Experimental data for continuous flushing settling basins are presented.The kinematic structure of flow in Dufour-type continuous flushing settling basins differs substantially from the pattern of motion of fluid in intermittent flushing settling basins. In contrast to the latter, the area of the hydraulic section in the process of silt settling is constant over the entire length of a Dufour settler and the velocity has a vertical component known as flushing flow that arrives at the accumulatingflushing gallery through a bottom grating. The presence of a vertical component in the velocity, which is directed downward, causes growth in the rate of deposition of particles and seems to promote a decrease in the effect of the irregular components of the velocity, which are caused by turbulence of the flow, on the settled particles. In addition, in the course of operation of such settling basins the flushing flow varies in accordance with the concentration of the suspended silt, thus affecting the action of the vertical component of the velocity on the particles.The distribution of homogeneous particles on the bottom as they settle in intermittent flushing basins has been studied quite in detail [1 -3]. For Dufour continuous flushing settlers such experimental data are virtually absent.A laboratory study of the distribution of particles settling in Dufour basins was performed at the department of water energy use of the Moscow State Construction University (MGSU) by a graduate student Kaushik Prakash Chandra. A model settler was placed in a glass trough (Fig. 1) with a slope of 0.2. The settler consisted of a head race with a reverse slope of 1:24 and a length of 1.2 m, an inlet baffle located 0.04 m above the bottom grating, a transition segment with direct slope of 1:25 from the inlet baffle to the working chamber of the settler, a working chamber with a accumulating-flushing gallery cut by the bottom grating 1.53 m long,