水动力学研究与进展A辑
水動力學研究與進展A輯
수동역학연구여진전A집
JOURNAL OF HYDRODYNAMICS
2010年
2期
147-154
,共8页
贺治国%WU Wei-ming
賀治國%WU Wei-ming
하치국%WU Wei-ming
堤坝溃决%泥沙%冲刷%水流泥沙耦合%数值模拟
隄壩潰決%泥沙%遲刷%水流泥沙耦閤%數值模擬
제패궤결%니사%충쇄%수류니사우합%수치모의
dam/levee breach%sediment transport%erosion%flow-sediment interaction%numerical simulation
该文建立了洪水漫堤导致河堤溃决的平面二维水沙运动数值模型,以模拟溃口扩展和堤身冲刷的过程.该模型基于有限体积法、采用显式格式求解平面二维水流运动和非平衡全沙泥沙输移方程,并考虑了边坡崩塌、底床急剧变形以及高浓度泥沙输移对水流运动的影响.溃口处的混合流场采用HLL approximate Riemann solver处理,非黏性土溃口边坡的崩塌采用不同干、湿静止角处理.通过对英国HR Wallingford实验室一组实验的计算,结果表明该模型能较好地模拟非黏性土堤坝溃决过程中的溃口展宽、坝体冲刷、流场分布以及溃口流量过程线.对模型参数的敏感性分析显示了水沙耦合溃决模型的非线性特征.
該文建立瞭洪水漫隄導緻河隄潰決的平麵二維水沙運動數值模型,以模擬潰口擴展和隄身遲刷的過程.該模型基于有限體積法、採用顯式格式求解平麵二維水流運動和非平衡全沙泥沙輸移方程,併攷慮瞭邊坡崩塌、底床急劇變形以及高濃度泥沙輸移對水流運動的影響.潰口處的混閤流場採用HLL approximate Riemann solver處理,非黏性土潰口邊坡的崩塌採用不同榦、濕靜止角處理.通過對英國HR Wallingford實驗室一組實驗的計算,結果錶明該模型能較好地模擬非黏性土隄壩潰決過程中的潰口展寬、壩體遲刷、流場分佈以及潰口流量過程線.對模型參數的敏感性分析顯示瞭水沙耦閤潰決模型的非線性特徵.
해문건립료홍수만제도치하제궤결적평면이유수사운동수치모형,이모의궤구확전화제신충쇄적과정.해모형기우유한체적법、채용현식격식구해평면이유수류운동화비평형전사니사수이방정,병고필료변파붕탑、저상급극변형이급고농도니사수이대수류운동적영향.궤구처적혼합류장채용HLL approximate Riemann solver처리,비점성토궤구변파적붕탑채용불동간、습정지각처리.통과대영국HR Wallingford실험실일조실험적계산,결과표명해모형능교호지모의비점성토제패궤결과정중적궤구전관、패체충쇄、류장분포이급궤구류량과정선.대모형삼수적민감성분석현시료수사우합궤결모형적비선성특정.
A two dimensionnal dam/levee breaching model was developed to simulate overtopping flows, breach development, and the related sediment transport processes. The depth-averaged 2-D flow and non-equilibrium total-load sediment transport equations were solved using an explicit finite volume method on a rectangular grid. The model considered interactions among transient flow, strong sediment transport and rapid bed distortion by including bed change and variable flow density in the continuity and momentum equations of flow. The HLL approximate Riemann solver was used to handle the mixed-regime flows near the breach, and different repose angles for the sediments below and above the water surface were adopted to handle the non-cohesive embankment slope avalanching. The model was checked against the laboratory experiment carried out by HR Wallingford, UK, and the results show that the developed model predicts well the breach dimension, flow hydrograph, and flow characteristics. The sensitivity analysis shows the nonlinear features of the model.