Geomorphologic analysis and physico-dynamic characteristics of Zhatai-Gully debris flows in SW China
Zhatai gully is a typical debris flow channel in Butuo county of Sichuan province, southwestern China. The geomorphologic features are analyzed and the physical-dynamic characteristics are discussed on the basis of field investigation and laboratory tests. Geomorphologic analysis indicates that Zhat...
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description | Zhatai gully is a typical debris flow channel in Butuo county of Sichuan province, southwestern China. The geomorphologic features are analyzed and the physical-dynamic characteristics are discussed on the basis of field investigation and laboratory tests. Geomorphologic analysis indicates that Zhatai-gully drainage in relation to debris flow can be divided into source area, transport area, and deposition area. The source area has a steep slope and has very limited vegetation cover, which favors runoff, allowing loose solid materials to be mobilized easily and rapidly. In the transport area, there are many small landslides, lateral lobes, and loose materials distributed on both banks. These landslides are active and constantly providing abundant source of soils for the debris flows. In the deposition area, three old debris-flow deposits of different ages can be observed. The dynamic calculation shows that within the recurrence intervals of 50 and lOO years, debris flow discharges are 155.77m^3/s and 178.19m^3/s and deposition volumes are 16.39 × 10^4 m^3 and 18.14 × 10^4 m^3, respectively. The depositional fan of an old debris flow in the outlet of the gully can be subdivided into six layers. There are three debris flow deposits on left and two on the right side of the gully. Grain-size tests of sediments from the soil, gulley bed deposits, and the fresh and old debris flow deposits showed that high amounts of clay and fine gravel were derived from the soil in the source area whereas much of the gravel fraction were sourced from the gully bed deposits. Comprehensive analysis indicates that Zhatai gully is viscous debris-flow gully with moderate to high frequency and moderate to large magnitude debris flows. The risk of a debris flow disaster in Zhatai-gully is moderate and poses a potential threat to the planned hydroelectric dam. Appropriate engineering measures are suggested in the construction and protection of the planned hydroelectric station. |
doi_str_mv | 10.1007/s11629-014-3267-y |
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The geomorphologic features are analyzed and the physical-dynamic characteristics are discussed on the basis of field investigation and laboratory tests. Geomorphologic analysis indicates that Zhatai-gully drainage in relation to debris flow can be divided into source area, transport area, and deposition area. The source area has a steep slope and has very limited vegetation cover, which favors runoff, allowing loose solid materials to be mobilized easily and rapidly. In the transport area, there are many small landslides, lateral lobes, and loose materials distributed on both banks. These landslides are active and constantly providing abundant source of soils for the debris flows. In the deposition area, three old debris-flow deposits of different ages can be observed. The dynamic calculation shows that within the recurrence intervals of 50 and lOO years, debris flow discharges are 155.77m^3/s and 178.19m^3/s and deposition volumes are 16.39 × 10^4 m^3 and 18.14 × 10^4 m^3, respectively. The depositional fan of an old debris flow in the outlet of the gully can be subdivided into six layers. There are three debris flow deposits on left and two on the right side of the gully. Grain-size tests of sediments from the soil, gulley bed deposits, and the fresh and old debris flow deposits showed that high amounts of clay and fine gravel were derived from the soil in the source area whereas much of the gravel fraction were sourced from the gully bed deposits. Comprehensive analysis indicates that Zhatai gully is viscous debris-flow gully with moderate to high frequency and moderate to large magnitude debris flows. The risk of a debris flow disaster in Zhatai-gully is moderate and poses a potential threat to the planned hydroelectric dam. Appropriate engineering measures are suggested in the construction and protection of the planned hydroelectric station.