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Dep. Crop and Soil Science, 3017 ALS Bldg., Oregon State Univ., Corvallis, OR 97331;
Delaware Agric. Exp. Stn., Dep. of Plant and Soil Sciences, College of Agriculture and Natural Resources, Univ. of Delaware, Newark, DE 19717-1303.
* Corresponding author (Mary.Schutter{at}orst.edu; or fuhrmann{at}udel.edu).
ABSTRACT
Coal fly ash may be a valuable soil amendment because it contains plant nutrients and liming agents and has a silty texture that can improve the water-holding capacities of sandy, drought-prone soils. Short-term laboratory studies have indicated that addition of unweathered fly ash to soil can stress microbial populations and their activities, but effects of fly ash addition at the field scale are not known. In this study, field plots received 0 or 505 Mg fly ash ha–1 (incorporated by conventional tillage to a depth of 40 cm) and were subsequently cropped to a fallow-corn (Zea mays L.)-wheat (Triticum aestivum L.) rotation or continuous fescue (Festuca arundinacea Schreb.). Twenty months later, during the wheat phase of the rotation, the plots were sampled (0–15 cm) and assayed for activity of soil enzymes (dehydrogenase, alkaline phosphatase, arylsulfatase, and denitrifying enzymes); numbers of aerobic heterotrophs, ammonium oxidizers, denitrifiers, and bradyrhizobia; and N mineralization, nitrification, and denitrification potentials. Nitrification potentials doubled in fly ash-amended soils, and numbers of denitrifiers were 200-fold higher in fescue-cropped, fly ash-amended soils relative to fescue-cropped, non-amended soils. No other large differences in microbial populations or activities were found. The lack of detrimental effects on microorganisms in the field was possibly due to reductions in fly ash's soluble salt and trace element concentrations with time, the mild alkalinity of the fly ash used in this study, and the positive responses of crops to fly ash amendment.
Published as Paper 1634 in the Journal Series of the Delaware Agric. Exp. Stn.
Received for publication November 24, 1997.
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