From d54fdc99d978f93d164b51609f02d52601793893 Mon Sep 17 00:00:00 2001
From: "Claudius \"keldu\" Holeksa" <mail@keldu.de>
Date: Tue, 11 Nov 2025 17:23:21 +0100
Subject: progress

---
 typst/main.typ | 12 +++++-------
 1 file changed, 5 insertions(+), 7 deletions(-)

(limited to 'typst')

diff --git a/typst/main.typ b/typst/main.typ
index 81dd6ae..10c7663 100644
--- a/typst/main.typ
+++ b/typst/main.typ
@@ -13,7 +13,7 @@
       email: "clho@norceresearch.no"
     ),
   ),
-  index-terms: ("Scientific writing", "Typesetting", "Document creation", "Syntax"),
+  index-terms: ("Fluid Mechanics", "Review"),
   bibliography: bibliography("refs.bib"),
   figure-supplement: [Fig.],
 )
@@ -36,7 +36,8 @@ This report delves into the central aspects governing the known behaviour past s
 Explores the effect of it in porous media and examines the more recent particle bridging behaviour found in porous structures.
 
 
-== Navier
+
+== Stokes Flow
 
 // Write about Navier
 The incompressible Navier Stokes equations are a set of equations
@@ -47,16 +48,13 @@ $ ρ((∂)/(∂t)u + (u · ∇)u) = −∇p + μ∇²u + f\
 ∇ · u = 0 $
 )
 
-// Introduction
-== Stokes flow
-
 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.
-Since we 
+Since we can assume the inertial term
 
 // Stokes
 #math.equation(
 block: true,
-$ ρ((∂)/(∂t)u + (u · ∇)u) = −∇p + μ∇²u + f\
+$ 0 = −∇p + μ∇²u + f\
 ∇ · u = 0 $
 )
 
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