Abstract

The action of a stream flowing from a nozzle 2mm. in diameter at the velocity of 100-300m/s in eroding solids is investigated. The effect on erosion of the distance from the nozzle and the angle of incidence of the stream is studied. Experiments show that the stream produces the most destruction when the streamis divided. The results can serve as a confirmation of the theory of the destructive action of cavitation, based on the multiple renewal of direct blows delivered to the surface of the solids by the liquid.

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