Laserfiche WebLink
original value obtained. The duplicate value for iron was 67% of the original value (0.09 <br />mg(l-original vs. 0.06 mg(l-duplicate). The duplicate sample value for manganese was 107% <br />of the original value (0.028 mg/1-original vs. 0.03 mg/1-duplicate). The duplicate sample <br />value for total suspended solids was 120% of the original value (5 mg/1-original vs. 6 mg/I- <br />duplicate). <br />The October duplicate for TR-B showed 8 out of 15 parameters to be within 5% of the <br />original value obtained. The duplicate sample value for calcium was 110% of the original <br />value (31.8 mg/1-original vs. 34.9 mg/1-duplicate). The duplicate sample value for iron was <br />110% of the original value (0.1 mg/1-original vs. 0.11 mg/1-duplicate). The duplicate sample <br />value for magnesium was 109% of the original value (16.8 mgfl-original vs. 18.3 mgfl- <br />duplicate). The duplicate sample value for potassium was 108% of the original value (1.2 <br />mg/1-original vs. 1.3 mg/1-duplicate). The duplicate sample value for sodium was 109% of the <br />original value (4.7 mg/1-original vs. 5.1 mg/I-duplicate). The duplicate sample value for total <br />suspended solids was 83% of the original value (6 mg/1-original vs. 5 mg/1-duplicate). The <br />duplicate sample value for sulfate was 150% of the original value (40 mg/1-original vs. 60 <br />mg/1-duplicate). <br />VII. SPRING AND SEEP SURVEY <br />A survey was conducted May 19 and 22, 2006 to evaluate springs and seeps which <br />existed during past surveys at the base of the ridge along Trout Creek from the northern <br />Moffat boundary to the base of West Ridge. A total of 15 springs locations were surveyed. <br />Of these I S spring locations, ten were either damp or had flowing water during the 2006 <br />survey. A total of 20 seeps locations were surveyed. Of these 20 seep locations, seven were <br />either damp or had flowing water during the 2006 survey. Appendix C contains a listing of <br />the springs and seeps observed from 1993 through 2006. <br />Nine of the 10 springs either damp or flowing exhibited sufficient discharge for flow <br />to be estimated or calculated and field parameters measured during the 2006 monitoring <br />period. Four of the 7 seeps either damp or flowing also exhibited sufficient dischazge for flow <br />to be estimated and field parameters measured. Several of the springs and seeps were sampled <br />53 <br />