8-20 Groundwater—Multidimensional Flow and Applications Chap. 8
Compute the total head for each equipotential line based on the total head in the reservoir
and the number of equipotential drops from the reservoir to that equipontential line. Then,
use this total head to compute the pressure head and the pore water pressure along the
bottom of the dam.
Equipotential
Line Number h (m) h
(m) u (kPa)
2 134.2 – 2/10.4 (8.1) = 132.6 132.6 – 122.0 = 10.6 (9.8)(10.6) = 104
8.22 A 30 m wide, 40 m long, 8 m deep construction excavation needs to be made in a silty
clay (CL). The groundwater table is at a depth of 2 m. The sides of the excavation will
be sloped at an angle of about 1 horizontal to 1 vertical, and no sensitive structures or
other improvements are nearby. Suggest an appropriate method of construction
dewatering for this site, and explain the reason for your choice. Include statements of
any assumptions, if any.
Solution
The Hydraulic conductivity of CL is very low, so the Q entering the excavation will be
8.23 After the analysis described in Example 8.6 was completed, the well was installed to the
depth indicated in Figure 8.18. However, when the pump was installed, it produced a
flow rate of only 102 gal/min. Is the difference between this value and the computed
flow rate within the normal range of uncertainty for these kinds of analyses? Explain.
What portion of the analysis usually introduces the greatest error?
Solution
The predicted flow rate was 276 gal/min, but the actual flow rate was only 102 gal/min.