A few aspects regarding sediment yield on the lower reach of Solonet Basin.

Florin OBREJA

Abstract


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.


Keywords


sediment yiled, erosion, aggradation, correlation, low-flow chanel

Full Text:

PDF

References


B c uanu V., i col. (1980), Podi ul Moldovei, Editura stiintific si Enciclopedic , Bucure ti

Diaconu C., Blaga O., Lazarescu D. (1978), Hidraulic i hidrologie, Editura Didactic i

Pedagogic , Bucure ti

Diaconu C., erban P. (1994), Sinteze i regionaliz ri hidrologice, Editura tehnic , Bucure ti

Olariu P. (2004), esul Sucevei Extracarpatice Studiu de geomorfologie aplicat , Editura

Alma Mater, Bac u

Posea G. (2002), Geomorfologia României, Editura Funda iei România de Mâine, Bucure ti

R doane N. (2002), Geomorfologia bazinelor hidrografice mici, Editura Universit ii

Suceava

R doane M., R doane N. (2007), Geomorfologie aplicat , Editura Universit ii Suceava