Water Resources Collections and Archives

Aquatic ecosystems in the Upper Klamath Basin (Upper Basin), Oregon are degraded as a result of more than a century of land use alterations due to logging, dams, irrigated agriculture, and cattle grazing. These changes have led to degraded habitat conditions including decreased baseflow, loss of vegetation, increased stream temperature, fish impediments, and nutrient loading. All these factors negatively impact watershed function and resident fish populations, which have experienced severe declines in recent decades. The primary threats to fish populations include habitat loss, degraded water quality, barriers and entrainment, and predation and competition from non-native species. Millions of dollars have been spent since the late-1900’s to restore aquatic habitat in the Upper Basin primarily to improve the distribution and abundance of endangered and threatened fish species. This project details the hydrologic characteristics of three primary tributaries in the Upper Klamath Lake Sub-Basin including Sevenmile Creek, Wood River, and the Williamson River (including spring tributaries). Available discharge data was assembled to plot seasonal fluctuations in flows and identify annual peak flow at different re-occurrence intervals. Stream systems in the UKL Sub-Basin show a range of hydrologic inflow due to groundwater and/or snow-melt run-off. Characteristics of spring-fed vs. run-off dominated stream systems are reviewed and recommendations are made for how to address restoration practices considering the hydrologic and geomorphic characteristics of stream channels.

Livestock grazing in the western United States has lead to riparian ecosystem and stream channel degradation. Establishing fenced-off exclosures is a common management strategy that aims to passively restore these areas, however, relatively few studies have assessed the evolution of exclosed reaches over time. We evaluated temporal trends in channel form and riparian vegetation along a 4.2 km reach of Long Creek (drainage area of 180 km2), a tributary to Sycan Marsh in western Lake County, Oregon. The Nature Conservancy implemented reduced livestock grazing along this reach in 1996 and complete exclosure in 1999. Based on previous studies that documented vegetation establishment and subsequent sediment accumulation on channel banks, we hypothesized that the channel would have narrowed and vegetation would have re-established after eleven years of cattle exclosure.   In October 2011, we surveyed seven previously-established cross sections and compared channel geometry in 2011 to surveys conducted since 1990. We also took photos at these locations and compared them to historical images. We found no consistent trend in channel morphology, but two cross sections demonstrated narrowing, one of which was likely driven by reduced flow velocity from a downstream beaver dam. Vegetation had successfully established along the streambanks, but in addition to the riparian species, upland lodgepole pines were also abundant along the channel and on the floodplain.  Our results suggest that beavers should be encouraged so their dams will increase overbank flow and discourage the invasion of upland plant species. We also propose improvements in monitoring methods to ensure repeatability of cross-sections over an extended monitoring period.  

Our study attempts to assess how different methods of engaging student volunteers on Berkeley’s campus impact student’s enthusiasm for stewardship, such as their willingness to participate in future on or off-campus restoration projects.  Using a questionnaire and targeting four different undergraduate student groups, including students who lived adjacent to Strawberry Creek, we attempted to gauge their current involvement and future involvement in stream restoration activities.  We found that academic work is the strongest method of engaging student volunteers and that some form of spontaneous use is the best indicator of each student’s enthusiasm for future stewardship. In summary, student stewards can provide the link between academic solutions and collaborative engagement with urban creeks.

In  California’s  Central  Valley,  dams  block  95  percent  of  historic  salmonid  habitat.    To  restore access by spring-run chinook salmon (Onocorhynchus tshawytscha) and other anadromous fish to approximately 12 miles of upstream spawning habitat on Clear Creek (drainage areas 720 km 2 ), the  US  Bureau  of  Reclamation  removed  the  McCormick-Saeltzer  Dam  in  November  2000.Previous  studies—the  most  recent  in  2004—identified  significant  sediment  mobilization  since dam removal at, and above, the former dam site.  In October 2011, we resurveyed two previously established  cross  sections at 26  m and 103.3  m upstream  of  the  dam  site  and  conducted  a  long profile  of  the  thalweg  from  the  dam  site  to  175  m  upstream.   We  also  replicated  previous  site photographs,  drew  vegetation  maps  and  compared  2010  aerial  photographs  to  those  from  1998 and  2004  to  assess  vegetation  change  and  erosion  patterns.   Our  results  documented  little incremental  erosion  at  and  upstream  of  the  dam  site  since  2004,  suggesting  that  sediment mobilization post-dam removal has largely stopped.  Establishment of riparian vegetation may be stabilizing remaining sediment deposits.

ABSTRACT

A 700-foot-long daylighted reach of Cerrito Creek defines the southern border of the 29-acre El Cerrito Plaza shopping center and receives a majority of the Plaza’s stormwater runoff. In 2003, this reach, between Talbot and Kains Avenues, underwent a restoration project that widened, re-graded and re-vegetated the channel as well as added a gravel pedestrian path parallel to the stream. The project was completed while the shopping center and parking lot underwent a major renovation. In this study, we assessed current creek conditions and compared them to the original project design as well as a 2005 post-project assessment. We found that there may have been minor channel incision since 2005, but this evidence was unreliable due to the cross section locations having not been permanently monumented. An increase in the number  of gravel bars, and an increase in the diversity of sediment size indicated that the stream was transporting sediment. Native vegetation planted during the restoration appeared to be flourishing, although we documented a few invasive species that have established as well. Although the creek restoration was successful at creating wildlife habitat and a new amenity for the public, it did not address the treatment of stormwater, raising concerns about the impacts of potentially harmful urban runoff on creek water quality. We considered options to retrofit stormwater management infrastructure and concluded that flow-through biofiltration structures such as sand filters, basins, or planters would be most feasible based on the local soil conditions and available land area.