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Residence time
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Created by
Judith
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Cards (11)
flow velocity/effective flow velocity (ve)
larger
than flux density
flow velocity
equation: ve = (k*ne)*[delta(H)/delta(x)]
ve (m/d) =
flow velocity
k (m/d) =
conductivity
ne =
porosity
[delta(H)/delta(x)] =
hydraulic head gradient
equation to determine how far a water droplet has
travelled
in certain
time period
or how long it takes to
travel a certain distance
ve = [delta(x)/delta(t)]
x = distance
t = time
residence time
(Tr): time water remains in certain volume
Tr = (D*ne)/R
D (m) =
thickness of aquifer
ne =
porosity
R (mm/year) =
precipitation surplus
longer residence time in soil results in
better water quality
buffer strips
are beneficial for spreading animals and plants, landscape and recreation
residence time in extraction wells
water flows
faster
closer to well
radial
flow pattern
use area of
25
year residence time to
protect
groundwater to make sure its water quality meets standards
measured with the use of radius of
25
year residence time
volume for
extraction well
= π*r2*ne*D
r =
radius
ne =
porosity
D =
thickness of aquifer
calculating
radius
= sqrt[(Q*Tr)/(π*D*ne)
calculating
residence time
= [(π*D*ne)/Q]*r2