Claudio Castelnovo, Roderich Moessner and Shivaji Sondhi- Magnetic Monopoles and Spin Ice

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    Magnetic Monopoles and Spin Ice

    Claudio Castelnovo (Oxford)

    Roderich Moessner (MPI-Dresden)

    Shivaji Sondhi (Princeton)

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    Outline

    Spin Ice

    The dipolar puzzle

    Dumbbells

    Monopoles

    Experiments A second gauge field

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    http://ej.iop.org/images/0953-8984/13/50/102/Full/3059601.gif

    The pyrochlore lattice

    FCC lattice with a foursite basis: uptetrahedra sit on theBravais lattice

    If we look along the

    [111] direction,

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    we get a set of

    interleavedKagome andtriangular planes

    These are found in two

    large families of materialsthat take their namesfrom two minerals:1) the pyrochlores A

    2

    B2

    O72) the spinels AB2O4

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    Spin Ice

    The pyrochlores Ho2Ti2O7 and Dy2Ti2O7 do not order tothe lowest temperatures. (Bramwell + Harris, 1997)

    Instead they exhibit a macroscopic low temperatureentropy (Ramirez et al, 1999)

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    Simplest explanation of this behavior is that we have an

    Ising antiferromagnet. However, the local easy axes arethe [111] axes so we postulate

    Anisotropy FM exchange Pseudospins:in and out

    The two in and two out ruleis precisely one of theBernal-Fowler rules for iceand thus we can take overPaulings celebrated

    estimate for the entropy ofice S=(1/2) Log(3/2)

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    Why does spin ice obey the ice rules?

    The ferromagnetic exchange actually arises from thedipolar interaction ferromagnetic when restricted toeasy axes and nearest neighbor sites.

    But then why is the rest of the dipolar interactioninnocuous? (Siddarthan & Shastry, 1999; Gingras andco-workers, 2000-)

    ANSWER The ice rules generate dipolar correlationsamong the spins these are entirely consistent with thelong ranged piece of the dipolar coupling!

    Isakov, Moessner and Sondhi, 2005

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    Dipolar spin ice (contd)

    More specifically could establish a

    THEOREM There exists a model dipole interaction with the

    same long distance asymptotics which has exactly andonly the ice rule ground states.

    Now we can show this much more simply by a related butdifferent route.

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    A step back: the magnetization process

    Moessner and Sondhi, 2003; Isakov, Raman, Moessner and Sondhi, 2004

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    A Second Gauge Field

    Despite the lack of a phase transition there is a

    correlation length (thermal monopole separation) thatdiverges as T->0. This is associated with the emergenceof a second gauge field that characterizes the statisticalproperties of the ground state manifold.

    To understand this think about the ground stateconstraint, which can be turned into a conservation law.This can be done for the O(N) case with vectors spins

    replacing Ising pseudospins:

    (S. Isakov, K. Gregor, R. Moessner and S. L. Sondhi, 2004)Also Henley, Hermele et al; Youngblood and Axe

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    Conservation law

    Orient bonds on the dual diamond lattice from one sublattice to the other

    Define N vector fields on each bond

    on each tetrahedron in grounds states, implies

    at each dual site

    Second ingredient: rotation of closed loops of B connects ground statesWhich implies large density of states near Bav = 0

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    Using these magnetic fields we can construct a coarse grained partitionfunction

    Solve constraint to get Maxwell theory for N gauge fields

    Leads to dipolar spin correlations and entropic Coulombinteractions between monopoles now proportional to T.

    AB

    rr

    =

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    PWA

    1956