https://repository.tudelft.nl/islandora/object/uuid:57936f2c-ea8f-414e-8d0f-5ad59b183ea6

Author

Blomme, Arthur
<https://repository.tudelft.nl/islandora/search/author%3A%22Blomme%2C%20Arthur%22>
(TU
Delft Aerospace Engineering)
Contributor

Hulshoff, S.J. (mentor)
<https://repository.tudelft.nl/islandora/search/contributor%3A%22Hulshoff%2C%20S.J.%20%28mentor%29%22>

Janssens, Martin (mentor)
<https://repository.tudelft.nl/islandora/search/contributor%3A%22Janssens%2C%20Martin%20%28mentor%29%22>
de Vries, Iris (mentor)
<https://repository.tudelft.nl/islandora/search/contributor%3A%22de%20Vries%2C%20Iris%20%28mentor%29%22>
Degree granting institution

Delft University of Technology
Programme

Aerospace Engineering
<https://repository.tudelft.nl/islandora/search/mods_note_programme_s%3A%22Aerospace%255C%2BEngineering%22>
Date

*2023-04*

*Master's Thesis*

Abstract

Stratospheric Aerosol Injection (SAI) is a geoengineering method to
mitigate the effects of increased greenhouse gas concentrations in the
Earth’s atmosphere, and to prevent further global warming. SAI does not
reverse climate change, it merely counteracts its symptoms by offsetting
the radiative forcing of greenhouse gases, and it should be accompanied by
aggressive programmes of Carbon Dioxide Removal to cool down the climate.
Operational studies suggest that the injection of condensable vapor from
specialized high-altitude aircraft would be a reasonable option to form the
desired aerosol particles. Yet, remarkably little is known about the growth
evolution of aerosol inside a jet engine wake, especially in light of SAI
where high initial concentrations of condensable vapor are injected into
the exhaust stream. The lack of resolution in the flow field obscures a lot
of the intricacies of the aerosol formation process, and raises serious
doubts on the steerability of SAI, which is the capacity to spatially and
temporally control its effects both in nature and scale. Without
reassurance that the steerability requirement can be satisfied, the
potential risks to the global ecosystem would be too high. In this respect,
the study investigates the mechanisms within the near-field of a jet engine
wake that lead to the creation of aerosols and subsequent growth, when
accounting for local variations in temperature and relative humidity. This
is done through a decoupled plume dispersion model that includes a flow
solver which resolves the average velocity and turbulent intensity of the
flow, a sectional chemistry module which includes all the relevant
microphysical processes that affect aerosol growth, and a
diffusion-advection model which calculates the displacement of aerosol,
vapor, and chemiions in the flow field. In addition, several modeling
errors are identified in classical thermodynamic approaches to high-density
aerosol formation. Results demonstrate that the onset of particle formation
in the plume is complex, and is heavily dependent on the injection
concentration of sulfuric acid vapor and the mixing rate of the plume.
Different aerosol particle sizes are formed depending on the location in
the plume, leading to a nonuniform distribution of the volume-mean radius
across the plume’s cross-sectional area. There is also a
strong indication that core particles experience preferential growth, which
implies that the final particle distribution at the end of the plume’s
lifetime might not be as uni-modal as self-limited theory predicts. The
study concludes with a list of recommendations to solve the challenges that
remain in order to truly
understand the early growth evolution of sulfate aerosol in a jet engine
wake.
Subject

SAI <https://repository.tudelft.nl/islandora/search/subject%3A%22SAI%22>
PDM <https://repository.tudelft.nl/islandora/search/subject%3A%22PDM%22>
Microphysics
<https://repository.tudelft.nl/islandora/search/subject%3A%22Microphysics%22>
Steerability
<https://repository.tudelft.nl/islandora/search/subject%3A%22Steerability%22>
To reference this document use:

http://resolver.tudelft.nl/uuid:57936f2c-ea8f-414e-8d0f-5ad59b183ea6

*Source: TU Delft*

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