceptually into three phases: external, internal, and cellular respiration.  External respiration is about the mechanics of breathing, moving gases (air) in and out of the lungs.  Internal respiration is about ensuring the transport of oxygen in the blood from the lungs to tissue cells, and then the transport of metabolic CO2 from tissue cells to the lungs for both its excretion and its reallocation to systemic circulation for acid-base regulation.  Cellular respiration is the utilization of oxygen in mitochondria for the synthesis of adenosine triphosphate (ATP), molecules that cells ultimately break down for their energy. 

 

Basic to external respiration is the subject of gas exchange.  Gases are measured by virtue of the pressures that they exert.  When gases are mixed, e.g., air, they each contribute to a total pressure.  Each gas contributes a partial pressure (P).  Total atmospheric air pressure at sea level, at 15 degrees C and zero humidity, is 760 mmHg (millimeters of mercury).  At sea level partial pressure oxygen, written PO2, is 159 mmHg (20.93%), and partial pressure carbon dioxide, written PCO2, is 0.3 mmHg (less than 0.04%).  Most of the gas exchange, O2 and CO2, takes place in the fundamental alveolar-capillary unit, the alveolus.  There are about 300 million alveoli in the lungs, surrounded by about 280 billion pulmonary capillaries.  Capnography is about measurement of average alveolar PCO2, which is observed/measured in the final portion of exhalation when gases are presumably 100 percent alveolar (not mixed with anatomical dead space gases); this measurement is known as End Tidal CO2, or ETCO2, or PCO2 at the “end of the tides of air,” that is, when the “tide is out.”

The Henderson-Hasselbach (H-H) equation is central to understanding internal respiration, which describes pH regulation in extracellular fluids:  pH = [HCO3] ÷ PCO2 (in its simplified conceptual format), wherein PCO2 is regulated by breathing, and bicarbonate concentration [HCO3] is regulated by the kidneys.  These fluids include blood plasma, interstitial (fluids that surround tissue cells), lymph, and cerebrospinal fluids.   Changes in the numerator of the equation, bicarbonate concentration, are generally slow (8 hours to 5 days), whereas changes in the denominator, partial pressure carbon dioxide (PCO2), are immediate.  This places breathing center stage in moment-to-moment acid-base regulation.  Arterial levels of PCO2, known as PaCO2, remain between 35 and 45 mmHg to keep plasma pH within its normal range (7.35 to 7.45).  In normal healthy lungs, when perfusion (blood) and ventilation (air) are matched, alveolar PCO2 (and hence, ETCO2) is approximately equivalent to PaCO2.

 

Balancing the Henderson-Hasselbach (H-H) equation is achieved through the presence of receptor sites in (1) the brainstem that are sensitive to interstitial pH and PCO2, and (2) the arterial system (aorta and carotid arteries) that are sensitive to plasma pH and PCO2.  Changes in pH and PCO2 in both locations together drive the respiratory centers in the brainstem, along with partial pressure oxygen (PO2) changes detected also at arterial receptor sites.  If pH is too low (< 7.35), or too high (>7.45), PaCO2 is reduced or increased by altering breathing rate and depth (minute volume).  Brainstem reflex-regulated breathing, under normal circumstances, maintains alveolar PCO2 at 35 to 45 mmHg, wherein rapid diffusion from alveolus to pulmonary capillary provides for almost immediate equilibration, thus ensuring a PaCO2 of about the same value.

 

Actual quantities of carbon dioxide generated by the body vary considerably based on metabolism, e.g., meditation vs. exercise, although the PaCO2 values required for maintaining acid-base balance remain the same.  At rest, for example, only about 15 percent of the CO2 arriving in the lungs is actually excreted; the balance is reallocated to systemic circulation.  Capnograph instrumentation does not indicate how much CO2 is being exhaled, rather it indicates the alveolar PCO2 being maintained, and thus the approximate PaCO2.

 

Levitzky, M. G.  Pulmonary Physiology.  New York: McGraw Hill, 2007 (7th edition).

 

Thomson, W. S. T., Adams, J. F., & Cowan, R. A.  Clinical Acid-Base Balance.  New York: Oxford University Press, 1997.

 

 

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