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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 />

A-15

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