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黏性泥石流残留层的床面减阻研究综述
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  • 英文篇名:A review of study on drag reduction of viscous debris-flow residual layer
  • 作者:刘晶晶 ; 李泳
  • 英文作者:LIU Jing-jing;LI Yong;State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering;Institute of Mountain Hazards and Environment,Chinese Academy of Sciences & Ministry of Water Resources;Key Laboratory of Mountain Hazards and Earth Surface Processes,Chinese Academy of Sciences;
  • 关键词:黏性泥石流 ; 铺床 ; 残留层 ; 减阻 ; 床面阻力
  • 英文关键词:viscous debris flow;;paving processes;;residual layer;;drag reduction;;bed resistance
  • 中文刊名:NSYJ
  • 英文刊名:Journal of Sediment Research
  • 机构:河海大学水文水资源与水利工程科学国家重点实验室;中国科学院-水利部成都山地灾害与环境研究所;中国科学院山地灾害与地表过程重点实验室;
  • 出版日期:2016-06-15
  • 出版单位:泥沙研究
  • 年:2016
  • 基金:中国科学院西部之光重点项目(Y5R2040040);; 水文水资源与水利工程科学国家重点实验室开放基金项目(2015491011)
  • 语种:中文;
  • 页:NSYJ201603011
  • 页数:9
  • CN:03
  • ISSN:11-2532/TV
  • 分类号:75-83
摘要
黏性泥石流运动理论的核心问题在于确定黏性泥石流运动阻力和流速。但由于其运动的复杂、流态的多样,导致了阻力准确计算的困难,也制约了泥石流运动流速和流量公式的建立和推广应用。关于黏性泥石流的运动阻力问题,目前多聚焦于泥石流固液间相互作用的内部阻力关系,鲜见对于其床面阻力的研究。介绍了黏性泥石流的典型运动过程—"铺床",描述了铺床过程形成的残留层导致床面减阻现象,概述了目前国内外各泥石流运动模型对泥石流阻力的研究,并总结了残留层导致减阻的可能原因和目前多采用的床面阻力计算方法。认为残留层导致的复杂减阻效应,是黏性泥石流运动尤其是高速运动研究中不可忽视的一部分,但目前各类模型和水力学经验公式都无法概化黏性泥石流运动床面的阻力变化。鉴于此,提出了未来可开展的工作:(1)认知"铺床"导致的残留层的形成和发展过程;(2)探讨残留层床面减阻机制;(3)研究残留层床面阻力计算。
        Key theoretical topics of study on viscous debris-flow are resistance and velocity. However it is so difficult to calculate movement resistance accurately,which also restrict the establishment and application of velocity and discharge formula,because of complex movement and various flow patterns of viscous debris-flow.Previous studies focus on internal resistance due to the solid-liquid interaction,but the studies in bed hindrance are uncommon. This paper introduces the typical processes in debris-flow movement — "paving process",describes drag-reduction phenomenon caused by residual layer,provides an overview of the studies in resistance based on debris-flow motion models,and summarizes the possible impact parameters of drag reduction and common calculation methods of bed resistance. The study shows that the complex drag-reduction effect caused by residual layer is so important,which cannot be ignored in motion study,especially in highspeed motion of viscous debris flow. However,the motion models and hydraulics formula cannot provide a characterization of bed resistance changes in viscous debris-flow movement. Based on the research status and available technologies at present,the future work is proposed:( 1) recognizing the formation and development of residual layer in paving process;( 2) exploring the drag-reduction mechanism by residual layer;( 3) studying the residual layer bed-resistance formula.
引文
[1]Takahashi T.Debris flow[J].Annual review of fluid mechanics,1981,13(1):57-77.
    [2]钱宁,王兆印.泥石流运动机理的初步探讨[J].地理学报,1984,39(1):33-43.
    [3]田连权,吴积善,康志成,等.泥石流侵蚀搬运与堆积[M].成都:成都地图出版社,1993:2-26.
    [4]吴积善,田连权,康志成.泥石流及其综合治理[M].北京:科学出版社,1993.
