Two important aspects of short-term thermally stratified energy storag
e, thermocline mixing and thermocline thickness, are studied analytica
lly, experimentally and numerically The storage detrimental aspects ar
e investigated for a simplified configuration, i.e. an adiabatic box c
ontaining a quasi-stationary thermocline. Numerical finite difference/
volume simulations agree well with experiments. The dissipation-free 1
D analytical model shows a large discrepancy. It appears that mixing i
nside thermally stratified stores is a two-stage process. First fluid
is withdrawn from the thermocline by viscous drag. Subsequent mixing t
akes place by stretching and folding of fluid particles, thereby enabl
ing diffusion to become active. Copyright (C) 1996 Elsevier Science Lt
d.