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- W2034672003 abstract "Selected chemical characteristics of 28 soils from upland sites in northwestern Massachusetts were examined in conjunction with a study of elemental cycling in northern hardwood forests. Acidic silt loam soils (Typic Dystrochrepts and Typic Haplorthods) contained large amounts of dissolved organic carbon (DOC) and soluble SO4 and Al. Chemical correlations in both Ochrepts and Orthods suggest that exchange acidity of organic matter controls pH values near 4.0 in O and A horizons, and that exchange reactions and mineral dissolution produce somewhat higher pH (4.5–5.5) in mineral horizons. The solubility of SO4 and monomeric Al at pH levels from about 3.8 to 5.5 is controlled by organic matter in O and A horizons, and by DOC, pH, and extractable Fe and Al in mineral horizons. Isotherms from three soils show that SO4 dissolved from the O and A horizons will be sorbed by the mineral soil only when concentrations exceed about 8 mg L−1. Stream chemistry suggests that acidic soil solutions are neutralized and soluble Al is sorbed as waters percolate beneath the mineral soil." @default.
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- W2034672003 date "1988-03-01" @default.
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- W2034672003 title "Relations Among Sulfate, Aluminum, Iron, Dissolved Organic Carbon, and pH in Upland Forest Soils of Northwestern Massachusetts" @default.
- W2034672003 doi "https://doi.org/10.2136/sssaj1988.03615995005200020037x" @default.
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