</description><identifier>ISSN: 1672-6316</identifier><identifier>EISSN: 1993-0321</identifier><identifier>EISSN: 1008-2786</identifier><identifier>DOI: 10.1007/s11629-014-3267-y</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Debris flow ; Detritus ; Earth and Environmental Science ; Earth Sciences ; Ecology ; Environment ; Flow channels ; Geography ; Geological engineering ; Geomorphology ; Gravel ; Gullies ; Laboratory tests ; Landslides ; Landslides & mudslides ; Slope stability ; Soils ; Vegetation cover ; 下线 ; 服务 ; 迁移</subject><ispartof>Journal of mountain science, 2016, Vol.13 (1), p.137-145</ispartof><rights>Science Press, Institute of Mountain Hazards and Environment, CAS and Springer-Verlag Berlin Heidelberg 2016</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c376t-dfcaf974b978988d9533174c2856b0a1bb6180f760a16e8ce1e382ff3e62544a3</citedby><cites>FETCH-LOGICAL-c376t-dfcaf974b978988d9533174c2856b0a1bb6180f760a16e8ce1e382ff3e62544a3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/87799X/87799X.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11629-014-3267-y$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11629-014-3267-y$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,4023,27922,27923,27924,41487,42556,51318</link.rule.ids></links><search><creatorcontrib>Liu, Xi-lin</creatorcontrib><creatorcontrib>Tang, Chuan</creatorcontrib><creatorcontrib>Ni, Hua-yong</creatorcontrib><creatorcontrib>Zhao, Yuan</creatorcontrib><title>Geomorphologic analysis and physico-dynamic characteristics of Zhatai-Gully debris flows in SW China</title><title>Journal of mountain science</title><addtitle>J. Mt. Sci</addtitle><addtitle>Journal of Mountain Science</addtitle><description>Zhatai gully is a typical debris flow channel in Butuo county of Sichuan province, southwestern China. The geomorphologic features are analyzed and the physical-dynamic characteristics are discussed on the basis of field investigation and laboratory tests. Geomorphologic analysis indicates that Zhatai-gully drainage in relation to debris flow can be divided into source area, transport area, and deposition area. The source area has a steep slope and has very limited vegetation cover, which favors runoff, allowing loose solid materials to be mobilized easily and rapidly. In the transport area, there are many small landslides, lateral lobes, and loose materials distributed on both banks. These landslides are active and constantly providing abundant source of soils for the debris flows. In the deposition area, three old debris-flow deposits of different ages can be observed. The dynamic calculation shows that within the recurrence intervals of 50 and lOO years, debris flow discharges are 155.77m^3/s and 178.19m^3/s and deposition volumes are 16.39 × 10^4 m^3 and 18.14 × 10^4 m^3, respectively. The depositional fan of an old debris flow in the outlet of the gully can be subdivided into six layers. There are three debris flow deposits on left and two on the right side of the gully. Grain-size tests of sediments from the soil, gulley bed deposits, and the fresh and old debris flow deposits showed that high amounts of clay and fine gravel were derived from the soil in the source area whereas much of the gravel fraction were sourced from the gully bed deposits. Comprehensive analysis indicates that Zhatai gully is viscous debris-flow gully with moderate to high frequency and moderate to large magnitude debris flows. The risk of a debris flow disaster in Zhatai-gully is moderate and poses a potential threat to the planned hydroelectric dam. Appropriate engineering measures are suggested in the construction and protection of the planned hydroelectric station.</description><subject>Debris flow</subject><subject>Detritus</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecology</subject><subject>Environment</subject><subject>Flow channels</subject><subject>Geography</subject><subject>Geological engineering</subject><subject>Geomorphology</subject><subject>Gravel</subject><subject>Gullies</subject><subject>Laboratory tests</subject><subject>Landslides</subject><subject>Landslides & mudslides</subject><subject>Slope stability</subject><subject>Soils</subject><subject>Vegetation cover</subject><subject>下线</subject><subject>服务</subject><subject>迁移</subject><issn>1672-6316</issn><issn>1993-0321</issn><issn>1008-2786</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kU9r3DAQxU1oINtNP0BuIr30olT_PLKOZWk3gUAPSQj0ImRZWit4rY3kpfjbV4tDKD30NA_m92aYN1V1RckNJUR-zZQCU5hQgTkDieezakWV4phwRj8UDZJh4BQuqo85vxACUjV0VXVbF_cxHfo4xF2wyIxmmHPIRXTo0BdpI-7m0exL0_YmGTu5FPIUbEbRo1-9mUzA2-MwzKhzbWkhP8TfGYURPTyjTR9Gc1mdezNk9-mtrqunH98fN7f4_uf2bvPtHlsuYcKdt8YrKVolG9U0nao5p1JY1tTQEkPbFmhDvISiwTXWUccb5j13wGohDF9XX5a5hxRfjy5Peh-ydcNgRhePWVMJtZKSCFLQz_-gL_GYyvEnquaqFiCgUHShbIo5J-f1IYW9SbOmRJ9y10vuuuSuT7nruXjY4smFHXcu_TX5P6brt0V9HHevxfe-CcrnBCMg-B9__pGS</recordid><startdate>2016</startdate><enddate>2016</enddate><creator>Liu, Xi-lin</creator><creator>Tang, Chuan</creator><creator>Ni, Hua-yong</creator><creator>Zhao, Yuan</creator><general>Science