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Biological Opinions - Bureau of Reclamation

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concentrations reach about 2 mg/L, and by about 1.5 mg/L most suckers die (Martin and Saiki<br />

1999). The lethal DO threshold for adult suckers is unknown, but likely is similar to juveniles.<br />

In tributaries to UKL, limited data indicate that DO varies from greater than 7 to 13 mg/L<br />

(ODEQ 2002). Concentrations in the lakes within the recovery unit exhibit seasonal and spatial<br />

variability, ranging from less than 4 mg/L to greater than 10 mg/L. Water quality datasets<br />

collected by the Klamath tribes include weeks during the summer months when DO levels in<br />

UKL are consistently below the ODEQ criterion <strong>of</strong> 5.5 mg/L for support <strong>of</strong> warm-water aquatic<br />

life (Kann 2010). Low (0 to 4 mg/L) DO concentrations occur most frequently in August, the<br />

period <strong>of</strong> declining algal blooms and warm water temperatures in the lake (Walker 2001, ODEQ<br />

2002). Morace (2007) provided a detailed review <strong>of</strong> DO concentrations in UKL, based on 17<br />

years <strong>of</strong> data (1990–2006), and Jassby and Kann (2010) conducted a similar review based on an<br />

additional 3 years (1990–2009) <strong>of</strong> data collection.<br />

Downstream in Keno Reservoir, DO reaches very low levels (< 1 to 2 mg/L) during July and<br />

October as algae transported from UKL settle out <strong>of</strong> the water and decay. Persistent low DO<br />

events in this reach, where the DO remains less than 2 mg/L, can last for several days or even<br />

weeks. Decomposition <strong>of</strong> algae transported from UKL appears to be the primary driver <strong>of</strong> low<br />

oxygen in the Keno Reservoir. Two water treatment facilities discharge treated wastewater to<br />

the Keno Reservoir; however, these facilities contribute a very small amount (100 percent saturation) in surface waters (due to high rates <strong>of</strong> internal<br />

photosynthesis by algae) and oxygen depletion in bottom waters (due to microbial decomposition<br />

<strong>of</strong> dead algae). Although J.C. Boyle Reservoir, a relatively long shallow reservoir, does not<br />

stratify, large variations in DO are observed at its discharge due to high oxygen demand from<br />

water conditions in the upstream reach from Link River Dam through the Keno Reservoir, and in<br />

UKL. Copco 1 and Iron Gate Reservoirs thermally stratify beginning in April/May and do not<br />

mix again until October/November (FERC 2007). DO in Iron Gate and Copco 1 surface waters<br />

during summer months is generally at or, in some cases, above saturation, while levels in<br />

hypolimnetic waters reach minimum values near 0 mg/L by July (Raymond 2008, 2009, 2010).<br />

7.10.1.3 Ammonia Toxicity<br />

Low DO events are <strong>of</strong>ten associated with high levels <strong>of</strong> un-ionized ammonia, which is toxic to<br />

fish at concentrations above 0.5 mg/L (Saiki et al. 1999, PacifiCorp 2004, Deas and Vaughn<br />

2006, ODEQ 2010, Sullivan et al. 2011). Ammonia toxicity is complex because it is a function<br />

<strong>of</strong> both pH and temperature, and is most toxic at higher pH (USEPA 2009). At a pH above 8,<br />

ammonia toxicity is mostly due to un-ionized ammonia, but below pH 8 toxicity is based on total<br />

ammonia concentrations. Saiki et al. (1999) reviewed the results <strong>of</strong> a variety <strong>of</strong> tests using<br />

ammonia alone and in conjunction with pH, DO, and temperature to assess how ammonia<br />

affected survival <strong>of</strong> larval and juvenile suckers, and found that median LC 50 (the concentration <strong>of</strong><br />

73

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