A-a Gradient Equation:
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The Alveolar-arterial oxygen gradient (A-a gradient) measures the difference between alveolar oxygen concentration and arterial oxygen concentration. It's a key indicator of lung function and gas exchange efficiency, helping to differentiate between various causes of hypoxemia.
The calculator uses the A-a Gradient equation:
Where:
Explanation: The equation calculates the alveolar oxygen tension using the alveolar gas equation and subtracts the measured arterial oxygen tension to determine the gradient.
Details: The A-a gradient is crucial for diagnosing the cause of hypoxemia. A normal gradient suggests hypoventilation, while an increased gradient indicates ventilation-perfusion mismatch, diffusion impairment, or shunt physiology.
Tips: Enter FiO2 as a fraction (0.21 for room air, 1.0 for 100% oxygen), atmospheric pressure (760 mmHg at sea level), water vapor pressure (47 mmHg), arterial blood gas values for PaCO2 and PaO2, and respiratory quotient (typically 0.8).
Q1: What is a normal A-a gradient?
A: In healthy young adults breathing room air at sea level, the normal A-a gradient is typically 5-15 mmHg. This increases with age (approximately 1 mmHg per decade over 20 years old).
Q2: Why does the A-a gradient increase with age?
A: Aging causes progressive loss of elastic recoil in the lungs and changes in ventilation-perfusion matching, leading to a gradual increase in the A-a gradient.
Q3: What conditions cause an elevated A-a gradient?
A: Pulmonary embolism, pneumonia, COPD, asthma, pulmonary fibrosis, congestive heart failure, and other conditions affecting gas exchange.
Q4: When is the A-a gradient normal despite hypoxemia?
A: In pure hypoventilation (e.g., drug overdose, neuromuscular disorders) where both alveolar and arterial oxygen decrease proportionally.
Q5: How does altitude affect the A-a gradient?
A: At higher altitudes, atmospheric pressure decreases, which affects the calculation. The normal range for A-a gradient also changes with altitude.