Final Project From USGS Hydrologic Atlas online.
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Transcript of Final Project From USGS Hydrologic Atlas online.
![Page 1: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/1.jpg)
Final Project
From USGSHydrologic Atlas online
![Page 2: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/2.jpg)
![Page 3: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/3.jpg)
Playa
Recharge Recharge
Conceptual Modelof the flow system
![Page 4: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/4.jpg)
![Page 5: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/5.jpg)
![Page 6: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/6.jpg)
Layer 3 – variable bottom
Layer 2
Layer 1
50 ft gap representsconfining bed
Layers
Datum
The problem of dry cells and re-saturation
![Page 7: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/7.jpg)
from GWV
Layer 1 = type 1Layer 2, 3 = type 3
![Page 8: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/8.jpg)
Leakance between layers where eachLayer belongs to a different hydrogeologic unit
See A&W, p. 81
Layer 1leakance
![Page 9: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/9.jpg)
Leakance“Quasi 3D” model
See A&W, p. 81
Layer 2leakance
![Page 10: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/10.jpg)
from GWV
![Page 11: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/11.jpg)
Playa
Recharge Recharge
Conceptual Modelof the flow system
![Page 12: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/12.jpg)
h
QET = RETM xy [h - (hs-d)] / dET
d
hs
extinction depth
RETM is the maximum ET rate,which occurs when h = hs.
for h hs-dand h < hs
![Page 13: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/13.jpg)
QET = 0 below theextinction depth.
QET = QETM at the land surface.
![Page 14: Final Project From USGS Hydrologic Atlas online.](https://reader030.fdocuments.us/reader030/viewer/2022032704/56649d4d5503460f94a2cbe2/html5/thumbnails/14.jpg)
Calibration Targets
calibration value
associated error
20.24 m
0.80 m
Target with relativelylarge associated error.
Target with smaller associated error.