Non-point
Source Pollution (continued)
Numerous other sedimentation-related
studies have been conducted of Illinois’ rivers, including the Illinois
River and its tributaries. The following is a summary of the findings from
these reports:
- Over 50% of the annual sediment yield of Illinois streams results from
stream bed erosion (Roseboom 1986);
- Only a small fraction of soil eroded from upland row crop fields actually
reaches an Illinois stream (Roseboom 1986);
- Total lead (Pb) concentrations in the Illinois River peak between 1920
and 1980; these concentrations sometimes exceed consensus-based Probable
Effects Concentration levels for freshwater sediments (Machesky et al, 2005);
- Local tributaries contribute 65% of the total sediment load to Peoria Lake
in 1989 (White 2005);
- Channel and near-channel sources of sediment have a higher rate of sediment
deliver to water bodies than do other areas within a river basin (White
2005);
- Stream bank
erosion can contribute a significant amount of sediment to rivers
(White 2005):
- In the Court Creek basin, streambank
erosion constitutes more than 50% of the sediment yield.
- More than 40% of the sediment in the Spoon
River results from bank erosion.
- Ninety percent of channel sediments eroded
from unstable stream systems originate from streambanks.
- In 1990, the average capacity loss of the 60 backwater lakes associated
with the Illinois River is 70%, with some losing as much as 100% of their
capacities (Bhowmik 1999).
Studies of Peoria Lake by researchers at the ISWS indicate the dramatic changes
that occur from 1903 and 1985. The lake has lost about 68% of its 1903 average
capacity and the average depth has reduced to 2 feet compared to the 1903 depth
of 8 feet. It is estimated that this lake lost an additional 15% or more of
its capacity by late 1999. Tables 39a and 39b show these changes in volume
and depth over this period.
Table 39a: Volume of Peoria Lake at 440 feet msl (Bhowmik 1999)
| |
Volume (acre-feet) |
| Year |
Upper Peoria Lake |
Lower Peoria Lake |
Peoria Lake
(Upper plus Lower) |
| 1903 |
96,000 |
24,000 |
120,000 |
| 1965 |
55,200 |
17,700 |
72,900 |
| 1976 |
42,200 |
14,400 |
56,600 |
| 1985 |
26,500 |
11,800 |
38,300 |
Table 39b: Average Depth of Peoria Lake at 440 feet msl (Bhowmik 1999)
| |
Average Depth (ft) |
| Year |
Upper Peoria Lake |
Lower Peoria Lake |
Peoria Lake
(Upper plus Lower) |
| 1903 |
7.6 |
9.8 |
8.0 |
| 1965 |
4.4 |
7.2 |
4.8 |
| 1976 |
3.4 |
5.9 |
3.8 |
| 1985 |
2.0 |
5.3 |
2.6 |