A-a Gradient Equation:
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The Alveolar-arterial (A-a) oxygen gradient is the difference between alveolar oxygen partial pressure (PAO2) and arterial oxygen partial pressure (PaO2). It's a valuable clinical tool for assessing gas exchange efficiency in the lungs and diagnosing various pulmonary conditions.
The calculator uses the A-a Gradient equation:
Where:
Explanation: The equation calculates the alveolar oxygen tension and subtracts the measured arterial oxygen tension to determine the gradient.
Details: The A-a gradient helps differentiate between hypoxemia due to ventilation-perfusion mismatch, diffusion defects, or shunting versus hypoventilation. It's crucial for diagnosing pulmonary embolism, pneumonia, ARDS, and other lung diseases.
Tips: Enter FiO2 as a fraction (0.21 for room air, 1.0 for 100% oxygen), atmospheric pressure in mmHg, water vapor pressure (typically 47 mmHg), PaCO2 and PaO2 from arterial blood gas analysis, 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, normal A-a gradient is 5-15 mmHg. It increases with age and higher FiO2.
Q2: Why does the gradient increase with age?
A: Aging causes changes in lung compliance and ventilation-perfusion matching, leading to a gradual increase in A-a gradient (approximately 1 mmHg per decade after age 20).
Q3: What conditions cause elevated A-a gradient?
A: Pulmonary embolism, pneumonia, ARDS, pulmonary fibrosis, atelectasis, and right-to-left cardiac shunts.
Q4: When is A-a gradient normal despite hypoxemia?
A: In pure hypoventilation (e.g., drug overdose, neuromuscular disease), where both PAO2 and PaO2 decrease proportionally.
Q5: How does altitude affect A-a gradient?
A: At higher altitudes, atmospheric pressure decreases, which affects the calculation. Always use the appropriate local atmospheric pressure.