summaryrefslogtreecommitdiff
diff options
context:
space:
mode:
-rw-r--r--typst/main.typ4
1 files changed, 2 insertions, 2 deletions
diff --git a/typst/main.typ b/typst/main.typ
index 1274795..0c2e9c6 100644
--- a/typst/main.typ
+++ b/typst/main.typ
@@ -30,7 +30,7 @@
Flow in porous subsurface structures often is dominated by extremely low velocity and high viscous fluids with low Reynolds numbers $"Re" << 1$.
In such a condition, the flow enters a state called the Stokes Flow or creeping flow, where inertial forces can be assumed to be zero and viscous
forces dominate the whole connected set.
-This kind of flow is found in geological processes, in carbohydrate recovery, filtration systems and $CO_2$ storage where the pore-scale motion
+This kind of flow is found in geological processes, in carbohydrate recovery, filtration systems and $"CO"_2$ storage where the pore-scale motion
of particles and their interaction with the surrounding porous medium strongly influence macroscopic properties such as the permeability of
rock layers.
Undestanding particle transport, bridging and in general clogging phenomena is critical for the effective use and management of subsurface
@@ -43,7 +43,7 @@ The study of the Stokes Flow has a long history, beginning with Stokes' study of
Subsequent work expanded his work to include a multitude of shapes and the interaction of multiple particles, different geometries and
boundary other conditions.
More recently, research was performed in the understanding of creeping flow, the particle transport and the clogging associated with it, and how those microscopic properties impact the macroscopic development. These carry implications which are essential in water treatment, medicine,
-carbohydrate recovery and $CO_2$ storage. // CITE
+carbohydrate recovery and $"CO"_2$ storage. // CITE
This report delves into the central aspects governing the known behaviour of Stokes Flow and the key extension results towards past single and multiple spheres.
Explores the effect of it in porous media and examines the more recent particle bridging behaviour found in porous structures.