Calculation record

Leading translation response of a scalar core in the same-field background.

The coefficient calculated here multiplies g*D. It is the first correction
in inverse ambient density at fixed omega_0=g*b and fixed target grade.
The background is kept in its original frame. This is a conditional
effective-action calculation, not full nonlinear particle stability.

Research context

Interpret numerical checks within the assumptions and limitations documented in these notes.