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HNA Summary Report
The Role of Disturbance in the UMRS Ecosystem

Large rivers are dynamic ecosystems where habitats evolved and persist in response to a variety of natural and human-caused disturbances (see Table 1). Floods and droughts are natural disturbances that occur seasonally, but exhibit an approximately decadal cycle of extreme events on the UMRS. Seasonal flooding drives a highly productive and diverse ecosystem.

Sediment transport and channel-forming processes are active continuously. Channel and floodplain geometry can change slowly over a period of decades or rapidly during extreme floods. Impoundment and river regulation for navigation have significantly modified the hydrologic regime and the pattern of sedimentation.

Table 1. Ecological Disturbances

Natural Man Made
Flood
Drought
Sedimentation
Channel migration
Sediment resuspension
Fire
Ice shear
Tree wind-throw
Log jam
Beavers
Water level regulation
Dredging and dredged
material disposal
Channel training structures
Boat generated waves
Levee construction
Agriculture
Nutrient enrichment
Logging
Urban development
Contaminants
Mississippi River - flood of 1993
The great flood of 1993 was one of the country’s worst disasters.

Fire was once a dominant force maintaining floodplain grassland-savanna landscapes. Ice flows, tree falls, and log jams are all natural occurrences that help define local habitats and maintain high habitat diversity. Biological disturbances (e.g., beavers) are important in the development of floodplain landscapes.

Impoundment, water level regulation, channelization, levee construction, logging, and urban and agricultural development are the dominant human activities affecting river habitats on the UMRS. Navigation dams converted free flowing rivers to a series of shallow impoundments. Portions of the floodplain were permanently flooded by the dams and backwater area increased significantly in some river reaches (Fig. 4). Since impoundment, sedimentation of backwaters, island loss, and loss of secondary channels have greatly modified the pattern of river habitats.

Rock wing dams, closing dams, and bank revetments are used to maintain the navigation channel and to reduce dredging requirements. These structures decrease bank erosion and force flow into the main river channel. In the Open River reach, channel training structures have greatly reduced the number and quality of secondary channels (Fig. 5). There has also been loss of channel area as sediment filled the area between wing dams.

Much of the floodplain south of Pool 16 on the Mississippi River and on the La Grange and Alton pools on the Illinois River has been isolated by levees. The distribution of levees as proportion of total floodplain area is about:

  • 3 percent north of Pool 13;
  • 50 percent from Pool 14 through Pool 26;
  • 80 percent in the Open River; and
  • 60 percent of the lower 160 miles of the Illinois River.

In total, more than 1.1 million acres, mostly agricultural land, are protected from moderate floods by levees.

Logging has caused significant habitat degradation throughout the river floodplains and northern parts of the basin. Logging was necessary to supply fuel-wood for steamboats and railroads, firewood for heat and cooking, and lumber to build cities. In most floodplain areas deforested land was rapidly converted to agriculture. The impact is particularly dramatic below the Kaskaskia River where the densely forested floodplain was almost completely cleared (Fig. 6). Deforestation and agricultural conversion throughout the basin increased sediment delivery to the mainstem rivers.

Urban development displaced native habitats, but also caused indirect impacts. Sewage and industrial pollution caused significant water quality problems that eradicated sensitive species downstream of large cities. The problem has subsided since the 1970s.

 
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