Title: 11: Ground Water
111 Ground Water
- Hydrogeology
- The study of
- ground-water/earth-material
- interactions
- Geology controls ground-water recharge, flow,
discharge and availability - Ground water acts as a geologic agent
Weathering, dissolution, volcanism, metamorphism,
slope stability, earthquakes.
2Ground WaterThe Unseen Part of the Water Cycle
Aquifer
Salt Groundwater
3Hydrogeology DefinedWater/Earth Interactions
- Earth materials
- Rock
- Sediment (Soil)
- Fluids (Water)
- Geologic processes
- Form,
- Distribute and
- Change Earth materials
- Water is a primary agent of many (all?) geologic
processes
4Hydrogeology DefinedWater/Earth Interactions
- Interactions go both ways
- Groundwater controls geologic processes
- Geology controls flow and availability of
groundwater
5Hydrogeology DefinedWater/Earth Interactions
- Geology controls groundwater flow
- Permeable pathways are controlled by
distributions of geological materials
6Hydrogeology DefinedWater/Earth Interactions
- Geology controls groundwater flow
- Permeable pathways are controlled by
distributions of geological materials - Where groundwater is available as a resource is
controlled by geology
7Hydrogeology DefinedWater/Earth Interactions
Geology controls groundwater flow
- 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
8Hydrogeology DefinedWater/Earth Interactions
Groundwater controls geologic processes
- Volcanic Processes
- Igneous Rocks Groundwater controls water content
of magmas - Metamorphic Rocks Groundwater injected by magmas
can metamorphose country rocks - Volcanism Geysers are an example of volcanic
activity interacting with groundwater
9Hydrogeology DefinedWater/Earth Interactions
- Groundwater controls geologic processes
- Earthquakes fluids control fracturing and fault
movement, lubrication and pressures - Landslides groundwater controls slope failure
- Landforms Valley development and karst topography
10Ground Water Zones
- Degree of saturation defines different soil water
zones
11Soil and Groundwater Zones
Unsaturated Zone
Water in pendular saturation
Caplillary Fringe Water is pulled above the
water table by capilary suction
Water Table where fluid pressure is equal to
atmospheric pressure
Saturated Zone Where all pores are
completely filled with water. Phreatic Zone
Saturated zone below the water table
12- Ground water and the Water cycle
- Infiltration
- Infiltration capacity
- Overland flow
- Ground water recharge
- GW flow
- GW discharge
13Bedrock Hydrogeology
- Hydraulic Conductivity of bedrock is controlled by
- Size of fracture openings
- Spacing of fractures
- Interconnectedness of fractures
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17Potentiometric Surfaces
18Potentiometric Surfaces
19Ground Water as a Geologic Agent
20Ground Water as a Geologic Agent
21Ground Water as a Geologic Agent
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27Ground Water Contamination
28Contaminant Transport
29Ohio Groundwater Law
- 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.
30Wisconsin 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.
- 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.
31English 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.
- Today Lingering effects of English Rule
- It is very difficult to prove cause and effect to
be defensible in court.