Magnetic Resonance Imaging

Phase Encoding

Consider a measured signal consisting of the sum of two unknown sinusoidal signals: S_1(t)=s_{11}(t)+s_{21}(t), where S_1(t)=A_1\sin (\omega t+\theta) and s_{11}(t)=a_{11}\sin (\omega t +\theta) and s_{21}(t)=a_{21}\sin(\omega t+\theta).  This received signal is measured at t_1.  Since s_{11} and s_{21} are both sinusoidal signals with the same frequency, we can combine them both and conclude that

A_1=a_{11}+a_{21}.

Next, we apply a gradient along the y direction.  This has the effect of modifying the frequency of precession of nuclei based on the location of their y-coordinate.  Let’s assume that the gradient field is linear and can be modeled as

B_y=my.

When the gradient is turned on, the signals are now

If the gradient is turned on for a duration of t=\Delta t, and then turned off, subsequently, then the signals will have experienced an increase in phase given by