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 useful index for evaluating the efficiency of oxygen transfer from alveoli to blood and helps differentiate causes of hypoxemia.
The calculator uses the A-a Gradient equation:
Where:
Explanation: The equation calculates the alveolar oxygen partial pressure using the alveolar gas equation, then subtracts the measured arterial oxygen partial pressure to determine the gradient.
Details: A-a gradient helps differentiate between ventilation-perfusion mismatch/diffusion defects (increased gradient) and hypoventilation (normal gradient). It's crucial for diagnosing pulmonary diseases and assessing gas exchange efficiency.
Tips: Enter FiO2 as fraction (0.21 for room air, 1.0 for 100% oxygen), use standard values for P_atm (760 mmHg) and P_H2O (47 mmHg) unless at altitude or different conditions. All values must be valid and positive.
Q1: What is a normal A-a gradient?
A: Normal is <10-15 mmHg on room air for young adults, increasing with age (approximately 2.5 + 0.25 × age).
Q2: When is A-a gradient increased?
A: Increased in conditions like pneumonia, pulmonary embolism, ARDS, fibrosis, and other causes of V/Q mismatch or diffusion impairment.
Q3: Why divide PaCO2 by 0.8?
A: This represents the respiratory quotient (R), typically 0.8, which accounts for the relationship between oxygen consumption and carbon dioxide production.
Q4: How does altitude affect A-a gradient?
A: At altitude, P_atm decreases, which affects alveolar oxygen pressure calculation. Adjust P_atm accordingly for accurate results.
Q5: What are limitations of A-a gradient?
A: Affected by FiO2 (less reliable at high FiO2), assumes steady state, and doesn't account for mixed venous oxygen content or shunt fraction.