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A Hall measurement drives a longitudinal current and records a transverse voltage while an axial magnetic field, magnetization, or another time-reversal-odd variable is controlled. The raw voltage is not yet a Hall coefficient. It can contain thermoelectric offset, longitudinal pickup from contact misalignment, inductive voltage, contact asymmetry, field history, nonlinear response, and several parallel conduction channels.

The central task is to separate a transverse response from offsets, then decide what physical model can explain it. Record both current polarities and both field directions, together with the preparation of any magnetic state. A carrier density follows only after geometry, linear response, and the relevant carrier model have been checked.

Required background. Transport Measurements supplies terminal labeling, contact geometry and linear-response checks. Hall Effect supplies the signed transverse response and the assumptions behind carrier-density inference. Conventions for Quantum Matter fixes charge, field orientation and conductivity-tensor conventions.

Fix a right-handed (x,y,z)(x,y,z) frame before connecting the voltmeter:

  • conventional current I>0I>0 flows along +x^+\hat{\mathbf x};
  • magnetic induction B=Bzz^\mathbf B=B_z\hat{\mathbf z};
  • the transverse voltage is Vy=Vbottom−VtopV_y=V_{\mathrm{bottom}}-V_{\mathrm{top}}, with the top edge at larger yy;
  • the longitudinal voltage is Vx=Vupstream−VdownstreamV_x=V_{\mathrm{upstream}}-V_{\mathrm{downstream}} under a declared lead order;
  • Ryx=Vy/IR_{yx}=V_y/I and Rxx=Vx/IR_{xx}=V_x/I are terminal resistances;
  • the magnetic field coordinate is BB, not an unlabeled mixture of BB and applied HH.

For labeled contacts, Vab=Va−VbV_{ab}=V_a-V_b. Since E=−∇V\mathbf E=-\nabla V, a uniform transverse field gives Vy=wEyV_y=wE_y. These conventions make the sign of a weak one-carrier Hall slope match the signed carrier charge: negative for electrons and positive for holes. Swapping the voltage leads changes the raw voltage sign. Reversing the physical current changes both the linear-response voltage and the signed current, so their ratio is unchanged. A sign error occurs if one polarity changes without updating its definition. Check the complete wiring and field direction, preferably with a known reference sample.

An ideal Hall bar has a long uniform channel, current contacts spanning the ends, narrow voltage arms, and paired transverse probes at the same longitudinal coordinate. The longitudinal pair samples the potential gradient along the bar; the transverse pair samples the cross-channel potential difference.

Six-terminal Hall bar with labeled voltage polarity and a displaced lower transverse probe

Current enters contact 1 and leaves contact 6. The longitudinal reading is V23=V2−V3V_{23}=V_2-V_3; the transverse reading is V52=V5−V2V_{52}=V_5-V_2. With uniform fields, the displacement shown gives V52=wEy−ΔxExV_{52}=wE_y-\Delta x E_x: the lower probe also samples the longitudinal voltage gradient. The ideal Hall pair has Δx=0\Delta x=0. Voltage probes draw negligible current, and Bz>0B_z>0 points out of the page.

For a homogeneous three-dimensional bar of thickness tt with uniform current density,

ρyx=t Ryx,ρxx=RxxwtL.\rho_{yx} = t\,R_{yx}, \qquad \rho_{xx} = R_{xx}\frac{wt}{L}.

The Hall conversion does not contain the channel width because the wider current cross section and the longer transverse voltage path cancel in the ideal continuum geometry. That cancellation is not universal for finite voltage arms, invasive metal overlaps, irregular shapes, current jets, edge-dominated transport, or spatially varying conductivity.

For a two-dimensional conducting sheet, RyxR_{yx} is already the sheet Hall resistivity. Converting it to a three-dimensional ρyx\rho_{yx} by multiplying by the physical thickness asserts that the current is uniformly distributed through that thickness. Surface states, parallel layers, accumulation regions, and partially depleted films violate that assertion.

