SUMMARYThis study employed a direct numerical simulation (DNS) technique to contrast the plume behaviours and mixing of passive scalar emitted from line sources (aligned with the spanwise direction) in neutrally and unstably stratiÿed open-channel ows. The DNS model was developed using the Galerkin ÿnite element method (FEM) employing trilinear brick elements with equal-order interpolating polynomials that solved the momentum and continuity equations, together with conservation of energy and mass equations in incompressible ow. The second-order accurate fractional-step method was used to handle the implicit velocity-pressure coupling in incompressible ow. It also segregated the solution to the advection and di usion terms, which were then integrated in time, respectively, by the explicit thirdorder accurate Runge-Kutta method and the implicit second-order accurate Crank-Nicolson method. The buoyancy term under unstable stratiÿcation was integrated in time explicitly by the ÿrst-order accurate Euler method. The DNS FEM model calculated the scalar-plume development and the mean plume path. In particular, it calculated the plume meandering in the wall-normal direction under unstable stratiÿcation that agreed well with the laboratory and ÿeld measurements, as well as previous modelling results available in literature.