What a metal detector hears, 10 Hz to 1 MHz

Response of a gold nugget, an iron sphere and magnetic, viscous, slightly salty ground across frequency. Below that, the noise floor of an air-cored coil versus a fluxgate. Drag the sliders. Hover any chart for values.

The quantity plotted is the response ratio: the field returned by the object, averaged over the receive coil, divided by the transmitter's own field at the coil centre, in parts per million (ppm). In-phase (I) is the part in step with the transmit current. Quadrature (Q) is the part lagging 90°; a lossy (resistive) response is plotted as positive Q. Phase φ = atan2(Q, I), in degrees.

Book links open your saved Zotero PDF at the right page in a new browser tab. Ripka = Magnetic Sensors and Magnetometers (2001); Overton = Overton & Moreland, Inside the Metal Detector. Page numbers in the link text are the printed book pages.

Glossary: read this first
Primary field
The magnetic field made by the detector's own transmit coil, Bp (tesla, T). Read: Overton, §5 Induction, p.47 · Overton, Induction balance, p.49
Secondary field
The field that objects in the ground send back in response to the primary. This is the only thing the detector actually wants to hear. Read: Overton, Eddy currents, p.50
ppm
Parts per million: secondary field ÷ primary field at the receive coil, × 10⁶. A 1.3 g nugget whose centre is 15 cm below a 30 cm coil is roughly 0.2 ppm; the soil under it is thousands of ppm.
In-phase (I)
The part of the secondary field that rises and falls exactly in step with the transmit current. A magnetic material (pulls field in) gives positive I. A good conductor (pushes field out) gives negative I. Read: Overton, Phase demodulation (X/R channels), p.70
Quadrature (Q)
The part that lags the transmit current by a quarter cycle (90°). It comes from energy loss: resistance in eddy currents, or magnetisation that can't keep up. Plotted here as positive for lossy responses. Read: Overton, Phase demodulation, p.70
Phase φ
The angle of the response, φ = atan2(Q, I), in degrees. 0° = purely magnetic, 90° = purely lossy, 180° = perfect conductor pushing field out. Read: Overton, Ch.7 Target discrimination, p.69
Phasor
A single frequency's response drawn as an arrow from the origin to the point (I, Q). Its length is the amplitude; its angle is the phase.
Response size |M|
How big an object's response is at one frequency, regardless of phase: the length of its phasor, |M| = √(I² + Q²), in ppm. (M is the object's complex response, holding I and Q together.)
Eddy currents
Loops of current induced in a piece of metal by a changing field. The changing field (∝ frequency) drives them; the metal's resistance limits them. Read: Overton, Eddy currents, p.50
Time constant τ and corner frequency fc
τ (seconds) is how long eddy currents in an object take to die away after the field stops. For a non-magnetic sphere of radius a (m) and conductivity σ (siemens per metre, S/m), τ = μ₀σa²/π², where μ₀ = 4π×10⁻⁷ H/m. A magnetic sphere (relative permeability μr) holds its currents longer: τ = μ₀μrσa²/q², with q between π and 4.49 (see the definitions at the bottom). The corner frequency fc = 1/(2πτ) (Hz) is where the quadrature response peaks. Far below fc the object is nearly invisible. Far above it the response is flat and says nothing about the material. Read: Overton, PI target response, p.146
Magnetic susceptibility χ
How strongly a material magnetises in an applied field (dimensionless, SI units). Air is ~0, quartz sand ~10⁻⁵, iron-rich soil 10⁻³ to 10⁻², pure magnetite ~3. Read: Ripka, §1.1.2 Field and matter, p.4
Magnetite, maghemite
Magnetic iron oxide minerals. Maghemite forms when iron-rich soil weathers in hot climates, and it is what makes Australian goldfield soil "hot". Read: Overton, Mineralization effects, p.60
Laterite, ironstone, hot rock
Laterite is deeply weathered, iron-rich soil. Ironstone is a rock cemented by iron oxides. A hot rock is a lump whose magnetic response differs from the surrounding soil, so the detector beeps on it as if it were metal. Read: Overton, Mineralization effects, p.60
Superparamagnetic grains
Magnetic grains so small (about 10–30 nm) that ordinary room-temperature thermal jiggling is enough to flip their magnetisation back and forth. Each grain flips on its own characteristic timescale, its relaxation time τN (s). Read: Ripka, §1.2.2 Ferromagnetism, p.11 (one-line mention only)
VRM (viscous remanent magnetisation)
