Geometric phase of open paths and a geodesic-selection rule at a level degeneracy
Abstract
When the control field of a qubit, a polarization state, or a spin- system is swept through a level degeneracy, its direction traces an open curve on the Bloch sphere whose endpoints are antipodal, and the geodesic rule for the open-path geometric phase becomes ambiguous: infinitely many geodesics close the path, and different closures enclose different solid angles. We resolve this ambiguity in closed form. A coordinate-free monopole connection defines the open-path solid angle intrinsically, and displacing the degeneracy by closes the path with enclosed solid angle , where is the azimuth of the transverse part of measured from the principal normal of the control curve at the crossing. The identity between geometric phase and enclosed solid angle therefore holds for exactly one closing geodesic—the great circle in the osculating plane ()—supplied by the curvature at the degeneracy. Berry’s invariant under reversal of the displacement and the values under a reflection symmetry follow as corollaries, and the pure-state limit of the finite-temperature Uhlmann phase selects the osculating-plane closure automatically, turning the heuristic closing rules of the open-path literature into a computable prescription.
Keywords: geometric phase, Berry phase, solid angle, open paths, geodesic rule, monopole connection, Uhlmann phase
1 Introduction
For a closed curve on the Bloch (or Poincaré) sphere , the relation between geometric phase and solid angle is well established: a spin- system acquires the Berry phase , where is the signed spherical area enclosed by [3, 10, 7]. When the curve is instead open, the kinematic formulation defines its geometric phase by completing the curve with a geodesic arc connecting the endpoints [1, 9, 6]. Because parallel transport along this geodesic contributes no geometric phase, the open-path geometric phase equals minus one-half of the solid angle enclosed by the resulting closed curve. This is known as the geodesic rule.
This construction, however, becomes ambiguous when the endpoints of the open curve are antipodal. Such a situation can arise naturally in systems with an effective two-level description, including a driven qubit, a spin- in a rotating field, and a light beam passing through a polarization singularity. Consider a two-level Hamiltonian
| (1) |
where is the vector of Pauli matrices, and is a smooth, -periodic control vector, . Thus, the path traced by is a closed curve in the control-parameter space. We assume that this curve passes through the origin at a single isolated point in each period and that the velocity is nonzero. We refer to such a passage through the origin as a transversal crossing. At , the two eigenvalues coincide, and the Hamiltonian becomes degenerate. Let denote the direction in which the curve crosses the origin. In the vicinity of the crossing, and therefore
| (2) |
where . Thus, as passes through , jumps discontinuously between two antipodal points on . Since is undefined at , its trajectory on is not a closed loop but an open curve , with the antipodal endpoints . Traversed over one period, begins at , immediately after the crossing, and ends at , immediately before it. Between such antipodal endpoints the geodesic rule no longer singles out a closure: just as all meridians join the north and south poles, infinitely many great-circle arcs of equal length join to .
At first sight, this ambiguity may appear harmless: a closing geodesic is commonly said to contribute no geometric phase. This argument is well defined for non-antipodal endpoints, which determine a unique shorter geodesic and correspond to non-orthogonal states with a well-defined Pancharatnam phase [7, 9]. For antipodal endpoints, however, the corresponding states are orthogonal, their relative phase is undefined, and infinitely many half-great-circle arcs are available. Different closures therefore produce closed loops with different solid angles and geometric phases. Although the relation remains valid for each closed loop, the geometric phase assigned to the original open path is not unique without an additional criterion. Selecting the appropriate closing geodesic thus carries physical content.
This “which geodesic” problem, together with the phase jumps that occur when the evolving state becomes orthogonal to the initial one—geometrically, when the trajectory passes through the point antipodal to its starting point on —has been recognized previously. Rakhecha and Wagh showed for a two-level system that, as the path passes through this antipodal point, the geometric-phase jump is determined by the azimuthal separation between the two geodesic branches, yielding a jump of for a smooth crossing [8]. More recently, a hierarchy of operational rules for the open-path Pancharatnam geometric phase was proposed, culminating in a prescription that selects the closing geodesic according to the direction from which the physical path approaches the endpoint [5]. Predictions of the geodesic rule, including the associated sign changes and phase jumps, have also been verified experimentally [18, 15]. These studies establish the operational prescription and its observable consequences, but a general coordinate-free derivation remains lacking.
