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<br /> nr,iil"'"''''!f- <br /> v 'v,' ~., -. >J .,- <br /> McKay Road <br /> 40 <br /> 30 <br /> 20 <br />W 10 <br />!;( <br />0: <br />t: <br />Zz 0 <br />oow <br />::;)(9 Henderson <br />-'0 40 <br />"-0: <br />wf- <br />f-- <br />_Z <br />0:00 <br />t:<( 30 <br />Zo: <br />Ow <br />wf- <br />>:J 20 <br />-'0: <br />Ow <br />00,,- <br />!!?oo <br />O~ 10 <br />"-<( <br />00: <br />Z(9 <br />O:J 0 <br />F::::! <br /><(~ Road 8 <br />~Z 40 <br />Z- <br />w <br />u <br />Z 30 <br />0 <br />U <br /> 20 0 <br /> 10 <br /> <br /> <br /> <br />D <br /> <br />D <br /> <br />o <br /> <br />o <br /> <br />o <br />8/1/92 <br /> <br /> <br />10/1/92 <br /> <br />12/1/92 <br /> <br />D welllA <br />o well1B <br />~ well 2A <br />~ well 28 <br /> <br /> <br /> <br />D <br /> <br /> <br />D <br /> <br />o <br /> <br />o <br /> <br />o <br /> <br /> <br />211/93 <br /> <br />4/1/93 <br /> <br />6/1/93 <br /> <br />8/1/93 <br /> <br />DATE <br />Figure 9. Concentrations of dissolved nitrite plus nitrate in water from wells at McKay Road, Henderson, and Road 8. <br /> <br />Small-Area Flow System <br /> <br />Values of pH in water from the piezometers <br />screened I It below the sediment/water interface <br />ranged from 6.71 to 8.64, with a median value of <br />7.33 (fig. 12 and table 9). As with values of pH in <br />ground water from the monitoring wells, values of <br />pH in ground water from the small-area flow system <br />generally were lower than values in the river (fig. 12). <br />Measurements of pH indicate that values of pH at <br />depths ofless than 84 in. below the sediment/water <br />interface were less than values in the surface water <br />(table 10 and fig. 13). These data indicate that water <br />discharging from the small-area flow system had the <br />potential to lower pH values in the river. <br /> <br />Concentrations of DO in water from the piezom- <br />eters ranged from less than 0.1 to 1.7 mg/L, with a <br />median value of 0.2 mg/L (fig. 14 and table 9). The <br />median concentration of DO in ground water from <br />below the sediment/water interface varied in different <br />reaches of the river from between 0.2 and 0.3 mg/L; <br />however, the median concentration in each reach was <br />substantially lower than the median DO concentration <br />(2.5 mg/L) in ground water from the lA/IB wells at <br />Henderson and Road 8. DO concentrations in ground <br />water from the INIB wells at Henderson and Road 8 <br />are considered to be representative of the DO concen- <br />trations in the large-area flow system in the agricultural <br />area. Concentrations of DO in ground water from the <br />small-area flow system were substantially lower than <br /> <br />QUALITY OF GROUND-WATER DISCHARGE 23 <br />