Gully erosion in the Siwalik Hills, Nepal: estimation of sediment production from active ephemeral gullies
A simple field‐based monitoring programme was established in a small catchment (area 4·6 km2) to find the rates of gully erosion in the Siwalik Hills, Nepal. The rates are used to estimate the amount of sediment produced by gully erosion in the catchment. Three large and active gullies were selected...
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description | A simple field‐based monitoring programme was established in a small catchment (area 4·6 km2) to find the rates of gully erosion in the Siwalik Hills, Nepal. The rates are used to estimate the amount of sediment produced by gully erosion in the catchment. Three large and active gullies were selected with areas ranging from 0·44 to 0·78 ha. Aerial photographs taken in 1964, 1978 and 1992 were ortho‐rectified and used to study the dynamics of gully heads. The same gullies were also monitored manually using an orthogonal reference system fixed by erosion pins around the gully heads. Results from the aerial photos indicated that the gullies expanded remarkably over the period from 1964 to 1992, by 34 to 58 per cent. Head‐retreat rates during that period were 0·48, 0·55 and 0·73 m a−1 and average annual sediment evacuation was estimated as 2534 ± 171, 959 ± 60 and 2783 ± 118 m3 a−1 for the three gullies respectively. From the field measurement, estimated volumes were found to vary from 731 ± 57 to 2793 ± 201 m3 a−1 over the monitoring period of two years. It was also found that the gullies produce sediment which accounts for up to 59 per cent of the sediment produced from surface erosion in the headwater catchment. The findings are useful for planning and executing appropriate control measures and constructing a sediment hazard map at the catchment scale. Copyright © 2006 John Wiley & Sons, Ltd. |
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The rates are used to estimate the amount of sediment produced by gully erosion in the catchment. Three large and active gullies were selected with areas ranging from 0·44 to 0·78 ha. Aerial photographs taken in 1964, 1978 and 1992 were ortho‐rectified and used to study the dynamics of gully heads. The same gullies were also monitored manually using an orthogonal reference system fixed by erosion pins around the gully heads. Results from the aerial photos indicated that the gullies expanded remarkably over the period from 1964 to 1992, by 34 to 58 per cent. Head‐retreat rates during that period were 0·48, 0·55 and 0·73 m a−1 and average annual sediment evacuation was estimated as 2534 ± 171, 959 ± 60 and 2783 ± 118 m3 a−1 for the three gullies respectively. From the field measurement, estimated volumes were found to vary from 731 ± 57 to 2793 ± 201 m3 a−1 over the monitoring period of two years. It was also found that the gullies produce sediment which accounts for up to 59 per cent of the sediment produced from surface erosion in the headwater catchment. The findings are useful for planning and executing appropriate control measures and constructing a sediment hazard map at the catchment scale. Copyright © 2006 John Wiley & Sons, Ltd.</description><identifier>ISSN: 0197-9337</identifier><identifier>EISSN: 1096-9837</identifier><identifier>DOI: 10.1002/esp.1320</identifier><identifier>CODEN: ESPLDB</identifier><language>eng</language><publisher>Chichester, UK: John Wiley & Sons, Ltd</publisher><subject>Bgi / Prodig ; Catchments. Hydrological cycle ; Freshwater ; gully erosion ; gully-head retreat ; Hydrometeorology ; Nepal ; Physical geography ; sediment production ; Siwalik Hills</subject><ispartof>Earth surface processes and landforms, 2006-02, Vol.31 (2), p.155-165</ispartof><rights>Copyright © 2006 John Wiley & Sons, Ltd.</rights><rights>Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2006</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a4840-eee0151d9ed998e46f19e57eb5c0e78c57767c601ccf718a0cbc93da90705bef3</citedby><cites>FETCH-LOGICAL-a4840-eee0151d9ed998e46f19e57eb5c0e78c57767c601ccf718a0cbc93da90705bef3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fesp.1320$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fesp.1320$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>309,310,314,776,780,785,786,1411,23909,23910,25118,27901,27902,45550,45551</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=18064939$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Ghimire, Sohan K.</creatorcontrib><creatorcontrib>Higaki, Daisuke</creatorcontrib><creatorcontrib>Bhattarai, Tara P.</creatorcontrib><title>Gully erosion in the Siwalik Hills, Nepal: estimation of sediment production from active ephemeral gullies</title><title>Earth surface processes and landforms</title><addtitle>Earth Surf. Process. Landforms</addtitle><description>A simple field‐based monitoring programme was established in a small catchment (area 4·6 km2) to find the rates of gully erosion in the Siwalik Hills, Nepal. The rates are used to estimate the amount of sediment produced by gully erosion in the catchment. Three large and active gullies were selected with areas ranging from 0·44 to 0·78 ha. Aerial photographs taken in 1964, 1978 and 1992 were ortho‐rectified and used to study the dynamics of gully heads. The same gullies were also monitored manually using an orthogonal reference system fixed by erosion pins around the gully heads. Results from the aerial photos indicated that the gullies expanded remarkably over the period from 1964 to 1992, by 34 to 58 per cent. Head‐retreat rates during that period were 0·48, 0·55 and 0·73 m a−1 and average annual sediment evacuation was estimated as 2534 ± 171, 959 ± 60 and 2783 ± 118 m3 a−1 for the three gullies respectively. From the field measurement, estimated volumes were found to vary from 731 ± 57 to 2793 ± 201 m3 a−1 over the monitoring period of two years. It was also found that the gullies produce sediment which accounts for up to 59 per cent of the sediment produced from surface erosion in the headwater catchment. The findings are useful for planning and executing appropriate control measures and constructing a sediment hazard map at the catchment scale. Copyright © 2006 John Wiley & Sons, Ltd.