Current contacts should spread current across the width before it reaches the voltage probes. Keep voltage arms narrow, measure their positions, and check for metal bridges, cracks, leakage, or nonlinear contacts. Invasive probes can shunt the Hall field rather than merely sample it (Gluschke et al., 2020). A uniform outline also does not guarantee a uniform carrier density; Bierwagen et al. (2008) discuss how inhomogeneity can even reverse the apparent carrier sign in van der Pauw measurements.

A uniform, isotropic, simply connected sheet with four sufficiently small contacts on its boundary supports both sheet-resistance and Hall measurements. Current is driven through one opposing contact pair and transverse voltage read across the other; current and field are reversed, and the diagonal configurations are exchanged.

The archived NIST procedure below gives an explicit acquisition sequence. Its redundant configurations test contact placement, sample uniformity, reversal consistency, and reciprocity. The method loses its guarantee when contacts lie in the interior, the sample contains a hole, thickness or carrier density varies appreciably, or anisotropy is ignored. Transport Measurements gives the sheet-resistance equation and its geometric assumptions.

A transverse record can be organized schematically as

Vyraw=Voff+IRyx(B,H)+ϵIRxx(B,H)+Vind(B˙)+Vth.V_y^{\mathrm{raw}} ={} V_{\mathrm{off}} + I R_{yx}(B,\mathcal H) + \epsilon I R_{xx}(B,\mathcal H) + V_{\mathrm{ind}}(\dot B) + V_{\mathrm{th}}.

ϵ\epsilon parameterizes longitudinal pickup, often from contact misalignment or current distortion. VoffV_{\mathrm{off}} and VthV_{\mathrm{th}} need not be field independent, while VindV_{\mathrm{ind}} depends on sweep rate and loop area. It is a small-signal approximation: heating or changes in magnetic state can couple these contributions, so a single subtraction need not remove them.

At fixed field and magnetic state, form the current-odd voltage

VyI−(B;H)=12[Vy(+I,B;H)−Vy(−I,B;H)].V_y^{I-}(B;\mathcal H) ={} \frac{1}{2} \bigl[ V_y(+I,B;\mathcal H) -V_y(-I,B;\mathcal H) \bigr].

This rejects static current-even offsets. It does not reject Joule-heating contributions that change resistance by an amount proportional to I2I^2 and therefore generate an odd I3I^3 voltage. Several excitation amplitudes are needed to establish a linear range.

Write VsI,sB=Vy(sII,sBB)V^{s_I,s_B}=V_y(s_I I,s_B B) for states prepared by a matched protocol. The current-odd, field-odd Hall channel is

RyxI−,B−(B)=14I[V+,+−V−,+−V+,−+V−,−].R_{yx}^{I-,B-}(B) ={} \frac{1}{4I} \bigl[ V^{+,+}-V^{-,+} -V^{+,-}+V^{-,-} \bigr].

The corresponding current-odd, field-even diagnostic is

RyxI−,B+(B)=14I[V+,+−V−,++V+,−−V−,−].R_{yx}^{I-,B+}(B) ={} \frac{1}{4I} \bigl[ V^{+,+}-V^{-,+} +V^{+,-}-V^{-,-} \bigr].

For a reversible nonmagnetic sample, longitudinal pickup is commonly field even and appears in RyxI−,B+R_{yx}^{I-,B+}, while the ordinary Hall signal appears in RyxI−,B−R_{yx}^{I-,B-}. The decomposition itself is exact for the four numbers. Interpreting the odd channel as Hall response requires matched sample states and controlled geometry. A field-even transverse voltage can also be physical, for example from in-plane anisotropy; it is not automatically a wiring error. In a mesoscopic four-terminal device, even a nominal longitudinal transfer resistance need not be even in field. Lead reciprocity is the more general constraint (Büttiker, 1986).

