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Stream energy distribution below Eleyele Dam in Southwestern Nigeria
Expressing the rate of energy dissipation either within a basin or in a downstream manner is important in understanding occurrence and association between various morphological variables. This study focuses on the downstream variation in stream power and its relationship with morphological variates...
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Published in: | Singapore journal of tropical geography 2017-09, Vol.38 (3), p.402-413 |
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container_title | Singapore journal of tropical geography |
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creator | Olusola, Adeyemi Oludapo Fashae, Olutoyin |
description | Expressing the rate of energy dissipation either within a basin or in a downstream manner is important in understanding occurrence and association between various morphological variables. This study focuses on the downstream variation in stream power and its relationship with morphological variates along the main channel of River Ona, Ibadan, Nigeria. River Ona stretches for 20.5 km downstream of Eleyele Dam. Twenty‐seven (27) points were sampled along this stretch. The 27 points were averaged into nine (9) reaches. At each cross‐section, channel characteristics were observed and measured. These include: width (W), depth (D), velocity (V), slope (S), Cross‐sectional area (A), discharge (Q), total stream power (TSP), specific stream power (SSP), width‐depth ratio (W/D), hydraulic radius (R) and wetted perimeter (P). This study confirmed that the influence of a dam present upstream of a river channel significantly alters the behaviour of slope and this in essence affects the distribution of energy along the river channel. Slope produces a logarithmic relationship with increasing distance downstream (Y = ‐32.79‐0.70InS, r = 0.70, r2 = 0.49, p |
doi_str_mv | 10.1111/sjtg.12204 |
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This study focuses on the downstream variation in stream power and its relationship with morphological variates along the main channel of River Ona, Ibadan, Nigeria. River Ona stretches for 20.5 km downstream of Eleyele Dam. Twenty‐seven (27) points were sampled along this stretch. The 27 points were averaged into nine (9) reaches. At each cross‐section, channel characteristics were observed and measured. These include: width (W), depth (D), velocity (V), slope (S), Cross‐sectional area (A), discharge (Q), total stream power (TSP), specific stream power (SSP), width‐depth ratio (W/D), hydraulic radius (R) and wetted perimeter (P). This study confirmed that the influence of a dam present upstream of a river channel significantly alters the behaviour of slope and this in essence affects the distribution of energy along the river channel. Slope produces a logarithmic relationship with increasing distance downstream (Y = ‐32.79‐0.70InS, r = 0.70, r2 = 0.49, p < 0.05) while there was no significant relationship between Q and distance downstream.</description><identifier>ISSN: 0129-7619</identifier><identifier>EISSN: 1467-9493</identifier><identifier>DOI: 10.1111/sjtg.12204</identifier><language>eng</language><publisher>Singapore: Wiley Subscription Services, Inc</publisher><subject>Creeks & streams ; Dams ; Downstream ; Energy dissipation ; Hydraulic radius ; Morphology ; Power ; Rivers ; Width</subject><ispartof>Singapore journal of tropical geography, 2017-09, Vol.38 (3), p.402-413</ispartof><rights>2017 Department of Geography, National University of Singapore and John Wiley & Sons Australia, Ltd</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3014-f858a5bb0cc2c3cdc359be6c51f121c0db164df0f72dd87d138c6997bd5fdce93</citedby><cites>FETCH-LOGICAL-c3014-f858a5bb0cc2c3cdc359be6c51f121c0db164df0f72dd87d138c6997bd5fdce93</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925,33223</link.rule.ids></links><search><creatorcontrib>Olusola, Adeyemi Oludapo</creatorcontrib><creatorcontrib>Fashae, Olutoyin</creatorcontrib><title>Stream energy distribution below Eleyele Dam in Southwestern Nigeria</title><title>Singapore journal of tropical geography</title><description>Expressing the rate of energy dissipation either within a basin or in a downstream manner is important in understanding occurrence and association between various morphological variables. This study focuses on the downstream variation in stream power and its relationship with morphological variates along the main channel of River Ona, Ibadan, Nigeria. River Ona stretches for 20.5 km downstream of Eleyele Dam. Twenty‐seven (27) points were sampled along this stretch. The 27 points were averaged into nine (9) reaches. At each cross‐section, channel characteristics were observed and measured. These include: width (W), depth (D), velocity (V), slope (S), Cross‐sectional area (A), discharge (Q), total stream power (TSP), specific stream power (SSP), width‐depth ratio (W/D), hydraulic radius (R) and wetted perimeter (P). This study confirmed that the influence of a dam present upstream of a river channel significantly alters the behaviour of slope and this in essence affects the distribution of energy along the river channel. Slope produces a logarithmic relationship with increasing distance downstream (Y = ‐32.79‐0.70InS, r = 0.70, r2 = 0.49, p < 0.05) while there was no significant relationship between Q and distance downstream.