海洋技术学报
海洋技術學報
해양기술학보
Journal Of Ocean Technology
2015年
2期
101-105
,共5页
河口海岸%泥沙输移%分组模型%地形演变%水动力
河口海岸%泥沙輸移%分組模型%地形縯變%水動力
하구해안%니사수이%분조모형%지형연변%수동력
estuarine and coastal waters%sediment transport%fractional model%bed evolution%hydrodynamics
根据河口海岸水沙输移的特点,建立了一个新的二维分组数学模型,用来预测该区域的水沙输移过程。该模型耦合了水动力模块、泥沙输移模块和床面演变模块。其中水动力模块基于浅水方程组,综合考虑了柯氏力、床面切应力以及表面风应力的影响,引入干湿判断法处理动边界。泥沙输移模块首先将泥沙按照粒径分组,针对不同泥砂性质,对各组泥沙分别进行建模求解。床面演变模块基于质量守恒方程,实时更新床面高程以及床沙级配变化,并传递给水动力模块,更新底部边界。该模型被应用在了英国塞汶(Severn)河口,其预测的泥沙浓度和实测数据以及不分组的模型的预测结果进行了比较,结果显示,文中建立的分组模型预测的结果要明显好于不分组模型。
根據河口海岸水沙輸移的特點,建立瞭一箇新的二維分組數學模型,用來預測該區域的水沙輸移過程。該模型耦閤瞭水動力模塊、泥沙輸移模塊和床麵縯變模塊。其中水動力模塊基于淺水方程組,綜閤攷慮瞭柯氏力、床麵切應力以及錶麵風應力的影響,引入榦濕判斷法處理動邊界。泥沙輸移模塊首先將泥沙按照粒徑分組,針對不同泥砂性質,對各組泥沙分彆進行建模求解。床麵縯變模塊基于質量守恆方程,實時更新床麵高程以及床沙級配變化,併傳遞給水動力模塊,更新底部邊界。該模型被應用在瞭英國塞汶(Severn)河口,其預測的泥沙濃度和實測數據以及不分組的模型的預測結果進行瞭比較,結果顯示,文中建立的分組模型預測的結果要明顯好于不分組模型。
근거하구해안수사수이적특점,건립료일개신적이유분조수학모형,용래예측해구역적수사수이과정。해모형우합료수동력모괴、니사수이모괴화상면연변모괴。기중수동력모괴기우천수방정조,종합고필료가씨력、상면절응력이급표면풍응력적영향,인입간습판단법처리동변계。니사수이모괴수선장니사안조립경분조,침대불동니사성질,대각조니사분별진행건모구해。상면연변모괴기우질량수항방정,실시경신상면고정이급상사급배변화,병전체급수동력모괴,경신저부변계。해모형피응용재료영국새문(Severn)하구,기예측적니사농도화실측수거이급불분조적모형적예측결과진행료비교,결과현시,문중건립적분조모형예측적결과요명현호우불분조모형。
A new two-dimensional fractional numerical model is established in this paper to simulate the hydrodynamics and graded sediment transport process in estuarine and coastal waters. The model is coupled by the hydrodynamic module, sediment transport module and bed evolution module. The Corlioli effect, bed shear and wind shear are introduced in the hydrodynamic module and the wetting-drying method is adopted to deal with the moving boundary. The sediment mixture is divided into several fractions according to the grain size and each fraction is simulated separately in the sediment transport module. Based on the mass conservation equation, the processes of bed elevation change and sediment grain size sorting are simulated in a real-time way in the bed evolution module, and the data are transferred to the hydrodynamic module immediately to renew the bottom boundary. The model has been applied in the Bristol Channel and Severn estuary in the UK. The predictions by the present model are compared with the field data and those by the single-fraction model. The results show that the present model predictions have better compliance with the field data than the non-fractional model results.