A transverse ensemble induces a voltage
A Lorentzian distribution of static offsets has an exponential characteristic function. This special distribution gives additive decay rates. The complex amplitude is unknown to the estimator.
NUCLEAR INDUCTION / FREQUENCY
Tip an ensemble with a radio-frequency pulse. Retain both quadratures of the induced voltage, transform those records into a spectrum, and estimate the signed frequency offset and effective transverse decay.
Vertical static field; horizontal transmit/receive coil. A switch isolates the receiver during the pulse, then routes the induced voltage to a phase-referenced quadrature receiver. Cable motion is schematic.
PULSE SEQUENCE / AVERAGED RECEIVER VOLTAGES
One fully reset acquisition contains 256 complex samples, every 0.4 milliseconds after a 0.4-millisecond dead time. Repeats are averaged sample by sample. The receiver resolves the slow beat against the RF reference, not the fast carrier.
Ready. Predict, then acquire.
RAW VOLTAGE RECORD / SEPARATE SOURCE EXPECTATION
Teal: in-phase voltage. Gold: quadrature voltage. Dots: retained observations. Thin lines: source expectations. Purple dashes: fit using records only. Gray: saved observations.
FINITE-WINDOW TRANSFORM OF THE RECORD
A uniformly spaced record is needed. Rectangular window, no zero filling. Magnitude and finite-window width are not a fitted absorption line or an independent relaxation measurement.
INFERENCE / SOURCE PARAMETERS EXCLUDED
Inferred effective transverse time
Inferred signed frequency offset
Inferred initial voltage magnitude
Retained complex samples
Voltage residual RMS
Global bounded search with profiled amplitude. Weak-information and boundary checks are diagnostic heuristics, not parameter confidence intervals. A synthetic recovery does not independently establish the physical law.
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SAVED COMPARISON / MODEL BOUNDARY
Single noninteracting resonance; no molecular chemical shifts, coupling multiplets, diffusion, radiation damping, coil loading or realistic pulse bandwidth. Gain and phase are calibrated; no drift or digitizer quantization. Instantaneous hard-pulse approximation; the Cauchy static-offset model is not a computed field map.
Physics tutorial
BackgroundTip an ensemble with a radio-frequency pulse. Retain both quadratures of the induced voltage, transform those records into a spectrum, and estimate the signed frequency offset and effective transverse decay.
Why it mattersA constant is inferred through a calibrated response and retained observations.
Start with the essentials
A Lorentzian distribution of static offsets has an exponential characteristic function. This special distribution gives additive decay rates. The complex amplitude is unknown to the estimator.
The displayed spectrum uses the actual finite, uniformly sampled record with a rectangular window. Its nonnegative magnitude loses phase; the signed frequency axis retains rotation direction. Partial records have coarser bins.
Profile out the complex amplitude at every candidate frequency and time. The source decay, broadening, phase and flip angle never enter this fit.
Typical misconceptionRecovering a source parameter independently confirms the law.
Better mental modelThese synthetic records test a measurement and inference workflow. They are not historical observations, a parameter confidence interval, or external scientific certification.
Acquire the reference pulse and inspect both raw voltage channels and the finite-window spectrum.
What to observe: The spectrum appears only after retaining a uniform record. It is not a separately drawn ideal line.Save the record, then broaden the field without changing the intrinsic source time.
What to observe: The effective time shortens. A single free decay cannot identify which process caused its width.Choose the negative-frequency preset, then remove transverse preparation.
What to observe: Complex sampling distinguishes frequency signs. With no coherent signal, the weak-information rule withholds the estimate.