Steady flows that optimize heat transport are obtained for two-dimensional Rayleigh-B'enard convection with no-slip horizontal walls for a variety of Prandtl numbers and Rayleigh number up to . Power law scalings of are observed with , where the Nusselt number is a non-dimensional measure of the vertical heat transport. Any dependence of the scaling exponent on is found to be extremely weak. On the other hand, the presence of two local maxima of with different horizontal wavenumbers at the same leads to the emergence of two different flow structures as candidates for optimizing the heat transport. For , optimal transport is achieved at the smaller maximal wavenumber. In these fluids, the optimal structure is a plume of warm rising fluid which spawns left/right horizontal arms near the top of the channel, leading to downdrafts adjacent to the central updraft. For at high-enough Ra, the optimal structure is a single updraft absent significant horizontal structure, and characterized by the larger maximal wavenumber.

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