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MW'MC FACILmES PLAN <br /> <br />Nutrients <br />The productivity of fish and their food base hinges on the amount of bioavailable nitrogen <br />and phosphorus in the water. In natural waters of the Pacific Northwest, phosphorus is <br />usually the nutrient that limits primary productivity, which includes algae and <br />zooplankton. This means that, unless extra phosphorus becomes available, there will still be <br />spare bioavailable nitrogen in the water column. <br /> <br />Phosphorous <br />The bioavailable form of phosphorus is referred to as soluble reactive phosphorus. There is <br />another portion that is attached to sediment particles that is not immediately available for <br />uptake by aquatic organisms, but has the potential to be released into the water column if <br />dissolved oxygen levels become low. Shallow reservoirs, such as Fern Ridge Reservoir, can <br />have low dissolved oxygen levels and release phosphorus from sediments, especially at <br />night and during early fall when plant material begins dying off. <br /> <br />Median values for total phosphorus concentrations are relatively low in the Willamette <br />River upstream of the urban growth boundary at 0.03mg/L, and rise slightly to 0.06 mg/L <br />downstream of the urban growth boundary near the Beltline Road bridge. <br /> <br />Nitrogen <br />Nitrogen has three bioavailable forms that include nitrate (NO3-), nitrite (NO2-), and <br />ammonia. The term ammonia refers to two chemical species that are in equilibrium in water: <br />un-ionized (NH3), and ionized (NH4+). Tests for ammonia usually measure total ammonia; <br />that is, NH3 plus NH4+. The toxicity of ammonia is primarily attributable to the un-ionized <br />NH3, as opposed to the ionized form NH4+. In general, the toxicity of NH3 to fish is a <br />function of pH and water temperature. In the presence of NH3, an increase in either pH or <br />temperature can be harmful to aquatic organisms. <br /> <br />Nitrate (NO3-) and ammonium (NH4+) are rarely found in Pacific Northwest streams and <br />rivers except immediately downstream of point sources of pollution because chemical and <br />biochemical processes in a river quickly transform them into nitrate. Consequently, most <br />bioavailable nitrogen in the Pacific Northwest is in the form of nitrate for streams, rivers, <br />and groundwater. Nitrate and nitrite data evaluated below are reported as nitrate plus <br />nitrite as nitrogen. This is abbreviated to the form NO3+NO2 (as N). <br /> <br />Median values for combined nitrate+nitrite as nitrogen (NO3+NO2 as N) are 0.03 mg/L in <br />the Willamette River upstream of the urban growth boundary, and rise slightly to <br />0.10 mg/L downstream of the Beltline Road bridge. Median values for combined <br />nitrate+nitrite as nitrogen (NO3+NO2 as N) are 0.03 mg/L in the Willamette River upstream <br />of the urban growth boundary, and rise slightly to 0.10 mg/L downstream of the Beltline <br />Road bridge. A review of the long-term trend of NO3+NO2 data downstream of the urban <br />growth boundary shows that concentrations are increasing with time. This is likely the <br />result of continued development of land immediately upstream of the monitoring location. <br /> <br />Stormwater <br />The median value for total phosphorus at all composite stormwater-monitoring sites in <br />Eugene is 0.25 mg/L, with values ranging from 0.09 to 11 mg/L. Concentrations of <br />NO3+NO2 (as N) in Eugene stormwater samples ranged from not detected to 3.7 mg/L; the <br />median was 0.06 mg/L. Sources for NO3+NO2 (as N) are similar to those for phosphorus. <br /> <br /> 2-22 MWMC_2.0_REV23.DOC <br /> <br /> <br />