The aim of this work is to develop a closed-form, coordinate-free treatment of the geodesic-selection problem, identify the mechanism underlying its dependence on the chosen closure, and formulate an explicit selection rule. Our analysis is based on the coordinate-free monopole one-form connection,
| (3) |
which allows us to obtain the following results:
- (i)
define the solid angle associated with an open curve having antipodal endpoints as a line integral over the curve alone, with its starting point taken as the base point, and define the corresponding open-path geometric phase as ;
- (ii)
show that, among the infinitely many geodesic closures of the antipodal endpoints, a unique oriented geodesic arc satisfies the geodesic rule for the open-path geometric phase defined in (i), and identify it as the closure selected by the osculating plane of at the degeneracy;
- (iii)
introduce a regularization and show that the solid angle of the resulting nonsingular closed path satisfies Here, is a signed angle between two directions transverse to the crossing: the direction in which the shift carries the curve past the degeneracy, and the direction in which the curve itself is bending there;
- (iv)
recover the universal phase difference under reversal of the regularization direction and the values under reflection symmetry;
- (v)
The deviation originates from the unequal contributions accumulated near the two antipodal endpoints as the regularized path avoids the degeneracy. To recover the open-path geometric phase defined above, the path should be closed using the oriented geodesic selected by the osculating plane, which is determined by the local curvature of at the degeneracy. Our analysis thus provides both a geometric explanation and an operational prescription. The rest of the manuscript is organized as follows. Sections 2–4 develop these results, Section 5 concludes, and Appendix A presents numerical verification.
2 The monopole connection on
2.1 Determining the connection
To construct a connection suitable for treating open paths, we choose a base point and seek a one-form whose circulation around a closed curve equals the enclosed solid angle. Since is a unit vector, lies in the tangent plane of and satisfies . Consequently, only the tangential component of contributes to : adding an arbitrary radial term leaves the one-form unchanged, so we may choose without loss of generality. Two tangential directions remain, the polar (meridional) direction and the azimuthal one , and we now show that only the latter carries physical content.
Consider first the component of along . Rotational symmetry about the axis restricts this component to the form . Since , its contribution to the one-form is , which is pure gauge: it leaves the curvature unchanged, since . Setting is thus a choice of gauge rather than a restriction. We adopt it here because it makes the great circles through parallel-transport paths: on such a circle points along , so with a geodesic joining any point to the base point contributes nothing to the line integral. This property is established in Lemma 3.1 and underlies the geodesic-closure construction for open paths developed below.
The remaining tangential component lies along the azimuthal direction , which is parallel to . Unlike , its coefficient does affect the curvature and cannot be chosen freely; it is fixed uniquely by Stokes’ theorem below. Rotational symmetry about the axis further requires this coefficient to depend only on the polar angle , defined by . We therefore write
| (4) |
To determine , take to be the circle at constant polar angle about the axis. The spherical cap it bounds has the solid angle
| (5) |
On the magnitude is constant, is parallel to , and the circumference is , so
| (6) |
Equating (5) and (6) through Stokes’ theorem gives , and restoring yields the coordinate-free form,
| (7) |
2.2 The one-form connection and its curvature
Introduce spherical coordinates with at the north pole, i.e., , so that . With the right-handed orthonormal frame one has , , and . A short computation using and gives the one-form connection
| (8) |
The exterior derivative of this is the coordinate-free two-form curvature, , so for a closed curve ,
| (9) |
Before proceeding we fix the relation to the familiar Berry phase. For the two-level Hamiltonian in equation (1), we follow the eigenstate of energy aligned with . A standard computation of its Berry connection in the gauge with base point gives the familiar monopole form , which by equation (8) is nothing but
| (10) |
The Berry connection and the one-form studied here therefore differ only by the constant factor , and we work with in this paper.
