A-a Gradient Equation:
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The Alveolar-arterial (A-a) gradient measures the difference between alveolar oxygen concentration and arterial oxygen concentration. It helps differentiate between causes of hypoxemia and assess gas exchange efficiency in the lungs.
The calculator uses the A-a gradient equation:
Where:
Explanation: The equation calculates the ideal alveolar oxygen pressure and subtracts the measured arterial oxygen pressure 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.
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), and arterial blood gas values. All values must be valid and positive.
Q1: What is a normal A-a gradient?
A: Normal A-a gradient is <10 mmHg in young healthy adults breathing room air, increasing with age (approximately 3 mmHg per decade).
Q2: When is A-a gradient increased?
A: Increased in conditions like pulmonary embolism, pneumonia, ARDS, pulmonary edema, and interstitial lung disease.
Q3: Why is the respiratory quotient assumed to be 0.8?
A: 0.8 represents the average respiratory quotient (CO₂ production/O₂ consumption) for a typical mixed diet.
Q4: How does altitude affect A-a gradient?
A: At higher altitudes, atmospheric pressure decreases, which affects the calculation. Use the actual local atmospheric pressure for accurate results.
Q5: What are the limitations of A-a gradient?
A: The calculation assumes steady-state conditions and may be less accurate with high FiO₂ levels or in rapidly changing clinical situations.