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Fig' 6'01

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Aquifer. Saturated permeable geologic unit that can transmit ' ... Water level in wells rise above the top of the aquifer forming a potentiometric surface. ... – PowerPoint PPT presentation

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Title: Fig' 6'01


1
Fig. 6.01
2
Fig. 11-28, p.283
3
Porous Media
  • Ground water moves through a porous media.

4
Porous Media A region of space occupied in part
by heterogeneous (mixed and different) solid
material, more or less evenly distributed through
the region, and void space, and which has a high
specific surface area on the solids exposed to
the voids. The void spaces must be
interconnected so that each point in a void space
is connected to each other point by more than one
path. A medium is something that transmits
something through it.
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Fig. 10.01
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Darcys Law for flow in porous media
9
Darcys Law for flow in porous media
  • At lab scale (Darcys experiment)

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Ground water discharge, Q
  • Analogous to Stream Discharge Q as a
  • Flux (velocity) x Area

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Flux
  • Length per time (m/s)
  • NOT velocity
  • Delivers a quantity per time.
  • In this case, 1-D volume per time

14
Fig. 10.01
15
The Ground Water Environment
16
Fig. 10.04
17
Aquifer
  • Saturated permeable geologic unit that can
    transmit significant quantities of water
  • Note definition is very subjective

18
Phreatic (water table) Aquifer
19
Fig. 10.02
20
Recharge
  • Entry into the saturated zone of water made
    available at the water table.

21
Fig. 10.07
22
Discharge
  • Removal of water from the saturated zone across
    the water-table surface.

23
Source to Sink
  • Recharge to Discharge Ground water flow is from
    regions of recharge to regions of discharge.

24
Fig. 10.03
25
Fig. 11-28, p.283
26
Confined aquifer
  • An aquifer confined between two aquitards,
    receiving recharge from a recharge zone rather
    than regionally.
  • Aquitard (aka aquiclude) are impermeable
  • Water level in wells rise above the top of the
    aquifer forming a potentiometric surface.

27
Fig. 10.05
28
Fig. 10.06
29
Cone of Depression
  • An inverted-cone shaped surface in the water
    table OR potentiometric surface induced by
    pumping.

30
Fig. 10.08
31
Fig. 10.09
32
Pumping and Subsidence
33
Fig. 10.11
34
Saltwater Encroachment
35
Fig. 10.12
36
Fig. 10.13
37
Fig. 10.18
38
Water Availability in the Hydrologic Cycle
39
Fig. 6.01
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Fig. 10.19
41
Table 10.01
42
Ground Water Mining
43
Fig. 10.10
Ground Water Mining Orange Areas where
withdrawal exceeds recharge
44
Fig. 10.20
45
Fig. 10.31
46
Water Use
47
Fig. 10.21
48
Fig. 10.22
49
Fig. 10.23
50
Fig. 10.27
51
Fig. 10.26
52
Fig. 16.02
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