基于TELEMAC-2D模型的嫩江干流洪水模拟分析研究OA
Numerical Simulation of the Nenjiang River Based on TELEMAC-2D Model
河道洪水演进模拟分析对流域防洪减灾具有重要意义,但宽浅型河道两岸滩地水流相互交织作用复杂,传统水动力学模型适用性和准确性有待进一步探索.针对嫩江干流宽浅型河道两岸滩地地形复杂、涉水建筑密集的特点,以富拉尔基-江桥河段为例,利用高精度地形地貌数据精细刻画河道内地形、围堤等对水流演进的影响,采用TELEMAC-2D模型构建二维河道洪水演进模拟模型,并以MIKE21模型结果作为比较基准,探讨分析模型在嫩江干流汛期洪水演进模拟的效果.结果显示:TELEMAC-2D模型的洪水演进模拟效果较好,模型模拟淹没范围与同期遥感影像的实际洪水淹没基本吻合,且模拟结果能够较好地反映河道内围堤、局部微地形等对洪水演进的阻水效果;水文站不同年份汛期洪水的模拟、实测洪峰流量相对误差均小于20%,且绝大多数年份汛期洪水的模拟、实测流量序列确定性系数均在0.9以上;TELEMAC-2D模型的模拟结果与MIKE21模型差异较小,两种模型不同年份的模拟洪水过程序列起涨、消退趋势基本一致,且均与实测洪水涨落过程较为吻合;研究河段河道洪水漫滩流量阈值约为1 100 m3/s,模型对不同洪水量级工况下的漫滩、非漫滩型洪水均具有较好的模拟效果.结果表明TELEMAC-2D模型具有较好的洪水模拟性能,能够应用于嫩江干流复杂宽浅型河道洪水演进模拟分析.
Numerical modeling of river flood evolution plays a crucial role in flood risk management and disaster prevention strategies.However,the interaction of water flow over the wide-shallow river is complex,and the applicability and accuracy of traditional hydrodynamic models needs to be further explored.Wide-shallow main stem of the Nenjiang River is characterized by intricate riverbank formations and highly concentrated water management infrastructure.To address the above-mentioned issues,the Fulaerji-Jiangqiao stationof the Nenjiang River was selected as the study area,and high-resolution terrain and geomorphological datasets were utilized to depict the impact of topography and embankments within the river on water flow evolution.On this basis,a two-dimensional flood evolution simulation model of the selected study area was constructed by the TELEMAC-2D.The simulated discharges obtained from the TELEMAC-2D model were then discussed and compared with those from the MIKE21 model during the flood season.The results showed that the built TELEMAC-2D model had satisfactory performance on flood modelling.The simulated inundation area was consistent with actual flood coverage observed in the concurrent remote sensing imagery.Also,the modelling results could effectively reflect the water-blocking effects of inner embankments and local microtopography on flood routing within the river channel.For different flood events,the relative errors of the flood peak flow at the gauged stations were all less than 20%.Furthermore,the coefficient of determination between the simulated and measured discharge series for most flood events was above 0.9.The modelling results of the TELEMAC-2D model were comparable to those from the MIKE21 model.The simulated flood process sequences from these two models exhibited similar trends in flood onset and recession stages,and both were consistent with the measured flood hydrographs.Additionally,the floodplain flow threshold for the studied river reach was determined to be approximately 1 100 m³/s,and the model demonstrated satisfactory performance in modelling both floodplain and non-floodplain flood events of different magnitudes.The results indicated that the TELEMAC-2D model had satisfactory modelling capability and was suitable for flood routing in wide and shallow rivers.
吴剑;杨婧瑶;王悦宇;杨彬;潘劭博;周之仪;刘子嘉;彭勇;丁勇
大连理工大学化工海洋与生命学院,辽宁 盘锦 124221大连理工大学建设工程学院,辽宁 大连 116024大连理工大学建设工程学院,辽宁 大连 116024内蒙古自治区水旱灾害防御技术中心,内蒙 呼和浩特 010000内蒙古自治区水旱灾害防御技术中心,内蒙 呼和浩特 010000大连理工大学建设工程学院,辽宁 大连 116024内蒙古自治区水旱灾害防御技术中心,内蒙 呼和浩特 010000大连理工大学建设工程学院,辽宁 大连 116024水利部松辽水利委员会,吉林 长春 130000
建筑与水利
嫩江宽浅型河道洪水演进模拟TELEMAC-2D
Nenjiangwide-shallow riverflood evolution simulationTELEMAC-2D
《中国农村水利水电》 2026 (1)
37-44,8
国家自然科学基金(52309009)辽宁省博士科研启动项目(2023-BSBA-074).
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