Inclassical andquantum mechanics, thegeometric phase is aphase difference acquired over the course of acycle, when a system is subjected to cyclicadiabatic processes, which results from the geometrical properties of theparameter space of theHamiltonian.[1] The phenomenon was independently discovered byS. Pancharatnam (1956)[2] in classical optics and byH. C. Longuet-Higgins (1958)[3] in molecular physics; it was generalized byMichael Berry in (1984).[4] It is also known as thePancharatnam–Berry phase,Pancharatnam phase, orBerry phase. In classical mechanics, the geometric phase is known as theHannay angle.
It can be seen in theconical intersection ofpotential energy surfaces[3][5] and in theAharonov–Bohm effect. The geometric phase around the conical intersection involving the ground electronic state of the C6H3F3+ molecular ion is discussed on pages 385–386 of the textbook by Bunker and Jensen.[6] In the case of the Aharonov–Bohm effect, the adiabatic parameter is themagnetic field enclosed by two interference paths, and it is cyclic in the sense that these two paths form a loop. In the case of the conical intersection, theadiabatic parameters are themolecular coordinates. Apart from quantum mechanics, it arises in a variety of otherwave systems, such as classicaloptics. As arule of thumb, it can occur whenever there are at least two parameters characterizing a wave in the vicinity of some sort of singularity or hole in the topology; two parameters are required because either the set of nonsingular states will not besimply connected, or there will be a nonzeroholonomy.
Waves are characterized byamplitude andphase, and may vary as a function of those parameters. The geometric phase occurs when both parameters are changed simultaneously but very slowly (adiabatically), and eventually brought back to the initial configuration. In quantum mechanics, this could involve rotations but also translations of particles, which are apparently undone at the end. One might expect that the waves in the system return to the initial state, as characterized by the amplitudes and phases (and accounting for the passage of time). However, if the parameter excursions correspond to a loop instead of a self-retracing back-and-forth variation, then it is possible that the initial and final states differ in their phases. This phase difference is the geometric phase, and its occurrence typically indicates that the system's parameter dependence issingular (its state is undefined) for some combination of parameters. Tomeasure the geometric phase in a wave system, aninterferenceexperiment is required.
TheFoucault pendulum is an example fromclassical mechanics that is sometimes used to illustrate the geometric phase. The geometric angle in an adiabatically driven harmonic oscillator is another simple example from classical mechanics.[7]
In a quantum system at then-theigenstate, anadiabatic evolution of theHamiltonian sees the system remain in then-th eigenstate of the Hamiltonian, while also obtaining a phase factor. The phase obtained has a contribution from the state's time evolution and another from the variation of the eigenstate with the changing Hamiltonian. The second term corresponds to the Berry phase, and for non-cyclical variations of the Hamiltonian it can be made to vanish by a different choice of the phase associated with the eigenstates of the Hamiltonian at each point in the evolution.
However, if the variation is cyclical, the Berry phase cannot be cancelled; it isinvariant and becomes an observable property of the system. By reviewing the proof of theadiabatic theorem given byMax Born andVladimir Fock, inZeitschrift für Physik51, 165 (1928), we could characterize the whole change of the adiabatic process into a phase term. Under the adiabatic approximation, the coefficient of then-th eigenstate under the adiabatic process is given bywhere is Berry's phase with respect to parametert. Changing the variablet into generalized parameters we can rewrite Berry's phase aswhere parametrizes the cyclic adiabatic process. Note that the normalization of implies that the integrand is imaginary, so that is real. Then there is a closed path in the appropriate parameter space. The geometric phase along the closed path can also be calculated by integrating theBerry curvature over the surface enclosed by.
One of the easiest examples is theFoucault pendulum. An easy explanation in terms of geometric phases is given by Wilczek and Shapere:[8]
How does the pendulum precess when it is taken around a general pathC? For transport along theequator, the pendulum will not precess. [...] Now ifC is made up ofgeodesic segments, theprecession will all come from the angles where the segments of the geodesics meet; the total precession is equal to the netdeficit angle which in turn equals thesolid angle enclosed byC modulo 2π. Finally, we can approximate any loop by a sequence of geodesic segments, so the most general result (on or off the surface of the sphere) is that the net precession is equal to the enclosed solid angle.