In detector usage: the soil's sluggish magnetic response from superparamagnetic grains. When the field changes, the soil's magnetisation doesn't jump to its new value. It creeps there over microseconds to seconds, because different grains relax at very different speeds. "Viscous" means lagging, like syrup. In a frequency-domain detector this shows up as χ dropping slightly as frequency rises, plus a small constant quadrature. In a pulse detector it shows up as a slow 1/t decay that mimics a target. (The term is borrowed from rock magnetism, where it strictly means magnetisation slowly acquired over geological time. Detector engineers use it for the same relaxation physics on short timescales.) Read: Overton, PI ground balance: "magnetic viscosity", 1/t, p.174 · Overton, PI for nugget hunting, p.155
FD (frequency dependence)
How much the soil's susceptibility drops per tenfold (one decade) increase in frequency, in %. A practical measure of how much VRM the soil has. Ordinary soil is ~0–2 %; soil rich in fine maghemite is ~5–15 %. Neither Zotero textbook covers frequency-dependent susceptibility of soils.
Ground conductivity σg
How well the soil carries current (S/m). Dry soil is ~0.001–0.01; salty groundwater is 1–5. Conductive ground behaves like a huge, weak conductor, so its quadrature rises steadily with frequency. Read: Overton, Multi-frequency: notching out salt, p.193
Clutter vs noise
Clutter is unwanted signal caused by the transmitter itself, here mainly soil the detector failed to cancel. It grows with transmit power exactly as the gold does, so more power never helps against it. Additive noise exists whether or not you transmit: coil thermal noise, amplifier noise, mains hum, lightning. More power or more averaging time does help against it.
Soil patchiness v and model error ε
Sweeping the coil removes the steady soil background, so only variation in the soil across a target-sized patch can mimic a target. v (%) is how much each soil ingredient varies over that distance. ε (%) is the share of that variation that follows none of the model's soil shapes. Neither is known for real goldfield soil, and your library has no numbers for them; they have to be measured.
Depth falloff (1/z⁶)
The transmit field reaching a target falls as 1/z³ with distance z (m), and the field the target sends back falls as 1/z³ again, so the signal falls as 1/z⁶ once z is larger than the coil radius R. Doubling the depth costs 64×. Detection depth for a coin-sized target is roughly the coil diameter, and for a target at depth z the best coil radius is about R ≈ z. A bigger coil sees deeper but small targets less well. Overton, Coil sensitivity, p.196–197
Ground balance
What a single-frequency detector does to ignore soil: it measures only the part of the response perpendicular to the soil's phasor. This fails when the soil's mix (and so its phase) changes from place to place. Read: Overton, VLF detector with ground exclusion balance, p.87 · Overton, PI ground balance, p.174
Probe frequency
One frequency you pick with the slider (Hz). It stands for what a classic single-frequency detector running at that frequency would see. It sets the solid "probe" line on the charts, the dots in the phasor plane, the table, the two "Single tone" boxes and the sensor ratio box. The multi-tone fit does not use it.
Tone
One transmit frequency. A multi-tone detector sends several at once and measures I and Q at each. Read: Overton, Multi-frequency design, p.193
Least-squares soil fit
Find the amounts of the three soil ingredients (χ, the VRM slope Δχ, σg) that best explain the readings at all tones. Whatever is left over (the residual) is signal the soil can't explain, which is a target. Read: Overton, Multi-frequency subtraction, p.193
Noise density (T/√Hz)
A sensor's random noise expressed as an equivalent magnetic field per square root of measurement bandwidth. For example, 10 pT/√Hz averaged over 100 Hz bandwidth gives 10 × √100 = 100 pT rms. 1 pT = 10⁻¹² T; 1 fT = 10⁻¹⁵ T. Read: Ripka, §1.4.4 Noise, p.41
Air-cored coil
A loop of wire. Its output voltage is V = ω·Nc·A·B, where ω = 2πf (rad/s), Nc is the number of turns, A the loop area (m²) and B the field (T). The output grows with frequency. Read: Ripka, §2.1 Air coils, p.48 · Ripka, §2.1.1 Voltage sensitivity, p.51 · Ripka, §2.1.2 Thermal noise, p.52
Self-resonance
The coil's own inductance L (henries, H) and stray self-capacitance Cs (farads, F) form a resonant circuit at f = 1/(2π√(LCs)). Just below it the coil gets a free boost; above it the coil stops working. Read: Ripka, §2.1.3 Parasitic capacitances, p.53 · Overton, App. A Air-cored coil calculator, p.207
Fluxgate
A sensor that drives a magnetic core in and out of saturation at the excitation frequency fexc (Hz) and reads the external field from the asymmetry. It measures B directly, down to DC, but can only follow fields slower than about fexc/10. Read: Ripka, Ch.3 Fluxgate sensors, p.75 · Ripka, Sensitivity rules, p.88 · Ripka, Tuned output, p.98
White floor, 1/f noise
White floor: noise density that is the same at all frequencies. 1/f noise: extra noise that grows at low frequencies, below the corner frequency fk (Hz). Read: Ripka, §1.4.4 Noise, p.41 · Ripka, §3.9 Fluxgate noise, p.105