Let Rab,cd=(Vc−Vd)/IabR_{ab,cd}=(V_c-V_d)/I_{ab}, where positive current enters aa and leaves bb. For a fixed sample in linear response, microscopic reversibility gives

Rab,cd(B,M)=Rcd,ab(−B,−M).R_{ab,cd}(B,\mathcal M) =R_{cd,ab}(-B,-\mathcal M).

Here M\mathcal M stands for every internal time-reversal-odd order parameter, not just the net magnetization. This compares exchanged current and voltage pairs, with the field and magnetic order reversed. It does not require Rab,cd(B)=Rab,cd(−B)R_{ab,cd}(B)=R_{ab,cd}(-B). Casimir (1945) gives the general principle; Büttiker (1986) applies it to coherent multiterminal conductors.

Plan lead exchange into the same measurement sequence. A mismatch first calls for checks of excitation, contact stability, temperature drift, and magnetic preparation before concluding that the assumed response regime fails.

Define the low-field sheet Hall slope

SH2D≡dRyxI−,B−dB∣B→0.S_{\mathrm H}^{2\mathrm D} \equiv \left. \frac{dR_{yx}^{I-,B-}}{dB} \right|_{B\to0}.

For one isotropic carrier type with Hall factor unity,

ns=1e∣SH2D∣,sgn⁡(q)=sgn⁡(SH2D).n_s = \frac{1}{e\lvert S_{\mathrm H}^{2\mathrm D}\rvert}, \qquad \operatorname{sgn}(q) = \operatorname{sgn}(S_{\mathrm H}^{2\mathrm D}).

Here e>0e>0 and nsn_s is a positive sheet density. A conducting thickness tt gives n=ns/tn=n_s/t only if the current-carrying layer is known and uniform.

If the same channel also produces sheet resistance R□R_{\square}, the one-carrier Hall mobility is

μH=∣SH2D∣R□=1ensR□.\mu_{\mathrm H} = \frac{ \lvert S_{\mathrm H}^{2\mathrm D}\rvert }{R_{\square}} = \frac{1}{e n_s R_{\square}}.

This is a model-derived mobility, not a directly recorded velocity. Parallel channels, anisotropic scattering, magnetic response, or an energy-dependent relaxation time break the simple identification.

In semiconductor transport, a Hall factor rHr_{\mathrm H} is often introduced so that the measured slope is rH/(nsq)r_{\mathrm H}/(n_s q). Then the apparent Hall density is ns/rHn_s/r_{\mathrm H} and μH=rHμdrift\mu_{\mathrm H}=r_{\mathrm H}\mu_{\mathrm{drift}}. The factor depends on band structure, scattering, degeneracy, and temperature. Setting it to one should be stated as an approximation.

A sign assignment needs a slope resolved from zero and calibrated field, current, and voltage polarities. Even then, a positive weak-field slope can coexist with electron pockets if higher-mobility holes dominate the transverse response. It does not identify the charge of every mobile excitation.

Ordinary, anomalous, and quantum Hall signals

Section titled “Ordinary, anomalous, and quantum Hall signals”

An ordinary one-carrier response is odd in field and, in the simplest model, linear. Check consistency across excitation amplitudes and lead configurations, then use longitudinal transport and another density-sensitive measurement to test that interpretation. A straight Hall trace alone is insufficient: a multiband conductor can look linear over a narrow field window, and an anomalous contribution can look linear before magnetization saturates. Hall factors and parallel conduction can change the inferred density even when the trace is straight.

In a magnetic conductor, analysts often write the measured Hall resistivity as an ordinary background plus an anomalous term. Treat this as a model decomposition. Subtracting a high-field line assumes that the ordinary coefficient is field independent and that the anomalous response has reached a known high-field behavior.

Measure longitudinal and transverse response together on both sweep branches, and compare with magnetization or another probe of magnetic order under the same preparation. Temperature, angle, thickness, and disorder dependence help distinguish mechanisms; Nagaosa et al. (2010) review their physical origins. If the Hall angle is appreciable, invert the full tensor rather than using a small-angle approximation.

