3.Starting at the southwest and northwest corners of Figure 16.6, and at Parris Island, construct flowlines showing the general direction of groundwater movement in 1961. See map above
a. in the southwest corner?
b.in the northwest corner?
c.at Parris Island?
4.Study Figure 16.7 and describe the changes from 1961 to 1984 at Hilton Head Island, Savannah, Georgia, and 25 miles up the Savannah River from the center of the cone of depression. At Hilton Head, the water level is down to –10 ft, from 0 ft.
5.How much has the water-pressure surface been lowered at Savannah between 1880 and 1984?
6.From what area do you expect the fresh water/saltwater interface to first reach the Savannah area? SW or NE (circle one) Why? (Hint: Examine the water-level contours, and the variation in depth of the aquifer described in the introduction.)
7.Figure 16.8 is a cross section extending into Port Royal Sound from the NE end of Hilton Head Island showing simulated changes in the brackish and salt water zones for the years 2000, 2016, and 2032. The model assumes no change in the rates of groundwater withdrawals on Hilton Head Island or inland near Savannah.
a. What value is used as the transition between freshwater and brackish water?
b.In the period between 2000 and 2032, how many meters will the brackish/freshwater interface have moved?
c.What is the average annual rate of projected advance of this interface between 2000 and 2032?
d.About when will the interface reach the edge of the island?
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