Geochemical stability of acid-generating pyrrhotite tailings 4 to 5 years after addition of oxygen-consuming organic covers.

Oxygen-consuming organic covers can serve as a reactive barrier to minimize sulfide oxidation in acid-generating tailings but may lead to metal mobilization in surface oxidized layers. We evaluated changes in the bio-geochemical stability of acid-generating, Cu-Ni pyrrhotite tailings 4 to 5 years after addition of a 50 cm-thick or a 1 m-thick biosolid cover planted with energy crops. The original tailings (pH 2.5) were oxidized in the first 10 to 40 cm, and goethite was the dominant sink for Cu and Ni, the main metal contaminants in these tailings. Both covers increased pH, nutrient availability, microbial activity and diversity in the oxidized tailings, and led to a reduction of water-soluble Cu, Ni, Fe and Al after 4 to 5 years of application. Changes in pH, humidity, organic C content, and redox conditions resulted in partial dissolution of jarosite and gypsum below the cover but goethite apparently remained stable. Under both covers, total Ni decreased in the oxidized layer, indicating remobilization, but Cu was retained. Significant accumulation of Cu as Cu sulfide at the oxidized/unoxidized tailings interface was detected only under the 1 m-thick cover, suggesting that the thinner cover may not sufficiently decrease the oxidizing conditions to mitigate acid mine drainage. Migration of nitrate and P down to the unoxidized tailings was observed under both covers and raises the concern of continued sulfide oxidation in unoxidized tailings. Although the implementation of thinner covers is economically more sustainable than thick covers, our results indicate that further research is required to establish their long-term suitability and performance to prevent acid mine drainage.

Measuring and modeling the effects of drainage water management on soil greenhouse gas fluxes from corn and soybean fields.

Controlled tile drainage can boost crop yields and improve water quality, but it also has the potential to increase GHG emissions. This study compared in-situ chamber-based measures of soil CH4, N2O, and CO2 fluxes for silt loam soil under corn and soybean cropping with conventional tile drainage (UTD) and controlled tile drainage (CTD). A semi-empirical model (NEMIS-NOE) was also used to predict soil N2O fluxes from soils using observed soil data. Observed N2O and CH4 fluxes between UTD and CTD fields during the farming season were not significantly different at 0.05 level. Soils were primarily a sink for CH4 but in some cases a source (sources were associated exclusively with CTD). The average N2O fluxes measured ranged between 0.003 and 0.028 kg N ha(-1) day(-1). There were some significantly higher (p ≤ 0.05) CO2 fluxes associated with CTD relative to UTD during some years of study. Correlation analyses indicated that the shallower the water table, the greater the CO2 fluxes. Higher corn plant C for CTD tended to offset estimated higher CTD CO2 C losses via soil respiration by ∼100-300 kg C ha(-1). There were good fits between observed and predicted (NEMIS-NOE) N2O fluxes for corn (R(2) = 0.70) and soybean (R(2) = 0.53). Predicted N2O fluxes were higher for CTD for approximately 70% of the paired-field study periods suggesting that soil physical factors, such as water-filled pore space, imposed by CTD have potentially strong impacts on net N fluxes. Model predictions of daily cumulative N2O fluxes for the agronomically-active study period for corn-CTD and corn-UTD, as a percentage of total N fertilizer applied, were 3.1% and 2.6%, respectively. For predicted N2O fluxes on basis of yield units, indices were 0.0005 and 0.0004 (kg N kg(-1) crop grain yield) for CTD and UTD corn fields, respectively, and 0.0011 and 0.0005 for CTD and UTD soybean fields, respectively.

Isotopic evidence for the provenance and turnover of organic carbon by soil microorganisms in the Antarctic dry valleys.

The extremely cold and arid Antarctic dry valleys are one of the most environmentally harsh terrestrial ecosystems supporting organisms in which the biogeochemical transformations of carbon are exclusively driven by microorganisms. The natural abundance of (13)C and (15)N in source organic materials and soils have been examined to obtain evidence for the provenance of the soil organic matter and the C loss as CO(2) during extended incubation (approximately 1200 days at 10 degrees C under moist conditions) has been used to determine the potential decay of soil organic C. The organic matter in soils remote from sources of liquid water or where lacustrine productivity was low had isotope signatures characteristic of endolithic (lichen) sources, whereas at more sheltered and productive sites, the organic matter in the soils that was a mixture mainly lacustrine detritus and moss-derived organic matter. Soil organic C declined by up to 42% during extended incubation under laboratory conditions (equivalent to 50-73 years in the field on a thermal time basis), indicating relatively fast turnover, consistent with previous studies indicating mean residence times for soil organic C in dry valley soils in the range 52-123 years and also with recent inputs of relatively labile source materials.

Controls on the distribution of productivity and organic resources in Antarctic Dry Valley soils.

The Antarctic Dry Valleys are regarded as one of the harshest terrestrial habitats on Earth because of the extremely cold and dry conditions. Despite the extreme environment and scarcity of conspicuous primary producers, the soils contain organic carbon and heterotrophic micro-organisms and invertebrates. Potential sources of organic compounds to sustain soil organisms include in situ primary production by micro-organisms and mosses, spatial subsidies from lacustrine and marine-derived detritus, and temporal subsidies ('legacies') from ancient lake deposits. The contributions from these sources at different sites are likely to be influenced by local environmental conditions, especially soil moisture content, position in the landscape in relation to lake level oscillations and legacies from previous geomorphic processes. Here we review the abiotic factors that influence biological activity in Dry Valley soils and present a conceptual model that summarizes mechanisms leading to organic resources therein.