2.3 Gauge, base point and Dirac string
The curvature derived above is that of a monopole located at . A gauge potential for a monopole cannot be chosen smoothly over the entire sphere. In the gauge defined by , the connection (7) is regular everywhere except at , where its denominator vanishes. This point is the intersection of the unit sphere with the Dirac string [4], an unphysical line singularity of the monopole gauge potential in the full parameter space. Changing moves this singularity and therefore corresponds to a change of gauge. For a closed curve, is independent of by equation (9) (exactly so if the curve does not cross the string, and up to an integer multiple of otherwise). For an open curve, however, a change of base point acts as a gauge transformation that leaves a boundary term . The choice of base point is thus an additional gauge—a path-dependent term—for open curves, and the value of depends on it. It is therefore natural to tie the base point to the curve itself. In the situation of interest this choice is essentially forced: taking (the starting direction) places the string at the opposite endpoint , so that terminates exactly on the string. As we show in section 3, this is precisely what renders the non-uniqueness of the closing geodesic harmless, and we adopt henceforth (Definition 3.2).
3 Solid angle of an open path with antipodal endpoints
3.1 Geodesic rule and intrinsic definition
Lemma 3.1 (coordinate-free geodesic rule).
Along the geodesic (great-circle) arc from any to the base point one has identically; consequently a geodesic arc contributes nothing to the geometric phase.
Proof.
The geodesic lies in the plane . Any point on it, and its tangent , lie in , whereas is by construction orthogonal to . The inner product of a vector normal to a plane with one lying in it vanishes, so . ∎
Definition 3.2 (open-path solid angle).
For an open curve starting at , define
| (11) |
with the base point taken to be the starting point of the curve.
The line integral (11) admits a purely geometric reading. Discretising as and letting be the signed solid angle, seen from the centre of the sphere, of the spherical triangle , one has . Indeed, the signed solid angle of a spherical triangle is given by the van Oosterom–Strackee formula [13],
| (12) |
and inserting , , and expanding to first order reproduces the integrand of equation (11). The “solid angle seen from the centre”, the “base-point triangulation”, and the “one-form line integral” therefore coincide.
3.2 Independence of the closing geodesic
Lemma 3.3 (antipodal endpoints).
If the endpoint of is the antipode of the base point, then any geodesic joining to contributes zero to the line integral in equation (11). Hence the line integral is determined by the curve alone, independently of the closing path.
Proof.
A great circle through is the intersection of the sphere with a plane for some unit . This plane contains , so Lemma 3.1 applies at each of its points; since was arbitrary, the claim follows. ∎
Remark 3.4.
Lemma 3.3 states that the line integral is intrinsic to ; it does not state that the solid angle enclosed after closing is independent of the chosen geodesic. Two different closings bound a spherical lune between them, whose area on the unit sphere equals twice the angle at which the two great circles meet at the shared endpoints. Consequently the identity “geometric phase enclosed solid angle” holds for exactly one closing geodesic, and —defined as the azimuth of the chosen closing relative to that canonical one—measures the failure of the identity for any other choice. Identifying the canonical geodesic (the osculating-plane great circle, ) and proving the deviation is the subject of section 4, and gives a closed form to the operational selection rule of [8, 5]. Finally, the base point is placed at the start of so that no closing geodesic passes through and the line integral carries no spurious endpoint contribution.
3.3 Osculating plane and Frenet frame
The point (the degeneracy) is, as noted in section 1, where jumps between the antipodes ; the “degeneracy” and the “antipodal endpoints of the -trajectory” are the same event. Set , , and . Then ,
| (13) |
where
| (14) |
so that as : the direction field jumps between antipodes.
Assume (equivalently ), i.e., that the curve has nonzero curvature at . Introduce the Frenet frame at , with orthonormal basis consisting of the tangent , principal normal , and binormal , and let be the osculating plane. The geometry is illustrated in figure 1. Since the -component of is , the curve lies in to second order. Decomposing in the Frenet frame, , with components
| (15) | ||||
To leading order the curve is the parabola
| (16) |
with vertex at the origin, opening towards .
We now fix the angular variables used below. The pole of the spherical coordinates has already been tied to the curve, ; we further choose the azimuthal origin in the transverse plane spanned by so that along and along . The transverse part of —its projection onto this plane, with as in equation (15)—then has azimuth , which is what we mean by the transverse azimuth of . We call the trajectory of the unregularized direction field of equation (13) the bare curve, in contradistinction to the regularized field introduced later, and write for its azimuth.
Lemma 3.5 (harmlessness of the degeneracy).
Near the degeneracy the transverse azimuth of the bare curve is
| (17) |
Regardless of , the contribution of any neighbourhood of the degeneracy to is and hence vanishes as : the degeneracy contributes nothing to the intrinsic solid angle.
