From 002c7acc656e101487d1cbc526b8d169604356ad Mon Sep 17 00:00:00 2001
From: "Claudius \"keldu\" Holeksa" <mail@keldu.de>
Date: Tue, 11 Nov 2025 18:11:37 +0100
Subject: progress

---
 typst/main.typ | 2 +-
 1 file changed, 1 insertion(+), 1 deletion(-)

(limited to 'typst/main.typ')

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
-- 
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