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dc.contributor.advisorFfolliott, Peter F.en_US
dc.contributor.authorDong, Chunying, 1962-
dc.creatorDong, Chunying, 1962-en_US
dc.date.accessioned2013-04-03T13:28:23Z
dc.date.available2013-04-03T13:28:23Z
dc.date.issued1996en_US
dc.identifier.urihttp://hdl.handle.net/10150/278539
dc.description.abstractThe sediment rating curve (SRC) method was used to study the effects of vegetative manipulations on sediment concentrations on the Beaver Creek watersheds of north-central Arizona. A linear model was best in the analysis of streamflow-sediment relationships. The corrected linear model eliminated some bias of the linear model and improved prediction. Partitioning data by streamflow-generating events and hydrograph stages produced significantly different SRCs and increased the descriptive and predictive powers. Due to insufficient data at the high streamflow range, SRCs for the pinyon-juniper watersheds had low values of ra SRCs for the ponderosa pine watersheds produced better results. More overstory removal resulted in higher sediment concentrations.
dc.language.isoen_USen_US
dc.publisherThe University of Arizona.en_US
dc.rightsCopyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author.en_US
dc.subjectBiology, Ecology.en_US
dc.subjectHydrology.en_US
dc.titleEffects of vegetative manipulations on sediment concentrations in north-central Arizonaen_US
dc.typetexten_US
dc.typeThesis-Reproduction (electronic)en_US
thesis.degree.grantorUniversity of Arizonaen_US
thesis.degree.levelmastersen_US
dc.identifier.proquest1378999en_US
thesis.degree.disciplineGraduate Collegeen_US
thesis.degree.disciplineRenewable Natural Resourcesen_US
thesis.degree.nameM.S.en_US
dc.identifier.bibrecord.b33956959en_US
dc.identifier.bibrecord.b34599617en_US
refterms.dateFOA2018-07-14T01:30:35Z
html.description.abstractThe sediment rating curve (SRC) method was used to study the effects of vegetative manipulations on sediment concentrations on the Beaver Creek watersheds of north-central Arizona. A linear model was best in the analysis of streamflow-sediment relationships. The corrected linear model eliminated some bias of the linear model and improved prediction. Partitioning data by streamflow-generating events and hydrograph stages produced significantly different SRCs and increased the descriptive and predictive powers. Due to insufficient data at the high streamflow range, SRCs for the pinyon-juniper watersheds had low values of ra SRCs for the ponderosa pine watersheds produced better results. More overstory removal resulted in higher sediment concentrations.


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