Change in channel morphology due to urbanization in Morningside Creek, Ontario

dc.contributor.advisorSnodgrass, W.
dc.contributor.advisorWhiteley, H.R.
dc.contributor.authorBadelt, Brad
dc.date.accessioned2020-08-24T15:44:39Z
dc.date.available2020-08-24T15:44:39Z
dc.date.copyright1999
dc.degree.departmentSchool of Engineeringen_US
dc.degree.grantorUniversity of Guelphen_US
dc.degree.nameMaster of Scienceen_US
dc.description.abstractA geomorphic assessment was conducted on the two branches of the Upper Morningside Tributary, located in Markham, Ontario. The morphology of each branch is influenced by urban development; on the North Branch a large stormwater detention pond has further altered conditions. Based on site observations, the current channel condition in the North Branch is characterized as morphologically inactive, while the West Branch is actively unstable. The lack of channel adjustment in the North Branch is attributed to the subdued discharge regime and the lack of sediment supply associated with the detention pond. The channel is characterized as 'sensitive' to change in the prevailing hydrologic condition, based on the boundary material erodibility and 'sediment starved' nature of the reach. Based on the findings of an erosion simulation study, the North Branch is expected to become morphologically unstable with a ten percent increase in the basin imperviousness, despite the detention storage provided by the pond.en_US
dc.identifier.urihttps://hdl.handle.net/10214/19843
dc.language.isoen
dc.publisherUniversity of Guelphen_US
dc.rights.licenseAll items in the Atrium are protected by copyright with all rights reserved unless otherwise indicated.
dc.subjectUpper Morningside Tributaryen_US
dc.subjectUrban developmenten_US
dc.subjectStormwater detention ponden_US
dc.subjectMorphologically inactiveen_US
dc.subjectActively unstableen_US
dc.titleChange in channel morphology due to urbanization in Morningside Creek, Ontarioen_US
dc.typeThesisen_US

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