In-phase I(f)

Positive means magnetic (pulls field in). Negative means eddy currents push field out. Read: Overton, Ch.7 Target discrimination, p.69

Quadrature Q(f)

A conductor peaks at its corner frequency fc. Viscous magnetic soil (VRM) gives a small constant quadrature. Salty, conductive ground rises in proportion to f. Read: Overton, PI target response, p.146 · Overton, Multi-frequency, p.193

Phase φ(f)

Ground sits near 0° at every frequency. Gold sweeps 90°→180°. Iron starts near 0° (magnetic) and only swings towards 180° far above its corner frequency; for a solid steel sphere that is above 1 MHz. Read: Overton, Table of target phase angles, p.70

Phasor plane at the probe frequency

Loci traced as f sweeps 10 Hz → 1 MHz, each normalised to its own largest magnitude. Dots mark the probe frequency. The three soil arrows show how the ground phasor moves when soil content changes. Read: Overton, Mineralization effects, p.60

Can a multi-frequency detector subtract the soil without subtracting the gold?

The problem. Over a nugget the detector measures soil + gold. The soil part is thousands of times bigger, and how much soil there is (and of which kind) changes from spot to spot, so it can't be measured once and subtracted forever. It has to be estimated from the same measurement that contains the gold. The danger is that the estimate absorbs the gold too: if some mix of soil could produce exactly the gold's signal, the detector subtracts it as soil and the nugget vanishes.

What this panel simulates.

  1. The detector transmits N tones (frequencies) spread evenly on a log scale across the shaded band, and measures I and Q at each: 2N numbers per spot.
  2. It models the soil as a mix of three known shapes: magnetic (χ, flat in-phase), viscous VRM (Δχ, sloping in-phase + flat quadrature), and salt (σg, quadrature rising with f). See the glossary. Two assumptions are compared. Mix known: the proportions of the three are known (from ground-balancing somewhere nearby) and only the total amount of soil under the coil is unknown, so there is 1 unknown. This is what a classic ground balance assumes. Mix unknown: all three amounts are free, so there are 3 unknowns. This is the honest case on patchy goldfield soil and hot rocks.
  3. It finds the soil amounts that best explain the 2N numbers (a least-squares fit) and subtracts that soil estimate.
  4. What remains is the residual: the part of the gold's signal that no mix of soil could imitate. That is all the detector can still see.

For the dots, the soil is assumed to follow the three shapes exactly and there is no noise, so only the gold needs to be fed through the fit: the dots show what of the gold survives the soil subtraction. The table below then adds back what this hides: the soil's departure from the model (clutter) and sensor noise.

How to read the chart. Orange lines: the gold's true in-phase (solid) and quadrature (dashed) response, scaled so gold's peak size is 1. Shaded band: where the tones are; the probe tone is added to them. Black dots: what is left at each tone after subtracting the fitted soil, under the assumption picked with the buttons (filled = in-phase, hollow = quadrature). Dots sitting on the orange lines would mean nothing was lost. Dots at zero mean the nugget is invisible.

Read: Overton, Multi-frequency design, p.193 · Overton, PI ground balance, p.174

The comparison table. Each cell is a ratio: the gold signal left after the soil fit, divided by whatever is left that could be mistaken for gold. Two things can be left:

  • Soil clutter: the detector sweeps and subtracts the running background ("motion mode", Overton p.92), so uniform soil cancels however badly it is modelled. What can hide a nugget is how the soil varies across a target-sized patch, set by "Soil patchiness v". The fit removes whatever part of that variation it can describe with its soil shapes. With the mix known, only a change in the amount of the same soil is removable, and any change in the mix leaks through. A further fraction ε of the variation follows no model shape at all. The detector compares what is left against the expected gold shape (a matched filter), so only clutter that resembles gold counts. The mix leak has a known shape and its resemblance is computed exactly. The unmodelled part ε has an unknown shape: by default it is treated as random, which over 2N measurements resembles gold by about 1/√(2N). The toggle switches to the worst case, where it is shaped exactly like gold. All of this is a response to the transmitter, like the gold, so transmit power cancels out of signal-to-clutter.
  • Additive noise: coil and amplifier noise from the sensor panel, averaged over the dwell time T. This does not scale with the transmitter, so more ampere-turns help here. Total transmit power is fixed and shared across the tones. Interference (mains, lightning, VLF stations) is also additive but is not modelled.