</description><subject>Bgi / Prodig</subject><subject>Catchments. Hydrological cycle</subject><subject>Freshwater</subject><subject>gully erosion</subject><subject>gully-head retreat</subject><subject>Hydrometeorology</subject><subject>Nepal</subject><subject>Physical geography</subject><subject>sediment production</subject><subject>Siwalik Hills</subject><issn>0197-9337</issn><issn>1096-9837</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqFkE1vEzEQhi1EJUKKxE_wBcShW8brXX9wg6qkFVWLVCBHy_HOUrfeD-xNS_59HRLBqeI0o9Gjd149hLxmcMwAyveYxmPGS3hGZgy0KLTi8jmZAdOy0JzLF-RlSrcAjFVKz8jtYh3ChmIckh966ns63SC99g82-Dt65kNIR_QSRxs-UEyT7-y05YaWJmx8h_1Exzg0a_fn3Mahozbv90hxvMEOow30Z37hMR2Sg9aGhK_2c06-fz79dnJWXFwtzk8-XhS2UhUUiAisZo3GRmuFlWiZxlriqnaAUrlaSiGdAOZcK5my4FZO88ZqkFCvsOVz8naXm4v9WufSpvPJYQi2x2GdTKlLJSsh_gsyCUKVWdqcvNuBLmtKEVszxmwibgwDs7VusnWztZ7RN_tMm5wNbbS98-kfr0BUmuvMFTvuwQfcPJlnTq-_7nP3vE8T_v7L23hnhOSyNsvLhamXtfiy_PTDcP4Ihs2grQ</recordid><startdate>200602</startdate><enddate>200602</enddate><creator>Ghimire, Sohan K.</creator><creator>Higaki, Daisuke</creator><creator>Bhattarai, Tara P.</creator><general>John Wiley & Sons, Ltd</general><general>Wiley</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>200602</creationdate><title>Gully erosion in the Siwalik Hills, Nepal: estimation of sediment production from active ephemeral gullies</title><author>Ghimire, Sohan K. ; Higaki, Daisuke ; Bhattarai, Tara P.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a4840-eee0151d9ed998e46f19e57eb5c0e78c57767c601ccf718a0cbc93da90705bef3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Bgi / Prodig</topic><topic>Catchments. Hydrological cycle</topic><topic>Freshwater</topic><topic>gully erosion</topic><topic>gully-head retreat</topic><topic>Hydrometeorology</topic><topic>Nepal</topic><topic>Physical geography</topic><topic>sediment production</topic><topic>Siwalik Hills</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ghimire, Sohan K.</creatorcontrib><creatorcontrib>Higaki, Daisuke</creatorcontrib><creatorcontrib>Bhattarai, Tara P.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Earth surface processes and landforms</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ghimire, Sohan K.</au><au>Higaki, Daisuke</au><au>Bhattarai, Tara P.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Gully erosion in the Siwalik Hills, Nepal: estimation of sediment production from active ephemeral gullies</atitle><jtitle>Earth surface processes and landforms</jtitle><addtitle>Earth Surf. Process. Landforms</addtitle><date>2006-02</date><risdate>2006</risdate><volume>31</volume><issue>2</issue><spage>155</spage><epage>165</epage><pages>155-165</pages><issn>0197-9337</issn><eissn>1096-9837</eissn><coden>ESPLDB</coden><abstract>A simple field‐based monitoring programme was established in a small catchment (area 4·6 km2) to find the rates of gully erosion in the Siwalik Hills, Nepal. The rates are used to estimate the amount of sediment produced by gully erosion in the catchment. Three large and active gullies were selected with areas ranging from 0·44 to 0·78 ha. Aerial photographs taken in 1964, 1978 and 1992 were ortho‐rectified and used to study the dynamics of gully heads. The same gullies were also monitored manually using an orthogonal reference system fixed by erosion pins around the gully heads. Results from the aerial photos indicated that the gullies expanded remarkably over the period from 1964 to 1992, by 34 to 58 per cent. Head‐retreat rates during that period were 0·48, 0·55 and 0·73 m a−1 and average annual sediment evacuation was estimated as 2534 ± 171, 959 ± 60 and 2783 ± 118 m3 a−1 for the three gullies respectively. From the field measurement, estimated volumes were found to vary from 731 ± 57 to 2793 ± 201 m3 a−1 over the monitoring period of two years. It was also found that the gullies produce sediment which accounts for up to 59 per cent of the sediment produced from surface erosion in the headwater catchment. The findings are useful for planning and executing appropriate control measures and constructing a sediment hazard map at the catchment scale. Copyright © 2006 John Wiley & Sons, Ltd.</abstract><cop>Chichester, UK</cop><pub>John Wiley & Sons, Ltd</pub><doi>10.1002/esp.1320</doi><tpages>11</tpages></addata></record> |
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subjects | Bgi / Prodig Catchments. Hydrological cycle Freshwater gully erosion gully-head retreat Hydrometeorology Nepal Physical geography sediment production Siwalik Hills |
title | Gully erosion in the Siwalik Hills, Nepal: estimation of sediment production from active ephemeral gullies |
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