SWMM 5, InfoSWMM, H20MAP SWMM, InfoSewer for Water Quality,Hydrology, Hydraulics
Robert Dickinson commented on Robert Dickinson's group Stream of Information
Robert Dickinson commented on Robert Dickinson's group Stream of Information
Robert Dickinson added a page to the group SWMM4 Input Files
Robert Dickinson commented on Robert Dickinson's group SWMM4 Input Files
Robert Dickinson added a page to the group Blog Links
Robert Dickinson commented on Robert Dickinson's group Stream of Information
Robert Dickinson commented on Robert Dickinson's group Weather
Robert Dickinson commented on Robert Dickinson's group Weather
Robert Dickinson commented on Robert Dickinson's group Weather
Robert Dickinson posted a video
Robert Dickinson commented on Robert Dickinson's group ExtraVariables
Robert Dickinson replied to Robert Dickinson's discussion How is the St Venant Equation Solved for in the Dynamic Wave Solution of SWMM 5?
Robert Dickinson left a comment for wu ze jian
Robert Dickinson posted a discussionSubject: An Example of the Importance of the Term DQ4 in the SWMM 5 St Venant Solution
The four terms are are used in the new flow for a time step of Qnew:
Qnew = (Qold – dq2 + dq3 + dq4) / ( 1 + dq1)
when the force main or gravity main is full dq3 and dq4 are zero and Qnew = (Qold – dq2) / ( 1 + dq1)
The dq4 term in dynamic.c uses the area upstream (a1) and area downstream (a2), the midpoint velocity, the sigma factor (a function of the link Froude number), the link length and the time step or
dq4 = Time Step * Velocity * Velocity * (a2 – a1) / Link Length * Sigma
where Sigma is a function of the Froude Number and the Keep, Dampen and Ignore Inertial Term Options. Keep sets Sigma to 1 always and Dampen set Sigma based on the Froude number, Ignore sets Sigma to 0 all of the time during the simulation.
The value of dq4 increases when there is a significant difference in the cross sectional area of the downstream end of the link and the upstream end of the link. In this example, the downstream storage node causes a backflow in the link (Figure 1). The flow may look unstable in the link flow time series but the change in flow is simply due to the water sloshing back and forth. There is no continuity error as the term dq4 keeps the water in the link in balance (Figure 2).
© 2012 Created by Robert Dickinson.
Powered by
You need to be a member of SWMM5 - Stormwater Management Model to add comments!
Join SWMM5 - Stormwater Management Model