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The magnitude of reject heat, the distances to which sensible heat cffects may be experienced in a river and alternate means of rejccting heat are discussed.Steam electric generating stations, fossil...
The longitudinal current sorting of graded sediment is analysed by use of a sediment transport formula developed recently by Engelund and Fredsae (1976). The analysis yields that for a given longitu...
A one-dimensional numerical model was used to simulate water stage and dispersion of matter in a stream. The calculated results show quite good agreement with field measurements. Studies concerning...
If the im$act of longitudinal density gradient on the hydrodynamics of estuaries is negligible, then in water quality simulations, the hydrodynamics can be decoupled from the mass transport which wo...
An Aggregated Dead Zone (ADZ) model is presented for longitudinal dispersion of tracer in river channels, in which the channel cross-section is divided into two parallel regions: the bulk flow and dea...
The classical one-dimensional advection-diffusion equation (ADE) gives an inadequate description of tracer cloud evolution in the River Severn, U.K. A solute transport model incorporating the effects ...
A tracer experiment using Rhodamine WT dye was carried out to measure longitudinal dispersion in a 14-km reach of the River Severn in Wales, U.K. The river’s discharge was measured at six points and t...

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