To put it in different words, there are no inertial forces that could make the pendulum precess, so the precession (relative to the direction of motion of the path along which the pendulum is carried) is entirely due to the turning of this path. Thus the orientation of the pendulum undergoesparallel transport. For the original Foucault pendulum, the path is a circle oflatitude, and by theGauss–Bonnet theorem, the phase shift is given by the enclosed solid angle.[9]
Consider a vector around a closed loop, e.g. a spherical triangle, on the sphere: The angle by which it twists,α, is proportional to the area inside the loop and will be considered below.
In a near-inertial frame moving in tandem with the Earth, but not sharing the rotation of the Earth about its own axis, the pendulum bob traces out a circular path during onesidereal day, i.e. a planar path since oscillation along the suspending rod is insignificant.
At the latitude of Paris, 48 degrees 51 minutes north, a full precession cycle takes just under 32 hours, so after one sidereal day, when the Earth is back in the same orientation as one sidereal day before, the oscillation plane has turned by just over 270 degrees. If the plane of swing was north–south at the outset, it is east–west one sidereal day later.
This also implies that there has been exchange ofmomentum; the Earth and the pendulum bob have exchanged momentum. The Earth is so much more massive than the pendulum bob that the Earth's change of momentum is unnoticeable. Nonetheless, since the pendulum bob's plane of swing has shifted, the conservation laws imply that an exchange must have occurred.
The precession of the oscillating plane can be demonstrated, by composing the infinitesimal rotations, that the precession rate is proportional to, in terms of the projection of theangular velocity of the Earth onto thenormal direction to the Earth. The area of the loop in form of a spherical triangle as referred to above is, where is the radius of the sphere and are spherical angles.[10] This spherical triangle can be expanded to a loop with so that After 24 hours, the difference between initial and final orientations of the trace in the Earth frame isα = −2π sinφ, which corresponds to the value given by theGauss–Bonnet theorem ( is the Gaussian curvature).α is also called theholonomy or geometric phase of the pendulum. When analyzing earthbound motions, the Earth frame is not aninertial frame, but rotates about the local vertical at an effective rate of2π sinφ radians per day. A simple method employing parallel transport within cones tangent to the Earth's surface can be used to describe the rotation angle of the swing plane of Foucault's pendulum.[11][12]
From the perspective of an Earth-bound coordinate system (the measuring circle and spectator are Earth-bounded, also if terrain reaction to Coriolis force is not perceived by spectator when he moves), using a rectangular coordinate system with itsx axis pointing east and itsy axis pointing north, the precession of the pendulum is due to theCoriolis force (otherfictitious forces as gravity and centrifugal force have no direct precession component). Consider a planar pendulum with constant natural frequencyω in thesmall angle approximation. There are two forces acting on the pendulum bob: the restoring force provided by gravity and the wire, and the Coriolis force (the centrifugal force, opposed to the gravitational restoring force, can be neglected). The Coriolis force at latitudeφ is horizontal in the small angle approximation and is given bywhereΩ is the rotational frequency of the Earth,Fc,x is the component of the Coriolis force in thex direction, andFc,y is the component of the Coriolis force in they direction.
