Muskingum Method
Trending Questions
Q. The Muskingum method of flood routing is a
- Form of hydraulic routing of a flood
- Form of reservoir routing
- Complete numerical solution of St. Venant equations
- Hydrological channel routing method
Q. For routing of flood in a given channel using the Muskingum method, two of the routing coefficients are estimated as C0=−0.25 and C1=0.55. The value of the third coefficient C2 would be
- 0.7
Q. Consider the following statements.
In case of flood routing in a river channel by Muskingum method, the coefficient x represents:
1. A dimensionless constant indicating the relative importance of inflow and outflow in determining storage.
2. A storage constant having the dimension of time.
3. In natural channels, x usually varies between 0.1 and 0.3.
4. When the values of x equals 0.5, there exists the influence of both inflow and outflow on storage.
Which of these statements are correct?
In case of flood routing in a river channel by Muskingum method, the coefficient x represents:
1. A dimensionless constant indicating the relative importance of inflow and outflow in determining storage.
2. A storage constant having the dimension of time.
3. In natural channels, x usually varies between 0.1 and 0.3.
4. When the values of x equals 0.5, there exists the influence of both inflow and outflow on storage.
Which of these statements are correct?
- 1, 2, 3 and 4
- 1, 3 and 4 only
- 1, 2 and 3 only
- 2, 3 and 4 only
Q. Muskingum method for routing of flood
- is used for routing floods through reservoirs
- is a method of routing that uses continuity and momentum
- is a hydrologic method of routing floods streams
- is one is which only energy equation is used
Q. The Muskingum model of routing a flood through a stream reach is expressed as O2=K0I2+K1I1+K2O1 where K0, K1, and K2 are routing coefficient for the concerned reach; I1 and I2 are the inflows to the reach and O1 and O2 are the outflows from the reach corresponding to time steps 1 and 2 respectively. The sum of K0, K1 and K2 of the model is
- -1
- -0.5
- 0.5
- 1
Q. For a river reach with k = 26 h and x = 0.22, the tow Muskingum routing coefficients for t = 12 h are 0.011 and 0.446, the third coefficient (correct upto three decimal places) is __________.
- 0.311
- 0.385
- 0.543
- 0.204
Q. The inflow (in cumecs) for a stream reach at time t1=6hr and t2=24hr are 15 and 30 respectively. The coefficients C1 and C2 in the Muskingum routing equation are 0.4 and 0.5 respectively. If outflow for the stream reach at t1=6hr is 10 cumecs, the outflow rate at t2=24 will be _____ cumecs.
- 14
Q. Muskingum method is used in
- Hydrologic reservoir routing
- Hydrologic channel routing
- Hydraulic reservoir routing
- Hydraulic channel routing