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• W2023666069 startingPage "1019" @default.
• W2023666069 abstract "We examined the ability of soils in six nontidal palustrine forested wetlands (PFOs) in Virginia's Piedmont (PD) and Coastal Plain (CP) to remove dissolved inorganic P from solution, and we compared the P sorption capacities of wetlands with those of streambanks (within wetlands) and adjacent uplands. We hypothesized that wetland soils would have higher P sorption capacities than streambank and upland soils due to the higher concentration of noncrystalline (oxalate‐extractable) Al and Fe (Al o and Fe o ) favored by periodic flooding. We found that P sorption capacities varied both as a function of landscape position and soil depth. Wetlands had higher P sorption capacities than uplands in surface soils (0–15 cm), while below 50 cm the relationship was reversed. Streambank areas within wetlands generally had the lowest P sorption capacities. As hypothesized, Al o was correlated with P sorption capacity in wetland soils , but so was soil organic matter (as estimated by mass loss on ignition [LOI]) ; in fact, Al o and organic matter were positively correlated in wetland soils In contrast, clay and silt content were the two soil parameters most highly positively correlated with P sorption capacity in upland soils Overall, these results suggest that differences in soil chemistry exist among landscape positions (wetland, streambank, upland) that have important implications with regard to P sorption capacity. Since wetlands and uplands may remove P from different hydrologic sources (i.e., surface runoff in wetlands and groundwater in uplands), hydrology may be a key factor in determining water quality functioning." @default.
• W2023666069 created "2016-06-24" @default.
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• W2023666069 date "1999-07-01" @default.
• W2023666069 modified "2023-10-12" @default.
• W2023666069 title "Phosphate Removal Capacity of Palustrine Forested Wetlands and Adjacent Uplands in Virginia" @default.
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• W2023666069 doi "https://doi.org/10.2136/sssaj1999.6341019x" @default.
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