The Water Quality Consequences of Restoring Wetland Hydrology to a Large Agricultural Watershed in the Southeastern Coastal Plain |
| |
Authors: | Marcelo Ardón Jennifer L Morse Martin W Doyle Emily S Bernhardt |
| |
Institution: | (1) Department of Biology, Duke University, Durham, North Carolina 27708, USA;(2) Department of Geography, University of North Carolina, Chapel Hill, North Carolina 27599, USA |
| |
Abstract: | To ameliorate local and coastal eutrophication, management agencies are increasingly turning to wetland restoration. A large
portion of restoration is occurring in areas that were drained for agriculture. To recover wetland function these areas must
be reflooded and disturbances to soils, including high nutrient content due to past fertilizer use, loss of organic matter
and soil compaction, must be reversed. Here, we quantified nitrogen (N) and phosphorus (P) retention and transformation in
a unique large-scale (440 ha) restored wetland in the North Carolina coastal plain, the Timberlake Restoration Project (TLRP).
For 2 years following restoration, we quantified water and nutrient budgets for this former agricultural field. We anticipated
that TLRP would export high concentrations of inorganic P immediately following reflooding, while retaining or transforming
inorganic N. In the first 2 years after a return to the precipitation and wind-driven hydrology, TLRP retained or transformed
97% of NO3–N, 32% of TDN, 25% of NH4–N, and 53% of soluble reactive phosphorus (SRP) delivered from inflows and precipitation, while exporting 20% more dissolved
organic nitrogen (DON), and 13% more total P (inorganic, organic, and particulate P) than inputs. Areal mass retention rates
of N and P at TLRP were low compared to other restored wetlands; however, the site efficiently retained pulses of fertilizer
NO3–N derived from an upstream farm. This capacity for retaining N pulses indicates that the potential nutrient removal capacity
of TLRP is much higher than measured annual rates. Our results illustrate the importance of considering both organic and inorganic
forms of N and P when assessing the benefits of wetland restoration. We suggest that for wetland restoration to be an efficient
tool in the amelioration of coastal eutrophication a better understanding of the coupled movement of the various forms of
N and P is necessary. |
| |
Keywords: | |
本文献已被 SpringerLink 等数据库收录! |
|