Carbon dioxide is transported in blood as dissolved gas, carbaminohemoglobin, and bicarbonate ion, with the bicarbonate buffer system playing the largest role (~87%) in CO2 carriage and pH regulation. The chloride shift and Haldane effect couple CO2 and oxygen transport, enabling efficient gas exchange.
From your understanding of blood composition and the respiratory system, you know that blood must carry metabolic waste products — including carbon dioxide — from tissues back to the lungs for elimination. But CO₂ presents a transport challenge: it is far more soluble than oxygen, yet the body produces enormous quantities of it (about 200 mL per minute at rest), and it is also an acid-forming molecule. The blood solves this problem through three simultaneous transport mechanisms, each serving a distinct role.
The simplest form is dissolved CO₂, which accounts for only about 7–10% of total CO₂ transport. CO₂ dissolves directly in plasma and is the form that actually exerts partial pressure and diffuses across membranes — so despite carrying a small fraction of the total, dissolved CO₂ is the form that drives the partial pressure gradients essential for gas exchange at the lungs and tissues. A second mechanism involves CO₂ binding directly to hemoglobin (not at the oxygen-binding heme site but at amino groups on the globin chains), forming carbaminohemoglobin. This accounts for roughly 20–23% of CO₂ transport. Importantly, deoxygenated hemoglobin binds CO₂ more readily than oxygenated hemoglobin — a fact that becomes critical at the tissues where oxygen has just been released.
The dominant mechanism — carrying about 70% of CO₂ — is the bicarbonate buffer system. Inside red blood cells, the enzyme carbonic anhydrase rapidly catalyzes the reaction CO₂ + H₂O → H₂CO₃ → H⁺ + HCO₃⁻. The bicarbonate (HCO₃⁻) is then shuttled out of the red blood cell into the plasma via an antiporter that exchanges it for chloride ions (Cl⁻) — this is the chloride shift, which maintains electrical neutrality. The hydrogen ions (H⁺) produced are buffered by binding to deoxygenated hemoglobin, which acts as a buffer and prevents dangerous drops in pH. At the lungs, the entire process reverses: bicarbonate re-enters the red blood cell, recombines with H⁺, carbonic anhydrase converts carbonic acid back to CO₂ and water, and the CO₂ diffuses into the alveoli for exhalation.
The elegance of this system lies in how oxygen and CO₂ transport are coupled through the Haldane effect: deoxygenated hemoglobin is a better CO₂ carrier (both as carbaminohemoglobin and as a H⁺ buffer) than oxygenated hemoglobin. At the tissues, as hemoglobin releases O₂, it simultaneously becomes better at picking up CO₂ and buffering the resulting acid. At the lungs, as hemoglobin binds O₂, it releases CO₂ and H⁺, facilitating CO₂ elimination. This reciprocal coupling means that the same molecule — hemoglobin — optimizes both oxygen delivery and CO₂ removal in a single pass through the circulation, and it explains why the bicarbonate buffer system is not just a transport mechanism but the body's first line of defense in maintaining blood pH within its narrow physiological range of 7.35–7.45.