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Free induction decay
Free induction decay
from Wikipedia
Free induction decay (FID) nuclear magnetic resonance signal seen from a well shimmed sample

In Fourier transform nuclear magnetic resonance spectroscopy, free induction decay (FID) is the observable nuclear magnetic resonance (NMR) signal generated by non-equilibrium nuclear spin magnetization precessing about the magnetic field (conventionally along z). This non-equilibrium magnetization can be created generally by applying a pulse of radio-frequency close to the Larmor frequency of the nuclear spins.

If the magnetization vector has a non-zero component in the XY plane, then the precessing magnetisation will induce a corresponding oscillating voltage in a detection coil surrounding the sample.[1] This time-domain signal (a sinusoid) is typically digitised and then Fourier transformed in order to obtain a frequency spectrum of the NMR signal i.e. the NMR spectrum.[2]

The duration of the NMR signal is ultimately limited by T2 relaxation, but mutual interference of the different NMR frequencies present also causes the signal to be damped more quickly. When NMR frequencies are well-resolved, as is typically the case in the NMR of samples in solution, the overall decay of the FID is relaxation-limited and the FID is approximately exponential (with the time constant T2 changed, indicated by T2*).[citation needed] FID durations will then be of the order of seconds for nuclei such as 1H.

Particularly if a limited number of frequency components are present, the FID may be analysed directly for quantitative determinations of physical properties, such as hydrogen content in aviation fuel, solid and liquid ratio in dairy products (time-domain NMR).[3]

Advances in the development of quantum-scale sensors, particularly NV centres, have enabled the observation of the FID of single nuclei.[4] When measuring the precession of a single nucleus, quantum mechanical measurement back action has to be considered. In this special case, also the measurement itself contributes to the decay as predicted by quantum mechanics.

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from Grokipedia
Free induction decay (FID) is the time-domain (NMR) signal generated by the and of transverse in a sample following the application of a radiofrequency (RF) in a . This decaying oscillatory signal, induced in a detection coil, captures the from excited nuclear spins relaxing toward equilibrium. In NMR spectroscopy and (MRI), FID is produced by a short, intense RF pulse—typically 90°—that tips the net magnetization from the longitudinal axis into the , where it precesses at the Larmor frequency specific to each nucleus. The pulse excites all resonant nuclei simultaneously, enabling efficient compared to older continuous-wave methods. As the spins dephase due to interactions like spin-spin relaxation (T₂) and magnetic field inhomogeneities (contributing to T₂*), the FID manifests as an exponentially decaying . The importance of FID lies in its role as the primary observable in pulsed NMR, where multiple FIDs are often averaged to enhance sensitivity, particularly for low-abundance nuclei like ¹³C. Subsequent Fourier transformation converts the time-domain FID into a frequency-domain , revealing chemical shifts, coupling constants, and other structural information essential for molecular analysis. In MRI, FID forms the basis for basic sequences, though it is often modified with gradients or refocusing pulses to mitigate rapid decay and encode spatial information.

NMR Fundamentals

Spin magnetization

Nuclear spins are intrinsic quantum mechanical properties of atomic nuclei, arising from the combined angular momenta of protons and neutrons within the nucleus. For nuclei, such as the proton (^1H), the I\mathbf{I} has eigenvalues corresponding to projections mI=±1/2m_I = \pm 1/2 along a quantization axis, with magnitude I(I+1)=3/4\sqrt{I(I+1)}\hbar = \sqrt{3/4}\hbar
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