Loughborough University
Leicestershire, UK
LE11 3TU
+44 (0)1509 263171
Loughborough University

Loughborough University Institutional Repository

Please use this identifier to cite or link to this item: https://dspace.lboro.ac.uk/2134/21755

Title: Warm discharges in cold fresh water: 2. Numerical simulation of laminar line plumes
Authors: George, Alabodite M.
Kay, Anthony
Keywords: Cold water
Line plume
Buoyancy reversal
Numerical simulation
Issue Date: 2017
Publisher: © Springer
Citation: GEORGE, A. and KAY, A., 2017. Warm discharges in cold fresh water: 2. Numerical simulation of laminar line plumes. Environmental Fluid Mechanics, 17 (2), pp. 231–246.
Abstract: The behaviour of a discharge of warm water upwards into a homogeneous body of cold fresh water was investigated by means of a numerical model. The discharge has a parabolic velocity profile, with Reynolds number Re = 50, Prandtl number Pr = 7 and Froude number varied over the range 0:2 Fr 2:5. Water density is taken to be a quadratic function of temperature, so that an initially positively buoyant discharge will experience buoyancy reversal as it mixes with an ambient below the temperature of maximum density. The resulting plume has some similarities to a fountain resulting from injection of negatively buoyant fluid upward into a less dense ambient. The plume is initially symmetric, but then its head detaches as it approaches its maximum height. The detached head is denser than the fluid in the plume below it, and the interaction between the sinking head and the rising plume causes a sideways deflection; as this cycle is repeated, the plume displays side-to-side flapping motion and vertical bobbing. As Froude number is increased (i.e. buoyancy reduced) the growth of the plume becomes slower, but the plume eventually reaches a greater height. We obtain empirical power-law scalings for maximum height and time taken to reach that height as functions of Froude number; these scalings are simlar to those for fountains with a linear dependence of density on temperature in the very weak regime.
Description: The final publication is available at Springer via http://dx.doi.org/10.1007/s10652-016-9468-x
Version: Accepted for publication
DOI: 10.1007/s10652-016-9468-x
URI: https://dspace.lboro.ac.uk/2134/21755
Publisher Link: http://dx.doi.org/10.1007/s10652-016-9468-x
ISSN: 1567-7419
Appears in Collections:Published Articles (Maths)

Files associated with this item:

File Description SizeFormat
George_Kay2.pdfAccepted version4.12 MBAdobe PDFView/Open


SFX Query

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.