Proof.
Carrying the expansion in equation (15) one order further, the binormal component is , while on both branches. Hence , an odd function that passes through zero with finite slope rather than remaining pinned at . For the contribution to through the one-form in equation (8), split the window by branch. On the branch the polar angle is , so the weight is ; with this branch contributes . On the branch the polar angle approaches , so the weight is , and the branch contributes . The total contribution goes to as the size of the window tends to zero, . ∎
The coefficient is proportional to the Frenet torsion of at the crossing, so the azimuth is frozen at precisely for the planar (reflection-symmetric) case of Corollary 4.4. The parabola in equation (16) and Lemma 3.5 together carry the two facts on which the rest of the paper turns. First, both branches () of the curve lie on the side, since the coefficient in is positive irrespective of the sign of ; the transverse direction of therefore agrees with to leading order on both sides of the degeneracy, deviating only at through the torsion, and by Lemma 3.5 the jump of from to leaves no concentrated contribution to the solid angle. Second, the tangent directions of the parabola at single out, among the infinitely many geodesics joining the antipodes, the one great circle actually tangent to the curve—the osculating-plane great circle; this tangency is a second-order statement, unaffected by the torsion. The identity of the “geodesic that realizes the enclosed solid angle”, anticipated in Remark 3.4, is thus supplied by the curvature at the degeneracy.
4 Dependence on the regularization direction
The open path terminates at the antipodal points , where the geodesic that closes it is not unique. One way to resolve this is by displacing the degeneracy off the origin: a small shift makes nonvanishing, so is a genuine closed loop with an unambiguous solid angle, and letting recovers a definite closing whose selection depends on the direction .
4.1 The regularized field
Let us introduce the regularization with and having a nonzero transverse component, i.e., . Then avoids the origin, and is a smooth closed curve. Decomposing as in equation (15),
| (18) | ||||
where . The transverse plane is spanned by with coordinates . Writing
| (19) |
so that , the transverse components become
| (20) |
Geometrically, is the angle specifying the direction of the transverse regularization within the plane, measured from the principal normal ; as we now show, it also parametrizes the closing geodesic: corresponds to the osculating-plane great circle (the canonical geodesic), and to a great circle rotated by about the axis (see figure 1).
The key structural fact is that the regularization contributes an -independent transverse shift . To leading order the transverse trajectory is then the horizontal line traced as runs through the crossing: the point comes in from large , reaches its closest approach to the origin at , where , and recedes back to large , staying at fixed height throughout. The azimuth is accordingly
| (21) |
According to equation (8), an azimuthal change contributes to the solid angle. Its contribution therefore depends strongly on the polar angle: the weight vanishes at the north pole and reaches its maximum value of at the south pole . To determine the net contribution of the azimuthal turn in equation (21), we compare the characteristic -scales over which and vary. The transverse vector entering equation (21) can be written as
| (22) |
which shows that the quadratic contribution becomes comparable to the magnitude of the regularization-induced transverse displacement at
| (23) |
The polar angle is governed by a different scale, which is best seen through its deviation from the nearer pole, . From and for small , to leading order, and the transverse part dominated by the regularization for , , the deviation obeys
| (24) |
Equation (24) yields the polar scale: the deviation is small precisely while , so that the polar angle stays pinned at its pole, for and for , whereas for the deviation is and sweeps continuously from to as crosses the origin. The two scales are therefore well separated, , and this separation splits the crossing into three regions.
The three regions are distinguished by which of and is in motion. In region () the polar angle has already reached its pole while the azimuth still sits at ; in region () the azimuth turns from to while stays pinned at its pole; and in region () sweeps from to , the azimuth being already fixed at .
The essential point is that the azimuthal turn of region takes place where the regularized curve passes the two poles , with settled at or . Evaluating equation (24) at the azimuthal scale gives , so expanding the monopole weight to second order in , with on the branch and on the branch,
| (25) |
The same turn is thus counted with weight near one pole and weight near the other; this asymmetry is what produces the net .
4.2 Main theorem
Theorem 4.1 (deviation of the solid angle).
Proof.
