Magnetic Field Equation:
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The World Magnetic Field equation calculates magnetic flux density (B) from the permeability of free space (μ₀), magnetic field strength (H), and magnetization (M). This fundamental equation describes how magnetic fields behave in different materials and environments.
The calculator uses the magnetic field equation:
Where:
Explanation: The equation shows how the total magnetic field depends on both the applied field (H) and the material's response (M), scaled by the fundamental constant μ₀.
Details: Accurate magnetic field calculations are essential for designing electrical devices, studying geophysical phenomena, and developing magnetic materials for various applications.
Tips: Enter μ₀ in H/m (default value provided), H and M in A/m. All values must be valid (μ₀ > 0, H ≥ 0, M ≥ 0).
Q1: What is the typical value of μ₀?
A: The permeability of free space is approximately 1.256637×10⁻⁶ H/m (or 4π×10⁻⁷ N/A²).
Q2: How does magnetization (M) affect the result?
A: Magnetization represents how a material responds to an applied field. In vacuum (M=0), B depends only on H and μ₀.
Q3: What are typical units for magnetic field strength?
A: H is commonly measured in amperes per meter (A/m) or oersteds (Oe), where 1 Oe ≈ 79.577 A/m.
Q4: What's the difference between B and H?
A: H is the applied magnetic field, while B is the total magnetic flux density including the material's response.
Q5: When is this equation most applicable?
A: This linear relationship works well for many materials, though ferromagnetic materials may show nonlinear behavior at high fields.