Abstract
Exchanges of total N and C between a river and its floodplain forest have been enhanced by sedimentation processes during flood pulses at a 5-ha bottomland hardwood forest located at the Olentangy River Wetland Research Park in central Ohio. In the spring of 2000, the forest was hydrologically restored by notching an artificial levee that had separated the Olentangy River and its floodplain forest for 100 years. One-hundred flat sediment traps (30 cmX30 cm) were used to collect sediment samples during spring/summer flooding events from 2003 to 2005. Results showed that sediment deposition is determined by the landscape variability during flooding events, Net sediment deposit in the wettest area averaged 134+ or -12 g-dry wt m (super -2) in 2003, 127+ or -17 g-dry wt m (super -2) in 2004 and 149+ or -23 g-dry wt m (super -2) in 2005. Total N and C sedimentation ranged from 0.49 to 0.92 g-N m (super -2) and 5.2 to 19.9 g-C m (super -2) . Fe dominates the sediment chemistry and results show the elemental abundance in the order of Al > Fe > Ca > K > Mg > S > P > Na > Mn > Zn > B > Cu > Mo. A hydrologic pulsing index (HPI) could be used as an indicator for mass changes of energies with hydrologic pulsing events. Restoration of seasonally flooded bottomland forests could stimulate potentially large nutrient and Fe releases, which would eventually lead to an enhanced forest productivity and biodiversity. Abstract Copyright (2007), Wiley Periodicals, Inc.