Natural convection heat transfer in simulated core debris beds has been examined. The debris beds are simulated using electrically heated packed tube bundles arranged in either a square or staggered lattice with porosities varying between 0.31 and 0.95. The effects of bed height, heat generation rate, particle size, porosity, overlying liquid layer height, and top surface boundary condition on the downward and upward power fractions and Nusselt numbers have been determined. Flow patterns within the bed and overlying fluid region have been visualized using particle tracing techniques. Correlations for the downward and upward Nusselt numbers, Nu /SUB B/ and Nu /SUB T/ , as functions of the internal Rayleigh number have been developed. In all cases, the beds are bounded from below by a cooled isothermal surface. When the overlying fluid is bounded from above by a cooled solid isothermal surface, the Nusselt numbers are given by Nu /SUB B/ = 0.424 Ra /SUP 0.226/ and Nu /SUB T/ = 1.61 Ra /SUP 0.220/ . When the upper surface of the overlying fluid is free, the downward Nusselt number is given by Nu /SUB B/ = 0.503 Ra /SUP 0.180/ . These correlations are valid for the ranges 10/sup 2/more » less than or equal to Ra less than or equal to 10/sup 7/ and 0.1 less than or equal to /eta/ less than or equal to 1.0, where /eta/ is the ratio between the heights of the overlying fluid layer and the bed.« less
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