Abstract

The main objectives of this study were to determine the biogeochemical changes taking place in wetlands constructed on coal mine spoil, and to determine the rate at which these constructed wetlands would develop the ecological characteristics of natural wetlands. In 1992 a multicell wetland was constructed. The cells were lined with two coal mine spoil types and one topsoil. In 1993, the cells were planted with cattail ( Typha latifolia), maidencane ( Panicum hemitomon), pickerelweed ( Pontederia lanceolota), and soft stem bulrush ( Scirpus validus). Pickerelweed spread most rapidly followed by maidencane and bulrush. Cattail did not establish uniformly but spread in an irregular manner. There was no difference in plant establishment between the topsoil or the two mine spoils. The pH of the most acidic spoil increased by more than one unit after flooding. Organic matter content fluctuated in all three substrates from year to year. The concentration of the nutrient and metal elements increased after flooding. Extractable Al, Fe, and Mn increased more than other elements. The data presented here indicate that, except for organic matter accumulation, these constructed wetlands have taken on the botanical and biogeochemical characteristics of natural wetlands within 3–4 years.

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