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nellevaporazione

Nellevaporation is a term used to describe a mode of vaporization that occurs when a liquid is confined in small pores, channels, or other restricted geometries. In such contexts, confinement and interfacial forces can modify the conditions under which phase change begins, leading to vapor formation at temperatures or pressures different from bulk boiling points. The concept emphasizes how micro- and nanoscale environments alter evaporation behavior compared with bulk fluids.

Key mechanisms include capillary pressure, wettability, surface roughness, and heat transfer rate. In nanoconfined spaces, Laplace

Applications and implications: Understanding nellevaporation is relevant for cooling of microelectronic devices, where confined-phase-change in microchannels

Status: The term nellevaporation is not a standard, widely adopted term in international physics. It appears

See also: evaporation, boiling, capillary action, porous media, phase-change materials.

pressure
ΔP
=
2σ
cosθ
/
r
can
raise
or
lower
the
threshold
for
nucleation,
and
heterogeneous
nucleation
on
solid
walls
often
dominates
over
bulk
(homogeneous)
nucleation.
Evaporation
can
proceed
as
filmwise
or
bubble-mediated,
and
mass
transport
through
porous
media
can
sustain
vapor
pockets
even
when
the
surrounding
liquid
would
not
boil
in
bulk.
Thermal
conditions,
including
temperature
gradients
and
localized
hot
spots,
influence
the
onset
and
dynamics
of
nellevaporation,
as
do
fluid
properties
such
as
surface
tension
and
latent
heat.
can
enhance
heat
removal,
and
for
energy
systems
using
porous
materials
for
heat
exchange
or
desalination
via
vapor-driven
transport.
It
also
informs
the
design
of
MEMS,
porous
insulators,
and
phase-change
materials,
where
unexpected
vapor
formation
can
impact
reliability.
primarily
in
Italian-language
discussions
as
a
descriptive
concept
related
to
evaporation
under
confinement;
in
English-language
literature
the
phenomenon
is
typically
described
in
terms
of
confined
boiling,
capillary
evaporation,
or
phase-change
in
porous
media.