Cordilleran Section - 109th Annual Meeting (20-22 May 2013)

5
HIGH VARIANCE OF PHYSICAL AND GEOCHEMICAL CHARACTERISTICS OF SALMONID SPAWNING RESTORATION SITES CREATES SUITABLE HABITAT WITHIN THE HYPORHEIC ZONE

Paper No. 5-7
Presentation Time: 3:30 PM

HIGH VARIANCE OF PHYSICAL AND GEOCHEMICAL CHARACTERISTICS OF SALMONID SPAWNING RESTORATION SITES CREATES SUITABLE HABITAT WITHIN THE HYPORHEIC ZONE


JANES, M. Katy, Geology, California State University, Sacramento, 6000 J Street, Sacramento, CA 95819, mkj53@saclink.csus.edu and HORNER, Timothy, Department Head and Professor, Geology, California State University, Sacramento, 6000 J Street, Sacramento, CA 95819
The Lower American River has historically provided natural spawning habitat for approximately one third of Northern California’s salmon population. However, since the construction of Folsom and Nimbus Dams, downstream reaches have become sediment starved and periodic high outflow from the dam has caused channel armoring and incision, thereby degrading the natural spawning habitat. Restoration work on spawning sites in the Lower American River has consisted primarily of importing gravel to create riffles during periods of moderate flow. This is an effort to mitigate armoring of the riverbed and to rehabilitate salmonid spawning habitat by providing suitable grain size for all stages of spawning (redd construction, incubation, and emergence). Since restoration activities began, all rehabilitated sites have not been equally used for spawning. This study attempts to examine and compare the physical properties of each site in order to ascertain which characteristic create more suitable rehabilitated habitat. To do this, we compared restored areas to pre-restoration conditions through the assessment of three main aspects of the restored spawning habitat; grain size and its natural mobility, water flow in the surface and subsurface, and intragravel water quality. We found that some augmentation sites are more heterogeneous than others, and this correlates with higher spawning use. Most spawning was at fin height, and salmonids tend to use sites with higher depth variance (surface features) and higher variance in flow directions and velocities. With time, salmonids alter the spawning sites, creating small ridges and valleys perpendicular to flow. This creates more variable subsurface flow and generates hyporheic flow through the new gravel. This may have an effect on spawning as the more seasoned additions have a higher frequency of spawning than the newer augmentations. In order to efficiently rehabilitate a site and expedite the “seasoning process”, creating variance through gravel contours during the gravel augmentation process may be effective as it mimics the small scale biophysical interactions.