Add-on to: Determination of Mercury Loads for Cache Creek Settling Basin Inflow and Outflows and Related Investigations Active

The CCSB acts as a sediment trap by capturing the flashy storm flows from Cache Creek and allowing the sediment to settle before exiting into the Yolo Bypass, a flood conveyance that protects the cities of Sacramento and West Sacramento and portions of Sacramento and Yolo County from high flows in the Sacramento River (Figure 1). Previous work by the Regional Water Quality Control Board – Central Valley Region indicates that CCSB traps about half of the input sediment and associated particulate mercury (Wood et al., 2010a). However, because of the flashy nature of Cache Creek and poor historical hydrologic data, available data on loads of sediment and mercury into and out of the CCSB have a large uncertainty. In recent years, DWR has become interested in increasing the storage capacity and the sediment and mercury trapping efficiency of the CCSB. Starting in 2008, DWR has provided funds to the USGS CAWSC Sacramento Field Office (SFO) to improve the flow and sediment record for the CCSB. Stream gages at the outflow and overflow weir of the CCSB were upgraded by USGS. Discharge and suspended sediment data have been collected by the USGS SFO since January 2009. In addition, DWR has contracted with Prof. Lev Kavvas at the Department of Civil Engineering at the Univ. of California, Davis to develop a model of sediment transport, deposition, and trapping efficiency within the CCSB.

In 2009, DWR approached the USGS CAWSC Sacramento Projects Office (SPO) with interest in expanding the monitoring in the CCSB to include mercury (Hg) and methylmercury (MeHg) of the inflow and outflows. There is considerable interest in the CCSB from the Regional Water Quality Control Board – Central Valley Region, as a place where potentially significant load reductions of Hg and MeHg may be achieved in the context of pending regulation under the Total Maximum Daily Loads (TMDL) process. Although the CCSB traps much of the total Hg (THg) from Cache Creek, it is unknown how effective the CCSB is in trapping methylmercury (MeHg), the predominant toxic and bioavailable form of Hg. There is also concern that seasonal wetlands and agricultural fields within the CCSB are areas where Hg is methylated such that there may actually be a net increase of MeHg loads as Cache Creek passes through the CCSB rather than a net removal from particle settling, as is the case with THg. DWR is also concerned that future excavation in the CCSB related to the TMDL might expose sediment with higher THg, possibly leading to higher MeHg.

The CAWSC SPO team has one primary objective and three secondary objectives. The primary objective is to determine THg and MeHg concentrations at the inlet and outlets of the CCSB during storm and non-storm flow (baseline) conditions over five water years and to compute associated loads. Secondary objectives are: (1) to assess the temporal variability of THg and MeHg in sediment and water within the CCSB, (2) to assess the spatial variability in THg and MeHg in sediment and water within the CCSB, and (3) to identify the vertical variability in THg in deep (~9 meter) sediment cores to identify potential layers of high concentration and to ascertain sedimentation history in the CCSB.

The study approach employs both standard monitoring activities and supporting research efforts. The monitoring activities are designed to address the cooperator requests whereas the research efforts are designed to address data gaps that may affect DWR’s ability to manage the CCSB to reduce loads of THg and MeHg. THg can be considered conservative with respect to particles – this allows the simple extension of the sediment model to include THg loadings – though THg concentration differs by particle source and grain size, which likely varies with storm intensity and season. In contrast, MeHg is not conservative and is likely is both produced within the CCSB and lost by settling and microbial and photolytic demethylation reactions. To address the complex behavior of MeHg, we are making some additional measurements to investigate spatial and temporal variations in MeHg and other constituents within the CCSB to ascertain possible factors controlling the magnitude and direction of net MeHg loads. The study approach is organized in six tasks: Task 1. Non-storm (baseline, wet season) sampling of inflow and outflows; Task 2. Storm sampling of inflows and outflows; Task 3a, Water gradient sampling, emphasizing spatial distribution of MeHg and ancillary constituents in riparian wetland (SW) vs. agricultural fields (NE), and upstream (NW) vs. downstream (SE); Task 3b, Biological sampling, emphasizing spatial distribution of MeHg in songbird eggs and blood and in caged mosquitofish; Task 4, Sediment gradient sampling (similar spatial emphasis as Task 3a, with seasonal component); Task 5, Deep cores; Task 6, Load calculations.

The products of the study will be a series of journal articles describing the methods used, data collected, and loads calculated with regard to the inflows and outflows of the CCSB and the spatial and temporal variability of THg and MeHg within the CCSB.