4. Look at the regional groundwater flow system shown below. This system is isotropic, homogeneous, and unconfined. Dashed lines are equipotentials. For each of the items listed, use the figure below for working out the results, then draw neatly on the diagram on the answer sheet. 40 30 20 10 -10 -20 Stream Cartoon is vertically exaggerated and not drawn to scale!!! Ground surface Lake Water table F E 40 30 20 10 1 -20 Elevation (m-msl) A. Label all of the head contours (dashed lines) to nearest 5 m. B. Fill out the table listing elevation head, pressure head, and total head for points A-J. Although the figure is not drawn exactly to scale, you should be able to estimate or calculate head values with accuracy of 5 m. Hint: do not try to estimate y from depth below the water table! C. Label one aquifer recharge location (R) and one discharge area (D) on the figure. These are places where there is net transport from the surface and to the surface, at the aquifer top. D. Add three flow lines indicating the paths of water particles starting at points X, Y, and Z. E. You should find that total head is greater at point D than it is at point H. Does this mean that water flows from point D to point H? Explain why or why not in a single sentence (under the table on the answer sheet).
Reservoir and Streamflow Routing
In hydrology, a reservoir is usually a natural pond that is enlarged or made using a dam to keep the water clean. Reservoirs or dams can be constructed in several ways, including controlling the existing watercourse, disrupting the watercourse to form embayment within it, by digging or building any number of retaining walls.
Water Resource Systems Analysis
Water resources are natural water sources that may be as useful as water sources. 97% of the world's water is saltwater and only 3% is pure water; just over two-thirds of this ice sheet is located in glaciers. The remaining pure frozen water is found primarily as groundwater, with only a small fraction present above the ground or in the air. Natural sources of freshwater include surface water, under river flow, groundwater, and ice water. Artificial water sources can include treated wastewater (recycled water) and saline seawater.
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