铁道学报
鐵道學報
철도학보
2014年
5期
82-87
,共6页
路堤%风沙两相流%数值模拟%运动特性
路隄%風沙兩相流%數值模擬%運動特性
로제%풍사량상류%수치모의%운동특성
embankment%wind-blown sand flow%numerical Simulation%motion characteristic
基于 FLENT欧拉双流体模型,对路堤周围风沙两相流运动特性进行数值模拟,并将模拟结果与现场实际调查进行比较。结果表明,所用模型能较好地模拟路堤周围风沙两相流的运动特性,数值模拟与现场调查相吻合。数值模拟分析表明:路堤周围气流速度产生分区,分别形成减速区、加速区、高速区、低速区与紊流区;沙粒速度与风速相互影响,形成一种反馈机制;在过渡区内,当风速大于起沙风速时,沙粒速度与风速呈正相关;正交单向来风条件下,揭示了迎风坡积沙量大于背风坡的形成机理;路堤顶面积沙量呈“正态形”分布,中间多,两边少;迎风坡积沙量随着风速增大而减小,背风坡无明显变化;不同地表条件对风沙流密度及结构影响显著,决定着工程防沙措施。
基于 FLENT歐拉雙流體模型,對路隄週圍風沙兩相流運動特性進行數值模擬,併將模擬結果與現場實際調查進行比較。結果錶明,所用模型能較好地模擬路隄週圍風沙兩相流的運動特性,數值模擬與現場調查相吻閤。數值模擬分析錶明:路隄週圍氣流速度產生分區,分彆形成減速區、加速區、高速區、低速區與紊流區;沙粒速度與風速相互影響,形成一種反饋機製;在過渡區內,噹風速大于起沙風速時,沙粒速度與風速呈正相關;正交單嚮來風條件下,揭示瞭迎風坡積沙量大于揹風坡的形成機理;路隄頂麵積沙量呈“正態形”分佈,中間多,兩邊少;迎風坡積沙量隨著風速增大而減小,揹風坡無明顯變化;不同地錶條件對風沙流密度及結構影響顯著,決定著工程防沙措施。
기우 FLENT구랍쌍류체모형,대로제주위풍사량상류운동특성진행수치모의,병장모의결과여현장실제조사진행비교。결과표명,소용모형능교호지모의로제주위풍사량상류적운동특성,수치모의여현장조사상문합。수치모의분석표명:로제주위기류속도산생분구,분별형성감속구、가속구、고속구、저속구여문류구;사립속도여풍속상호영향,형성일충반궤궤제;재과도구내,당풍속대우기사풍속시,사립속도여풍속정정상관;정교단향래풍조건하,게시료영풍파적사량대우배풍파적형성궤리;로제정면적사량정“정태형”분포,중간다,량변소;영풍파적사량수착풍속증대이감소,배풍파무명현변화;불동지표조건대풍사류밀도급결구영향현저,결정착공정방사조시。
The motion characteristics of wind-blown sand flow around the railway embankment were simulated by the FLENT eulerian two-fluid model,and the simulation results were compared with field surveys.Results show that the model can well simulate the motion characteristics of wind-blown sand flow around the railway embankment,and the numerical simulation is in conformity with field investigations.Numerical simulation a-nalysis shows as follows:Air velocities surrounding the embankment produce partitioned area,i.e.,the decel-eration area,acceleration area,high-speed area,low-speed area and turbulent area;sand speeds and wind speeds influence one another,forming a feedback mechanism;in the transition zone,when the wind speed is greater than the initial sand speed,the velocity of sand grain is positively correlated with the wind speed;the formation mechanism that the sand sediment on the windward slope is more than on the leeward slope is re-vealed under the condition of the single orthogonal wind direction;sand sediment on the top of the embankment is in normal distribution,more in the middle and less on both sides;as the wind speed raizes,windward slope sediment decreases whereas leeward slope sediment has no obvious changes;different ground surface conditions have significant effects on the sand flow density and structure,thus determining the engineering sand preven-tion measures to be taken.