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authorClaudius "keldu" Holeksa <mail@keldu.de>2025-11-11 18:04:27 +0100
committerClaudius "keldu" Holeksa <mail@keldu.de>2025-11-11 18:04:27 +0100
commit8e2255d8d2801284da45fde4bcad4421e7ac7116 (patch)
tree770a41b5638729ea97acf3b19a2143715b842aec /typst
parent07bbaaddfa0b725572e4c3a166edc6a915a4a374 (diff)
downloadphd-fluid_mechanics_report-8e2255d8d2801284da45fde4bcad4421e7ac7116.tar.gz
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@@ -25,7 +25,7 @@ often referred to as Stokes flow or creeping flow.
It occurs when the viscous forces are significantly larger compared to inertial forces.
For the understanding of porous media, where particle transport, bridging and clogging phenomena are critical to the use of subsurface
reservoirs. Be it either for carbohydrate resource recovery or storage of CO2. Understanding the behaviour of particles in Stokes flow
-is key to analyzing more complex phenomena emerging over time such as permeability reduction over periods of time.
+is key to analyzing more complex phenomena emerging over time such as permeability reduction over periods of time.\
The study of the Stokes Flow has a long history, beginning with Stokes' solution flow along a sphere@stokes1851.\
Subsequent work expanded to explore a multitude of shapes and the interaction of multiple particles.