Table 11. d2H (deuterium/hydrogen isotopic ratio) and d18O (oxygen-18/oxygen-16 isotopic ratio) values for ground-water samples collected from springs discharging from clinker and wells completed in the Wasatch aquifer and coalbed aquifers
[‰, parts per thousand or per mil]
|
Site number |
Hydrogeologic unit |
d2H (‰) |
d18O (‰) |
|---|---|---|---|
|
S1 |
Springs discharging from clinker |
-138.5 |
-18.04 |
|
S2 |
Springs discharging from clinker |
-142.6 |
-18.41 |
|
W1 |
Wasatch aquifer |
-139.0 |
-18.03 |
|
W2 |
Wasatch aquifer |
-124.0 |
-15.57 |
|
W3 |
Wasatch aquifer |
-140.7 |
-18.40 |
|
W4 |
Wasatch aquifer |
-148.6 |
-19.02 |
|
W5 |
Wasatch aquifer |
-147.8 |
-19.03 |
|
W6 |
Wasatch aquifer |
-131.1 |
-18.14 |
|
W7 |
Wasatch aquifer |
-146.5 |
-18.95 |
|
W8 |
Wasatch aquifer |
-138.9 |
-18.46 |
|
C1 |
Coalbed aquifers |
-137.9 |
-17.84 |
|
C2 |
Coalbed aquifers |
-141.9 |
-18.31 |
|
C4 |
Coalbed aquifers |
-144.2 |
-18.54 |
|
C5 |
Coalbed aquifers |
-138.1 |
-17.92 |
|
C6 |
Coalbed aquifers |
-140.9 |
-18.25 |
|
C8 |
Coalbed aquifers |
-143.5 |
-18.79 |
|
C10 |
Coalbed aquifers |
-143.4 |
-18.51 |
|
C11 |
Coalbed aquifers |
-132.9 |
-17.80 |
|
C12 |
Coalbed aquifers |
-136.6 |
-18.56 |
|
C13 |
Coalbed aquifers |
-141.3 |
-18.40 |
|
C151 |
Coalbed aquifers |
-151.0 |
-19.99 |
|
C16 |
Coalbed aquifers |
-134.9 |
-18.66 |
|
C17 |
Coalbed aquifers |
-143.7 |
-18.78 |
1A petroleum product is present in this well but it is unlikely to affect d2H and d18O values (Carol Kendall, oral comm., 2000).
2Replicate sample.
