Intensive Survey of the Guadalupe River Segment 1806
Intensive Survey of the Guadalupe River Segment 1806
Intensive Survey of the Guadalupe River Segment 1806
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Ckr<br />
R =-J^- (3)<br />
Lh<br />
where: C. = concentration <strong>of</strong> krypton-85 in water at<br />
time <strong>of</strong> peak concentration<br />
C. = concentration <strong>of</strong> tritium in <strong>the</strong> water at time <strong>of</strong> peak<br />
concentration<br />
Applying this ratio concept, equation 1 can be modified to:<br />
-W- - - Kkr R (*)<br />
with terms as previously defined<br />
Equation 4 can be transformed to:<br />
where: Ru and Rj = peak ratios <strong>of</strong> krypton-85 to tritium concentrations<br />
at an upstream and downstream station<br />
tf = travel time between <strong>the</strong> upstream and down<br />
stream station determined by dye peaks<br />
The tracers are used to evaluate <strong>the</strong> actual krypton-85 transfer coefficient<br />
(Ki,J, (K. ), and <strong>the</strong> conversion to <strong>the</strong> 0) oxygen transfer coefficient (K„w) is from<br />
4-UM ..A.L1 2 ~l~~ J I J.*^ OX<br />
<strong>the</strong> established gas exchange ratio:<br />
K0X = Kkr<br />
ox ~rar<br />
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