Beam steering in a transverse field
For q = +1.6 microC, v = (3,4,0) km/s, and B = (0,0,250) mT, the force is (0.0016,-0.0012,0) N with magnitude 0.002 N.
Physics and electromagnetism
Solve all three components of the magnetic Lorentz force from signed charge, velocity, and magnetic-field vectors with SI conversions and orthogonality checks.
Three-dimensional Lorentz force
Enter velocity and magnetic-field components in one right-handed Cartesian frame. The calculator evaluates the cross product before applying the signed charge, exposing direction reversals that a scalar |q|vB sin(theta) calculation cannot show.
Current model evidence
Use component signs for direction and the norm for magnitude; preserve the same coordinate frame for v and B.

| Vector stage | Displayed input | Conversion / rule | Current value | Scope / unit |
|---|
DETAILED CALCULATION PROCESS
F = q(v x B); Fx = q(vy Bz - vz By), Fy = q(vz Bx - vx Bz), Fz = q(vx By - vy Bx)
Normalize microcoulombs, kilometres per second, and millitesla to SI units; compute v x B in a right-handed basis; multiply every component by the signed charge; then verify F dot v and F dot B.
| Symbol | Meaning | Unit | Default basis |
|---|---|---|---|
| q | Signed particle charge | C | +1.6 microC |
| v | Particle velocity vector | m/s | (3, 4, 0) km/s |
| B | Magnetic flux-density vector | T | (0, 0, 250) mT |
| F | Magnetic Lorentz-force vector | N | Solved |
| theta | Smaller angle between v and B | deg | Derived |
| dot | Scalar product used for orthogonality | mixed | F dot v and F dot B |
HOW TO USE THIS CALCULATOR
ELECTROMAGNETIC FOUNDATIONS
DEEP ANALYSIS 1
Each component depends on a different pair of velocity and field components. A single angle loses the directional information needed for steering, detector placement, or sign diagnosis.
DEEP ANALYSIS 2
The computed force must be perpendicular to both v and B. Dot products test this property without repeating the original component formulas.
DEEP ANALYSIS 3
q = 0, v = 0, B = 0, and v parallel to B all return zero, but they represent different experimental states and should not be conflated.
RESULT INTERPRETATION
A positive Fx, Fy, or Fz points along the positive coordinate axis selected by the user; the page cannot infer a physical compass direction without that frame definition.
The result is instantaneous. A particle trajectory also needs mass, initial position, electric fields, and time integration.
REAL USE CASES
For q = +1.6 microC, v = (3,4,0) km/s, and B = (0,0,250) mT, the force is (0.0016,-0.0012,0) N with magnitude 0.002 N.
Keeping v and B fixed while changing q from positive to negative reverses all force components. That sign change distinguishes carrier polarity without altering |F|.
EVIDENCE AND DATA QUALITY
Retain the axis drawing, sensor sign conventions, calibration records, charge state, component inputs before unit conversion, timestamp, and exported dot-product checks. A magnitude-only record cannot reconstruct force direction.
LIMITS AND EXCLUSIONS
TERMS USED HERE
RELIABLE SOURCES
FREQUENTLY ASKED QUESTIONS
The signed charge determines whether the magnetic force follows or opposes v x B.
Yes. A stationary charge has zero magnetic force, although an electric field could still accelerate it.
The sine of the angle between v and B is zero, so their cross product vanishes.
It should be zero within floating-point roundoff; the exported value exposes any small residual.
Convert first: 1 gauss = 0.1 mT. This page accepts mT components.
No. Radius requires particle mass and the perpendicular speed; use the energy page for that model.
IMPORTANT BOUNDARY
This classical instantaneous-force calculation is not a charged-particle trajectory, magnet safety assessment, accelerator design certification, or relativistic analysis.