[1]李琪敏,等.叠覆堆积过程中泥石流偏移的实验研究[J].山地学报,2024,(2):249-259.[doi:10.16089/j.cnki.1008-2786.000820]
　LI Qimin,LIU Jingjing,et al.Experiments on Debris Flow Migration in the Process of Overlapping Deposition[J].Mountain Research,2024,(2):249-259.[doi:10.16089/j.cnki.1008-2786.000820]
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叠覆堆积过程中泥石流偏移的实验研究
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2024年第2期
页码:
249-259
栏目:
山地灾害
出版日期:
2024-06-15

文章信息/Info

Title:
Experiments on Debris Flow Migration in the Process of Overlapping Deposition
文章编号:
1008-2786-(2024)2-249-11
作者:
李琪敏1;  2; 刘晶晶1;  2*; 汪 洋1; 刘兆旭3; 龚 旭1;  2
(1. 中国科学院、水利部成都山地灾害与环境研究所 山地自然灾害与工程安全全国重点实验室,成都 610299,2. 中国科学院大学,北京 100049; 3. 西藏大学 工学院,拉萨 850000)
Author(s):
LI Qimin1;  2;  LIU Jingjing1;  2*; WANG Yang1; LIU Zhaoxu3; GONG Xu1;  2
(1. State Key Laboratory of Mountain Hazards and Engineering Resilience, Institude of Mountain Hazards and Environment,Chinese Academy of Science, Chengdu 610299, China; 2. University of Chinese Academy of Science,Beijing 100049,China; 3. College of Engineering, Tibet University, Lhasa 850000, China)
关键词:
泥石流堆积扇;  叠覆堆积;  流态变化;  主流偏移
Keywords:
debris flow fan;  multi-phase deposition;  flow transition;  deviation from mainstream
分类号:
642.23
DOI:
10.16089/j.cnki.1008-2786.000820
文献标志码:
A
摘要:
泥石流堆积扇经过多期叠覆堆积,其在空间和时间分布上有随机性,存在主流偏移和堆积摆动等各向异性现象,给合理规划与利用泥石流滩地带来困难。本文在野外调查四川平武县碓窝梁子沟堆积扇的基础上,开展室内水槽模型实验,结合3D扫描技术和基底压力传感器,探讨泥石流在叠覆堆积过程中的阶段性流态变化以及主流偏移的成因和发展。实验发现:(1)泥石流密度差异导致不同的偏移形式,高密度泥石流易出现层面整体偏移; 低密度泥石流易形成插入式的叠覆堆积。(2)泥石流多期堆叠过程中偏移行为并不一定是沿地势更低处,而是取决于后期来流的性态。(3)泥石流偏移角度和距离依赖于流体密度、流速和堆积体几何特征,可以建立以上述参数为变量的堆积偏移角度与偏移距离的计算公式。本研究成果可以为了解泥石流堆积扇的形成机制、致灾范围和演化趋势提供依据。
Abstract:
A debris flow fan is a typical debris flow sedimentary facies, which generally suffered from overlapping and accumulating by multiple debris flow torrents, and has randomness in spatial and temporal distribution, with anisotropic features such as mainstream migration and oscillating sedimentation, all of which brings difficulties in rational planning and utilization of piedmont beach-land created by debris flow sedimentation.
In this paper, a debris flow fan located at the Duiwoliangzi gully, Lianghebao village, Pingwu county, Sichuan province, China was surveyed and exemplified to reveal the formation of debris flow fan created by overlapping and accumulating of multiple debris flow torrents; a series of flume experiments equipped with 3D scanning devices and a set of pressure sensors was conducted to measure the phrasal changes of fluid regime in the process of creating a debris flow fan by artificial multiple debris flow release. The genesis of mainstream migration in the fan and resulting debris accumulation shift was examined.
(1)Mainstream migration in debris flow fan was controlled mainly by the density of debris flow fluid. The higher density of the fluid, the more possible it was to an overall mainstream deviation; the lower the density, the easier it to form debris body wedging into old underlying fan.
(2)The migration occured not quite along lower relief of the fan, but depended mainly on the properties of a following wave of flows.
(3)An empirical formula for estimating of deviation angle and distance was proposed in terms of flow density, velocity and fan morphology.
The research provides a theoretical basis for understanding the formation, disaster range and evolutionary trend of debris flow fans.

