In this paper, a two-phase flow model is presented which simulates the flui
d and sediment motions in the sheet flow regime on a flat bed under oscilla
tory flow conditions. The model is developed based on the continuity equati
ons and linearised momentum equations for the fluid and sediment phases, re
spectively. All major forcing terms such as the intergranular stresses and
the turbulent stress are included in the model. From the detailed computati
ons and comparison with the available laboratory data it has been demonstra
ted that the model is capable of predicting fairly accurately both flow kin
ematics and sediment concentrations. In particular, the model predicts that
the well known phenomenon of fluid velocity over-shoot that exists in clea
r water also appears in the case of lighter sediments but vanishes when the
materials are heavier, which is in perfect accord with the experimental ob
servations considered. (C) 1999 Elsevier Science B.V, All rights reserved.