河海大学学报(自然科学版)
河海大學學報(自然科學版)
하해대학학보(자연과학판)
JOURNAL OF HOHAI UNIVERSITY (NATURAL SCIENCES)
2015年
3期
189-196
,共8页
李勇%张振廷%花剑岚%黄漫丽%周超%倪利晓%朱亮
李勇%張振廷%花劍嵐%黃漫麗%週超%倪利曉%硃亮
리용%장진정%화검람%황만려%주초%예리효%주량
排污口%悬浮物沉降%底泥悬浮%数值模拟%水槽试验
排汙口%懸浮物沉降%底泥懸浮%數值模擬%水槽試驗
배오구%현부물침강%저니현부%수치모의%수조시험
sewage outlet%sedimentation of suspended solids%resuspension of sediments%numerical simulation%flume experiment
采用数值模拟和水槽试验相结合的方法,研究河道排污口不同排污流速比( R分别为4.5、7.2和9.9)对悬浮物在排污口下游区域沉降和底泥再悬浮的影响。结果表明:随着流速比的增加,紊动越剧烈,污染云团扩散范围越大,沉降和悬浮作用也越明显。不同流速比情况下,通过底部水平面的沉降通量变化趋势基本一致,即先增加、后稳定,通量总量随着流速比增大而增加;由于临界起动流速(对应于R=5.8)的存在导致低流速比(R=4.5)情况下再悬浮通量增长缓慢,而中流速比(R=7.2)和高流速比(R=9.9)情况下再悬浮通量增长迅速。由此可见,排污流速对排污口下游区域悬浮物的沉降和底泥再悬浮具有重要的影响。
採用數值模擬和水槽試驗相結閤的方法,研究河道排汙口不同排汙流速比( R分彆為4.5、7.2和9.9)對懸浮物在排汙口下遊區域沉降和底泥再懸浮的影響。結果錶明:隨著流速比的增加,紊動越劇烈,汙染雲糰擴散範圍越大,沉降和懸浮作用也越明顯。不同流速比情況下,通過底部水平麵的沉降通量變化趨勢基本一緻,即先增加、後穩定,通量總量隨著流速比增大而增加;由于臨界起動流速(對應于R=5.8)的存在導緻低流速比(R=4.5)情況下再懸浮通量增長緩慢,而中流速比(R=7.2)和高流速比(R=9.9)情況下再懸浮通量增長迅速。由此可見,排汙流速對排汙口下遊區域懸浮物的沉降和底泥再懸浮具有重要的影響。
채용수치모의화수조시험상결합적방법,연구하도배오구불동배오류속비( R분별위4.5、7.2화9.9)대현부물재배오구하유구역침강화저니재현부적영향。결과표명:수착류속비적증가,문동월극렬,오염운단확산범위월대,침강화현부작용야월명현。불동류속비정황하,통과저부수평면적침강통량변화추세기본일치,즉선증가、후은정,통량총량수착류속비증대이증가;유우림계기동류속(대응우R=5.8)적존재도치저류속비(R=4.5)정황하재현부통량증장완만,이중류속비(R=7.2)화고류속비(R=9.9)정황하재현부통량증장신속。유차가견,배오류속대배오구하유구역현부물적침강화저니재현부구유중요적영향。
Based on numerical simulations and flume experiments, the processes of sedimentation of suspended solids and resuspension of sediments in the region downstream of a sewage outlet in a river were analyzed at three velocity ratios ( R=4. 5 , 7. 2 , and 9. 9 , where R is the ratio of discharge velocity at the sewage outlet to the flow velocity in the river ) . Results show that the relative turbulence intensity and the area of the pollution zone increased with the velocity ratio;this also resulted in significant sedimentation of suspended solids and resuspension of sediments in the river. At the three velocity ratios, the sedimentation fluxes of suspended solids through the bottom horizontal plane have similar distributions: first increasing and then reaching respective stable values; and the total fluxes of suspended solids increased with the velocity ratio. At a low velocity ratio ( R=4. 5 ) , the resuspension fluxes of suspended solids increased slowly due to the existence of a critical incipient velocity ( corresponding to R=5. 8 ) , while at the medium velocity ratio ( R=7. 2 ) and high velocity ratio ( R=9. 9 ) , the resuspension fluxes increased rapidly. As a result, the discharge velocity of the sewage significantly affected the sedimentation of suspended solids and resuspension of sediments in the region downstream of the outlet.