Riparian roots through time, space and disturbance

Riparian zones are landscape features adjacent to streams and are widely recognized as important in reducing erosion and filtering groundwater. Few studies directly investigate rooting dynamics of riparian areas, and little information exists concerning riparian root densities, biomass, depth profiles, changes through time, or vulnerability to disturbance. This study examined spatial and temporal patterns in root systems in streamsides influenced by season, hydrologic regime, vegetative composition, and ice storm disturbance in the eastern Adirondacks, New York. Sequential root cores and in-growth cores were collected from June 2000 through August 2001 in a riparian area with minimal ice storm damage adjacent to a third-order stream. Data were used to assess seasonal trends in root biomass and to provide a reference for spatial comparisons. The biomass and surface area of roots collected in the reference site cores were compared with cores collected at nine additional riparian sites differing in degree of canopy damage from the January 1998 ice storm. Average root biomass at the reference site was 1330 g/m², comparable to or greater than values reported for terrestrial and other riparian systems. Root biomass varied seasonally with a maximum root biomass in August, 2000; this result was not repeated the following year after the water table inundated much of the rooting zone in mid-June. Root biomass was spatially variable on a range of scales. Although the maximum root surface area occurred in the upper 10 cm, root biomass peaked at 20–30 cm belowground, unlike observations from most other root studies where the maximum root biomass has been found in the top 10 cm. Areas severely damaged by the ice storm had significantly less root biomass and surface area than areas with low damage. This study demonstrates that root biomass in riparian areas is highly dynamic over time, space, and across disturbance sites. Our findings suggest that the spatial variability in root densities has direct implications for riparian vulnerability to erosion.