A-a Gradient Equation:
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The Alveolar-arterial (A-a) oxygen gradient measures the difference between alveolar oxygen partial pressure (PAO₂) and arterial oxygen partial pressure (PaO₂). It assesses the efficiency of gas exchange in the lungs and helps differentiate causes of hypoxemia.
The calculator uses the A-a gradient equation:
Where:
Explanation: The equation calculates the theoretical alveolar oxygen pressure and compares it to measured arterial oxygen to assess gas exchange efficiency.
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 arterial blood gas values including PaO₂, FiO₂, and PaCO₂. Use standard values for atmospheric pressure (760 mmHg), water vapor pressure (47 mmHg), and respiratory quotient (0.8) unless specific conditions apply.
Q1: What is a normal A-a gradient?
A: Normal is <10 mmHg in young adults breathing room air, increasing with age (approximately [age/4] + 4).
Q2: When is the A-a gradient increased?
A: Increased in conditions like pulmonary embolism, pneumonia, ARDS, pulmonary edema, and interstitial lung disease.
Q3: Why is RQ typically 0.8?
A: 0.8 represents the average respiratory quotient for a mixed diet where carbohydrates, fats, and proteins are metabolized.
Q4: How does altitude affect the calculation?
A: At higher altitudes, atmospheric pressure decreases, requiring adjustment of P_atm value in the calculation.
Q5: What are the limitations of A-a gradient?
A: Less reliable at high FiO₂ levels and in patients with significant ventilation-perfusion inequality. Does not differentiate between different causes of impaired gas exchange.