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Geography AS
hydrology and fluvial geomorphology
drainage basin system
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Hannah Mundi
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Cards (22)
Precipitation
water
falling
from the
atmosphere
, in any
3 states
channel precipitation
Precipitation
that
falls
directly into the
river
channel
Interception
Water
being
prevented
from
reaching
the
surface
by
trees
or
grass
Stemflow
the flow of
intercepted
water down the
trunk
or
stem
of a plant
Through
fall
Water
dripping from one
leaf
to
another
Infiltration
movement
of water
downwards
from the
surface
into the
soil
infiltration
capacity
the
maximum
rate at which
soil
can
absorb
water
Percolation
movement
of
water
down through the
pores
in the
soil
into the
groundwater
zone
Throughflow
water
flowing through the
pores
in the
soil
,
parallel
to the
surface
, to the
river
channel
Porosity
proportion
of
pore
space to
solid
material
Permeability
ease with which
water
will
pass
through a
substance
Hortonian
overland flow
water
runs
over the
surface
because the
intensity
of the
precipitation
is
higher
than the
infiltration
capacity
of the surface
Saturated
overland flow
water
runs over the
surface
because the
ground
below has become
saturated
and no further
infiltration
can occur
water
table
upper
layer of
permanently
saturated
pore
spaces in the
ground
water zone
saturated zone
area of
subsurface
where all
pore
space is filled with
water
Base
flow
the
slowest
form of water
movement
through
rock
, and accounts for the
constant
flow of water in
rivers
during periods of
low
rainfall
Recharge
new water from precipitation that refills the baseflow levels after abstraction
Hydrostatic
pressure
force
exerted by water in the
groundwater
zone
Aquifer
a
sufficiently
permeable
water-bearing
rock that is
above
a
layer
of
rock
that
prevents
the
water
from seeping away
Aquitard
an area of
low
permeability
Aquiclude
an area of
zero
permeability
Spring
water seeps
directly out of the
ground
where an
aquifer
reaches the
surface