Turbulent mixing in stratified fluids : layer formation and energetics
Turbulent mixing in stratified fluids : layer formation and energetics
Date
1993-09
Authors
Park, Young-Gyu
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DOI
10.1575/1912/5537
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Keywords
Turbulence
Oceanic mixing
Oceanic mixing
Abstract
A turbulent mixing experiment was conducted to observe the dynamics and
the energetics of layer formation along with the region of layer formation in the
Reynolds number (Re) and the overall Richardson number (Rio) space. A salt
stratified fluid was mixed uniformly throughout its depth with a vertical rod that
moved horizontally at a constant speed. The evolution of density was measured
with a conductivity probe.
As the instability theory of Phillips (1972) and Posmentier (1977) shows, an
initially uniform density profile turns into a series of steps when Rio is larger than
a critical value Ric, which forms a stability boundary. For fixed Re, as Rio decreases
to Ric, the steps get weaker; the density difference across the interface and
the difference of density gradient between layers and interfaces become small. Ric
increases as Re increases with a functional relation log Ric ≈ Re/900. The steps
evolve over time, with small steps forming first, and larger steps appearing later
through merging and decay of the interfaces. After some time the interior seems to
reach an equilibrium state and the evolution of the interior steps stops. The length
scale of the equilibrium step, ls, is a linear function of U /Ni, where U is the speed
of the rod and Ni is the buoyancy frequency of the initial profile. The functional
relationship is ls = 2.6U / Ni + l.Ocm. For Rio < Ric, the mixing efficiency, Rf,
monotonically decreases to the end of a run. However, for Rio > Ric, the evolution
of Rf is closely related to the evolution of the density field. Rf changes rapidly
during the initiation of the steps. For Rio » Ric, R1 increases initially, while for
Rio ≥ Ric, Rf ecreases initially. When the interior reaches an equilibrium state,
Rf becomes uniform. Posmentier (1977) theorized that when steps reach an equilibrium
state, a density flux is independent of the density gradient. The present
experiments show a uniform density flux in the layered interior irrespective of the
density structure, and this strongly supports the theory of Posmentier. The density
flux generated in the bottom boundary mixed layer goes through the interior
all the way to the top boundary mixed layer without changing the interior density structure. Thus, turbulence can transport scalar properties further than the characteristic
length scale of active eddies without changing a density structure. When
the fluid becomes two mixed layers, the relation between Rf and Ril was found for
Ril > 1. Here, Ril is the local Richardson number based on the thickness of the
interface. R, does decrease as Ril increases, which is the most crucial assumption
of the instability theory.
Description
Submitted in partial fulfillment of the requirements for the degree of Master of Science at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution September 1993
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Citation
Park, Y. (1993). Turbulent mixing in stratified fluids : layer formation and energetics [Doctoral thesis, Massachusetts Institute of Technology and Woods Hole Oceanographic Institution]. Woods Hole Open Access Server. https://doi.org/10.1575/1912/5537