Hill differential equation

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In mathematics, the Hill equation or Hill differential equation is the second-order linear ordinary differential equation

d2ydt2+f(t)y=0,

where f(t) is a periodic function with minimal period π and average zero. By these we mean that for all t

f(t+π)=f(t),

and

0πf(t)dt=0,

and if p is a number with 0<p<π, the equation f(t+p)=f(t) must fail for some t.[1] It is named after George William Hill, who introduced it in 1886.[2]

Because f(t) has period π, the Hill equation can be rewritten using the Fourier series of f(t):

d2ydt2+(θ0+2n=1θncos(2nt)+m=1ϕmsin(2mt))y=0.

Important special cases of Hill's equation include the Mathieu equation (in which only the terms corresponding to n = 0, 1 are included) and the Meissner equation.

Hill's equation is an important example in the understanding of periodic differential equations. Depending on the exact shape of f(t), solutions may stay bounded for all time, or the amplitude of the oscillations in solutions may grow exponentially.[3] The precise form of the solutions to Hill's equation is described by Floquet theory. Solutions can also be written in terms of Hill determinants.[1]

Aside from its original application to lunar stability,[2] the Hill equation appears in many settings including in modeling of a quadrupole mass spectrometer,[4] as the one-dimensional Schrödinger equation of an electron in a crystal,[5] quantum optics of two-level systems, accelerator physics and electromagnetic structures that are periodic in space[6] and/or in time.[7]

References

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  1. 1.0 1.1 Template:Cite book
  2. 2.0 2.1 Template:Cite journal
  3. Template:Cite book
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  5. Template:Cite journal
  6. Brillouin, L. (1946). Wave Propagation in Periodic Structures: Electric Filters and Crystal Lattices, McGraw–Hill, New York
  7. Template:Cite journal