“…An equivalent current J eq in air that generates an identical magnetic field in the coil of the receiving EMAT to what is generated by the current sheet, J ed, at depth z 0 , is assumed and is given by, Considering the magnetic source of size of w 0 wide and l 0 long with its centre at the origin of the coordinate system, the static magnetic field B 0 is mainly limited to this area. The magnetic field, B, at point (x, y, z) produced by the current sheet element due to the particle vibration within the area between -w 0 /2 to +w 0 /2 in x-axis and -l 0 /2 to +l 0 /2 in y-axis, where B 0 has significant amplitude, is given by 10) where r is the distance between the eddy current element and the field point .…”