The relationship between morphometric parameters of alluvial fans’ upland catchment basin and soil resistance properties

نوع مقاله : مقاله پژوهشی

نویسندگان

Department of Geography, Faculty of Literature and Humanities, Razi University, Kermanshah, Iran

چکیده

Morphometric properties of alluvial fans’ upland catchment basin e.g. the area, length of the main flow channel, and slope can affect particles’ features like roundedness, surface texture, and shear resistance i.e. grains’ angle of internal friction and cohesion. To carry out the current study, first 21 alluvial fans were selected through examining satellite images and conducting field observations. The selected alluvial fans were similar in terms of lithological features and different with regard to their morphology. Samples were obtained from the top, middle, and bottom of alluvial fans. The results showed that, through geomorphological processes, alluvial fans’ area and length of the main flow channel increases and their slopes declines from the top to the bottom. These features make grains at the bottom more rounded and less rough. The highest degree of roundedness and smoothness were observed in particles in the largest area, the longest main flow channel, and the lowest average slope of catchment basin. Depending on the morphometric parameters of the catchment basin, the angle of internal friction ranged from 44.3 ˚at the top to at the bottom of alluvial fans. Indeed, the highest angle of friction was detected in alluvial fans with the smallest catchment basin area, shortest main flow channel, and highest slope. Thus, the rise in catchment basins’ area and length of the main channel flow and the reduction in their slope will lead to smaller angle of internal friction.

کلیدواژه‌ها

موضوعات


عنوان مقاله [English]

The relationship between morphometric parameters of alluvial fans’ upland catchment basin and soil resistance properties

نویسندگان [English]

  • Amjad Maleki
  • Kazem Bahrami
  • Solmaz Moradi
Department of Geography, Faculty of Literature and Humanities, Razi University, Kermanshah, Iran
چکیده [English]

Morphometric properties of alluvial fans’ upland catchment basin e.g. the area, length of the main flow channel, and slope can affect particles’ features like roundedness, surface texture, and shear resistance i.e. grains’ angle of internal friction and cohesion. To carry out the current study, first 21 alluvial fans were selected through examining satellite images and conducting field observations. The selected alluvial fans were similar in terms of lithological features and different with regard to their morphology. Samples were obtained from the top, middle, and bottom of alluvial fans. The results showed that, through geomorphological processes, alluvial fans’ area and length of the main flow channel increases and their slopes declines from the top to the bottom. These features make grains at the bottom more rounded and less rough. The highest degree of roundedness and smoothness were observed in particles in the largest area, the longest main flow channel, and the lowest average slope of catchment basin. Depending on the morphometric parameters of the catchment basin, the angle of internal friction ranged from 44.3 ˚at the top to at the bottom of alluvial fans. Indeed, the highest angle of friction was detected in alluvial fans with the smallest catchment basin area, shortest main flow channel, and highest slope. Thus, the rise in catchment basins’ area and length of the main channel flow and the reduction in their slope will lead to smaller angle of internal friction.

کلیدواژه‌ها [English]

