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Phase Cycling and Gradient Pulses - The James Keeler Group

Phase Cycling and Gradient Pulses - The James Keeler Group

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magnetization from z onto –y, whereas the same pulse applied about the y-axis<br />

rotates the magnetization onto the x-axis. <strong>The</strong> idea of the receiver phase is<br />

slightly more complex <strong>and</strong> will be explored in this section.<br />

<strong>The</strong> NMR signal – that is the free induction decay – which emerges from the<br />

probe is a radiofrequency signal oscillating at close to the Larmor frequency<br />

(usually hundreds of MHz). Within the spectrometer this signal is shifted down<br />

to a much lower frequency in order that it can be digitized <strong>and</strong> then stored in<br />

computer memory. <strong>The</strong> details of this down-shifting process can be quite<br />

complex, but the overall result is simply that a fixed frequency, called the<br />

receiver reference or carrier, is subtracted from the frequency of the incoming<br />

NMR signal. Frequently, this receiver reference frequency is the same as the<br />

transmitter frequency used to generate the pulses applied to the observed<br />

nucleus. We shall assume that this is the case from now on.<br />

<strong>The</strong> rotating frame which we use to visualise the effect of pulses is set at the<br />

transmitter frequency, ω rf<br />

, so that the field due to the radiofrequency pulse is<br />

static. In this frame, a spin whose Larmor frequency is ω 0<br />

precesses at (ω 0<br />

–<br />

ω rf<br />

), called the offset Ω. In the spectrometer the incoming signal at ω 0<br />

is downshifted<br />

by subtracting the receiver reference which, as we have already decided,<br />

will be equal to the frequency of the radiofrequency pulses. So, in effect, the<br />

frequencies of the signals which are digitized in the spectrometer are the offset<br />

frequencies at which the spins evolve in the rotating frame. Often this whole<br />

process is summarised by saying that the "signal is detected in the rotating<br />

frame".<br />

9.2.1 Detector phase<br />

<strong>The</strong> quantity which is actually detected in an NMR experiment is the transverse<br />

magnetization. Ultimately, this appears at the probe as an oscillating voltage,<br />

which we will write as<br />

S = cosω FID 0t<br />

where ω 0<br />

is the Larmor frequency. <strong>The</strong> down-shifting process in the<br />

spectrometer is achieved by an electronic device called a mixer; this effectively<br />

multiplies the incoming signal by a locally generated reference signal, S ref<br />

,<br />

which we will assume is oscillating at ω rf<br />

Sref<br />

= cosω<br />

rft<br />

<strong>The</strong> output of the mixer is the product S FID<br />

S ref<br />

S S = Acosω<br />

tcosω<br />

t<br />

9–2<br />

FID ref rf 0<br />

1<br />

=<br />

2<br />

A[ cos( ωrf<br />

+ ω0) t + cos( ωrf<br />

−ω0)<br />

t]<br />

<strong>The</strong> first term is an oscillation at a high frequency (of the order of twice the<br />

Larmor frequency as ω 0<br />

≈ ω rf<br />

) <strong>and</strong> is easily removed by a low-pass filter. <strong>The</strong><br />

second term is an oscillation at the offset frequency, Ω. This is in line with the<br />

previous comment that this down-shifting process is equivalent to detecting the<br />

precession in the rotating frame.

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