Dynamics of the Selenga river network and delta structure

Geography and Natural Resources

Volumn 29, Issue 4, 2008, Pages 343-347

  Ilyicheva, E A ^a  

^a V B SOCHAVA INSTITUTE OF GEOGRAPHY   (Russian Federation)

Author keywords

channel network; channel forming flow rate; delta; distribution of water flow rate; dynamics of the river system; granulometric composition of bottom sediments; lateral erosion; plane deformation; sediment loads

Indexed keywords

DELTA; EROSION; FLUVIAL DEPOSIT; RIVER BASIN; WATER FLOW;

EURASIA; SELENGA RIVER;

EID: 56549119385     PISSN: 18753728     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.gnr.2008.10.011     Document Type: Article

References (5)

1. Bazhenova O. I. and Martyanova G. N. Formation of extreme morphoclimatic situations in southern Siberia. Geografiya i prirod. resursy, 2004, No. 4, pp. 87-94.
2. Ilyichyova E. A. Structure and dynamics research on the delta of the Selenga river. Proc. 10th Intern. Symp. On River Sedimentation. Moscow, 2007, v. 4, pp. 72-80.
3. Potemkina T. G. Distribution of the runoff and sediments in water streams within the delta of the Selenga river. Geografiya i prirod. resursy, 1995, No. 1, pp. 75-78.
4. Khazheyeva Z. I. and Tulokhonov A. K. Mineral composition of bottom sediments in the branches within the delta of the Selenga river. Proc. Scient. Conf. "Main Factors and Regularities in Different landscape Zones". Ulan-Ude, 2005, pp. 143-146.
5. Ainbund M. M., Davtyan N. A., Sudolsky A. S., and Fialkov V. A. A study on the dynamics of river mouths and near-delta portions of water bodies as exemplified by the Selenga river and Lake Baikal. Proc. IV All-Union Hydrol. Congress. Leningrad, 1975, v. 5, pp. 356-365.