Sediments and sediment-derived soils in Illinois: pedological and agronomic assessment

Dredging sediments from water bodies in Illinois is done topreserve reservoir capacity, maintain navigation and recreationchannels, and restore habitats, but the fate of the sediments is an issue. In anticipation of a major sediment dredging operationin Lake Peoria in the Illinois River, a retrospective study ofsediment placement operations was performed. Sedimentspreviously dredged from reservoirs and placed in retaining pondswere sampled along with adjacent upland soils which served asreferences. Sediments from the Illinois River above Peoria weresampled from islands, river bottom, and adjacent floodplain. Dredged sediment retention ponds initially support wetlandvegetation. After dewatering, the physical properties of sediments tend to become similar to upland soils and theretention basins are then able to support conventionalagriculture. Sediment organic matter content was similar to localreference surface soils, and soil pH of the sediments wasneutral or above. Sediment textures are dominated by silts and clays, with the Lake Peoria samples being most clayey. Calcium was the dominant cation in all the samples, and micronutrientsmeasured were in adequate supply for plant growth. However,because the Illinois River watershed includes industrial inputs,river sediments contained elevated levels of some metals, butthey were generally below levels of regulatory concern. Resultsindicated that properly handled dredge sediments could make highquality agricultural soils. In addition, sediment placement onpoor soils could improve their productivity.