The big number combines both, 1/√(1/SCR² + 1/SNR²). The line underneath says which one limits. With the default settings soil clutter is the limit by a wide margin, so detection barely depends on power. In deep-target cases noise can take over: try a 0.5 m target with a small coil. Read down a column to compare one tone with many under the same soil assumption, and across a row to see what not knowing the soil mix costs.

gold in-phase (true) gold quadrature (true) in-phase left after soil subtraction quadrature left after soil subtraction

Things to try.

  • Number of tones = 1. Nothing survives. One tone gives 2 numbers (I and Q) but the soil has 3 unknown amounts, so some soil mix can always match the reading exactly. A single-frequency detector can't tell gold from a change in the soil without extra assumptions.
  • Shrink the nugget until its corner fc is above the band. Inside the band its quadrature then rises with frequency, just like salt, and it gets absorbed.
  • Grow the nugget until fc is below the band. It then looks like flat negative in-phase, the same as slightly less magnetic soil, and it gets absorbed.
  • Conclusion: gold survives when the band brackets its fc, because only there does it show its peak, which no soil shape has. Wider bands keep more sizes of nugget visible.

Why "mix known" is a trap. With the mix known, even one tone keeps most of the gold. But that rests on the soil's proportions being exactly right under the coil. The last box above shows how small an error in the soil's phase produces a fake signal as large as the nugget. On the defaults it's a few hundredths of a degree. Real soil varies far more than that from spot to spot, which is why single-frequency detectors chatter on mineralised ground. In the "mix unknown" column one tone gives nothing (2 numbers can't pin down 3 unknowns), while many tones still recover the gold, without needing the soil to stay the same.

Why adding tones stops helping. The clutter and the gold are both measured on the same tones, so adding tones grows both together. Signal-to-clutter depends only on shapes: how unlike any soil mix the gold looks across the band (the "share" box), and how big the soil error is. Extra tones help only until the band brackets the gold's corner frequency and the soil shapes are pinned down; after that the limit is ε.

Sensor noise floor: field-equivalent noise Bn(f)

Lower is better. A coil's output is V = ω·N·A·B, so its noise referred to field falls as 1/f until the coil's self-resonance, then rises steeply. A fluxgate measures B directly with a flat floor down to near DC, but its bandwidth is borrowed from its excitation (≈ fexc/10). Read: Ripka, §2.1.1 Coil sensitivity, p.51 · Ripka, §2.1.3 Coil parasitic capacitance, p.53 · Ripka, §3.9 Fluxgate noise, p.105 · Ripka, §10.3.1 UXO, p.380

air-cored coil (same radius as the search coil) fluxgate published air coil published cored induction coils published best fluxgates

Where the comparison comes from. The dots are published measurements; the lines are this page's model. Air coil: the MEDA ACM-1 (45 cm diameter, voltage noise 0.32 pT/√Hz at 20 Hz and 0.1 pT/√Hz at 100 Hz). Ripka Table 2.2, p.66 · p.48. Ferromagnetic-cored induction coils: 10–20 fT/√Hz at 1 kHz, 4 fT/√Hz at 10 kHz, 2 fT/√Hz at 50 kHz. Table 2.2, p.66 · Fig. 2.10, p.65. Best fluxgates: 4.2 pT/√Hz at 1 Hz (17 mm amorphous ring core) and 8–11 pT rms below 10 Hz. Ripka §3.4, p.89–90. Ripka's own summary is that fluxgates win at ultralow frequency or where size is limited. p.65.

Limits of this evidence. No source here gives fluxgate noise above about 10 Hz, so the flat fluxgate floor out to fexc/10 is an assumption, and probably a generous one. The published coils are optimised instruments, mostly with ferromagnetic cores, not detector search coils. Read the gap as "hundreds to a thousand times at kHz", not as the model's exact ratio. Also, in a detector neither floor is the limit: ground and interference are thousands of times larger. In your own bench test at 8.5 kHz the coil's SNR (signal-to-noise ratio) was only 20× better, because interference, not sensor noise, set the floor.

