Digital Repository

Flow regime prediction via froude number calculation in a rock-bedded stream

DSpace/Manakin Repository

Show simple item record

dc.contributor.author Meyers, Michael J.
dc.date.accessioned 2010-10-27T14:28:27Z
dc.date.available 2010-10-27T14:28:27Z
dc.date.issued 2010-10-27
dc.identifier.uri http://hdl.handle.net/10464/3073
dc.description.abstract Mathematical predictions of flow conditions along a steep gradient rock bedded stream are examined. Stream gage discharge data and Manning's Equation are used to calculate alternative velocities, and subsequently Froude Numbers, assuming varying values of velocity coefficient, full depth or depth adjusted for vertical flow separation. Comparison of the results with photos show that Froude Numbers calculated from velocities derived from Manning's Equation, assuming a velocity coefficient of 1.30 and full depth, most accurately predict flow conditions, when supercritical flow is defined as Froude Number values above 0.84. Calculated Froude Number values between 0.8 and 1.1 correlate well with observed transitional flow, defined as the first appearance of small diagonal waves. Transitions from subcritical through transitional to clearly supercritical flow are predictable. Froude Number contour maps reveal a sinuous rise and fall of values reminiscent of pool riffle energy distribution. en_US
dc.language.iso eng en_US
dc.publisher Brock University en_US
dc.subject Stream measurements en_US
dc.subject Streamflow en_US
dc.title Flow regime prediction via froude number calculation in a rock-bedded stream en_US
dc.type Electronic Thesis or Dissertation en_US
dc.degree.name M.Sc. Earth Sciences en_US
dc.degree.level Masters en_US
dc.contributor.department Department of Earth Sciences en_US
dc.degree.discipline Faculty of Mathematics and Science en_US


Files in this item

This item appears in the following Collection(s)

Show simple item record

Search The Repository


Browse

My Account

Statistics


About the Digital Repository