An anomalous Hall loop need not be proportional to net magnetization. Berry curvature, skew scattering, side jump, noncollinear order, and multiple magnetic regions can contribute. Hall Effect develops those mechanisms.

A quantum Hall claim is based on a correlated longitudinal and transverse pattern, not a flat-looking segment:

  • ∣Ryx∣\lvert R_{yx}\rvert approaches h/(νe2)h/(\nu e^2) for an identified positive integer or fractional filling magnitude ν\nu;
  • RxxR_{xx} develops a corresponding minimum and ideally becomes unresolved;
  • the feature persists over a field or density interval;
  • current is below the breakdown threshold;
  • contact and lead mixing are tested;
  • temperature and device-size dependence are consistent with the proposed gap and edge transport.

A useful magnitude residual is

δν≡∣Ryx∣h/(νe2)−1.\delta_\nu \equiv \frac{\lvert R_{yx}\rvert}{h/(\nu e^2)} -1.

The sign of RyxR_{yx} is recorded separately under the terminal and field convention above; using a magnitude for this residual does not discard that sign from the data. A small δν\delta_\nu with appreciable RxxR_{xx} is not yet a metrological plateau. The finite longitudinal signal can mix into RyxR_{yx} and indicates dissipation or incomplete quantization. Integer Quantum Hall Effect explains plateau formation and edge transport, starting from the measurements of von Klitzing, Dorda, and Pepper (1980).

Coexisting bulk carrier types add conductivity tensors before inversion. Distinct layers instead add sheet conductance tensors, provided they share the same in-plane electric field and their contacts equilibrate the layers:

Gtot=∑ataσ(a),ρ□=Gtot−1.\mathbf G_{\mathrm{tot}}=\sum_a t_a\boldsymbol\sigma^{(a)}, \qquad \boldsymbol\rho^{\square}=\mathbf G_{\mathrm{tot}}^{-1}.

Each taσ(a)t_a\boldsymbol\sigma^{(a)} has units of siemens; a genuinely two-dimensional channel contributes its sheet tensor directly. Do not add a bulk conductivity in S m−1\mathrm{S\,m^{-1}} to a sheet conductance in S\mathrm S. A channel confined to an edge, or layers with poorly equilibrated contacts, need a terminal-transport model rather than this local uniform-field sum. See Landauer–Büttiker Formalism for the contact-based description.

For an isotropic sheet with antisymmetric Hall part, inversion gives

Gxx=ρxx□(ρxx□)2+(ρyx□)2,Gyx=−ρyx□(ρxx□)2+(ρyx□)2.G_{xx}=\frac{\rho_{xx}^{\square}} {(\rho_{xx}^{\square})^2+(\rho_{yx}^{\square})^2}, \qquad G_{yx}=\frac{-\rho_{yx}^{\square}} {(\rho_{xx}^{\square})^2+(\rho_{yx}^{\square})^2}.

Convert the longitudinal terminal resistance first: ρxx□=Rxxw/L\rho_{xx}^{\square}=R_{xx}w/L, while ρyx□=Ryx\rho_{yx}^{\square}=R_{yx} in an ideal Hall bar. Taking the reciprocal of each measured resistance separately misses both geometry and tensor mixing. An anisotropic sheet requires its complete tensor.

The familiar two-carrier model contains four positive parameters, n,p,μe,μhn,p,\mu_e,\mu_h, before offsets, geometry uncertainty, or field dependence are added. A short weak-field Hall trace generally cannot determine all four independently. A wide field range can contain more information, but parameter count alone does not establish whether a fit is identifiable. At minimum:

  1. fit ρxx(B)\rho_{xx}(B) and ρyx(B)\rho_{yx}(B) simultaneously in tensor form;
  2. report parameter covariance and sensitivity to the field window;
  3. repeat across temperature or gate voltage with physically justified shared parameters;
  4. constrain density or Fermi-surface area with capacitance, stoichiometry, spectroscopy, or quantum oscillations;
  5. test whether an additional parallel channel changes the conclusion.

