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WANG Yu-yi, JAN Chyan-deng, HAN Wen-liang, ZOU Ren-yuan. A Study on Forming Mechanism of the Bedding Structure of the Gravel Accumulated at Surface, and Rough Bedding Structure in Deposits of Viscous Debris Flows with Hyperconcentration[J]. Acta Sedimentologica Sinica, 2003, 21(2): 205-210.
Citation: WANG Yu-yi, JAN Chyan-deng, HAN Wen-liang, ZOU Ren-yuan. A Study on Forming Mechanism of the Bedding Structure of the Gravel Accumulated at Surface, and Rough Bedding Structure in Deposits of Viscous Debris Flows with Hyperconcentration[J]. Acta Sedimentologica Sinica, 2003, 21(2): 205-210.

A Study on Forming Mechanism of the Bedding Structure of the Gravel Accumulated at Surface, and Rough Bedding Structure in Deposits of Viscous Debris Flows with Hyperconcentration

  • Received Date: 2002-02-15
  • Rev Recd Date: 2002-04-08
  • Publish Date: 2003-06-10
  • According to observational data of viscous debris flows with hyper-concentration , distinct causes of formation for different graded bedding in debris flow deposits have been analyzed by use of its rheology and the ratio of flow plug . The paper specially analyzed that the gravel in squirm condition of hyper-concentration viscous flows would tend to have vertical motion due to the effect of Weissenberg , then they would form the bedding structure of the gravel accumulated at surface, and they are different from rough bedding structure.
  • [1] 王裕宜,费祥俊.自然界泥石流流变模型的探讨[J].科学通报,1999,44(11): 1 211 ~ 1 214[Wang Yuyi and Fei Xiangjun, A modifiedrheological model of natural debris flows[J]. Chinese Science Bulletin,2000,45 (8) :743~747]
    [2] 王裕宜,邹仁元等.泥石流堆积坡度预测模式研究[J].海峡两岸山地灾害与环境保育研究,1998,(1):144~148[Wang Yuyi,Zou Renyuan, et al. Predicting deposit model of debris flow[J]. Research on mountain disasters and environmental protection across Taiwan Strait,1998,(1):149~154]
    [3] 爱文森R M等.美国俄勒岗大型泥石流水槽实验实施[J].滑坡信息,1993,7:29~31[Iverson R M, et al. Large-scale debris-flow flume becomes operational in Oregon USA[J]. Landslide News,1993,7:29~31]
    [4] 崔之久.论泥石流沉积与环境[J].海峡两岸山地灾害与环境保育研究,1998,(1):133~138[Cui Zhijui.Debrisflow sediment action and environment [J]. Research on mountain disasters and environmental protection across Taiwan Strait, 1998, (1): 133 ~ 138 ]
    [5] 唐川,刘希林.泥石流动力堆积模凝和危险范围预测模型[M].北京:科学出版社,1992.57~59[Tan Chuan,Liu Xingli.Predicting model of hydraulic deposit simulate and dangerous arrange in debris flows[M]. Beijing: Science Press, 1992.57~59]
    [6] 王裕宜,熊刚等.泥石流体应力衰减和堆积形貌的初探.流变学进展Ⅱ[M].上海:华东化工学院出版社,1990.56~63[Wang Yuyi,Xiong Gong at all. A study on stress attenuation and deposit geomorphology. Advance Rheology Ⅱ [M]. Shanghai: Press of Chemical Industry College in East China, 1990.56~63]
    [7] 李依,康帝.新西兰北塞奥柏利托玛思山泥石流沉积物的预测.地球表面过程[C].1980.227~247[Lee E,Coundy W.Predicting deposition of debris flow at Mt Thomas, North Cent Orbury, New Zealand.Earth Surface Process[C]. 1980.227~247]
    [8] 麦介尔J J.美国俄勒岗大型水槽泥石流沉积的实验研究[R].美国地质调查局野外报告.1994.0~28[Major J J.Experimental studies of deposition at a debris-flow flume[R]. USGS Open-file Report. 1994.0~28]
    [9] 刘耕年,崔之久等.泥石流的宏观构造与形成机理.泥石流观测与研究[M].成都:科技出版社,1996.24~32[Lui Gennian,Cui Zhijui et al. Sediment macro-structures and forming mechanism of debris flow .Bulletin of Debris Flow Observation and Research Contents [M].Chengdu: Scientific and Technological Press, 1996.24~ 32 ]
    [10] 依偌斯P.泥石流的流态[J].沉积学.1977,24(1):133~142[Enos P. Flow regimes in debris flows[J]. Sedimentology, 1977,24(1): 133~ 142]
    [11] 吴积善等.泥石流及其综合治理[M].北京:科学出版社,1993.99~110[Wu Juesan et al. Debris flow and control[M]. Beijing:Science Press, 1993.99~110 ]
    [12] 许元译.高分子结构流变学[M].成都:四川教育出版社,1985.14~21 [ Xu Yuanze translation . Texture rheology of macromolecule[M]. Chengdu:Sichuan Education Press , 1985.14~21 ]
    [13] 约翰逊A M著,张之立,李兴才译.地质学中的物理过程[M].北京:科学出版社,1983.12~14[Jo hson A M.Physical presses in geography(in Chinese)[M].Beijing:Science Press,1983.12~14]
    [14] 崔之久.初探沟谷泥石流及其扇形地的沉积类型、宏观特征与形成机理[J].沉积学报,1985,3(2):59~79[Cui Zhijui.A study on deposit type ,macro-characteristics and forming mechanism in ravine debris flows and its fans[J]. Acta Sedimentology Sinica, 1985,3(2) :59~79]
    [15] 吴积善,康志成等.云南蒋家沟泥石流观测研究[M].北京:科学出版社,1990.4~6[WuJuesan,Kang Chicheng,et al.Observation and research of debris flow in Jiangjia ravine , Yunnan Province[M]. Beijing: Science Press,1990.4~6]
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  • Received:  2002-02-15
  • Revised:  2002-04-08
  • Published:  2003-06-10

A Study on Forming Mechanism of the Bedding Structure of the Gravel Accumulated at Surface, and Rough Bedding Structure in Deposits of Viscous Debris Flows with Hyperconcentration

Abstract: According to observational data of viscous debris flows with hyper-concentration , distinct causes of formation for different graded bedding in debris flow deposits have been analyzed by use of its rheology and the ratio of flow plug . The paper specially analyzed that the gravel in squirm condition of hyper-concentration viscous flows would tend to have vertical motion due to the effect of Weissenberg , then they would form the bedding structure of the gravel accumulated at surface, and they are different from rough bedding structure.

WANG Yu-yi, JAN Chyan-deng, HAN Wen-liang, ZOU Ren-yuan. A Study on Forming Mechanism of the Bedding Structure of the Gravel Accumulated at Surface, and Rough Bedding Structure in Deposits of Viscous Debris Flows with Hyperconcentration[J]. Acta Sedimentologica Sinica, 2003, 21(2): 205-210.
Citation: WANG Yu-yi, JAN Chyan-deng, HAN Wen-liang, ZOU Ren-yuan. A Study on Forming Mechanism of the Bedding Structure of the Gravel Accumulated at Surface, and Rough Bedding Structure in Deposits of Viscous Debris Flows with Hyperconcentration[J]. Acta Sedimentologica Sinica, 2003, 21(2): 205-210.
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