    [5]崔之久.泥石流沉积与环境[M].北京:海洋出版社,1996.
    [6]康志成,李焯芬,马蔼乃.中国泥石流研究[M].北京:科学出版社,2004.
    [7]陈光曦,王继康,王林海.泥石流防治[M].北京:中国铁道出版社,1983.
    [8]吴积善,康志成,田连权,等.云南蒋家沟泥石流观测研究[M].北京:科学出版社,1990.
    [9]Enos P.Flow regimes in debris flow[J].Sedimentology,1977,24(1):133-142.
    [10]周富春,刘立平.紊流性泥石流对渡槽的作用力分析[J].重庆大学学报:自然科学版,2001(5):78-80+88.
    [11]Imran J,Harff P,Parker G.A numerical model of submarine debris flow with graphical user interface[J].Computers&geosciences,2001,27(6):717-729.
    [12]Takahashi T.Debris flow:mechanics,prediction and countermeasures[M].Taylor&Francis,2007.
    [13]吴积善.泥石流特性分析[J].中国水土保持,1987(5):4-10.
    [14]吴积善.蒋家沟泥石流流态[J].山地研究,1987(4):237-246+301.
    [15]余斌.黏性泥石流的平均运动速度研究[J].地球科学进展,2008(5):524-532.
    [16]张军.泥石流运动流型与流态特征[J].山地研究,1991(3):197-203.
    [17]胡凯衡,韦方强,李泳,等.泥石流的阵性波状运动[J].山地学报,2004(6):707-712.
    [18]杨重存,曾思伟,张又安.泥石流的波状流动及计算[C]//第四届亚太可持续发展交通与环境技术大会,西安,2005.
    [19]弗莱施曼C M.泥石流[M].北京:科学出版社,1986:69-91.
    [20]Bagnold R A.Experiments on a gravity-free dispersion of large solid spheres in a Newtonian fluid under shear[J].Proceedings of the Royal Society of London.Series A.Mathematical and Physical Sciences,1954,225(1160):49-63.
    [21]Walton O R.Numerical simulation of inelastic,frictional particle-particle interactions[M].Particulate Two-Phase Flow,Butterworth-Heinemann,Newton,Mass.,1993:884-911
    [22]Savage S B.The mechanics of rapid granular flows[J].Advances in applied mechanics,1984,24:289-366.
    [23]Malekzadeh M J.Flow of liquid-solid mixtures down inclined chutes[D].Mc Gill University,1993.
    [24]费祥俊,舒安平.泥石流运动机理与灾害防治[M].北京:清华大学出版社,2004.
    [25]Iverson R.The physics of debris flows[J].Reviews of geophysics,1997,35:245-296.
    [26]张军,吴积善,游勇,等.黏性泥石流残留层的形成及减阻作用——以云南蒋家沟泥石流为例[J].山地学报,2003(2):223-227.
    [27]吴积善,张军,程尊兰,等.黏性泥石流的泥深与残留层关系及其确定[J].泥沙研究,2003(6):7-12.
    [28]刘晶晶,李泳,程尊兰,等.阵性泥石流的流量衰减特征[J].中国科学院研究生院学报,2008(2):177-184.
    [29]杜榕桓,康志成,陈循谦.云南小江泥石流综合考察与防治规划研究[M].重庆:科学技术文献出版社重庆分社,1987:57-71.
    [30]康志成.黏性泥石流加速运动的力学分析[J].山地研究,1991(3):193-196.
    [31]王兆印,崔鹏,余斌.泥石流的运动机理和减阻[J].自然灾害学报,2001(3):37-43.
    [32]Hungr O.Analysis of debris flow surges using the theory of uniformly progressive flow[J].Earth surface processes and landforms,2000,25(5):483-495.
    [33]Ghilardi P,Natale L,Savi F.Two mathematical models simulating a real-world debris-flow[C].Proc.IAHR Symposium on River,Coastal and Estuarine Morphodynamics,Genova,1999.
