Respiration and Gas Exchange Concepts
Goal of Respiration
To transport O₂ from the air to muscles for energy, health, and metabolism
CO₂ has to return via pulmonary and cellular respiration
Pulmonary and Cellular Respiration
Pulmonary Respiration: Exchange of gases in the lungs
Cellular Respiration: O2 utilization and CO2 production by the tissues
Conducting Zone: Filters, humidifies, and warms air; includes anatomical dead space
Few liters of air remain unutilized in the conducting zone
Respiratory Zone: Site of gas exchange between air and blood – includes alveoli, bronchial tree, and terminal bronchioles
Gas Flow Principles
Gas flows from higher to lower pressure
pressure gradients crucial for continuous flow from the atmosphere to muscles
Distinction Between Capillaries and Other Vessels
Capillaries are extremely thin, allowing easier gas exchange compared to veins and arteries
Red blood cells slow down in capillaries, enhancing gas exchange
Blood Pressure: Lower in capillaries than in arteries due to increased cross-sectional area
Blood flows through many capillaries, lowering overall pressure despite their small size
Diaphragm Function
Diaphragm: Facilitates breathing by contracting and expanding
Inspiration: Diaphragm contracts, creating a vacuum that pulls air into the lungs
Expiration: Passive relaxation allows air to flow out
Altitude Masks
Mimic altitude by restricting airflow
Claims of increased red blood cell production through EPO stimulation are questionable
Partial Pressures at Altitude:
Total atmospheric pressure decreases; thus, the partial pressure of gases, including O₂, falls.
Dalton's Law: Total pressure is the sum of individual gas pressures.
The Importance of Partial Pressure
O₂ at Sea Level: 21% of atmospheric pressure is 760 mmHg, making the partial pressure roughly 159 ext{ mmHg}.
At Altitude: Partial pressure of O₂ decreases due to lower overall pressure
Gas Exchange Mechanism
Gas exchange in alveoli driven by pressure gradients
When comparing gases:
O₂ goes from 159 o 104 ext{ mmHg}
CO₂ goes from 46 o 40 ext{ mmHg}
CO₂ is more soluble; hence, it exchanges effectively even with a smaller gradient
Breathing Rates in Exercise
During physical activity, breathing depth increases first, then frequency
Tidal Volume: Volume of air breathing in/out during normal resting breath
Inspiratory Reserve Volume: Maximum volume after a normal breath taken in
Expiratory Reserve Volume: Maximum volume pushed out after a normal breath
Residual Volume: Air remaining after maximal exhalation
Hemoglobin and Oxygen Carrying Capacity
Hemoglobin carries O₂; contains 4 binding sites
Ranges of Hemoglobin: 15g/dL considered healthy; lower levels indicate anemia
Risks for vegetarians/vegans: Lower iron absorption can result in anemia, impacting performance
Clinical Implications
COPD patients may benefit from diaphragm strengthening
Understanding differences in blood flow and oxygenation is essential for therapy and training adaptations
Summary of Key Laws
Dalton’s Law: The sum of partial pressures equals total pressure.
Henry’s Law: Gas solubility in liquid proportional to partial pressure; crucial for understanding gas exchange.
Final Thoughts
Balancing the biological rationale with clinical practicality is crucial in applying respiration concepts in health and exercise settings.