Adding a third carrier because residuals remain does not automatically improve physical inference. It may only make a flexible inverse problem less identifiable.

In a magnetic sample, write Ryx(B;H)R_{yx}(B;\mathcal H), where H\mathcal H specifies sweep direction, saturation or cooling preparation, maximum field, wait time, and any gate or current pulse that may change domains. Field alone does not specify the state.

For a symmetric major hysteresis loop, an upsweep prepared at negative saturation and a downsweep prepared at positive saturation can satisfy

M↑(B)=−M↓(−B).\mathcal M_{\uparrow}(B)=-\mathcal M_{\downarrow}(-B).

These opposite-branch points are then the appropriate time-reversed pair; remaining on one branch is not inherently safer. Exchange bias, incomplete saturation, training, relaxation, or different domain patterns can destroy this relation. Preserve both branches and test their magnetic preparation before pairing points. Even equal and opposite net magnetizations need not establish that the full internal configurations are time reverses.

Anisotropic magnetoresistance can generate a planar Hall voltage when magnetization lies in the plane. Its field parity and angular dependence differ from an axial ordinary Hall signal, but domain reversal and misalignment can mix channels. A three-axis angle study should report the actual field vector and mechanical zero, not only the rotator readout.

Residual humps are not direct topology measurements

Section titled “Residual humps are not direct topology measurements”

A common procedure fits an ordinary background, subtracts an anomalous term proportional to magnetization, and labels the remaining hump “topological Hall.” The residual inherits every error in both backgrounds. Multiple magnetic regions with different coercivities and opposite anomalous-Hall signs can create a similar feature without a skyrmion phase (Gerber, 2018).

A real-space-topology claim needs orthogonal evidence such as imaging or scattering, a texture model, field-angle and thickness systematics, and agreement among magnetization, transport, and phase boundaries. Skyrmions and Magnetic Textures explains how magnetic texture produces an emergent field and what additional observations test that interpretation.

For a one-carrier sheet density ns=1/(e∣SH2D∣)n_s=1/(e|S_{\mathrm H}^{2\mathrm D}|), the relative standard uncertainty is approximately

u(ns)ns≃u(SH2D)∣SH2D∣,\frac{u(n_s)}{n_s} \simeq \frac{ u(S_{\mathrm H}^{2\mathrm D}) }{ \lvert S_{\mathrm H}^{2\mathrm D}\rvert },

when the slope uncertainty is small compared with its magnitude and the one-carrier model is valid. The charge ee is exact in the SI. The slope uncertainty must include voltage noise, current calibration, field calibration, drift, field-window choice, and correlated residuals. For bulk density n=ns/tn=n_s/t, thickness uncertainty and uncertainty in the electrically active layer must be added.

When a symmetric two-field estimate is appropriate,

SH2D≃VyI−(+B)−VyI−(−B)2IB.S_{\mathrm H}^{2\mathrm D} \simeq \frac{ V_y^{I-}(+B)-V_y^{I-}(-B) }{ 2IB }.

This estimator assumes linearity between the two fields. A regression over many points should report the model, weighting, covariance, and sensitivity to the fit interval. If a plausible slope interval crosses zero, neither a carrier sign nor a finite upper density bound follows from this inverse formula. The uncertainty of 1/∣SH2D∣1/|S_{\mathrm H}^{2\mathrm D}| is then strongly asymmetric; a symmetric error bar obtained by linear propagation is misleading. Model uncertainty from additional channels is separate from voltage noise.

For μH=∣SH2D∣/R□\mu_{\mathrm H}=|S_{\mathrm H}^{2\mathrm D}|/R_{\square}, slope and sheet-resistance uncertainties can be correlated because the same contacts, geometry, temperature, and conduction channels enter both. Propagating them as independent can misstate the mobility uncertainty. The covariance treatment in JCGM 100:2008 applies; a fit should also show its field interval and residuals so the reader can assess the assumed linear law.