    [34]Bollschweiler M,Stoffel M,Ehmisch M,et al.Reconstructing spatio-temporal patterns of debris-flow activity using dendrogeomorphological methods[J].Geomorphology,2007,87(4):337-351.
    [35]Yano K,Daido A.Fundamental study on mud-flow[J].Bulletin of the Disaster Prevention Research Institute,1965,14(2):69-83.
    [36]O'Brien J S,Julien P Y.Laboratory analysis of mudflow properties[J].Journal of hydraulic engineering,1988,114(8):877-887.
    [37]Major J J,Pierson T C.Rheological analysis of fine-grained natural debris-flow material[R].Hydraulics/Hydrology of Arid Lands.American Society of Civil Engineers,New York.1990.225-231.
    [38]Phillips C J,Davies T R H.Debris flow material rheology direct measurement[J].Proc.of Inter.Sym.on Erosion and Volcanic Debris Flow Fechnology,Indonesia,1989:21-28.
    [39]Wang G,Sassa K,Fukuoka H,et al.Experimental study on the shearing behavior of saturated silty soils based on ringshear tests[J].Journal of geotechnical and geoenvironmental engineering,2007,133(3):319-333.
    [40]Iverson N R,Mann J E,Iverson R M.Effects of soil aggregates on debris-flow mobilization:results from ring-shear experiments[J].Engineering Geology,2010,114(1):84-92.
    [41]张军,熊刚.云南蒋家沟泥石流运动观测资料集[M].北京:科学出版社,1997.
    [42]Johnson,A.,Rahn,P.Mobilization of debris flows[J].Zeitschrift fur Geomorphologie,1970,9:168-186.
    [43]周必凡.黏性泥石流阻力和运动方程验证分析[J].山地学报,1999(1):56-59.
    [44]Chen Cheng-lung.General solutions for viscoplastic debris flow[J].Journal of Hydraulic Engineering,1988,114:259-282.
    [45]Savage S,Hutter K.The motion of a finite mass of granular material down a rough incline[J].Journal of Fluid Mechanics,1989,199(1):177-215.
    [46]Takahashi T.Mechanical characteristics of debris flow[J].Journal of the Hydraulics Division,1978,104(8):1153-1169.
    [47]王光谦,倪晋仁.颗粒流研究评述[J].力学与实践,1992(1):7-19.
    [48]王光谦,倪晋仁.泥石流动力学基本方程[J].科学通报,1994(18):1700-1704.
    [49]王勇智.固液两相泥石流运动计算力学[D].重庆:重庆交通大学,2008.
    [50]沈寿长,谢慎良.黏性泥石流的结构模式和流变特性[J].铁道工程学报,1986(4):26-33.
    [51]王光谦,倪晋仁.固液两相流流速分布特性的试验研究[J].水利学报,1992(11):43-49.
    [52]倪晋仁,王光谦.泥石流的结构两相流模型:I.理论[J].地理学报,1998(1):67-77.
    [53]倪晋仁,王光谦,熊育武,等.泥石流的结构两相流模型:Ⅱ.应用[J].地理学报,1998(1):78-86.
    [54]费祥俊.黏性泥石流的输沙浓度与运动速度[J].水利学报,2003(2):15-18.
    [55]杨红娟,韦方强,胡凯衡.黏性泥石流运动模型在蒋家沟的对比检验[J].水土保持通报,2012,32(3):182-187.
    [56]杜榕桓.我国泥石流研究的进展[J].山地研究,1986(4):249-254.
    [57]刘大有,徐胜利,章书成,等.Bingham流体阵性流动立面二维计算及分析:阵流速度、形态和床面阻力[J].科学通报,2003,48(9):981-987
    [58]吴积善,程尊兰,耿学勇,等.黏性泥石流产流机理探讨[J].泥沙研究,2007(2):17-23.
    [59]田昭一,徐海鹏,曾思伟.黏性泥石流的堆积地貌及沉积物的特征[J].水土保持通报,1985(1):30-34+41.