The restoring force, in thesmall-angle approximation and neglecting centrifugal force, is given by

UsingNewton's laws of motion, this leads to the system of equations
Switching to complex coordinatesz =x +iy, the equations read
To first order inΩ/ω, this equation has the solution
If time is measured in days, thenΩ = 2π and the pendulum rotates by an angle of−2π sinφ during one day. The mathematics of these equations, i.e. derivation and so on, can be found in many textbooks on classical mechanics.[13]
The derivation of the solid angle which the pendulum bob sweeps out in one day at angular latitude is practically trivial if one recalls a theorem ofPappus.[14] This theorem says that the surface area of a sphere of radius (that of the Earth here), i.e., is equal to that of an enveloping circular cylinder of radius, i.e.. The theorem says, as one can check easily, that this equality applies to every section of the sphere. Thus if the spherical cap defined by the orbit of the pendulum bob has maximum height at latitude, we have The solid angle enclosed by the cap is then given by
and hence At the equator and at the north pole The period of oscillation is, where
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A second example is linearly polarized light entering asingle-mode optical fiber. Suppose the fiber traces out some path in space, and the light exits the fiber in the same direction as it entered. Then compare the initial and final polarizations. In semiclassical approximation the fiber functions as awaveguide, and the momentum of the light is at all times tangent to the fiber. The polarization can be thought of as an orientation perpendicular to the momentum. As the fiber traces out its path, the momentum vector of the light traces out a path on the sphere inmomentum space. The path is closed, since initial and final directions of the light coincide, and the polarization is a vector tangent to the sphere. Going to momentum space is equivalent to taking theGauss map. There are no forces that could make the polarization turn, just the constraint to remain tangent to the sphere. Thus the polarization undergoesparallel transport, and the phase shift is given by the enclosed solid angle (times the spin, which in case of light is 1).[15]
A stochastic pump is a classical stochastic system that responds with nonzero, on average, currents to periodic changes of parameters.The stochastic pump effect can be interpreted in terms of a geometric phase in evolution of the moment generating function of stochastic currents.[16]
The geometric phase can be evaluated exactly for a spin-1⁄2 particle in a magnetic field.[1]
While Berry's formulation was originally defined for linear Hamiltonian systems, it was soon realized by Ning and Haken[17] that similar geometric phase can be defined for entirely different systems such as nonlinear dissipative systems that possess certain cyclic attractors. They showed that such cyclic attractors exist in a class of nonlinear dissipative systems with certain symmetries.[18] There are several important aspects of this generalization of Berry's phase: 1) Instead of the parameter space for the original Berry phase, this Ning-Haken generalization is defined in phase space; 2) Instead of the adiabatic evolution in quantum mechanical system, the evolution of the system in phase space needs not to be adiabatic. There is no restriction on the time scale of the temporal evolution; 3) Instead of a Hermitian system or non-hermitian system with linear damping, systems can be generally nonlinear and non-hermitian.
There are several ways to compute the geometric phase in molecules within theBorn–Oppenheimer framework. One way is through the "non-adiabatic coupling matrix" defined bywhere is the adiabatic electronic wave function, depending on the nuclear parameters. The nonadiabatic coupling can be used to define a loop integral, analogous to aWilson loop (1974) in field theory, developed independently for molecular framework by M. Baer (1975, 1980, 2000). Given a closed loop, parameterized by where is a parameter, and. TheD-matrix is given by(here is a path-ordering symbol). It can be shown that once is large enough (i.e. a sufficient number of electronic states is considered), this matrix is diagonal, with the diagonal elements equal to where are the geometric phases associated with the loop for the-th adiabatic electronic state.
For time-reversal symmetrical electronic Hamiltonians the geometric phase reflects the number of conical intersections encircled by the loop. More accurately,where is the number of conical intersections involving the adiabatic state encircled by the loop
An alternative to theD-matrix approach would be a direct calculation of the Pancharatnam phase. This is especially useful if one is interested only in the geometric phases of a single adiabatic state. In this approach, one takes a number of points along the loop with and then using only thej-th adiabatic states computes the Pancharatnam product of overlaps:
In the limit one has (see Ryb & Baer 2004 for explanation and some applications)
An electron subjected to magnetic field moves on a circular (cyclotron) orbit.[2] Classically, any cyclotron radius is acceptable. Quantum-mechanically, only discrete energy levels (Landau levels) are allowed, and since is related to electron's energy, this corresponds to quantized values of. The energy quantization condition obtained by solving Schrödinger's equation reads, for example, for free electrons (in vacuum) or for electrons ingraphene, where.[3] Although the derivation of these results is not difficult, there is an alternative way of deriving them, which offers in some respect better physical insight into the Landau level quantization. This alternative way is based on the semiclassicalBohr–Sommerfeld quantization conditionwhich includes the geometric phase picked up by the electron while it executes its (real-space) motion along the closed loop of the cyclotron orbit.[19] For free electrons, while for electrons in graphene. It turns out that the geometric phase is directly linked to of free electrons and of electrons in graphene.
^ For simplicity, we consider electrons confined to a plane, such as2DEG and magnetic field perpendicular to the plane.
^ is the cyclotron frequency (for free electrons) and is the Fermi velocity (of electrons in graphene).
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