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authorClaudius "keldu" Holeksa <mail@keldu.de>2025-11-11 18:11:37 +0100
committerClaudius "keldu" Holeksa <mail@keldu.de>2025-11-11 18:11:37 +0100
commit002c7acc656e101487d1cbc526b8d169604356ad (patch)
treee814b200d4e47c47f9c227b391e61a55da74e012 /typst
parentbb5e20410ff6ec1d1aa4cc600b002e8b227f2dff (diff)
downloadphd-fluid_mechanics_report-002c7acc656e101487d1cbc526b8d169604356ad.tar.gz
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Diffstat (limited to 'typst')
-rw-r--r--typst/main.typ2
1 files changed, 1 insertions, 1 deletions
diff --git a/typst/main.typ b/typst/main.typ
index 51d36f6..d1951a5 100644
--- a/typst/main.typ
+++ b/typst/main.typ
@@ -49,7 +49,7 @@ $ ρ((∂)/(∂t)u + (u · ∇)u) = −∇p + μ∇²u + f\
∇ · u = 0 $
)
-While we are often interested in Navier-Stokes flows, on higher viscous fluid such as in the earth's mantle the inertial term is negligable.
+While we are often interested in Navier-Stokes flows, on fluid which tends $Re \to 0$ fluid the inertial term is negligable.
// Stokes