Title: Baseline Deposition Rates, LeadRich Sediment, Coeur dAlene CdA River Floodplain, Idaho Arthur Bookst
1Baseline Deposition Rates, Lead-Rich Sediment,
Coeur dAlene (CdA) River Floodplain, Idaho
Arthur Bookstrom, Stephen Box, Robert Fousek
- Mill tailings and floods in the CdA drainage
basin, - Lead-rich sediments on the CdA River floodplain,
- Baseline rates of sediment deposition,
- Baseline concentrations of lead (Pb) in
sediments, - Secondary sources of Pb-rich sediment,
- Continuing deposition of Pb-rich sediments.
2Location map
3Production and Tailings Management
4History of Flooding
5Block Diagram of Floodplain
6Star Mill - south fork Coeur d Alene River
71933 Flood Smelterville Flats, Idaho
Rose Lake, Idaho
8Lead in Surficial Sediments
9Section of Pb-Rich Sediments
1980 Mt. St. Helens volcanic ash layer
Riverbank near Medimont in 1993
Base of section of Pb-rich sediments
10Lead-Concentration Profiles
11Pre- and Post-1969 Rates of Sediment Deposition
in Medicine Lake
12Summary of Baseline Depositional Rates and Lead
Concentrations
13Baseline Depositional Rates
1.8
3.0
7.4
14Lateral Variation in Baseline Rates of Sediment
Deposition
28.5
15Baseline Lead Concentrations
1500
2800
4500
16Lateral Variation in Baseline Lead Concentrations
7500
17Box plots of historic and baseline
sediment-deposition rates
18Box plots of Pb concentrations in sediments of
successive time intervals
n 13
n 13
90th percentile
75th
4000
50th
3300
25th
10th
Figure 23. Box-and-whisker plots, comparing
interval-weighted average lead
(ppm Pb) in sediments of the early
post-tailings-release (BA1) and baseline (AA)
time-stratigraphic intervals.
19Percentages of tailings-derived Pb in
sediments by drainage basin, and by
depositional setting
20Lead Concentrations in Suspended Sediment
211996 Scour of Pb-Rich Sediments in the River
near Dudley
Approximate location of drill hole 94VCD2
River bottom before 1996 flood
Sandy active bed sediment (poorly stratified)
Scoured zone
Stored Pb-rich sediments (well stratified)
Log exposed by flood scour
22Secondary Sourcesof Pb-Rich Sedimentin the
River Channel