P. A. McMurtry
University of Utah
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Featured researches published by P. A. McMurtry.
Journal of Fluid Mechanics | 1989
P. A. McMurtry; James J. Riley; Ralph W. Metcalfe
The effects of chemical heat release on the large-scale structure in a chemically reacting, turbulent mixing layer are investigated using direct numerical simulations. Three-dimensional, time-dependent simulations are performed for a binary, single-step chemical reaction occurring across a temporally developing turbulent mixing layer. It is found that moderate heat release slows the development of the large-scale structures and shifts their wavelengths to larger scales. The resulting entrainment of reactants is reduced, decreasing the overall chemical product formation rate. The simulation results are interpreted in terms of turbulence energetics, vorticity dynamics, and stability theory. The baroclinic torque and thermal expansion in the mixing layer produce changes in the flame vortex structure that result in more diffuse vortices than in the constant-density case, resulting in lower rotation rates of the large-scale structures. Previously unexplained anomalies observed in the mean velocity profiles of reacting jets and mixing layers are shown to result from vorticity generation by baroclinic torques.
Journal of Fluid Mechanics | 2005
Tie Wei; Paul C. Fife; Joseph Klewicki; P. A. McMurtry
The properties of the mean momentum balance in turbulent boundary layer, pipe and channel flows are explored both experimentally and theoretically. Available highquality data reveal a dynamically relevant four-layer description that is a departure from the mean profile four-layer description traditionally and nearly universally ascribed to turbulent wall flows. Each of the four layers is characterized by a prexad dominance of two of the three terms in the governing equations, and thus the mean dynamics of these four layers are unambiguously defined. The inner normalized physical extent of three of the layers exhibits significant Reynolds-number dependence. The scaling properties of these layer thicknesses are determined. Particular signixad ficance is attached to the viscous/Reynolds-stress-gradient balance layer since its thickness defines a required length scale. Multiscale analysis (necessarily incomplete) substantiates the four-layer structure in developed turbulent channel flow. In partixad cular, the analysis verifies the existence of at least one intermediate layer, with its own characteristic scaling, between the traditional inner and outer layers. Other information is obtained, such as (i) the widths (in order of magnitude) of the four layers, (ii) a flattening of the Reynolds stress profile near its maximum, and (iii) the asymptotic increase rate of the peak value of the Reynolds stress as the Reynolds num ber approaches infinity. Finally, on the basis of the experimental observation that the velocity increments over two of the four layers are unbounded with increasing Reynolds num ber and have the same order of magnitude, there is additional theorexad tical evidence (outside traditional arguments) for the asymptotically logarithmic character of the mean velocity profile in two of the layers; and (in order of magnitude) the mean velocity increments across each of the four layers are determined. All of these results follow from a systematic train of reasoning, using the averaged momentum balance equation together with other minimal assumptions, such as that the mean velocity increases monotonically from the wall.
Journal of Fluid Mechanics | 2005
Paul C. Fife; Tie Wei; Joseph Klewicki; P. A. McMurtry
Steady Couette and pressure-driven turbulent channel flows have large regions in which the gradients of the viscous and Reynolds stresses are approximately in balance (stress gradient balance regions). In the case of Couette flow, this region occupies the entire channel. Moreover, the relevant features of pressure-driven channel flow throughout the channel can be obtained from those of Couette flow by a simple transformation. It is shown that stress gradient balance regions are characterized by an intrinsic hierarchy of ‘scaling layers’ (analogous to the inner and outer domains), filling out the stress gradient balance region except for locations near the wall. The spatial extent of each scaling layer is found asymptotically to be proportional to its distance from the wall. There is a rigorous connection between the scaling hierarchy and the mean velocity profile. This connection is through a certain function
Philosophical Transactions of the Royal Society A | 2007
Joseph Klewicki; Paul C. Fife; Tie Wei; P. A. McMurtry
A(y^+)
Physics of Fluids | 1995
Alan R. Kerstein; M. A. Cremer; P. A. McMurtry
defined in terms of the hierarchy, which remains
Journal of Crystal Growth | 1997
D. Maynes; Joseph Klewicki; P. A. McMurtry; H. F. Robey
O(1)
Physics of Fluids | 1997
James Guilkey; Alan R. Kerstein; P. A. McMurtry; Joseph Klewicki
for all
Experiments in Fluids | 1996
James Guilkey; Kyle R. Gee; P. A. McMurtry; Joseph Klewicki
y^+
Journal of Fluid Mechanics | 1999
Daniel Maynes; Joseph Klewicki; P. A. McMurtry
. The mean velocity satisfies an exact logarithmic growth law in an interval of the hierarchy if and only if
Journal of Fluids Engineering-transactions of The Asme | 1998
Daniel Maynes; Joseph Klewicki; P. A. McMurtry
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