参考文献/References:

[1] 康志成, 李焯芬, 马蔼乃, 等. 中国泥石流研究[M]. 北京: 科学出版社, 2004: 24-39. [KANG Zhicheng, LEE Chackfan, MA Ainai, et al. Study on debris flow in China [M]. Beijing: Science Press, 2004: 24-39]
[2] 陈德明. 泥石流与主河水流交汇机理及其河床响应特征[D]. 北京: 中国水利水电科学研究院, 2000: 2-10, 60-90. [CHEN Deming. Mechanism of confluence between debris flow and the main river [D]. Beijing: China Institute of Water Resources and Hydropower Research, 2000: 2-10,60-90]
[3] 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: 20-30. [FEI Xiangjun, SHU Anping. Movement mechanism and disaster control for debris flow [M]. Beijing: Tshinghua University Press, 2004: 20-30]
[4] DING Mingtao, TANG Chuan, MIAO Cheng. Response analysis of valley settlements to the evolution of debris flow fans under different topographic conditions: A case study of the upper reaches of Min River, China [J]. Bulletin of Engineering Geology and the Environment, 2020, 79(1): 1639-1650. DOI: 10.1007/s10064-019-01641-9
[5] BRIGHENTI R, SPAGGIARI L, SEGALINI A, et al. Debris flow impact on a flexible barrier: Laboratory flume experiments and force-based mechanical model validation [J]. Natural Hazards, 2021, 106(1): 735-756. DOI: 10.1007/s11069-020-04489-5
[6] BRANNEY M J, KOKELAAR P. A reappraisal of ignimbrite emplacement: progressive aggradation and changes from particulate to non-particulate flow during emplacement of high-grade ignimbrite [J]. Bulletin of Volcanology, 1992, 54(6): 504-520. DOI: 10.1007/BF00301396
[7] 崔鹏, 何易平, 陈杰. 泥石流输沙及其对山区河道的影响[J]. 山地学报, 2006, 24(5): 539-549. [CUI Peng, HE Yiping, CHEN Jie. Debris flow sediment transportation and its effects on rivers in mountain area [J]. Mountain Research, 2006, 24(5): 539-549] DOI: 10.3969/j.issn.1008-2786.2006.05.005
[8] 李彦稷, 颜春达, 胡凯衡, 等. 典型暴雨泥石流堆积扇危害范围演变规律[J]. 长江流域资源与环境, 2017, 26(5): 789-796. [LI Yanji, YAN Chunda, HU Kaiheng, et al. Variation of hazard areas of typical rainstorm debris flow alluvial fans [J]. Resources and Environment in the Yangtze Basin, 2017, 26(5): 789-796] DOI: 10.11870/cjlyzyyhj201705017
[9] DENSMORE A L, HAAS T D, MCARDELL B, et al. Making sense of avulsions on debris-flow fans [C]//Colorado School of Mines Golden, Colorado USA. 7th International Conference on Debris-Flow Hazards Mitigation. 2019:54.
[10] DE HAAS T, VAN DEN BERG W, BRAAT L, et al. Autogenic avulsion, channelization and backfilling dynamics of debris-flow fans [J]. Sedimentology, 2016, 63(6): 1596–1619. DOI: 10.1111/sed.12275
[11] ZHOU Wei, FANG Jiaoyong, TANG Chuan, et al. Empirical relationships for the estimation of debris flow runout distances on depositional fans in the Wenchuan earthquake zone [J]. Journal of Hydrology, 2019, 577: 123932. DOI: 10.1016/j.jhydrol.2019.123932
[12] KORUP O. Landslide-induced river channel avulsions in mountain catchments of south-west New Zealand [J]. Geomorphology, 2004, 63(1-2): 57-80. DOI: 10.1016/j.geomorph.2004.03.005
[13] THOMOS D S G. Arid zone geomorphology [M]. John Wiley & Sons, Ltd, 2011: 62-97.
[14] CHAKRABORTY T, KAR R, GHOSH P, et al. Kosi megafan: Historical records, geomorphology and the recent avulsion of the Kosi River [J]. Quaternary International, 2010, 227(2): 143-160. DOI: 10.1016/j.quaint.2009.12.002.
[15] DAVIES T R, MCSAVENEY M J. Principles of sustainable development on fans [J]. Journal of Hydrology(New Zealand), 2008, 47(1): 43-65.
[16] SUWA H, OKANO K, KANNO T. Behavior of debris flows monitored on test slopes of Kamikamihorizawa Creek, Mount Yakedake, Japan [J]. International Journal of Erosion Control Engineering, 2009, 2(2): 33-45. DOI: 10.13101/ijece.2.33
