<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-09-19T21:14:19Z</responseDate><request verb="GetRecord" identifier="oai:drum.lib.umd.edu:1903/33643" metadataPrefix="dim">https://api.drum.lib.umd.edu/server/oai/request</request><GetRecord><record><header><identifier>oai:drum.lib.umd.edu:1903/33643</identifier><datestamp>2025-02-11T08:47:58Z</datestamp><setSpec>com_1903_2206</setSpec><setSpec>com_1903_1654</setSpec><setSpec>com_1903_2</setSpec><setSpec>col_1903_2737</setSpec><setSpec>col_1903_3</setSpec></header><metadata><dim:dim xmlns:dim="http://www.dspace.org/xmlns/dspace/dim" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.dspace.org/xmlns/dspace/dim http://www.dspace.org/schema/dim.xsd">
   <dim:field mdschema="dc" element="contributor" qualifier="advisor" lang="en_US">Laurence, Stuart J</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="author" lang="en_US">Schoneich, Antonio Giovanni</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="publisher" lang="en_US">Digital Repository at the University of Maryland</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="publisher" lang="en_US">University of Maryland (College Park, Md.)</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="department" lang="en_US">Aerospace Engineering</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="accessioned">2025-01-25T06:52:44Z</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="available">2025-01-25T06:52:44Z</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="issued" lang="en_US">2024</dim:field>
   <dim:field mdschema="dc" element="identifier">https://doi.org/10.13016/ip2c-pfqv</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="uri">http://hdl.handle.net/1903/33643</dim:field>
   <dim:field mdschema="dc" element="description" qualifier="abstract" lang="en_US">The understanding of high-speed aerodynamics is becoming evermore pertinent with thegrowth of space tourism, continued interest in space exploration, and pursuit of advanced highspeed
aircraft for both military and commercial use. For initial investigations, ground test facilities
are preferred to flight tests as they are far cheaper and carry significantly less risk, although
wind tunnels can only replicate a subset of the conditions experienced in actual flight. One of
these conditions that has not been adequately captured in wind tunnels is the effect of particulates
in the atmosphere.

Typical wind tunnels use a pure, clean gas (air, nitrogen, etc.) for testing, but this does notcapture the aerosolized nature of the atmosphere, where humidity and condensation can produce
a distribution of liquid droplet sizes ranging from the average rain drop of 2mm to sub-micron
diameter particles. Similarly, volcanic eruptions and ever-present wildfires result in solid particles
exhibiting a variety of species and sizes that are transported to every layer of the atmosphere. At
supersonic speeds, encounters with particulates have been shown to lead to detrimental effects,
such as material erosion and boundary layer transition.

Previous attempts to study this problem in wind tunnels have focused mainly on sub-micronsized solid particles, since aerosol settling time is a major limiting factor. On the other hand,
most high-speed experiments involving large liquid droplet impacts have been carried out in
gas guns or ballistic ranges due to the difficulty of trying to accelerate a droplet to high speeds
without causing it to break up. While these facilities can be used to study impacts, the moving
model means that detailed aerodynamic studies are nearly impossible, leading to a large gap in
knowledge.

To perform high-speed wind tunnel testing with liquid aerosols representative of cloud-likeenvironments (5-20 μm), a Mach-4 facility, referred to as the Multi-phase Investigations Supersonic
Tunnel (MIST) has been designed and developed at the University of Maryland (capable
of producing supersonic, particle-laden flows). This range of aerosol sizes makes MIST a unique
facility with significant potential for expanding the state of the art in high-speed multi-phase
flows. The present work discusses the design and characterization of MIST as well as two major
experimental investigations carried out using this new facility. The first investigation examines
the force augmentation on a free-flying sphere exposed to supersonic, particle-laden flows. Freeflight
measurements are performed with five different particle size and concentration combinations.
When comparing the results for particle-free flow in the same facility, the drag coefficient
of the sphere was shown to be 1.75-4.5% greater for all multi-phase cases; this is significantly
higher than simple estimates based on the increased momentum flux in the freestream would
indicate.

In addition to force measurements, an experimental investigation into the effect of particle-ladenflows on boundary-layer transition was conducted. It is important to characterize the disturbance
environment in wind tunnels since they typically do not represent the levels in atmospheric
flight and can lead to earlier onset of boundary-layer transition. In performing such measurements
using a single-point Focused Laser Differential Interferometer, it was discovered that the
presence of particles in the flow could significantly attenuate the acoustic disturbances generated
by the wind tunnel. This finding was further reinforced when investigating the boundary-layer
transition on a 5◦ half-angle, sharp cone using high-speed schlieren visualization. For each case
presented in this work, the boundary-layer disturbance amplitudes were reduced and transition
Reynolds numbers increased in the particle-laden flow cases. This was contrary to expectations,
given that prior numerical studies have indicated that particles can induce early transition. These
findings potentially open a path to substantially reduce freestream disturbance levels in conventional
hypersonic wind tunnels.</dim:field>
   <dim:field mdschema="dc" element="language" qualifier="iso" lang="en_US">en</dim:field>
   <dim:field mdschema="dc" element="title" lang="en_US">AEROSOL EFFECTS IN HIGH SUPERSONIC FLOWS</dim:field>
   <dim:field mdschema="dc" element="type" lang="en_US">Dissertation</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="pqcontrolled" lang="en_US">Aerospace engineering</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="pqcontrolled" lang="en_US">Fluid mechanics</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="pquncontrolled" lang="en_US">Aerodynamics</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="pquncontrolled" lang="en_US">Boundary Layer Transition</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="pquncontrolled" lang="en_US">Multi-phase Flow</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="pquncontrolled" lang="en_US">Supersonic</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="pquncontrolled" lang="en_US">Wind Tunnel</dim:field>
   <dim:field mdschema="others" element="access-status">open.access</dim:field>
</dim:dim>
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