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Last modified
11/23/2009 12:49:17 PM
Creation date
5/15/2007 10:43:07 AM
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Floodplain Documents
County
Delta
Title
North Fork Volunteer Water Quality Monitoring Project - April 2001-April 2002 Data Report
Date
9/30/2002
Prepared For
North Fork River Improvement Association
Prepared By
CSU Cooperative Extension and North Fork River Improvement Association
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />3.2 Nutrients <br /> <br />Nitrogen <br /> <br />Nitrogen concentrations in the North Fork watershed were measured by nitrate-nitrite, <br />ammonia, and total kjeldahl nitrogen analyses. There were no exceedances of the State's <br />nitrate standard of 10 mgIL. In fact, most of the samples had nitrate-nitrite <br />concentrations below the laboratory detection limits. These limits changed during the <br />period of the study. Initially, the detection limit was <0.05 mgIL, then the limit was <br />raised to <0.3 mgIL in August of2001. <br /> <br />The State's chronic ammonia standard is 0.02 mg/L for these segments; however, over <br />most of the study period the laboratory's minimum detection limits (based on lab <br />technology) were higher than the standard, ranging from <0.05 to <1 mg/L. 'The highest <br />ammonia concentration was 0.21 mgIL, recorded at NF-3 on July 11, 2001. Potential <br />sources of nitrogen pollution in rivers can include fertilizer and wastewater treatment <br />plants. <br /> <br />Total Suspended Solids and Total Phosphates <br /> <br />TSS concentrations varied from station to station. The largest increases in suspended <br />solids could be correlated to storm events and spring runoff, where sudden large amounts <br />of rainfall or snowmelt eroded soil into the rivers. The East Muddy Station (EM-I) for <br />example, reflects the high concentrations of sediment in this system during spring runoff <br />(490 mgIL on April 25, 2001), and also after a large storm event (570 mg/L on August 9, <br />2001). The highest suspended sediment loads during the whole year were recorded <br />during or shortly after stormwater runoff events at NF-2, below Somerset, on August 9, <br />2001 (940 mg/L); and at NF-4, Hotchkiss, on October 10,2001 (620 mg/L). <br /> <br />TSS loads can also be correlated with increases in total phosphate concentrations. The <br />chart below shows how total phosphate concentrations increase in conjunction with major <br />stormwater and snowmelt runoff events. This is likely a reflection of the inorganic <br />phosphate that is sorbed to soil particles and washes into the river during erosion events. <br /> <br />Total Dissolved Solids <br /> <br />TDS are comprised primarily of calcium, sodium, and magnesium salts. TDS <br />concentrations increase dramatically starting near Paonia. This is likely a reflection of <br />inputs from irrigation. Irrigation water leaches through saline soils and washes out the <br />water-soluble salts. These salts then end up in the river. The highest TDS value was <br />recorded at NF-4, Hotchkiss, with a concentration of 1,270 mgIL on September 12, 2001. <br />Although there is no state standard for TDS, based on CSU references, waters above <br />1,000 mg/L TDS "may have adverse affects on crops and require careful management <br />practices" (SIA No. 0.506, Irrigation Water Quality Criteria, CSU). <br /> <br />Sulfates <br /> <br />Sulfate concentrations rose dramatically starting in the Paonia area and continuing <br />downstream. Above Paonia, sulfate concentrations are generally low, often below <br />10 mg/L. However, after Paonia they started to rise. The highest sulfate concentration <br /> <br />3-6 <br />
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