Why the signal fades faster than T2
Suppose the field in a small region of the sample exceeds by . In the frame turning at the magnetization there drifts round at and after a time has gained a phase . The coil measures the vector sum of the transverse magnetization of all regions, and the more the phases spread, the smaller the sum.
When Bloch defined he already put “small and irregular inhomogeneities” of the static field together with the action of neighbouring nuclei, as one effective field irregularity. Today the two are kept apart: the irreversible decay caused by fluctuating fields is still called , the extra decay from the static field spread is , and the total decay we observe is .
If the static frequency offsets follow a Lorentzian distribution, their average is exactly an exponential and the two decay rates add. The nuclear induction experiment is set up this way, which is why its fitted effective decay cannot tell the two apart.
A 180° pulse turns the phases round
At apply a 180° pulse. It flips every transverse magnetization about a transverse axis, so every phase changes sign: a spin ahead is now behind. After the pulse each region keeps turning at its old rate, because its field has not changed.
At every region therefore has phase . All arrows line up again and the signal reappears: the spin echo, with echo time . The static unevenness cancels completely and only the decay remains.
Hrabe and co-workers sketch the history in their introduction: Hahn noticed as early as 1950 that self-diffusion weakens spin echoes, and Carr and Purcell then used many echoes to reduce the effect. The ISMRM diffusion problem set treats the two same-sign gradients on either side of the 180° pulse as one dephasing vector that grows during the first pulse and returns to zero during the second, which is the phase flip in another form.
Source: J. Hrabe · F. Szczepankiewicz and J. Hutter · F. Bloch
What the echo cannot recover: motion
The derivation relies on each region keeping its field. A water molecule that sits in different places during the two halves feels different fields, and its phases do not cancel. Many molecules each keep a random leftover phase, and the echo weakens.
Hrabe and co-workers point out that uneven magnetic susceptibility creates local gradients that act like unknown weak diffusion gradients. A spin echo reduces this weighting, and the more echoes, the smaller the b-value these local gradients contribute. Chapter 7 turns the weakness round: it applies a known, strong pair of gradients on purpose and uses the lost echo to measure how far molecules travel.
Source: J. Hrabe · F. Szczepankiewicz and J. Hutter
Worked example: the same echo time read two ways
Problem: a tissue has and a static field spread with (both values assumed for the calculation). Read the signal 50 ms after excitation in two ways: by simply waiting, and with a 180° pulse at 25 ms.
First the total decay: , so . Waiting leaves of the signal; the spin echo leaves , 3.49 times as much.
How small is this unevenness? The Lorentzian half width is , which corresponds to , or 0.031 ppm of 3 T. A field difference of a few parts in a hundred million wipes out most of the signal within tens of milliseconds.
Now one pair of spins, one 4 Hz faster than the other. At 25 ms they differ by , or 36°. The 180° pulse turns the difference into −36°, the faster spin keeps catching up, and at 50 ms the difference is exactly zero again.