jamie m. martin-hayden associate professor
DESCRIPTION
Hydrogeology EEES 4410/5410. Jamie M. Martin-Hayden Associate Professor. (419) 530-2634 [email protected]. Ground Water The Unseen Part of the Water Cycle. Aquifer. Salt Groundwater. Hydrogeology Defined Water/Earth Interactions. Earth materials Rock Sediment (Soil) Water - PowerPoint PPT PresentationTRANSCRIPT
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Jamie M. Martin-HaydenAssociate Professor
Jamie M. Martin-HaydenAssociate Professor
(419) [email protected]
HydrogeologyEEES 4410/5410EEES 4410/5410
HydrogeologyEEES 4410/5410EEES 4410/5410
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Ground WaterThe Unseen Part of the Water Cycle
Salt Groundwater
Aquifer
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Hydrogeology DefinedWater/Earth InteractionsHydrogeology DefinedWater/Earth InteractionsEarth materials
• Rock• Sediment (Soil)• Water
Geologic processes• Form,• Distribute and• Change earth materials• Water is a primary agent of
many (all?) geologic processes
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Hydrogeology DefinedWater/Earth InteractionsHydrogeology DefinedWater/Earth InteractionsInteractions go both ways• Groundwater controls
geologic processes• Geology controls flow
and availability of groundwater
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Hydrogeology DefinedWater/Earth InteractionsHydrogeology DefinedWater/Earth InteractionsGeology controls groundwater flow
Permeable pathways are controlled by distributions of geological materials
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Hydrogeology DefinedWater/Earth InteractionsHydrogeology DefinedWater/Earth InteractionsGeology controls groundwater flow
Permeable pathways are controlled by distributions of geological materials
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Hydrogeology DefinedWater/Earth InteractionsHydrogeology DefinedWater/Earth InteractionsGeology controls groundwater flow
Permeable pathways are controlled by distributions of geological materials
Where groundwater is available as a resource is controlled by geology
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Hydrogeology DefinedWater/Earth InteractionsHydrogeology DefinedWater/Earth Interactions
Permeable pathways are controlled by distributions of geological materials
Where groundwater is available as a resource is controlled by geology
Contaminant transport in the subsurface is controlled by geology
Geology controls groundwater flow
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Hydrogeology DefinedWater/Earth InteractionsHydrogeology DefinedWater/Earth Interactions
Groundwater controls geologic processes
Volcanic Processes: Groundwater controls water
content of magmas Groundwater injected by
magmas can metamorphose country rocks
Geysers are an example of volcanic activity interacting with groundwater
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Hydrogeology DefinedWater/Earth InteractionsHydrogeology DefinedWater/Earth InteractionsGroundwater controls geologic processes
Earthquakes: fluids control fracturing and fault movement, lubrication and pressures
Landslides: groundwater controls slope failure Landforms: Valley development and karst topography
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Trends in population and freshwater withdrawals by source, 1950-2000.
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Trends in total water withdrawals by water-use category, 1950-2000.
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Ohio Groundwater Law
1843: Acton v. Blundell “English Rule”
The landowner can pump groundwater at any rate even if an adjoining property owner were harmed.
1843: Acton v. Blundell “English Rule”
The landowner can pump groundwater at any rate even if an adjoining property owner were harmed.
1861: Frazier v. Brown English Rule in Ohio
Groundwater is
“…occult and concealed…”
and legislation of its use is
“…practically impossible.”
1861: Frazier v. Brown English Rule in Ohio
Groundwater is
“…occult and concealed…”
and legislation of its use is
“…practically impossible.”
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Wisconsin Groundwater Law
1903: Huber v. Merkel
English Rule in Wisconsin
A property owner can pump unlimited amounts of groundwater,
even with malicious harm to a neighbor.
1903: Huber v. Merkel
English Rule in Wisconsin
A property owner can pump unlimited amounts of groundwater,
even with malicious harm to a neighbor.
1974: Wisconsin v. Michels Pipeline Constructors Inc.
English Rule Overturned
Landowners no longer have
“an absolute right to use with impunity all water that can be pumped from the subsoil underneath.”
1974: Wisconsin v. Michels Pipeline Constructors Inc.
English Rule Overturned
Landowners no longer have
“an absolute right to use with impunity all water that can be pumped from the subsoil underneath.”
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English Rule Overturned in Ohio
1984: Cline v. American Aggregates English Rule overturned in Ohio
Justice Holmes: “Scientific
knowledge in the field of hydrology has advanced in the past decade…” so it
“…can establish the cause and
effect relationship of the tapping of underground water to the existing water level.”
1984: Cline v. American Aggregates English Rule overturned in Ohio
Justice Holmes: “Scientific
knowledge in the field of hydrology has advanced in the past decade…” so it
“…can establish the cause and
effect relationship of the tapping of underground water to the existing water level.”
Today: Lingering effects of English Rule
It is very difficult to prove cause and effect to be defensible in court.
Today: Lingering effects of English Rule
It is very difficult to prove cause and effect to be defensible in court.
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Who Uses Ground Water?
Eg. Groundwater use in Ohio
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Most available freshwater is ground water
Oceans97.2%
Atmosphere0.0001%
0.61%(97%)
Streams and Lakes
0.01%(3%)
The Hydrologic Cycle
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The Hydrologic Cycle
Ocean (salt water)
Evaporation &Transpiration
Precipitation
Overland flow
Infiltration
Ground Water (Ground-Water Flow)
Baseflow
Fresh Surface Water(Lakes, Streams, wetlands) Stream flow (runoff)
Atmosphere (global moisture transport)
Precipitation
Evaporation
Component
Transfer
Runoff
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The Hydrologic Cycle
Ocean 1.32 b km3
Evaporation &Transpiration 70,000 km3
Precipitation 100,000 km3
Overland flow
Infiltration
Ground 8.35 m km3
Water
Baseflow
Fresh Surface Water125,000 km3
(runoff)
Atmosphere 13,000 km3/yr
Evaporation350,000 km3/yr
Component
Transfer
Runoff38,000
Precipitation320,000 km3
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