Technical Abstract: Apparent permittivity often has soil-specific temperature responses as well as soil water responses. These variations affect dielectric sensors, often requiring site-specific calibrations. Variations of permittivity as a function of frequency and temperature can be used to calculate activation energies. The purpose of this study was to examine permittivity-temperature responses for six soils, and variation in calculated activation energies. Each of the six soils was packed into a truncated coaxial cell, and the permittivity spectra was determined for a range of water contents and temperatures. Then activations energies were calculated due to ion migration or due to rotation. The rotational activation energy was not correlated with temperature, did not vary across frequencies, and was not significantly affected by soil differences. Ion migration activation energy was significantly less for Cecil (kaolinite and quartz dominant mineralogy) than for Weld or Okoboji (smectites dominant mineralogy). There were significant positive temperature correlation for the dc electrical conductivity and for the real permittivity at low frequencies, but not at higher frequencies. Fraction of sorbed water had a significant correlation with electrical conductivity and real permittivity at a range of frequencies. Delineation of these temperature and activation energy responses is necessary for describing how various soils respond to electromagnetic measurements.