Date of Award
Spring 2019
Project Type
Dissertation
Program or Major
Mechanical Engineering
Degree Name
Doctor of Philosophy
First Advisor
Christopher M White
Second Advisor
Gregory P Chini
Third Advisor
Yves Dubief
Abstract
Flow-induced erosion encompasses all processes in which fluid-solid interactions result in the
removal and transport of material from the solid. The removed material may change its physical
state and/or chemical composition and may be redeposited onto the solid body or advected away
by the fluid and deposited elsewhere. Common to all flow induced erosion processes is that they
involve an eroding surface, and eroding agent, and a fluid flow which delivers the eroding agent to
the eroding surface. Consequently, the study of erosion is difficult as it requires detailed knowledge
of the material, mechanical, and/or thermophysical properties of the eroding surface; the transport
mechanisms that deliver the eroding agent to the eroding surface; and the transport mechanisms
that entrain and advect the eroded material into and within the fluid flow. This difficulty is compounded
by the fact that that there is a feedback coupling between the eroding surface and the
fluid dynamics that control the transport mechanisms important to erosion. Specifically, during
erosion, surface morphological changes to the eroding surface will alter the flow field thereby increasing
or decreasing the rate at which the eroding agent is delivered to the eroding surface. This
in turn alters the surface morphology. Thus a complex feedback cycle exists between the fluid
and surface dynamics. The study of this feedback cycle has received little attention in the fluid
mechanics community. This relative neglect is understandable due to its non-equilibrium nature,
yet surprising when one considers how much erosion by the action of a flow is an integral part
of major scientific and engineering fields, for example geophysics, environmental, manufacturing,
and aerospace.
The underlying research objective of this dissertation is to better understand the two-way coupling
between an eroding body and the surface flux of the eroding agent by evaluating the shape dynamics of eroding bluff bodies through the erosion process. The problem is challenging since,
as described above, the surface flux of the eroding agent will vary as the surface morphology of
the eroding body evolves. In order to investigate the complex interdependence between the flow
and surface morphology of an eroding body during flow-induced erosion, physical ablation and
dissolution experiments will be performed and existing numerical datasets will be analyzed to:
(i) re-evaluate existing scaling laws regarding geometric properties (cross-sectional area, wetted
perimeter, and curvature) of bluff bodies undergoing erosion in (a) uniform, unidirectional flow,
(b) in spatially and temporally varying flow, and (c) in convectively driven flow; (ii) identify a
shape parameter of the eroding surface that is well-correlated with local evolutional changes to
the eroding agent surface flux; and (iii) develop a simple feedback erosion model that bypasses
the fluid dynamics and adjusts the local eroding agent surface flux based on the evaluation of the
identified shape parameter. The focus on the erosion of bluff bodies was chosen because, in principle,
it is more amenable to the study of the erosion feedback cycle as the evolution of the shape
dynamics and morphological changes to the surface of the eroding bluff body are a direct result of
the, unknown, instantaneous magnitude of the local eroding agent surface flux. Since the evolution
of the local eroding agent surface flux is a direct consequence of the feedback from the eroding
surface on the flow dynamics, an improved understanding of the erosion feedback cycle is possible
by evaluating only the morphological changes to the surface of the eroding bluff body.
Recommended Citation
Allard, Michael Paul, "Interdependence of Flow and Shape Morphological Dynamics For Flow-Induced Erosion of
Bluff Bodies" (2019). Doctoral Dissertations. 2434.
https://scholars.unh.edu/dissertation/2434