Title: Can structural and functional characteristics be used to identify riparian zone width in southern Appalachian headwater catchments?
Author: Clinton, Barton ; Vose, James ; Knoepp, Jennifer ; Elliott, Katherine ; Reynolds, Barbara ; Zarnock, Stanley
Source: Canadian Journal Forest Research 40(2):235-253
Description: We characterized structural and functional attributes along hillslope gradients in headwater catchments. We endeavored to identify parameters that described significant transitions along the hillslope. On each of four catchments, we installed eight 50 m transects perpendicular to the stream. Structural attributes included woody and herbaceous vegetation; woody debris and forest floor mass, nitrogen (N) and carbon (C); total soil C and N; litterfall amount and quality by species; and microclimatic conditions. Functional attributes included litter decomposition, soil microarthropods, soil CO2 evolution, soil solution chemistry, and soil extractable N. Forest floor mass, N and C, and soil depth increased with distance from the stream and transitioned between 10 and 20 m. In contrast, litterfall N rate (kilograms of nitrogen per hectare per day), downed woody debris, soil A-horizon C and N, and soil solution NO3 concentration all decreased with distance, and exhibited significant transitions. Certain overstory species were more abundant in the uplands than near the stream. Herbaceous diversity and richness were similar across the hillslope, but species distributions varied in response to hillslope moisture content. Taken together, these results suggest that at 10–20 m from the stream, transitions occur that separate riparian from upland conditions and may provide valuable insight into riparian zone definition.
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Clinton, Barton D.; Vose, James M.; Knoepp, Jennifer D.; Elliott, Katherine J.; Reynolds, Barbara C.; Zarnock, Stanley J. 2010. Can structural and functional characteristics be used to identify riparian zone width in southern Appalachian headwater catchments? Canadian Journal Forest Research 40(2):235-253
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