Debris flows of 28 June 2014 near the Arshan village (Siberia, Republic of Buryatia, Russia)

详细信息    查看全文

• 作者：Alena V. Kadetova ; Artem A. Rybchenko ; Elena A. Kozireva ; Vadim A. Pellinen
• 关键词：Central Asia ; Debris flow ; Tunka Ridge ; Mountain areas
• 刊名：Landslides
• 出版年：2016
• 出版时间：February 2016
• 年：2016
• 卷：13
• 期：1
• 页码：129-140
• 全文大小：5,283 KB
• 参考文献：Allen SK, Rastner P, Arora M, Huggel C, Stoffel M (2015) Lake outburst and debris flow disaster at Kedarnath, June 2013: hydrometeorological triggering and topographic predisposition. Landslides, 1–13. doi:10.​1007/​s10346-015-0584-3
  Bregoli F, Medina V, Chevalier G, Hürlimann M, Bateman A (2015) Debris-flow susceptibility assessment at regional scale: validation on an alpine environment. Landslides 12(3):437–454. doi:10.​1007/​s10346-014-0493-x CrossRef
  Engineering geology of the Baikal region (1968) Publishing house “Nauka”, Moscow (in Russian)
  Hürlimann M, Copons R, Altimir J (2006) Detailed debris flow hazard assessment in Andorra: a multidisciplinary approach. Geomorphology 78(3):359–372CrossRef
  Jakob M, McDougall S, Weatherly H, Ripley N (2013) Debris–flow simulations on Cheekye River, British Columbia. Landslides 10(6):685–699. doi:10.​1007/​s10346-012-0365-1 CrossRef
  Jarvis A, Reuter HI, Nelson A, Guevara E (2008) Hole-filled seamless SRTM data V4, International Centre For Tropical Agriculture (CIAT), available from http://​srtm.​csi.​cgiar.​org [27 October 2011]
  Klimeš J, Vilímek V (2011) A catastrophic landslides near Rampac Grande in the Cordillera Negra, northern Peru. Landslides 8(3):309–320. doi:10.​1007/​s10346-010-0249-1 CrossRef
  Laperdin VK, Trzhtsinskii YB (1976) The role of weathering in formation of the solid mudflow phase (a case study of East Sayan). In: geological factors of landslides and mudslide formation, and the problem of their evaluation. Moscow State University, Moscow, pp 49–55, in Russian
  Laperdin VK, Levi KG, Lekhatiniv AM, Kadetova AV, Pellinen VA, Rybchenko АА (2014) Causes and consequences of a catastrophic mudflows on 28 June 2014 near Arshan village in the Republic of Buryatia, Russia. Geodyn Tectonophysics 5(3):799–816CrossRef
  Leshchikov FN (1978) Frozen rocks of Priangaria and Pribaikalia. Nauka, Novosibirsk (in Russian)
  Leshchikov FN, Shats MM (1983) Permafrost in the southern part of Middle Siberia. Nauka, Novosibirsk, p 169 (in Russian)
  Makarov SA (2012) Debris flows in the Cis-Baikalia. The V.B. Sochava Institute of Geography SB RAS, Irkutsk (in Russian)
  Martha TR, Priyom R, Babu Govindharaj K, Vinod Kumar K, Diwakar PG, Dadhwal VK (2015) Landslides triggered by the June 2013 extreme rainfall event in parts of Uttarakhand State, India. Landslides 12:135–146. doi:10.​1007/​s10346-014-0540-7 CrossRef
  Mateos RM, García-Moreno I, Azañón JM (2012) Freeze-thaw cycles and rainfall as triggering factors of mass movements in a warm Mediterranean region: the case of the Tramuntana Range (Majorca, Spain). Landslides 9(3):417–432. doi:10.​1007/​s10346-011-0290-8 CrossRef
  Melton MA (1965) The geomorphic and paleoclimatic significance of alluvial deposits in southern Arizona. J Geol 73:1–38CrossRef
  Meteorological monthly magazine (1972) 22(13) Irkutsk Hydrometeorological Senter, Irkutsk (in Russian)
  Ni H, Zheng W, Song Z, Xu W (2014) Catastrophic debris flows triggered by a 4 July 2013 rainfall in Shimian, SW China: formation mechanism, disaster characteristics and the lessons learned. Landslides 11(5):909–921CrossRef
  Perov VF (2012) Mudflow research. Study guide. MSU Faculty of Geography, Moscow (in Russian)
  Pinneker EV, Pisarsky BI, Lomonosov IS, Koldysheva RY, Didenko AA, Sherman SI (1968) Hydrogeology of Baikal region. Nauka, Moscow, in Russian
  Poznanin VL (1991) Laws of hydrothermal interaction of water flows frozen soil. In: Denudation in cryolithzone. Nauka, Moscow, pp 62–73, in Russian
  Rickenmann D (1999) Empirical relationships for debris flows. Nat Hazards 19:47–77CrossRef
  Sepúlveda SA, Moreiras, SM Lara M, Alfaro A (2014) Debris flows in the Andean ranges of central Chile and Argentina triggered by 2013 summer storms: characteristics and consequences
  Shetnikov AA (2001) Geomorphology of Tunkin rift. Geomorphology 2:93–103 (in Russian)
  Solonenko VP (1960) Engineering geology of East Siberia. Irkutsk (in Russian)
  Sumburgh AL (1971) Geological map of the Soviet Union. 1: 200 000. East Sayan. Sheet M–48–I. Explanatory note. Moscow (in Russian)
  Ufimtsev GF, Shchetnikov AA (2003) The Tunka rift. Priroda 8:43–49 (in Russian)
  Wilford DJ, Sakals ME, Innes JL, Sidle RC, Bergerud WA (2004) Recognition of debris-flow, debris-flood and flood hazard through watershed morphometrics. Landslides 1:61–66. doi:10.​1007/​s10346-003-0002-0 CrossRef
  Xiao H, Luo Z, Niu Q, Chang J (2013) The 2010 Zhouqu mudflow disaster: possible causes, human contributions, and lessons learned. Nat Hazards 67(2):611–625CrossRef
  Youssef AM, Al-kathery M, Pradhan B, El-sahly T (2014) Debris flow impact assessment along the Al–Raith Road, Kingdom of Saudi Arabia, using remote sensing data and field investigations. Geomatics, Natural Hazards and Risk, (Published online), 1–19. doi:10.​1080/​19475705.​2014.​933130
  Yueping Y, Ping S, Jiliang Z, Shengyuan Y (2011) Research on catastrophic rock avalanche at Guanling, Guizhou, China. Landslides 8:517–525. doi:10.​1007/​s10346-011-0266-8 CrossRef
  
