Suprathermal electron fluxes measured in the Venus dayside ionosphere in the energy range from 20 to 50 eV are presented for different altitudes, solar zenith angle (SZA), and solar F-10.7 flux. The average flux is nearly constant for SZAs between 0 degrees and 70 degrees and decreases with increasing altitude. The flux increases with the F-10.7 index more rapidly than the square of the plasma peak density does. Close to the terminator, where the production rate of the photoelectrons is small, strong depletions of nearly 1 order of magnitude occur, often at altitudes above 300 km. The photoelectron fluxes were calculated using the two-stream approximation. The calculations reproduce the shape of the observed photoelectron energy spectrum, the SZA, and the solar F-10.7 dependence reasonably well. The decrease of the flux with altitude needs the introduction of either a loss term or a vertical electric field. The best agreement with the data was obtained for an ionosphere with a reflecting ionopause and either a height and energy integrated flow of 1.10(10) cm(-2) s(-1) toward the terminator or an electric field of 12 mV/km.