Table at the probe frequency

Model and variable definitions
f: frequency (Hz). ω = 2πf: angular frequency (rad/s). μ₀ = 4π×10⁻⁷ H/m: permeability of free space.
Sphere response M(ω) (dimensionless), from Wait's (1951) conducting, permeable sphere: M = ½·[2μr(T−α) + (α²T − α + T)] / [μr(T−α) − (α²T − α + T)], with α = a·√(iωμ₀μrσ) and T = tanh α. Limits: M → (μr−1)/(μr+2) at low f and −½ at high f.
a: sphere radius (m). σ: conductivity (S/m). μr: relative permeability (dimensionless, 1 for gold).
τ = μ₀μrσa²/q²: fundamental eddy-current decay time constant (s) of a sphere, where q solves tan q = (μr−1)q/(μr−1+q²): q = π for non-magnetic metal (gold), rising to 4.49 for μr ≫ 1. fc = 1/(2πτ): corner frequency (Hz).
R: search-coil radius (m). h: coil height above ground (m). d: target depth below the surface (m). Response ratio: the secondary field averaged over the receive-loop area, divided by the primary field at the loop centre Bp = μ₀NI/(2R), where NI is transmit ampere-turns (A). For a sphere on the axis at distance z = h + d: ratio = 2·M·(a/R)³·[1+(z/R)²]⁻³. This is exact for a small sphere (a ≪ z) under a single coincident transmit/receive loop; real detectors use separate, often double-D, coils.
χ: soil volume magnetic susceptibility at 1 kHz (SI, dimensionless). FD: frequency dependence, the fractional drop in χ per decade of f (%). Δχ = χ·FD/ln 10: drop per natural-log unit.
VRM soil (log-uniform relaxation times): χ′(f) = χ − Δχ·ln(f/1 kHz), χ″ = (π/2)·Δχ (constant). Valid while the band sits well inside the grains' range of relaxation times. Magnetic ground: a uniform permeable half-space acts exactly (quasi-statically) like an image of the coil at distance 2h with strength χ/(2+χ), so ratio = χ/(2+χ)·M12(2h)·2/(μ₀πR), where M12(2h) is the mutual inductance (H) of two coaxial loops of radius R a distance 2h apart (Maxwell's elliptic-integral formula). Real ground is layered and lumpy.
σg: ground conductivity (S/m); salt water is ~1–5 S/m. Conductive ground, to first order in σg: the coil's vector potential Aφ drives ring currents J = −iωσgAφ in the ground, and their flux back through the coil gives Q = ωσg·Ksalt, with Ksalt = 2/(μ₀πR)·∬M12(R,ρ,h−z)²/(2πρ) dρ dz over the ground, integrated numerically (checked to ~1.5%). Valid while the skin depth δ = √(2/(ωμ₀σg)) (m) is much larger than R + h.
Nc: coil turns. dw = 0.4 mm: wire diameter. Rdc = Nc·2πR·ρCu/(π dw²/4) (Ω), with ρCu = 1.72×10⁻⁸ Ω·m. L ≈ μ₀Nc²R[ln(8R/rb)−2] (H), with bundle radius rb = (dw/2)√Nc. Cs: self-capacitance (F).
Coil noise: Bn = √(en² + (in|Z|)² + 4kBTKRac|H|²) / (ω·Nc·πR²·|H|) (T/√Hz). H = 1/(1 − ω²LCs + iωRacCs) is the self-resonance transfer function and Z = (Rac + iωL)·H the coil impedance seen by the amplifier (Ω). en is amplifier voltage noise (V/√Hz) and in amplifier current noise (A/√Hz). kB = 1.38×10⁻²³ J/K, TK = 300 K. Rac is Rdc raised by skin effect in the wire; proximity effect between turns, which makes real multilayer coils worse at high frequency, is ignored.
Fluxgate noise: Bn = Bw·√(1 + fk/f)·√(1 + (f/fbw)⁴), where Bw is the white floor (T/√Hz), fk the 1/f corner (Hz) and fbw = fexc/10 the usable bandwidth (Hz) for excitation frequency fexc (Hz).
Signal-to-clutter SCR = |rgold| / C, where rgold is the gold signal left after the soil fit, r̂ = rgold/|rgold|, and C the clutter seen by a matched filter: C² = Σk(r̂·fit residual of v·Sk)² + (ε·o)²·Σk|v·Sk|², with overlap o = 1/√(2N) for a random-shaped error ("typical") or 1 with the residuals' full size ("worst case"). Here Sk is the k-th soil ingredient (magnetic, VRM, salt) on the same tones, v the patchiness and ε the model error. This assumes motion filtering has removed the uniform background. Signal-to-noise SNR: the same residual against coil noise averaged over dwell time T, with total transmit power shared across tones. Combined: 1/√(1/SCR² + 1/SNR²).
Models are idealised: spheres on the coil axis, a uniform half-space, no interaction between target and soil, no interference. Real nuggets are irregular, so treat fc as ±3×.