A-a Gradient Equation:
From: | To: |
The Alveolar-arterial (A-a) gradient measures the difference between alveolar oxygen concentration and arterial oxygen concentration. It helps assess the efficiency of oxygen transfer from alveoli to blood and is used to differentiate causes of hypoxemia.
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: A-a gradient is crucial for diagnosing ventilation-perfusion mismatch, diffusion defects, and right-to-left shunts. It helps differentiate between pulmonary and non-pulmonary causes of hypoxemia.
Tips: Enter FiO₂ as decimal (0.21 for room air), atmospheric pressure (typically 760 mmHg at sea level), PaCO₂ and PaO₂ from arterial blood gas analysis. All values must be valid positive numbers.
Q1: What is a normal A-a gradient?
A: Normal A-a gradient is <10 mmHg in young healthy adults, increasing with age (approximately 3 mmHg per decade).
Q2: When is A-a gradient elevated?
A: Elevated in conditions like pneumonia, pulmonary embolism, ARDS, pulmonary fibrosis, and congestive heart failure.
Q3: What does a normal A-a gradient with hypoxemia indicate?
A: Suggests hypoventilation (e.g., drug overdose, neuromuscular disorders) rather than intrinsic lung disease.
Q4: How does altitude affect A-a gradient?
A: At higher altitudes, atmospheric pressure decreases, requiring adjustment of P_atm value in the calculation.
Q5: Are there limitations to A-a gradient?
A: Less reliable with high FiO₂ (>0.6) and in patients with significant ventilation-perfusion inequality.