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tortuosity

Tortuosity is a geometric measure of how winding a path is compared with the straight-line distance between two points. In most contexts it is defined as the ratio τ = L_eff / L_free, where L_eff is the actual length of a transport path and L_free is the direct distance between its endpoints. The value is dimensionless and satisfies τ ≥ 1, with higher values indicating more convoluted paths.

In porous media, tortuosity describes how pore structure hinders diffusive and advective transport. It factors into

Measurement and estimation of tortuosity employ several approaches. Imaging-based reconstruction from micro-CT or similar techniques can

Applications of tortuosity span disciplines. In geology and hydrogeology, it influences groundwater diffusion and contaminant migration.

models
of
diffusion,
electrical
conductivity,
and
fluid
flow,
where
transport
coefficients
in
a
porous
medium
are
often
expressed
as
the
product
of
a
porosity
factor
and
a
tortuosity
factor
(for
example,
D_eff
≈
D_0
ε
/
τ
in
simple
homogenization
schemes).
Tortuosity
tends
to
increase
with
poorer
connectivity,
greater
pore-scale
curvature,
and
anisotropy,
and
it
often
depends
on
the
scale
and
the
method
used
to
measure
it.
reveal
pore
paths
for
geometric
calculations.
Tracer
diffusion
experiments
and
impedance
or
conductivity
measurements
provide
hydrodynamic
or
transport-based
estimates.
Different
communities
may
emphasize
geometric
versus
transport-based
definitions,
yielding
related
but
not
identical
tortuosity
values.
In
chemical
engineering
and
energy
storage,
it
affects
ion
transport
in
porous
electrodes
and
membranes.
In
physiology
and
medicine,
tissue
tortuosity
describes
the
twisted
architecture
of
vessels
and
capillaries,
impacting
oxygen
delivery,
nutrient
transport,
and
drug
diffusion.