With the bottom-minus-top voltage convention of this page, a device carrying I=10.0 μAI=10.0\,\mu\mathrm A at B=+1.00 TB=+1.00\,\mathrm T has current-odd transverse voltage VyI−=−2.00 mVV_y^{I-}=-2.00\,\mathrm{mV} after field-even pickup is removed. Assume one-carrier linear response. Find the sheet Hall slope, carrier sign, and sheet density.

Solution

The Hall resistance at this field is

Ryx=−2.00 mV10.0 μA=−200 Ω.R_{yx} = \frac{-2.00\,\mathrm{mV}} {10.0\,\mu\mathrm A} = -200\,\Omega.

Linearity through the origin gives SH2D=−200 Ω T−1S_{\mathrm H}^{2\mathrm D}=-200\,\Omega\,\mathrm T^{-1}. The negative sign identifies electrons under the declared convention. The sheet density is

ns=1e∣SH2D∣=3.12×1016 m−2=3.12×1012 cm−2.\begin{aligned} n_s &= \frac{1}{ e\lvert S_{\mathrm H}^{2\mathrm D}\rvert } \\ &= 3.12\times10^{16}\,\mathrm m^{-2} \\ &= 3.12\times10^{12}\,\mathrm{cm}^{-2}. \end{aligned}

The result is model conditional: it assumes one carrier type and Hall factor unity.

At one field magnitude and I=100 μAI=100\,\mu\mathrm A, the transverse voltages in microvolts are

V+,+=310,V−,+=−250,V+,−=150,V−,−=−90.\begin{aligned} V^{+,+}&=310, & V^{-,+}&=-250, \\ V^{+,-}&=150, & V^{-,-}&=-90. \end{aligned}

Find the current-odd response at each field, then the field-odd and field-even transfer resistances.

Solution

At positive and negative field,

VyI−(+B)=310−(−250)2 μV=280 μV,VyI−(−B)=150−(−90)2 μV=120 μV.\begin{aligned} V_y^{I-}(+B) &= \frac{310-(-250)}{2}\,\mu\mathrm V \\ &= 280\,\mu\mathrm V, \\ V_y^{I-}(-B) &= \frac{150-(-90)}{2}\,\mu\mathrm V \\ &= 120\,\mu\mathrm V. \end{aligned}

The odd and even voltages are therefore 80 μV80\,\mu\mathrm V and 200 μV200\,\mu\mathrm V. Dividing by current gives

RyxI−,B−=0.80 Ω,RyxI−,B+=2.00 Ω.R_{yx}^{I-,B-} = 0.80\,\Omega, \qquad R_{yx}^{I-,B+} = 2.00\,\Omega.

The larger field-even channel is consistent with substantial longitudinal pickup. It should be reported and investigated, not silently discarded.

Under a one-carrier model, an estimate gives S=−2.0 Ω T−1S=-2.0\,\Omega\,\mathrm T^{-1} with standard uncertainty u(S)=1.5 Ω T−1u(S)=1.5\,\Omega\,\mathrm T^{-1}. Treat [−5,1] Ω T−1[-5,1]\,\Omega\,\mathrm T^{-1} as an approximate coverage interval. What goes wrong with quoting only the central Hall density and a symmetric uncertainty? How does an unknown conducting thickness affect the conclusion?

Solution

The central estimate is nH=1/(e∣S∣)=3.12×1018 m−2n_{\mathrm H}=1/(e|S|)=3.12\times10^{18}\,\mathrm m^{-2}. Linear propagation would give a 75% relative uncertainty, already too large to justify linearizing the reciprocal. The stated interval includes positive and negative slopes and arbitrarily small nonzero magnitudes. It therefore leaves the carrier sign unresolved and maps to unbounded density above; its largest slope magnitude gives a conditional lower bound 1/(5e)=1.25×1018 m−21/(5e)=1.25\times10^{18}\,\mathrm m^{-2}. Exactly zero slope has no finite-density realization in this ideal single-carrier formula.

