Test 4 Flashcards
what rock type can typically hold and transmit groundwater most efficiently
sandstone
How much of the worlds water is freshwater?
4%
Hydrologists
geologists that study water on and under the Earth’s surface
Hydrologists
geologists that study water on and under the earths surface
groundwater is contained in
voids
pores in soil
sediment
rocks
Flow Rate depends on:
slope of water table or hydraulic gradient
material through which water is flowing
void space in rock: porosity
connection between voids: permeability
Void space in rock
porosity
connections between voids
permeability
Aquifers
layers that stare and transmit groundwater
like a sponge
Good aquifers
sandstones, conglomerates and rock layers with connected fractures (limestones)
Bad Aquifers
(aquitards)
shale: cant transmit
metamorphic and igneous = bad
aquifer types
based on connection to the surface
confined: water can be pressurized
Artesian Wells: water under pressure
Ground Water flow rate determined by:
porosity
permeability
hydraulic gradient
Stream Gain Water
gaining streams
Stream Loss Water:
losing streams
Spring:
surface discharge or groundwater
dissolution of limestones
forms caves and caverns
Calcite Precipitation in Caves
Cave Formations
H2O in Limestones
pressure rises
CaCO3 dissolves
Stagmite
icicle-like deposit growing from the cave floor
Stalactite
icicle-like deposit suspended from a cave ceiling
Column
forms when a stalactite and a stalagmite grow together
Lost World Caverns:
Lewisburg, WV
Karst Regions:
characterized by sinkholes , caverns and disappearing streams
Morgantown Water Sources:
Surface
Contamination
Surface Water
easily contaminated by surface and underground sources
contaminants quickly move downstream
can be identified and treated quickly
Contamination (Ground Water)
Easily contaminated by underground and surface sources
contaminants will spread out as they move
difficult to identify, harder to clean up
Contamination Clean Up
Expensive and take a few years or even decades
Overpumping:
flow can’t keep up with withdrawl
After Pumping:
loss of volumn and land sinks or subsides
Most oil and gas form from the remains of:
marine algae and bacteria
Oil and Gas can be trapped underground by:
salt domes
faults
folds
Petroleum
comes from mostly marine algae and bacteria
Organic material is buried with
mud
Aquitards
high porosity, low permeability
Petroleum Window:
60-200 degrees celsius
2-6 km