M_{1} water-surface profile. M_{1} WATER-SURFACE PROFILE CALCULATED ONLINE
Professor of Civil and Environmental Engineering San Diego State University, San Diego, California
1. INTRODUCTION A water-surface profile is a feature of the hydraulics of open channels which describes the variation of the water-surface elevation in the longitudinal direction (one dimension x in space), under a steady equilibrium flow condition. There are twelve (12) types of water-surface profiles, depending on the Froude number F and the ratio S_{o} /S_{c} , in which S_{o} = bottom slope, and S_{c} = critical slope. The critical slope S_{c} is equal to 1/8 of the Darcy-Weisbach friction factor f. Table 1 lists the twelve types of profiles (Ponce, 2014).
In this article, we describe the M_{1} water-surface profile, a retarded (backwater) subcritical/subnormal profile, which may well be the most common profile in practice. The M_{1} profile depicts flow in a mild channel, upstream of a reservoir (Fig. 1). We present two examples and show the respective online calculations.
Fig. 1 M_{1} water-surface profile.
2. GOVERNING EQUATION Chow (1959) has presented the classical way of expressing the governing equation of steady, gradually varied flow. A more cogent, dimensionless presentation, focusing on critical slope, has been advanced by Ponce (2014) and is presented here. In terms of critical slope, the general equation for flow-depth gradient dy/dx is:
in which S_{o} = channel (bottom) slope, S_{c} = critical slope,
P = wetted perimeter,
T = channel top width, For (P / T ) = (P_{c} / T_{c} ), Eq. 1 reduces to:
For conciseness, the flow-depth gradient may be written as:
Substituting Eq. 3 into Eq. 2, the flow-depth gradient is:
Equation 2, or Equation 4, its reduced
form,
is the steady gradually varied flow equation (Fig. 2).
Fig. 2 Definition sketch for energy balance in open-channel flow.
3. ONLINE CALCULATION: EXAMPLE A We pose an example of the calculation of an M_{1} profile in a natural channel using the online calculator ONLINE_WSPROFILES_21. The following box shows the input data.
Output. The results show that the (flow) depth at the downstream boundary (y_{d} = 5 m) will decrease gradually to the normal depth in the upstream end y_{n} = 2.962 m. The total distance, from downstream boundary to upstream end, is: L = 13,114.5 m.
4. ONLINE CALCULATION: EXAMPLE B We pose an example of the calculation of an M_{1} profile in a lined channel using the online calculator ONLINE_WSPROFILES_21. The following box shows the input data.
Output. The results show that the (flow) depth at the downstream boundary (y_{d} = 5 m) will decrease gradually to the normal depth in the upstream end y_{n} = 1.821 m. The total distance, from downstream boundary to upstream end, is: L = 1,771.6 m.
5. SUMMARY An online calculation of an
M_{1} open-channel flow water-surface profile is shown in detail.
REFERENCES Chow, V. T. 1959. Open-channel hydraulics. McGraw-Hill, Inc, New York, NY.
Ponce, V. M. 2014b.
Fundamentals of Open-channel Hydraulics.
Online textbook. |
231025 |