If the one-carrier model is wrong, even that bound need not apply: cancellation between electron and hole contributions can give zero Hall slope at finite density. A thickness uncertainty enters only the conversion n=ns/tn=n_s/t after a reliable sheet density exists. It cannot rescue an unresolved Hall slope.

In the weak-field two-carrier model, the Hall numerator is proportional to pμh2−nμe2p\mu_h^2-n\mu_e^2. Consider n=4n=4 and p=2p=2 in common density units, with μe=1000\mu_e=1000 and μh=2000\mu_h=2000 in common mobility units. Determine the Hall sign and explain the lesson.

Solution

The two weighted terms are

pμh2=2(2000)2=8.0×106,p\mu_h^2 = 2(2000)^2 = 8.0\times10^6,

and

nμe2=4(1000)2=4.0×106.n\mu_e^2 = 4(1000)^2 = 4.0\times10^6.

The numerator is positive, so the weak-field Hall slope is hole-like even though electrons are twice as numerous. Hall sign is mobility weighted in a multiband conductor; it is not a census of every carrier or Fermi-surface pocket.

5. Which hysteresis branches should be paired?

Section titled “5. Which hysteresis branches should be paired?”

A toy symmetric magnetic loop has

m↑(B)=tanh⁡[(B−Bc)/b],m↓(B)=tanh⁡[(B+Bc)/b],\begin{aligned} m_{\uparrow}(B)&=\tanh[(B-B_c)/b],\\ m_{\downarrow}(B)&=\tanh[(B+B_c)/b], \end{aligned}

where m=M/Msm=M/M_s, Bc>0B_c>0, and b>0b>0 sets the switching width. Suppose Ryx=S0B+AmR_{yx}=S_0B+A m. Which branch at −B-B is the time reverse of an upsweep point at +B+B? Does the half-difference isolate the ordinary term S0BS_0B? What changes if both loops are shifted by the same exchange-bias field BEB_E?

Solution

Oddness of tanh⁡\tanh gives m↓(−B)=−m↑(B)m_{\downarrow}(-B)=-m_{\uparrow}(B). Thus

R↑(B)−R↓(−B)2=S0B+Am↑(B).\frac{R_{\uparrow}(B)-R_{\downarrow}(-B)}2 =S_0B+A m_{\uparrow}(B).

Opposite branches form the correct pair in this model. Antisymmetrization retains the anomalous term as well as the ordinary one; it cannot separate them by parity. Same-branch pairing generally does not compare reversed magnetizations, particularly near switching.

With exchange bias, replace BB by B−BEB-B_E in both magnetic curves. At fixed BE≠0B_E\ne0, m↓(−B)m_{\downarrow}(-B) is no longer −m↑(B)-m_{\uparrow}(B). Reversing the pinning order, represented here by BE→−BEB_E\to-B_E, restores the relation. Real samples can have additional domain-state and relaxation differences beyond this one-variable model.

Near a proposed filling-magnitude ν=2\nu=2 plateau, a device gives ∣Ryx∣=12.910 kΩ\lvert R_{yx}\rvert=12.910\,\mathrm{k}\Omega and Rxx=20 ΩR_{xx}=20\,\Omega. Use h/e2=25 812.807 Ωh/e^2=25\,812.807\,\Omega to calculate the magnitude residual δ2\delta_2. Does the measurement establish a metrological plateau?

Solution

The ideal value is

h2e2=12 906.404 Ω.\frac{h}{2e^2} = 12\,906.404\,\Omega.

Therefore

δ2=12 91012 906.404−1=2.79×10−4.\begin{aligned} \delta_2 &= \frac{12\,910}{12\,906.404}-1 \\ &= 2.79\times10^{-4}. \end{aligned}

The Hall value is close at the 10−410^{-4} level, but Rxx=20 ΩR_{xx}=20\,\Omega is clearly nonzero and can mix into the transverse channel. The observation is consistent with an emerging plateau, not by itself with metrological quantization. Current dependence, contact configuration, temperature, field width, and uncertainty must also be checked.