Transport with
Steady-State Water Flow Exercises
- A
chemical solution is being added to a soil at a constant rate (flux
density) of 1.2 cm per day. The concentration of the inflowing solution is
100 micrograms per ml. This solution is allowed to flow into the soil for
1 day. After that, pure water continues to enter the soil at the same
rate. The chemical is not adsorbed on the soil surfaces. The soil has a
volumetric water content of 0.3 m3 m-3.
The chemical is not undergoing degradation. The dispersivity of the
chemical in this soil is 0.5 cm.
a. What
is the pore water velocity for this flow system? (Recall that the pore water
velocity is the flux density divided by the volumetric water content.)
b. Describe
the location and shape of the pulse of chemical 2, 4, 8, and 16 days after flow
begins.
2. Repeat
exercise 1 for a flux density of 2.4 cm per day. Compare these results with
those in that exercise. Compare the positions of the curves, their shapes, and
the areas under them.
3. Describe
the effect of pore water velocity upon the shape of the curves at these times.
Experiment with additional pore water velocities as needed.
4. Consider
again the soil described in exercise 1. This time the chemical solution is
allowed to enter the soil for 100 days.
a. At
what times will the concentration reach one half of its maximum value (or 50
micrograms per ml) for positions 10, 20, 40, and 80 cm from the inlet?
b. Do
the times required depend upon the dispersivity value? Examine this for
positions near the inlet as well as far from it. Summarize your findings.
c. Consider
the time required to reach 50 micrograms per ml concentration at 80 cm. How
much solution has entered into the soil by this time?
d. How
much water is stored in the pores of the soil from the soil surface to the
80-cm depth? Compare this amount with the amount found in part c. Does the same
relationship hold for positions of 10, 20, and 40 cm?
- Use
the retain line features of the software to compare the curves 4 hours
after application with a flux density of 2.4 cm per hour with the curve
for 8 hours after application with a flux density of 1.2 cm per hour. What do
you find? Can you adjust a parameter to make these 2 curves coincide? If
so, how?
- Another
experiment was conducted with a pesticide as the chemical. This product
was adsorbed somewhat on the soil surfaces. In fact it had a retardation
factor of 2. All other parameters were the same as those in exercise 1.
- Describe
the location and shape of the pulse of chemical 2, 4, 8, and 16 days
after flow begins
- Compare
these curves with those for the non-adsorbed material in exercise 1. What
similarities and differences do you observe?
- Since
the flow rate and the concentration of chemical in the inflowing solution
in this case were the same as those used in exercise 1, the amount of
chemical entering the soil was the same as in exercise 1. Why then is the
concentration much less in this case? Hint: What concentration is being
shown on these graphs?
- Simulate
flow for several additional chemicals with larger retardation factors.
Draw a graph of the position of the center of the pulse 10 days after flow
begins for different retardation factors. How does the retardation factor
influence the position of the pulse?
- Consider
a soil with an initial concentration of 100 micrograms per ml. Pure water
enters the soil with a pore water velocity of 2.0 cm/day. At what time will the concentration of chemical
at 30 cm equal one half its initial value? At what time will the
concentration at 40 cm be one half its initial value? Does the answer to
this question depend upon the dispersivity? At what time will the value at
200 cm be one-half its original value?