[17] 柳金峰, 游勇, 范建容, 等. 汶川地震触发潜在性泥石流研究——以岷江上游关山沟为例[J]. 四川大学学报(工程科学版), 2009, 41(S1): 70-75. [LIU Jinfeng, YOU Yong, FAN Jianrong, et al. The study on the potential debris flow triggered by Wenchuan Earthguake: A case study of the Guanshan Gully in the upper reaches of Miniiang River [J]. Journal of Sichuan University(Engineering Science Edition), 2009, 41(S1): 70-75] DOI: 10.15961/j.jsuese.2009.s1.010
[18] 崔之久. 混杂堆积与环境[M]. 河北: 河北科学技术出版社, 2013: 20-30. [CUI Zhijiu. Diamicton and Environment [M]. Hebei: Hebei Science and Technology Press, 2013: 20-30]
[19] 陈杰, 韦方强, 崔鹏. 小江流域泥石流堆积扇形成的制约因素及其特征[J]. 地理科学, 2005, 25(6): 6704-6708. [CHEN Jie, WEI Fangqiang, CUI Peng. Restricting conditions and their characteristics for debris flow fans in Xiaojiang River valley [J]. Scientia Geographica Sinica, 2005, 25(6): 6704-6708] DOI: 10.3969/j.issn.1000-0690.2005.06.009
[20] 范念念, 吴保生, 刘乐. 地震导致河流改道与古蜀文明的变迁[J]. 山地学报, 2010, 28(4): 453-462. [FAN Niannian, WU Baosheng, LIU Le. River avulsion by earthquake and the transition of ancient Shu civilization [J]. Mountain Research, 2010, 28(4): 453-462] DOI: 10.3969/j.issn.1008-2786.2010.04.008
[21] 李春雨, 刘晶晶, 陈晓清, 等. 泥石流叠加堆积形态演化特征的实验研究[J]. 山地学报, 2022, 40(2): 235-248. [LI Chunyu, LIU Jingjing, CHEN Xiaoqing, et al. Experimental investigation on the morphological evolution of superimposed deposition of debris flow [J]. Mountain Research, 2022, 40(2): 235-248] DOI: 10.16089/j.cnki.1008-2786.000668
[22] 周必凡, 李德基, 罗德富, 等. 泥石流防治指南[M]. 北京: 科学出版社, 1991: 50-90. [ZHOU Bifan, LI Deji, LUO Defu, et al. Guide for debris flow prevention and control [M]. Beijing: Science Press, 1991: 50-90]
[23] MAJOR J J, IVERSON R M. Debris-flow deposition: Effects of pore-fluid pressure and friction concentrated at flow margins [J]. Geological Society of America Bulletin, 1999, 111(10): 1424-1434. DOI: 10.1130/0016-7606(1999)111<1424:DFDEOP>2.3.CO; 2
[24] IVERSON R M. Elementary theory of bed-sediment entrainment by debris flows and avalanches [J]. Journal of Geophysical Research: Earth Surface, 2012, 117: F03006. DOI: 10.1029/2011JF002189
[25] DE HAAS T, KRUIJT A, DENSMORE A L. Effects of debris flow magnitude-frequency distribution on avulsions and fan development [J]. Earth Surface Processes and Landforms, 2018, 43(13): 2779-2793. DOI: 10.1002/esp.4432
[26] HAAS T D, BRAAT L, LEUVEN I R, et al. Effects of debris flow composition on runout, depositional mechanisms, and deposit morphology in laboratory experiments [J]. Journal of Geophysical Research: Earth Surface, 2015, 120(9): 1949-1972. DOI: 10.1002/2015JF003525

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备注/Memo

备注/Memo:
收稿日期(Received date): 2024- 01-27; 改回日期(Accepted date):2024- 04-20
基金项目(Foundation item): 国家自然科学基金(42271092,41877261); 中国科学院特别交流计划(E3R5050050); 中国科学院西部青年学者项目(E2R2180180)。[National Natural Science Foundation of China(42271092,41877261); Special Exchange Program of Chinese Academy of Sciences(E3R5050050); West Young Scholars Program of Chinese Academy of Sciences(E2R2180180)]
作者简介(Biography): 李琪敏(1998-),女,河北沧州人,硕士研究生。主要研究方向:山地灾害理论及工程防治。[LI Qimin(1998-), female, born in Cangzhou, Heibei province, M.Sc. candidate, research on mountain disaster theory and engineering prevention] E-mail: 913971668@qq.com
*通讯作者(Corresponding author): 刘晶晶(1981-),女,博士,副研究员。主要研究方向:山地灾害理论及工程防治。[LIU Jingjing(1981-), female, Ph.D., associate professor, research on mountain disaster theory and engineering prevention] E-mail: liujingjing@imde.ac.cn
更新日期/Last Update: 2024-03-30