• 作者单位：Alena V. Kadetova (1)
  Artem A. Rybchenko (1)
  Elena A. Kozireva (1)
  Vadim A. Pellinen (1)
  
  1. Institute of the Earth’s Crust, Siberian Branch of Russian Academy of Sciences, 128 Lermontov Street, Irkutsk, 664033, Russia
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：Earth sciences
  Applied Geosciences
  Geography
  Agriculture
  Civil Engineering
  
• 出版者：Springer Berlin Heidelberg
• ISSN：1612-5118

文摘

On 28 June 2014, high intensity rainfall resulted in seven simultaneous debris flows going down the slopes of the Tunka Ridge in the vicinity of Arshan village, which is a balneological and alpine resort (51° 54′ 31″ N, 102° 25′ 44″ E). The debris flows caused one life loss and several injuries, 112 buildings were damaged, and 15 were completely destroyed. The total volume of the transported deposits amounted to 3 × 106 m3. Debris flows’ formation began with the failure of weak sediments in the hanging cirques. Similar phenomena had not been recorded in the study area for over 40 years. The article presents a complete picture of the event and analysis of geological, geomorphological, and meteorological conditions for debris flows formation, for which extreme local rainfall was the major cause. Keywords Central Asia Debris flow Tunka Ridge Mountain areas