murdock
Chemical
- Jun 17, 2002
- 48
I am working on a model of some underground storage chambers with a catch basin upstream acting as a diversion structure. The catch basin has two outlets, one 2' higher than the other to bypass larger storm events.
The chamber system is designed to infiltrate/detain the 1-year storm. This part works OK, it's the larger storm events where the model goes off. During the 10-year storm, the storage range for the chambers peaks 8' above storage level (elev. 230.39), while the upstream diversion structure peaks at 224.03, well within its limits (overflow culvert inlet at 224).
I have my model setup with the dyn-stor-ind routing method, so the two structures should be dependent on each other, correct? What is triggering the chambers' high peak elevation? In real life, will the water simply peak at 224.03 in both the chambers and overflow structure?
Let me know if you need some more detail.
TIA
The chamber system is designed to infiltrate/detain the 1-year storm. This part works OK, it's the larger storm events where the model goes off. During the 10-year storm, the storage range for the chambers peaks 8' above storage level (elev. 230.39), while the upstream diversion structure peaks at 224.03, well within its limits (overflow culvert inlet at 224).
I have my model setup with the dyn-stor-ind routing method, so the two structures should be dependent on each other, correct? What is triggering the chambers' high peak elevation? In real life, will the water simply peak at 224.03 in both the chambers and overflow structure?
Let me know if you need some more detail.
TIA