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unsaturatedzone

Unsaturated zone, also called the vadose zone, is the part of the subsurface between the land surface and the water table where pore spaces contain both air and water. Its properties depend on soil texture, structure, and organic matter, and moisture content varies with depth, rainfall, and vegetation.

Water in this zone is held by capillary and gravitational forces and moves slowly through unsaturated flow.

Functions: stores plant-available water, drives groundwater recharge, and acts as a natural filter and biogeochemical reactor

Measurement and relevance: engineers and hydrologists assess soil moisture with tensiometers, time-domain reflectometry, or neutron probes;

Infiltration
of
rainfall
or
irrigation
adds
water;
evapotranspiration
from
vegetation
removes
water
from
the
upper
portions;
near
the
water
table,
capillary
rise
can
lift
water
into
the
zone
above
the
saturated
layer,
creating
a
capillary
fringe.
The
vertical
and
horizontal
transport
is
described
by
Richards
equation;
the
pseudo-saturated
hydraulic
conductivity
is
a
function
of
water
content.
for
dissolved
and
particulate
contaminants.
The
unsaturated
zone
delays
and
alters
pollutant
migration
compared
with
the
saturated
zone,
depending
on
sorption,
degradation,
and
dispersion.
flow
is
sensitive
to
soil
moisture
retention
curves
and
hydraulic
conductivity.
The
depth
and
characteristics
of
the
unsaturated
zone
influence
groundwater
sustainability,
agricultural
productivity,
and
environmental
risk
assessment.