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A few aspects regarding sediment yield on the lower reach of Solonet Basin. The sediment yield represents the link between the erosion from the basin and aggradation. Linear and vertical erosion from the low-flow channel as well as slope processes, constitute the main factor in supplying the material for the sediment transport. The Solonet River represents one of the most important affluents of the Suceava River regarding the sediment yield. The correlations made in the current work indicate the particularity of the sediment transporting in the Solonet Basin. In this general context, the informations regarding this phenomenon are very important for knowing the evolution of transporting capacity of the stream.