Huma Alvarado's research while affiliated with University of North Carolina at Asheville and other places

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Publications (1)


Figure 1: Mean water table depth in depression and ridge plots at Tulula Wetlands Mitigation Bank during the study period. Site hydrology was restored in winter 2001.
Figure 2: Total precipitation received at Tulula Wetlands Mitigation Bank from March to August each year during the study period.
Figure 3: Total cover (per 0.25-m2 quadrat) in depression and ridge plots at Tulula Wetlands Mitigation Bank over a 6-year period for (a) OBL species, (b) FACW species, (c) FAC species, (d) FACU species, and (e) UPL species.
Mean (SD) soil properties of six depression and ridge plots at Tulula Wetlands Mitigation Bank in 2000 and 2005.
Succession of a Southern Appalachian Mountain Wetland Six Years following Hydrologic and Microtopographic Restoration
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April 2008

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229 Reads

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20 Citations

Restoration Ecology

Irene M. Rossell

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Kevin K. Moorhead

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Huma Alvarado

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Microtopography, which is known to play a key role in the structure and function of wetland communities, is receiving increasing attention in wetland restoration projects. One goal of the Tulula Wetlands Mitigation Bank, which was the first large-scale wetland restoration project in the Blue Ridge Province, was to restore the microtopography in a degraded swamp forest–bog complex. This wetland type has become increasingly rare in the southern Appalachians and is characterized by a distinct microtopography of depressions and low ridges. We examined vegetation and soils in depression and ridge plots over a 6-year period, during which the hydrology and microtopography of the floodplain were restored. Our results showed that the flora of the depression and ridge plots differed, with greater coverage by obligate wetland species in the depression plots but greater overall taxonomic richness in the ridge plots. The edaphic characteristics that we measured varied very little during the study period. Creating microtopographic relief during the restoration of this wetland seems to have provided a variety of niches and may have increased the likelihood that the site will succeed back to a swamp forest–bog complex, rather than as a forested terrace of Tulula Creek.

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Citations (1)


... Mixing highly compacted underlying peat with the anthropogenic aquifer materials is likely to produce several important changes that will contribute to a successful restoration. One increasingly popular technique for breaking up these layers is through the creation of microtopography, which is showing promising results (e.g., Moser et al., 2007;Rossell et al., 2009). Microtopography creates ground surface elevations that span from below the water table (generating small ponds where amphibians and other aquatic creatures can thrive), to well above it, creating a range of habitats. ...

Reference:

Recovering groundwater for wetlands from an anthropogenic aquifer
Succession of a Southern Appalachian Mountain Wetland Six Years following Hydrologic and Microtopographic Restoration

Restoration Ecology