Solar wind data is used to estimate the autocorrelation function for the stochastic process x(tau) = y(t + tau) - y(t), considered as a function of tau, where y(t) is any one of the quantities B-2(t), n(p)(t) V-2(t), or n(p()t). This process has stationary increments and a variance that increases like a power law tau(2y) where gamma is the scaling exponent. For the kinetic energy density and the proton density the scaling exponent is close to the Kolmogorov value gamma = 1/3, for the magnetic energy density it is slightly larger. In all three cases, it is shown that the autocorrelation function estimated from the data agrees with the theoretical autocorrelation function for a self-similar stochastic process with stationary increments and finite variance. This is far from proof, but it suggests that these stochastic processes may be self-similar for time scales in the small scale inertial range of the turbulence, that is, from approximately 10 to 10(3) s. (C) 2007 COSPAR. Published by Elsevier Ltd. All rights reserved.