Soil microbiological properties 20 years after surface mine reclamation: spatial analysis of reclaimed and undisturbed sites

Abstract

Spatial characteristics of soil microbial community structure and selected soil chemical factors were analyzed in soil surrounding Agropyron smithii (Western wheatgrass) and Artemisia tridentata (Wyoming big sagebrush) plants in sites reclaimed after surface mining and adjacent undisturbed sites in Wyoming. Microbial biomass C (MBC) and fatty acid methyl ester (FAME) biomarkers for total biomass, bacteria, and fungi were used as indicators of soil microbial community abundance and structure. In soil 20 years after reclamation FAME total microbial biomass, bacterial and fungal biomarkers, MBC and soil organic matter (SOM) averaged only 20, 16, 28, 44 and 36% of values found in undisturbed soils. In contrast to undisturbed soils, FAME biomarkers and MBC of reclaimed soils exhibited spatial correlation up to 42 cm. Reclaimed soils also exhibited localized enrichment of bacterial, fungal, and total microbial biomass, as well as depletion of inorganic N concentrations, around plant bases (<10 cm), suggesting relatively poor soil exploration by roots and microorganisms compared to the undisturbed ecosystem. Strong spatial stratification of undisturbed SOM and soil NH 4 + pools was found with highest concentrations on the leeward side of shrubs, likely due to localized changes in microclimate and plant litter deposition. This indicates that shrub cover plays a central role in the establishment of site heterogeneity and regulation of ecological processes, such as C and N mineralization and immobilization, which has important implications for reclamation.