688 MODELS IN HYDRAULIC ENGINEERING
Solution
- Utilizing fully the discharge capacity gives a discharge scale 4
106 /27148 150. From equation (16.7), Mh(MQ/Ml)2/3(148 150/
250)2/370.57. Therefore let us choose Mh75, giving a distortion of
3.33, which is probably quite acceptable in this case.
- MQMh3/2Ml 75 3/2 250 162 380. The maximum model discharge
will be 4 106 /162 38024.6 l s^1.
- MtMl/MMlMh^ 1/2250/751/228.87 (equation (16.3)).
- MwsMh3/2/Ml 75 3/2/2502.6 (equation (16.13)).
- From the Manning–Strickler equation for a wide channel with Ry,
MMn^1 Mh2/3M1/2s Md^ 1/6Mh2/3Mh1/2Ml^ 1/2Md^ 1/6Mh7/6Ml^ 1/2Mh1/2,
MdM^4 hM^ l^3 754 /250^3 2.0252.
6.
M∆
2
11.11 (equation (16.12)).
Note that the answer to 5 assumes that there is no effect of bedforms (i.e.
that the bed is flat) which may be unrealistic; this has to be checked by
further computation, and the final value of Mdmay influence the whole
model design.
References
Abbott, M.B. (1991) Hydroinformatics: Information Technology and the Aquatic
Environment, Avebury Technical, Aldershot.
Abbott, M.B. and Minns, A.W. (1998) Computational Hydraulics, 2nd edn,
Ashgate, Brookfield, USA.
Abbott, M.B., Babovic, V.M. and Cunge, J.A. (2001) Towards the hydraulics of the
hydroinformation era. Journal of Hydraulic Engineering, ASCE, 39, No. 4:
339–49.
Allen, J. (1947) Scale Models in Hydraulic Engineering, Longman, London.
Anderson, J.D. (1995) Computational Fluid Dynamics, McGraw Hill, New York.
ASCE (1982) American Society of Civil Engineers, Task Committee on Glossary
of Hydraulic Modeling Terms, Modeling hydraulic phenomena – a glossary
of terms. Journal of the Hydraulics Division, Proceedings of the American
Society of Civil Engineers, 108 (NY7): 45–852.
—— (1988) Turbulence modelling of surface water flow and transport, Part I–V;
Task Committee on Turbulence Models in Hydraulic Computations. Journal
of Hydraulic Engineering, ASCE, 114, No. 9: 970–1073.
Assy, T.M. (2001) Solution for spillway flow by finite difference method. Journal of
Hydraulic Research, IAHR, 39, No. 3: 241–7.
250
75
M^2 l
M^2 h
M^2 hM^3 l
M^4 hMl
M^2 h
MlMd