Press</general><general>Springer Nature B.V</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>SOI</scope></search><sort><creationdate>2016</creationdate><title>Geomorphologic analysis and physico-dynamic characteristics of Zhatai-Gully debris flows in SW China</title><author>Liu, Xi-lin ; Tang, Chuan ; Ni, Hua-yong ; Zhao, Yuan</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c376t-dfcaf974b978988d9533174c2856b0a1bb6180f760a16e8ce1e382ff3e62544a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Debris flow</topic><topic>Detritus</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Ecology</topic><topic>Environment</topic><topic>Flow channels</topic><topic>Geography</topic><topic>Geological engineering</topic><topic>Geomorphology</topic><topic>Gravel</topic><topic>Gullies</topic><topic>Laboratory tests</topic><topic>Landslides</topic><topic>Landslides & mudslides</topic><topic>Slope stability</topic><topic>Soils</topic><topic>Vegetation cover</topic><topic>下线</topic><topic>服务</topic><topic>迁移</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liu, Xi-lin</creatorcontrib><creatorcontrib>Tang, Chuan</creatorcontrib><creatorcontrib>Ni, Hua-yong</creatorcontrib><creatorcontrib>Zhao, Yuan</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Journal of mountain science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liu, Xi-lin</au><au>Tang, Chuan</au><au>Ni, Hua-yong</au><au>Zhao, Yuan</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geomorphologic analysis and physico-dynamic characteristics of Zhatai-Gully debris flows in SW China</atitle><jtitle>Journal of mountain science</jtitle><stitle>J. Mt. Sci</stitle><addtitle>Journal of Mountain Science</addtitle><date>2016</date><risdate>2016</risdate><volume>13</volume><issue>1</issue><spage>137</spage><epage>145</epage><pages>137-145</pages><issn>1672-6316</issn><eissn>1993-0321</eissn><eissn>1008-2786</eissn><abstract>Zhatai gully is a typical debris flow channel in Butuo county of Sichuan province, southwestern China. The geomorphologic features are analyzed and the physical-dynamic characteristics are discussed on the basis of field investigation and laboratory tests. Geomorphologic analysis indicates that Zhatai-gully drainage in relation to debris flow can be divided into source area, transport area, and deposition area. The source area has a steep slope and has very limited vegetation cover, which favors runoff, allowing loose solid materials to be mobilized easily and rapidly. In the transport area, there are many small landslides, lateral lobes, and loose materials distributed on both banks. These landslides are active and constantly providing abundant source of soils for the debris flows. In the deposition area, three old debris-flow deposits of different ages can be observed. The dynamic calculation shows that within the recurrence intervals of 50 and lOO years, debris flow discharges are 155.77m^3/s and 178.19m^3/s and deposition volumes are 16.39 × 10^4 m^3 and 18.14 × 10^4 m^3, respectively. The depositional fan of an old debris flow in the outlet of the gully can be subdivided into six layers. There are three debris flow deposits on left and two on the right side of the gully. Grain-size tests of sediments from the soil, gulley bed deposits, and the fresh and old debris flow deposits showed that high amounts of clay and fine gravel were derived from the soil in the source area whereas much of the gravel fraction were sourced from the gully bed deposits. Comprehensive analysis indicates that Zhatai gully is viscous debris-flow gully with moderate to high frequency and moderate to large magnitude debris flows. The risk of a debris flow disaster in Zhatai-gully is moderate and poses a potential threat to the planned hydroelectric dam. Appropriate engineering measures are suggested in the construction and protection of the planned hydroelectric station.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s11629-014-3267-y</doi><tpages>9</tpages></addata></record> |
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subjects | Debris flow Detritus Earth and Environmental Science Earth Sciences Ecology Environment Flow channels Geography Geological engineering Geomorphology Gravel Gullies Laboratory tests Landslides Landslides & mudslides Slope stability Soils Vegetation cover 下线 服务 迁移 |
title | Geomorphologic analysis and physico-dynamic characteristics of Zhatai-Gully debris flows in SW China |
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