| 000 | 04089nam a2200421 4500 | ||
|---|---|---|---|
| 005 | 20260818170258.0 | ||
| 008 | 150698 th eng | ||
| 035 | _a.b10471066 | ||
| 099 | 9 | _aAIT Thesis no. WA-91-26 | |
| 100 | 0 | _aWinyu Rattanapitikon | |
| 245 | 1 | 0 | _aNumerical modelling of propagation of dam break wave front and resulting flash flood |
| 260 |
_aBangkok : _bAsian Institute of Technology, _c1991 |
||
| 300 | _a104 p. | ||
| 490 | 1 |
_aThesis ; _vno. WA-91-26 |
|
| 500 | _aA thesis submitted in a partial fulfillment of the requirements for the degree of Master of Engineering, School of Engineering and Technology | ||
| 502 | _aThesis (M.Eng.) - Asian Institute of Technology, 1991 | ||
| 520 | _aFlood waves resulting from instantaneous breaking of a dam are computed by using a 2-D mathematical model consisting of the unsteady free surface flow equations. The equations namely the continuity, x- and y- momentum equations are solved numerically using the two step predictor-corrector method in conjunction with the asymmetric finite difference scheme. The computed results of the present model are verified by using the experimental results obtained from a physical laboratory model simulating two dimensional propagation of dam-break wave over a dry bed flood plain. The results of verification indicate that the present model can be applied to simulate 2-D propagation and spreading of dam-break wave front very well. The model can predict the flood depth hydrographs fairly near the dam-break section but a prediction of depth is achieved at a further distance downstream. This is envisaged to be due to the effect of the moving hydraulic jump caused by hydraulic resistance of flood plain and reflection from the downstream end. The computed results from the present model and the previous model developed by Wattanaprateep (1987) are also compared. It is found that the results of the present model are closer to the experimental results than those of Wattanaprateep's model. Sensitivity analysis on the performance of the present model is carried out. It is found that (i) the Manning roughness coefficient has significant effect on the computed results, (ii) the small depth in the friction terms and the limiting depth of wave front have a small effect on the computed results of wave front spreading pattern and speed of the wave front propagation over the dry flood plain, (iii) no slip condition at closed wall boundary is suggested in this study and also the use of predictor-corrector method conjunction with the asymmetric finite difference scheme is suggested to simulate the flood wave propagation on dry bed before the reflection of moving hydraulic jump from the downstream end occur. After that only the asymmetric finite difference scheme is suggested. | ||
| 650 | 0 |
_aFlood control _xMathematical models |
|
| 650 | 0 | _aDam failures | |
| 700 | 0 |
_aTawatchai Tingsanchali, _eChairperson |
|
| 700 | 0 |
_aSuphat Vongvisessomjai, _eExamination Committee |
|
| 700 | 1 |
_aShibayama, Tomoya, _eExamination Committee |
|
| 710 | 2 |
_aThe Government of Netherlands, _eScholarship Donor |
|
| 810 | 2 |
_aAsian Institute of Technology. _tThesis ; _vno. WA-91-26 |
|
| 856 |
_3Full-Text _uhttp://203.159.5.9/ait-thesis/detail.php?q=B17771 |
||
| 907 |
_a.b10471066 _bmnait _cs |
||
| 902 | _a240402 | ||
| 998 |
_b2 _c951012 _dm _ea _fs _g0 |
||
| 945 | _lmnait | ||
| 945 | _lmnait | ||
| 945 | _lmnarc | ||
| 942 | _c20 | ||
| 942 | _c40 | ||
| 909 |
_aBarcode : 30050003054987 _bCREATED : 1994-05-18 _cRECORD # : i10590055 _dLPATRON : 1028257 _eLCHKIN : 2018-08-28 _f# RENEWALS : 0 _g# OVERDUE : 0 _hIUSE3 : 2 _iTOT CHKOUT : 2 _jTOT RENEW : 0 |
||
| 909 |
_aBarcode : 30050003054995 _bCREATED : 1994-05-18 _cRECORD # : i10590067 _dLPATRON : 1019708 _eLCHKIN : 2006-02-06 _f# RENEWALS : 0 _g# OVERDUE : 0 _hIUSE3 : 0 _iTOT CHKOUT : 3 _jTOT RENEW : 1 |
||
| 909 |
_aBarcode : 30050160033360 _bCREATED : 2016-02-15 _cRECORD # : i12882276 _dLPATRON : 0 _eLCHKIN : - _f# RENEWALS : 0 _g# OVERDUE : 0 _hIUSE3 : 0 _iTOT CHKOUT : 0 _jTOT RENEW : 0 |
||
| 999 |
_c82070 _d82070 |
||