</description><subject>Creeks & streams</subject><subject>Dams</subject><subject>Downstream</subject><subject>Energy dissipation</subject><subject>Hydraulic radius</subject><subject>Morphology</subject><subject>Power</subject><subject>Rivers</subject><subject>Width</subject><issn>0129-7619</issn><issn>1467-9493</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>8BJ</sourceid><recordid>eNp9kMtOwkAUhidGEwmy8QmauDMpzplL21kaQNQQXYDrSedSHFJanGlDeHsG69p_czbfuX0I3QOeQsxT2HXbKRCC2RUaAcvyVDBBr9EIAxFpnoG4RZMQnMIECx7DRmi-7rwt94ltrN-eEuNC553qO9c2ibJ1e0wWtT3Z2ibzSLkmWbd99320obO-ST7c1npX3qGbqqyDnfzVMfp6WWxmr-nqc_k2e16lmmJgaVXwouRKYa2JptpoyoWymeZQAQGNjYKMmQpXOTGmyA3QQmdC5Mrwymgr6Bg9DHMPvv3p4w1y1_a-iSslCEY4MEpJpB4HSvs2BG8refBuX_qTBCwvouRFlPwVFWEY4KOLf_5DyvX7Zjn0nAFVgGuX</recordid><startdate>201709</startdate><enddate>201709</enddate><creator>Olusola, Adeyemi Oludapo</creator><creator>Fashae, Olutoyin</creator><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8BJ</scope><scope>FQK</scope><scope>JBE</scope></search><sort><creationdate>201709</creationdate><title>Stream energy distribution below Eleyele Dam in Southwestern Nigeria</title><author>Olusola, Adeyemi Oludapo ; Fashae, Olutoyin</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3014-f858a5bb0cc2c3cdc359be6c51f121c0db164df0f72dd87d138c6997bd5fdce93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Creeks & streams</topic><topic>Dams</topic><topic>Downstream</topic><topic>Energy dissipation</topic><topic>Hydraulic radius</topic><topic>Morphology</topic><topic>Power</topic><topic>Rivers</topic><topic>Width</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Olusola, Adeyemi Oludapo</creatorcontrib><creatorcontrib>Fashae, Olutoyin</creatorcontrib><collection>CrossRef</collection><collection>International Bibliography of the Social Sciences (IBSS)</collection><collection>International Bibliography of the Social Sciences</collection><collection>International Bibliography of the Social Sciences</collection><jtitle>Singapore journal of tropical geography</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Olusola, Adeyemi Oludapo</au><au>Fashae, Olutoyin</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Stream energy distribution below Eleyele Dam in Southwestern Nigeria</atitle><jtitle>Singapore journal of tropical geography</jtitle><date>2017-09</date><risdate>2017</risdate><volume>38</volume><issue>3</issue><spage>402</spage><epage>413</epage><pages>402-413</pages><issn>0129-7619</issn><eissn>1467-9493</eissn><abstract>Expressing the rate of energy dissipation either within a basin or in a downstream manner is important in understanding occurrence and association between various morphological variables. This study focuses on the downstream variation in stream power and its relationship with morphological variates along the main channel of River Ona, Ibadan, Nigeria. River Ona stretches for 20.5 km downstream of Eleyele Dam. Twenty‐seven (27) points were sampled along this stretch. The 27 points were averaged into nine (9) reaches. At each cross‐section, channel characteristics were observed and measured. These include: width (W), depth (D), velocity (V), slope (S), Cross‐sectional area (A), discharge (Q), total stream power (TSP), specific stream power (SSP), width‐depth ratio (W/D), hydraulic radius (R) and wetted perimeter (P). This study confirmed that the influence of a dam present upstream of a river channel significantly alters the behaviour of slope and this in essence affects the distribution of energy along the river channel. Slope produces a logarithmic relationship with increasing distance downstream (Y = ‐32.79‐0.70InS, r = 0.70, r2 = 0.49, p < 0.05) while there was no significant relationship between Q and distance downstream.</abstract><cop>Singapore</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1111/sjtg.12204</doi><tpages>12</tpages></addata></record> |
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language | eng |
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source | International Bibliography of the Social Sciences (IBSS); Wiley |
subjects | Creeks & streams Dams Downstream Energy dissipation Hydraulic radius Morphology Power Rivers Width |
title | Stream energy distribution below Eleyele Dam in Southwestern Nigeria |
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