    [60]康志成.云南东川蒋家沟黏性泥石流流速的初步分析[C]//中国科学院兰州冰川冻土研究所集刊(4),北京:科学出版社,1985:119-123.
    [61]杨针娘.暴雨型黏性泥石流流速的初步分析[C]//中国科学院兰州冰川冻土所研究集刊(4),北京:科学出版社,1985:199-206.
    [62]Toms B A.Some observations on the flow of linear polymer solutions through straight tubes at large Reynolds numbers[C].Proc.of the 1st International Congress on Rheology,Vol.II,135,North-Holland,Amsterdam,1949.135-141.
    [63]窦国仁.高分子聚合物减阻流的紊流结构[J].水利水运工程学报,1981(1):1-11.
    [64]Heywood N I,Richardson J F.Head loss prediction by gas injection for highly shear-thinning suspensions in horizontal pipe flow[C].In Proc.,Hydrotransport,1978,1-22.
    [65]Sakamoto M,Mase M,Nagawa Y,et al.A hydraulic transport study of coarse materials including fine particles with hydrohoist[C].Hydrotransport 5,BHM Fluid Engineering,1978,79-80.
    [66]Gust G.Observations on turbulent-drag reduction in a dilute suspension of clay in sea-water[J].Journal of Fluid Mechanics,1976,75(1):29-47.
    [67]侯晖昌.明流泥沙降阻原因和计算方法[J].泥沙研究,1981(1):30-41.
    [68]杨德昌,樊明.含盐稀淤泥悬浮液的紊流减阻试验[J].水利水运科学研究,1983(2):24-35.
    [69]周国栋,刘琼轶,王桂仙,等.非均匀沙床面阻力特性的试验研究[J].泥沙研究,1999(3):42-49.
    [70]练继建,洪柔嘉.淤泥质床面的阻力特征[J].科学通报,1994,39(19):1796-1798.
    [71]王裕宜,詹钱登,邹仁元.黏性泥石流体应力过冲特征与阵性流形成机理初探[J].中国地质灾害与防治学报,2000,11(3):56-60.
    [72]王裕宜,詹钱登,邹仁元,等.黏性泥石流体阵性流形成机理研究[J].自然灾害学报,2002,11(2):46-50.
    [73]王裕宜,詹钱登,韩文亮,等.黏性泥石流体的应力应变特性和流速参数的确定[J].中国地质灾害与防治学报,2003,14(1):9-13.
    [74]王兆印,林秉南,张新玉.非牛顿体不稳定流的研究[J].力学学报,1990,22(3):266-275.
    [75]王兆印,崔鹏,余斌.泥石流的运动机理和减阻[J].自然灾害学报,2001,10(3):37-43.
    [76]徐永年,匡尚富,舒安平.阵性泥石流的平均流速与加速效应[J].泥沙研究,2001(6):8-13.
    [77]韩文亮,王裕宜,詹钱登.黏性泥石流掺气减阻作用初探——云南东川蒋家沟泥石流[J].泥沙研究,2000(5):1-5.
    [78]田密.动床条件下泥石流阻力特性的实验研究[D].北京:中国科学院大学,2013.
    [79]韦方强,胡凯衡.泥石流流速研究现状与发展方向[J].山地学报,2009,27(5):545-550.
    [80]Takahashi T,Sawada T,Suwa H.IAHR monography series[M].The Netherlands:Balkema Publishers,1991.
    [81]Rickenmann D.Empirical relationships for debris flows[J].Natural Hazards,1999,19(1):47-77.
    [82]Koch T.Testing various constitutive equations for debris flow modelling[M].IAHS Publications-Series of Proceedings and Reports-Intern Assoc Hydrological Sciences,1998,248:249-258.
    [83]Jin M,Fread D L.1D modeling of mud/debris unsteady flows[J].Journal of hydraulic engineering,1999,125(8):827-834.
    [84]Iverson R M.Differential equations governing slip-induced pore-pressure fluctuations in a water-saturated granular medium[J].Mathematical geology,1993,25(8):1027-1048.

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