The thermal conductivity of epitaxial layers of Si is measured in the temperature range 300<550 K using time-domain thermoreflectance. The analysis of the thermoreflectance data uses the ratio of the in-phase and out-of-phase signals of the lock-in amplifier to achieve a precision of +/-5%. Comparisons are made between epitaxial layers of isotopically pure Si-28, Si with a natural isotope abundance, and Ge-doped Si. At 297 K, the thermal conductivity of Si-28 epitaxial films is 16+/-5 % larger than the thermal conductivity of natural Si. The thermal resistance created by mass-disorder scattering of phonons is in good agreement with theory for natural Si and for Ge-doped Si with a Ge concentration of 1.4x10(19) cm(-3).
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