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This Week (and next)

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Pollution of Groundwater Need a sense of ground water flow warmup responses to The velocity of groundwater flow is dependent on: porosity and permeability 28% ... – PowerPoint PPT presentation

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Title: This Week (and next)


1
This Week (and next)
  • Today
  • Finish Floods
  • Groundwater
  • Friday Glaciers

2
Finally, a flood of possibly mythic proportions
  • Noahs Flood hypothesis
  • William Ryan Walter Pittman (Columbia U.)
  • Controversial, not universally accepted, but
    intriguing

3
Noahs Flood
  • Coming out of last ice age 7600 years ago (5600
    B.C.), sea level was low but rising
  • Why?
  • Black Sea was freshwater, surrounded by farms

4
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5
Noahs Flood
  • Rising global sea level raised Mediterranean
    above the Bosporus Strait
  • Broke through natural dam
  • Water rose 6 inches / day
  • Flooded lakeshore communities

6
some Noahs Flood evidence
  • Many cultures have a flood story, many can be
    traced to the Black Sea area
  • Remains of houses villages have been found on
    the pre-flood lakeshore
  • But New work finds no evidence for a sudden
    rise in water level of Black Sea.

7
Noahs Flood
  • More info
  • book Noahs Flood The new scientific
    discoveries about the event that changed
    history, Ryan Pittman, 1998, Simon Schuster

8
Todays Plan Groundwater
  • aquifer / aquitard
  • water table
  • groundwater flow
  • groundwater contamination

9
Groundwater aquifers
  • Any geologic unit through which water can move
    easily (i.e. its permeable)( high
    permeability)
  • Porosity how much water a geologic material can
    hold

10
Opposite of an aquifer?
  • Aquitard / aquiclude
  • retards the flow of groundwater (its almost
    never really zero

11
Groundwater aquifers
  • What would be the properties (porosity/permeabilit
    y) of conglomerate?
  • High porosity, high permeability

12
Groundwater aquifers
  • What would be the properties (porosity/permeabilit
    y) of unfractured granite?
  • Low porosity, low permeability

13
Groundwater aquifers
  • Can you think of a rock/sediment with high
    porosity and low permeability?

14
Groundwater aquifers
  • Can you think of a rock/sediment with low
    porosity and high permeability?

15
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16
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17
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18
How is this possible?
19
Ground Water and Surface Water
  • These are almost always connected
  • If a stream contributes water to the aquifer its
    called a losing stream
  • If a stream receives water from the aquifer its
    called a gaining stream
  • Same stream can be both at different places or at
    different times

20
Pumping Animation
  • Go to animation at http//almandine.geol.wwu.edu/
    dave/courses/2003/spring/101/lectures/water_level
    .swf

21
Your WarmUp AnswersPart B Pumping wells
  • That was a really cool animation but I just dont
    understand what is happening.
  • Lets look at the situation again go!

22
Your WarmUp AnswersPart B Pumping wells
  • In the low permeability case the water is pumped
    primarily from the area directly around the well,
    whereas with the higher permeability the water
    seems to be drawn from a more broad area
    surrounding the well "hole". Since permeability
    refers to the ability of a material to let a
    fluid move through it, the low permeability
    doesn't allow the water to venture far from the
    path of pressure change (the "hole" of the well).

23
  • What happens when this well is heavily pumped?

24
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25
Pollution of Groundwater
  • Need a sense of ground water flow
  • warmup responses to The velocity of groundwater
    flow is dependent on
  • porosity and permeability 28
  • permeability and hydraulic gradient 61
  • porosity and hydraulic gradient 7
  • pressure gradient 4

26
Groundwater Flow
  • Groundwater velocity
  • Depends on permeability and hydraulic gradient
    (slope of water table)
  • Ranges from 100 m/day to mm/day
  • A good round number 1 ft/day

27
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28
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29
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30
  • What happens when a new well here is heavily
    pumped?

31
Flow direction can change
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