Record Display for the EPA National Library Catalog

RECORD NUMBER: 724 OF 868

OLS Field Name OLS Field Data
Main Title Spodosol Variability and Assessment of Response to Acidic Deposition.
Author David, M. B. ; Vance, G. F. ; Fuller, R. D. ; Fernandez, I. J. ; Nodvin., S. C. ;
CORP Author Illinois Univ. at Urbana-Champaign. Dept. of Forestry. ;State Univ. of New York Coll. at Plattsburgh. ;Maine Univ., Orono. ;Tennessee Univ., Knoxville. Dept. of Forestry, Wildlife and Fisheries.;Corvallis Environmental Research Lab., OR.
Publisher c1990
Year Published 1990
Report Number EPA/600/J-90/187;
Stock Number PB91-116798
Additional Subjects Deposition ; Soil analysis ; Chemical properties ; Physical properties ; Experimental design ; Air pollution ; pH ; Reprints ; Forest trees ; Soil-water-plant relationships ; Environmental impact assessments ; Spodosols ; Soil chemistry ; Acid rain
Holdings
Library Call Number Additional Info Location Last
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Status
NTIS  PB91-116798 Most EPA libraries have a fiche copy filed under the call number shown. Check with individual libraries about paper copy. NTIS 03/04/1991
Collation 10p
Abstract
Variability in forest soils makes it difficult to observe short-term changes in chemical properties under field conditions. A buried soil-bag technique was developed to examine the chemical response of a Maine forest soil to loadings of strong acids (HNO3 and H2SO4). Acids were added by irrigation on 18 hardwood plots, 15 by 15 m, American beech (Fagus grandifolia Ehrh.) dominating. Treatments with three replicates each, were control, low S, high S, low N, high N, and N plus S. Soils were typical northeastern Spodosols, with acidic forest floors (pH 3.6) and upper mineral soils (pH 3.4-4.0), low concentrations of base cations in mineral horizons, and enrichment of the spodic horizons with organic C, N, and S. Relative standard deviations (RSD) of horizon means for all chemical properties except pH showed large variability over the small (2.2 h) area encompassed by the plots. Twenty-five 250-micrometers-mesh nylon bags filled with 300 g of homogeneous B horizon soil were placed directly below the forest floor in each plot. After a 1 year of treatment, collection and analysis of three bags per plot showed significant differences. Mean adsorbed SO(-2)4 concentrations were 48 and 92 micrograms S/g in control and high-S treatments, respectively. Exchangeable Ca(2+) and Mg(2+) were greater in the high-S treatment than the control; base saturation increased from 5.9 to 8.5% (possibly due to displacement of cations from the forest floor). The buried soil-bag technique detected small alterations in forest soil chemistry under field conditions, with minimal disturbance to study plots.