AN APPROXIMATION OF THE SEDIMENT BUDGET OF THE LOWER MISSISSIPPI RIVER PRIOR TO MAJOR HUMAN-MODIFICATION

被引:94
作者
KESEL, RH
YODIS, EG
MCCRAW, DJ
机构
[1] NICHOLLS STATE UNIV,DEPT EARTH SCI,THIBODAUX,LA 70310
[2] LOUISIANA GEOL SURVEY,BATON ROUGE,LA 70803
关键词
MISSISSIPPI; RIVER; SEDIMENT BUDGET; SEDIMENT DISCHARGE; BEDLOAD; ALLUVIAL RIVER; HUMAN MODIFICATION;
D O I
10.1002/esp.3290170707
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
A sediment budget is constructed for the Lower Mississippi River prior to the introduction of most human modifications. Components of the budget are derived from historical data including Mississippi River Commission hydrographic survey maps for the period from 1877 to 1924. A quantitative estimate of major sediment sources, sinks and storage locations in the Lower Mississippi Valley suggest that the most important sediment source was from bank caving and that at least 50 per cent more sediment was deposited in short-term channel storage than in longer-term overbank storage. The budget indicates that the proportion of sediment transported as bedload was significantly greater than previously estimated. The magnitude and variability of these sediment budget components are discussed. The results of the study suggest that prior to modifications the river was aggrading over much of its length.
引用
收藏
页码:711 / 722
页数:12
相关论文
共 31 条
[1]  
[Anonymous], 1977, FLUVIAL SYSTEM
[2]  
ELLIOTT DO, 1932, IMPROVEMENT LOWER MI
[3]  
Fisk H.N., 1960, J SEDIMENT PETROL, V24, P76, DOI [10.1306/D4269661-2B26-11D7-8648000102C1865D, DOI 10.1306/D4269661-2B26-11D7-8648000102C1865D]
[4]  
Fisk H.N., 1944, GEOLOGICAL INVESTIGA
[5]  
FISK HN, 1943, UNPUB GEOLOGICAL REP
[6]  
HOLLE CG, 1952, 2ND P C COAST ENG, P111
[7]  
Ikeda H., 1989, RIVER MEANDERING, P51, DOI [10.1029/WM012p0051, DOI 10.1029/WM012P0051]
[8]   HISTORIC TRENDS IN THE SEDIMENT FLOW REGIME OF THE MISSISSIPPI RIVER [J].
KEOWN, MP ;
DARDEAU, EA ;
CAUSEY, EM .
WATER RESOURCES RESEARCH, 1986, 22 (11) :1555-1564
[9]  
Kesel R.H., 1974, GEOLOGY, P461, DOI [10.1130/0091-7613(1974)22.0.CO
[10]  
2, DOI 10.1130/0091-7613(1974)2<461:LEAODO>2.0.CO