By Lemma 3.5, the neighbourhood of the degeneracy point contributes to an amount that vanishes with the window but is not zero for any fixed window. We therefore compare the regularized and the bare solid angles window by window rather than discarding this contribution. Fix with and split both solid angles at ,
| (28) |
where and denote the integrals of over the far region and the near window , for the regularized and the bare curve, respectively. We estimate the two differences and in turn.
Far part. On the field is bounded away from the origin, , so uniformly there; the weight and the azimuth of the regularized curve then reduce to their bare counterparts with error, so that .
Near part. The near window spans regions , , and , which locate the difference as follows. In region the bare curve term dominates the regularization in equation (18), so in the integrand of the common bare part cancels identically while the regularization perturbs the azimuthal measure and the weight only at ; the region therefore contributes to the difference. In region the transverse vector of the regularized curve reduces to , the curve term being only there, so its azimuth is constant, , and there is no azimuthal motion to weight despite the sweep of ; the bare integrand there is itself , by the window estimate of Lemma 3.5 with .
The difference is therefore generated in region , and it can be read off by comparing the two factors of the integrand, and . The azimuthal factor supplies the same net turn on both branches: relative to the common bare measure—which cancels in —the regularization produces one turn of size , executed on the side and undone on the side. Near the north pole , the returning turn of size is counted with weight by equation (25), while the bare contribution over region is bounded by the window estimate of Lemma 3.5 with —and in fact vanishes faster on this branch, the weight being there, integrating to . Hence
the returning turn leaving no trace at this pole. Near the south pole , however, the weight is pinned at throughout region ; since regions and contribute only , it factors out of the integral and each curve contributes twice its net azimuthal change across the window,
The endpoint values are sharp: by Lemma 3.5, because the transverse vector at is exactly , and because lies in region . Subtracting the bare from the regularized contribution,
the torsion term , common to both curves, dropping out.
Remark 4.2 (mechanism).
Around the closed loop the azimuth returns to its initial value, so its net change vanishes; the deviation is entirely a matter of where the change takes place. The turn imposed by the regularization is executed next to the Dirac string, where the monopole weight is , and undone at the opposite pole, where it vanishes, so the weighted change is —the finite analogue of the boundary term in the proof of Lemma 3.5. For , i.e. , the regularization is aligned with the bare transverse direction and no turn is imposed at all: the osculating-plane regularization is the unique neutral choice.
4.3 Corollaries
Corollary 4.3 (Berry’s invariant).
For any , .
Proof.
Corollary 4.4 (reflection symmetry).
If a plane through the origin contains for all (reflection symmetry) and the regularization is taken along the mirror normal , then , , and .
Proof.
Corollary 4.5 (non-universality of the average).
, so the average of the two regularized values depends on the regularization direction through and is not universal; under a reflection symmetry, where and , it equals or , agreeing with modulo .
The contrast between Corollary 4.3 and Corollary 4.5 is instructive: the difference is universal because cancels, whereas the average is not because survives; universality of the average would require the two half-loop contributions to be exactly opposite, which only a mirror symmetry guarantees. A numerical verification of Theorem 4.1 and its corollaries, over several representative fields and across a range of , is given in Appendix A.
4.4 Application: the Uhlmann phase selects the osculating-plane regularization
For the two-level Hamiltonian the Gibbs state is with . Near the degeneracy , so by the expansion of , : inside the Bloch ball passes through the origin along the straight line , without discontinuity. The pure state (Berry) lives on the sphere and suffers the jump, whereas the mixed-state (Uhlmann) path is closed and unbroken from the outset. This is the origin of the selection we now establish; it also connects to the known behaviour of the Uhlmann phase for one-dimensional fermion systems and for the Kitaev chain, where the state curve may pass through the maximally mixed point [14, 2].
