00:01
Forces that promote
the filtrate formation include
three different forces.
00:06
First,
we have the hydrostatic pressure
that's found in the
glomerular capillaries.
00:12
This is essentially the
glomerular blood pressure.
00:17
This is the chief force
that is pushing the water
and solute out of the blood
into the glomerulus.
00:24
The pressure is
actually quite high
at 55 millimeters of mercury.
00:30
This is compared to the lower
26 millimeters of mercury
that you seen in most other
capillary beds in the body.
00:39
The reason why the hydrostatic
pressure is so high
is because the
efferent arteriole
has a high resistance
with a smaller diameter
than the afferent arteriole.
00:52
This causes the plasma to pull
in the glomerular capillaries,
which increases the
hydrostatic pressure.
01:01
While hydrostatic pressure
is higher than normal
and are glomerular
capillaries to other pressures
caused fluid to remain in the
capillaries and not filter out.
01:14
These include the
hydrostatic pressure
and the glomerular capsule.
01:20
The filtrate pressure
and this capsule
is 15 millimeters of mercury.
01:25
And this pressure is going
to push back up against
the glomerular capillaries.
01:32
The third pressure is our
colloid osmotic pressure
or the pull from most proteins
that remain in the blood.
01:42
The colloid osmotic pressure
is 30 millimeters of mercury.
01:48
So if we put all
of them together,
we get our net
filtration pressure.
01:55
So this is going to include
our 55 millimeter mercury
forcing out from our
hydrostatic pressure
of the glomerular capillaries -
the 45 millimeters
of mercury opposing
or pushing in
from our colloid
osmotic pressure
and our hydrostatic pressure
of the glomerular capsule.
02:19
This pressure or the
net filtration pressure
is going to be responsible
for the formation
of our field trip.
02:28
And this is the main
controllable factor
that determines our glomerular
filtration rate or GFR.