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Diffstat (limited to 'typst/main.typ')
| -rw-r--r-- | typst/main.typ | 12 |
1 files changed, 5 insertions, 7 deletions
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 $ ) |