  • Alluvial fans
  • Morphometric
  • Geomorphological
  • Geotechnic
  • Soil
Bahrami, K., Fatemi Aghda, S.M., Noorzad, A. and Talkhablou, M., 2018. Investigation of abrasion and impact resistance of aggregates in different environments in Direh, Kermanshah, Iran. Geotechnical and Geological Engineering, v. 37, p. 2015-2028. https://doi.org/10.1007/s10706-018-0741-2.
Bahrami, K., Fatemi Aghda, S.M., Noorzad, A. and Talkhablou, M., 2019. Effect of morphometric characteristics of catchments on the aggregates resistance of freeze- thaw and sodium sulfate soundness: a case study of alluvial fans of Direh, Kermanshah, Iran, geomorphology, Iranian Journal of science and technology, v. 2, p. 137-155. https://doi.org/10.1007/s40995-019-00686-5.
Bahrami, Sh., 2013. Tectonic controls on the morphometry of alluvial fans around Danehkoshk anticline, Zagros, Iran, Geomorphology, v. 180, p. 217-230. https://doi.org/10.1016/j.geomorph.2012.10.012
Bahrami, Sh., Fatemi Aghda, S.M., Bahrami, K., Motamedi Rad, M. and Poorhashemi, S., 2015. Effects of weathering and lithology on the quality of aggregate in the alluvial fans of northeast Rivand, Sabzevar, Iran, Geomorphology, v. 241, p. 19-30. https://doi.org/10.1016/j.geomorph.2015.03.028
Barton, M.E., 1993. Cohesive Sands: the natural transition from sand to sandstone. In: anagnostopoulose, I.G. et al., (Ed) proceedings of geotechnical engineering of soft rocks-hard soil. Balkem, Rotterdam, p. 367-374.
Blair, T.C. and Mcpherson, J.G., 2009. Processes and frams of alluvial fans. Chapter 14 in: Parsons, A.J., Abrahams, A.D.)Eds(, geomorphology and desert, Environments, p. 413- 467.
Blair, TC., 2003. Features and origin of the giant cucomungo canyon alluvial fan, eureka valley, California. In: Chan MA, Archer AW (eds.) extreme depositional environments: nega end members in geologic time. Geological Society of America special, v. 370, p. 105-126. https://doi.org/10.1130/0-8137-2370-1.105.
Blatt, H., Middleton, G.V. and Murray, R., 1980. Origin of sedimentary rocks. (Second Edition) Prentice- Hall, New Jersey, 785 p.
Bridg, J. and Demicco, R., 2008. Earth surface processes, landform and sediment deposits, Cambridge University press. https://doi.org/10.1017/CBO9780511805516.
Ferrill, D.A., Stakamatos, J.A., Jones, S.M., Rahe, B., Mckague, H.L., Martin, R.H. and Morris, A.P., 1996. Quaternary slip history of the Bare Mountain fault )Nevada( from the morphology and distribution of alluvial fan deposits. Geology, v. 24, p. 559-652. https://doi.org/10.1130/0091-7613(1996)024<0559:QSHOTB>2.3.CO;2
Fookes, P.G., Lee, E.M. and Griffiths, J.S., 2007. Engineering geomorphology, theory and practice. CRC Press. Taylor and Francis Group, 281. https://doi.org/10.1177/03091333080320030502.
Harvey, A., 2002. The role of base-level change in the dissection of alluvial fans: Case studies from Southeast Spain and Nevada. Geomorphology, v. 45, p. 67-87. https://doi.org/10.1016/S0169-555X(01)00190-8.
Lustig, L.K., 1965. Clastic sedimentation in deep springs valley, California.U.S. Geological Survey Professional, 352-F. https://doi.org/10.3133/pp352F.
Mirghasemi, A.A., Rothenburg, L. and Matyas, E.L., 2002. Influence of particle shape on engineering properties of assembles of two-dimensional polygon-shaped particles. Geotechnique, v. 52(3), p. 209-217. https://doi.org/10.1680/geot.2002.52.3.209.
Mitarai, N. and Nori, F., 2006. Wet granular materials. Advances in physics, v. 55, p. 1-2, 1-45. https://doi.org/10.1080/00018730600626065.
Moscariello, A., 2018. Alluvial fans and fluvial fans at the margins of continental sedimentary basins: geomorphic and sedimentological distinction for geo-enrgy exploration and development, Geological Society, London, Special Publication, v. 440, p. 215-243. https://doi.org/10.1144/SP440.11.
Ritter, J., Miller, J. and Walforst, J., 2000. Environmental controls on the evolution of alluvial fans in Buena Vista Valley, North Central Nevada, during late Quaternary time. Geomorphology, v. 36, p. 63-87. https://doi.org/10.1016/S0169-555X(00)00048-9.
Santamarina, J.C. and Cho, G.C. ,2004. Soil behavior: the role of particle shape proc. Skemptonconf., march, London, 14. https://doi.org/10.1061/40659(2003)2.
Seif, A. and Mokarram, M., 2013. Quantitative relationships between characteristics of drainage. Basin and alluvial fan. Journal of Environrnent, v. 2(4), p.90-93.
Snyder, N.P., Whipple, K.X., Tucker, G.E. and Merritts, D.M., 2003. Channel response to tectonic forcing: fiehd analysis of stream morphology and hydrology in the mendocino triple junction region. Northern Clifornia ,Geomorphology, v. 53, p. 97-127. https://doi.org/10.1016/S0169-555X(02)00349-5.
Sukumaran, B. and Ashmawy, A.K., 2001. Quantitative characterization of geometry of discrete particles. Geotechnique , v. 51(7), p. 619-627. https://doi.org/10.1680/geot.2001.51.7.619.
Talling. P.J., 2000. Self-organization of river networks to threshold states. Water Resources Research, v. 36, p. 40119-1128. https://doi.org/10.1029/1999WR900339.
Terzaghi, K., 1967. Soil mechanics in engineering practice, Wiley, London.
Tomczyk ,A.M., 2021. Morphometry and morphology of fan-shaped landforms in the high-Arctic settings of central spitsbergen, svalbard. Faculty of Geographical and Geological, v. 392, p. 27. https://doi.org/10.1016/j.geomorph.2021.107899.
Tucker, G.E. and Hancock, G.R., 2010. Modelling landscape evolution. Earth Surface Processes and Land Forms, v. 35 ,p. 28-50. https://doi.org/10.1002/esp.1952.
Valkanou, K., Karymbalis, E., Papanastassiou, K. and Giles, P.T., 2013. Analysis of relationships among costal alluvial fans their contributing catchments in North Evoikos Gulf (Central Greece). 8th International Conference on Geomorphology.  https://doi.org/10.12681/bgsg.10961.
Zhao, L., Liang, X. and Wu F., 2014. Soil surface roughness change and its effect on runoff and erosion on the Loess Plateau of China. Journal of Arid Land, v. 6(4), p. 400-409. https://doi.org/10.1007/s40333-013-0246-z