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Water Quality 19 <br />w <br />U 400 <br />Z? <br />UWWw 380 <br />U2wLUcn <br />pw2OO 360 <br />W Fn <br />U pfZ0-j 340 <br />_U U N U <br />? 75 Cr 320 <br />UZL <br />LU - 300 <br />U) <br />A <br />B <br />70 <br />O Z U) <br />>?QLU 60 <br />OJ <br />(nU?OC <br />?QJa 50 <br />U ? <br />40- <br />C <br />6.0 r- <br />Z <br />p2Z>= 5.5 <br />U.j w <br />J w 5.0 <br />OCw7J <br />U) z J W <br />?Q? 4.5 <br />4.0 <br />D <br />10 F-- <br />ZU) <br />8 <br />0 , Cr <br />0E(D <br />U) _j _j w 6 <br />CL <br />U <br />4 <br />J <br />E <br />14 r- <br />0ZU) <br />w 2 Q W <br />OQ(DJ <br />U) wziCr <br />(nJ Jw <br />? a <br />U) ? <br />12 <br />10 <br />8 <br />6 <br />01101/1999 0110112000 01/0112001 01/01/2002 <br />TIME <br />Figure 8. (A) Specific conductance and dissolved (B) calcium, (C) magne- <br />sium, (D) chloride, and (E) sulfate concentrations over time for well 7 in the <br />Fraser River watershed, 1998-2001. <br />thunderstorms in summer), base flow from ground-water Suspended sediment is important in nutrient analysis because a <br />discharges, and discharge from wastewater-treatment facilities. large proportion of phosphorus carried by streams tends to <br />Concentrations of suspended sediment in the Fraser River adhere to the sediment. <br />at Tabernash were low overall, ranging from 3 to 29 mg/L, Measurements of specific conductance ranged from 74 to <br />with a median of 8 mg/L (table 4). Elevated concentrations 146 pS/cm (table 4) and indicated slightly mineralized water. <br />occurred during early spring or during snowmelt runoff. Minimum specific conductance was detected during times of