We consider a shallow water equation
of Camassa-Holm type, which contains nonlinear dispersive effects
as well as fourth order dissipative effects.
We prove that as the diffusion and dispersion
parameters tend to zero, with a condition on
the relative balance between these two parameters,
smooth solutions of the shallow water equation
converge to discontinuous weak solutions
of a scalar conservation law. The
proof relies on deriving
suitable a priori estimates together
with an application of the compensated
compactness method in the Lp setting
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