The Uhlmann connection is with and . Writing with smooth across , the sign squares out, , so the directional part of the connection is smooth and bounded through the degeneracy, while makes . The central segment therefore contributes nothing, and is well defined without regularization for all and continuous in ; geometrically, the line of sight from the centre stays on the straight segment and sweeps no solid angle (cf. Lemma 3.5). As , and becomes the pure-state Berry generator, the central segment still contributing nothing, so
| (30) |
Combining (30) with Theorem 4.1 gives at once
| (31) |
i.e. the pure-state limit of the finite-temperature mixed state automatically selects the osculating-plane regularization (); any other direction is offset by . The prescription “close the open path in the way the physical path approaches the endpoint” [5] is thus realized here in closed form: the selected geodesic is the osculating-plane great circle , the curvature at the degeneracy supplying the “third point”, and the mixed-state construction realizes that choice on its own. That the Uhlmann and Berry phases agree in this pure-state limit is an instance of the Uhlmann–Berry correspondence [12, 11, 17]; the correspondence is known to fail at genuine level degeneracies (Dirac points) [16], which is consistent with the special role the degeneracy plays throughout the present analysis.
5 Conclusion
We have analysed the geometric phase and solid angle of an open curve on with antipodal endpoints—the generic situation when the control vector of a two-level system crosses the origin transversally. The monopole connection (7) defines the open-path solid angle intrinsically (Definition 3.2); every geodesic closing the antipodal endpoints contributes zero to the phase line integral (Lemma 3.3); and the degeneracy itself leaves no concentrated contribution, despite the torsion-induced tilt of the transverse azimuth (Lemma 3.5). Yet exactly one closing geodesic realizes the identity “geometric phase enclosed solid angle”. Theorem 4.1 quantifies the deviation of any other choice, , and traces it to the asymmetry of the monopole weight between the two poles: the azimuthal turn imposed by the regularization is counted with weight next to the Dirac string and with weight at the opposite pole (Remark 4.2). Berry’s invariant and the reflection values follow as corollaries, and the finite-temperature Uhlmann phase selects the osculating-plane regularization in its pure-state limit.
The practical content is a selection rule. To assign an enclosed solid angle—and hence a geometric phase—to an open antipodal path, the path should be closed with the great circle in the osculating plane of at the degeneracy, the unique geodesic tangent to the curve at both endpoints; any other closing overcounts by , with computable from the local -jet of the control curve—its velocity and acceleration at the crossing. This replaces the heuristic closing rules of the open-path literature [8, 5] by a closed-form prescription, and explains why they succeed when they do.
Several directions remain open. The analysis assumes a transversal crossing with nonvanishing transverse curvature, ; inflectional crossings, where the osculating plane degenerates, and trajectories with multiple crossings, where the geodesics selected at successive degeneracies need not coincide, call for an extension of Theorem 4.1. On the physical side, the invariant and the reflection values are directly testable in neutron and atom interferometry [15, 18], and the interplay with mixed-state phases beyond the Uhlmann construction—the interferometric phase of [11], and the fate of the Uhlmann–Berry correspondence at genuine level crossings [16]—deserves a systematic study.
Acknowledgments
This work was supported by the Institute of Information & Communications Technology Planning & Evaluation (IITP) grant funded by the Korea government (MSIT) (RS-2022-II221029).
Appendix Appendix A Numerical verification
We verify Theorem 4.1 and its corollaries on three representative fields: Fields A and B are generic, whereas Field C has reflection symmetry:
| Field A | (32) | |||
| Field B | (33) | |||
| Field C | (34) |
Fields A and B cross the origin transversally at , and Field C at ; Field C is confined to the mirror plane (the -plane), and its regularization is taken along the mirror normal . For Field A, and , giving , and .
Method. For each field the parameter is discretised on a uniform grid over a period. The open-path solid angle is computed from the line integral (11), equivalently from the van Oosterom–Strackee triangle sum (12); the regularized value is computed the same way for the closed curve , with the polar and azimuthal angles obtained by projecting onto the frame and applying . The Uhlmann value is obtained by integrating the connection of section 4.4 at temperature . Convergence is monitored by halving from to .
Main theorem. For Field A, , and at the measured deviation tracks across directions—for the predicted against measured , respectively. Halving from to reduces the error from to , by a factor per halving, consistent with the correction in equation (26).
Three scales. For , the predicted transition scale is ; numerically for , for , and near , while the weight is for and below for , confirming the weight asymmetry of (25).
Corollaries. At the difference for and a tilted direction, confirming Corollary 4.3. For Field C, as , converging to (Corollary 4.4), with the sum vanishing to machine precision.
Uhlmann selection. At the values and agree to within for Field A, for Field B, and exactly for Field C; halving from to reduces the difference from to , confirming equation (31). The code reproducing these data is available from the authors.
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