物理模拟材料流变性质研究现状
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摘要
模拟材料的选用以及其相关参数的测定是物理模拟实验的基础。当前采用的延性材料能通常有粘泥、石蜡、松香、塑化松香、塑胶粘土等,国内使用的流变仪主要为毛细管流变仪、旋转流变仪、落球式流变仪,国外对三轴流变仪的研制、应用已见成效。今后应加强新型模拟材料的研制、开发,同时积极研制、引进合适的流变仪。
Physical modeling experiments are based on the choice of the materials and the determination of the rheological parameter.The flexible materials nowadays used in the experiments include generally clay mud,paraffin wax,rosin,plasticized rosin and plastic clay.Rheometers used in China are mainly capillary rheometer, rotary rheometer,falling sphere rheometer.Abroad,development and application of 3-axial rheometers have won successes.In the future,we should strengthen development of new modeling materials and proper rheometers and their introduction.
引文
[1]曾佐勋,刘立林.构造模拟[M].武汉:中国地质大学出版社,1992.
    [2]Neurath C,Smith R B.Effect of material properties on growthrates of folding and boudinage:experiments with wax models[J].J.Struct.Geol.,1982,4(2):215-229.
    [3]Cobbold,P.R.,Jackson M.P.A.Gum rosin(colophony):A suitable material for thermomechanical modeling of the litho-sphere[J].Tectonophysics,1992,210:255-271.
    [4]周永胜,王绳祖,李建国.物理模拟理想材料———塑化松香和有关物理参数测定[J].世界地质,2000,19(4):313-319.
    [5]李建国,周永胜,宋瑞卿,等.岩石圈塑性流动网络与多层构造变形的物理模拟[J].地震地质,1997,19(3):248-257.
    [6]周永胜,李建国,王绳祖,等.用物理模拟实验研究大陆伸展构造[J].地质力学学报,2002,8(2):141-148.
    [7]周永胜,李建国,王绳祖.用物理模拟研究地幔上隆与大陆裂陷伸展[J].地质力学学报,2000,6(1):22-32.
    [8]王绳祖.亚洲大陆岩石圈多层构造模型和塑性流动网络[J].地质学报,1993,67(1):1-18.
    [9]McClay K R.The rheology of plasticine[J].Tectonophysics,1976,33:T7-T15.
    [10]Ruud W.Flow behaviour and physical chemistry of bouncingputties and related polymers in view of tectonic laboratory ap-plications[J].Tectonophysics,1985,124:325-358.
    [11]Ramberg H.Natural and experimental boudinage and pinch-and-swell structures[J].J.Struct.Geol.,1955,63(6):512-526.
    [12]Haakon F,Roy H Gabrielsen.Experimental modeling of ex-tensional fault systems by use of plaster[J].J.Struct.Ge-ol.,1996,18(5):673-687.
    [13]Kobber G,Zulauf G.Experimental folding and boudinageunder pure constrictional conditions[J].J.Struct.Geol.,1995,17(7):1055-1063.
    [14]Janet Z,Gernold Zulau.Rheology of plasticine used as rockanalogue:the impact of temperature,composition and strain[J].J.Struct.Geol.,2004,26:725-737.
    [15]Cobbold P R.Fold propagation in single embedded layers[J].Tectonophysics,1975,27,333-351.
    [16]Hailemariam H,Mulugeta G.Temperature-dependent rhe-ologies of bouncing putties used as rock analogus[J].Tec-tonophysics,1998,294:131-141.
    [17]Kidan T W,Cosgrove J W.The deformation of multilayersby layer-normal compression;an experimental investigation[J].Journal of Structural Geology,1996,18:461-474.
    [18]Martin P J S,Gernold Z.Strain-dependent rheology and thememory of plasticine[J].Tectonophysics,2002,354:85-99.
    [19]周彦豪.聚合物加工流变学基础[M].西安:西安交通大学出版社,1988.
    [20]沈崇棠,刘鹤年.非牛顿流体力学及其应用[M].北京:高等教育出版社,1989.
    [21]赵洪,王暄,崔思海,等.基于计算机测控技术的转矩流变仪的研制[J].塑料工业,2002,30(3):52-54.
    [22]侯克鹦,杨晓雷.浆液体流变性及其测试研究[J].试验技术与试验机,2002,42(1):18-22.
    [23]段鸿杰,孙恒虎.高浓度浆体流变参数测定的新方法[J].中国矿业大学学报,2001,30(4):371-374.
    [24]曾佐勋,刘立林,黄定华,等.高粘度非牛顿模型材料流变性能的实验测定[J].地质力学学报,1995,1(2):35-39.
    [25]Cobbold P R.A biaxial press for model deformation and rheo-logical tests[J].Tectonophysics,1975,26:1-5.
    [26]Zulauf G.,Zulauf J,Hastreiter P,et al.A deformation ap-paratus for three-dimensional coaxial deformation and its ap-plication to rheologically stratified analogue material[J].J.Struct.Geol.,2003,25:469-480.

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