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Our new Biological Assessment is out - Klamath Basin Crisis

Our new Biological Assessment is out - Klamath Basin Crisis

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<strong>Klamath</strong> Project Operations <strong>Biological</strong> <strong>Assessment</strong><br />

Endangered Suckers: Environmental Baseline for Suckers<br />

Table 2-5. Sediment accumulation rate from UKL sediment core analys<strong>is</strong>.<br />

Year Sediment Accumulation<br />

Rate (g/m 2 /year)<br />

1880 18<br />

1900 20<br />

1920 20<br />

1940 30<br />

1960 40<br />

1980 60<br />

1995 120<br />

Source: Eilers et al. 2001<br />

Water Temperature<br />

Temperature plays a major role in water quality by directly causing stress to f<strong>is</strong>h,<br />

as well as exacerbating other processes affecting water quality such as:<br />

• DO. Temperature directly influences DO solubility as well as accelerate<br />

oxygen consuming microbial processes (Biochemical Oxygen Demand<br />

[BOD] and Sediment Oxygen Demand [SOD]).<br />

• AFA production. Higher water temperature stimulates amplified AFA<br />

production leading to further water quality degradation. The greatest<br />

density of AFA coincides with warmer water temperature (Wood et al.<br />

2006).<br />

Water temperature within UKL annually exceeds 25 degrees Celcius (ºC) during<br />

summer months, typically reaching a maximum in late July to early August.<br />

These excessively warm water temperatures can be stressful and at times leathal<br />

to f<strong>is</strong>hes within UKL. The Oregon Department of Environmental Quality<br />

(ODEQ) has identified nearly 25 stream segments flowing into UKL as<br />

“temperature limited” (ODEQ 1998). Increased temperatures are symptomatic of<br />

degraded stream conditions resulting from increased sedimentation, loss of<br />

riparian vegetation, and channel modifications associated with logging, intensive<br />

grazing, flow reductions, and agricultural activities. However, air temperature<br />

and solar radiation likely have a greater effect on increasing water temperature of<br />

UKL than tributary inflows under the current tributary hydrology.<br />

Nutrient Loading<br />

High nutrient loading promotes correspondingly high algae production, which, in<br />

turn, modifies physical and chemical water quality character<strong>is</strong>tics that can directly<br />

dimin<strong>is</strong>h the survival and production of f<strong>is</strong>h populations. Accelerated phosphorus<br />

loading <strong>is</strong> likely a key factor driving the massive AFA blooms that now dominate<br />

UKL. ODEQ establ<strong>is</strong>hed a Total Maximum Daily Load (TMDL) for UKL in<br />

2002 targeted at reduction of phosphorous as a means to reduce AFA production<br />

and improve water quality conditions such that water quality criteria would be<br />

attained. Through modeling and analys<strong>is</strong> efforts, ODEQ (2002) determined that<br />

phosphorous reduction would be the most effective means of improving water<br />

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