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<br />0135 <br /> <br />EXPLANATION <br /> <br />1977.88 - Penod of record <br />209 _____ <br />--- Number of values <br /> <br />o Far out value (greater than 3 times <br />lOR from the boxl <br /> <br />o OutsIde value (greater tt"\an 1.5 times <br />lOR from the box I <br /> <br />Largest value withIn 1.5 times lOR <br />of the box <br /> <br />- 75th percentile (upper quartilel <br /> <br />Q) <br />'" <br />c: <br />!" <br />~a: <br />~Q <br />:o- <br />cr <br />Q; <br />E <br /> <br />- Median <br /> <br />\ <br /> <br />- 25th percentile (lower quart,lel <br /> <br />Smallest value wIthin 1.5 times lOR <br />of the box <br /> <br />Figure 2.--Example diagram of a box plot. <br /> <br />Median values of instantaneous streamflow (fig. 3) were larger down- <br />stream on Monument Creek, and were larger downstream on Fountain Creek to <br />Fountain Creek below CSWWTP. Streamflow was smaller at downstream stations <br />on Fountain Creek because of irrigation withdrawals in this reach (Edelmann <br />and Cain, 1985). <br /> <br />Median values of specific conductance (fig. 4) and median concentrations <br />of dissolved chloride (fig. 11) and dissolved sulfate (fig. 12) were larger <br />downstream on both creeks probably because of increasing urbanization, which <br />increased wastewater effluent and urban runoff along Monument Creek (Edelmann, <br />1990, p. 15) and ground-water inflow and irrigation-return flow along Fountain <br />Creek (Cain and Edelmann, 1986, p. 8). Median pH values (fig. 5) were smaller <br />at station 07105530 Fountain Creek below CSWWTP. Median values of temperature <br />(fig. 6) generally were higher downstream, and median dissolved-oxygen concen- <br />trations (fig. 7) generally were smaller downstream because of warmer stream <br />temperatures. Median dissolved-oxygen concentrations were smaller downstream <br />from the wastewater-treatment plant at Colorado Springs probably because of <br />the smaller dissolved-oxygen concentrations in the effluent. <br /> <br />9 <br />