Economic and Engineering Geology Flashcards
What is porosity?
Amount of pore spaces in a rock shown as a percentage
What is the equation for porosity?
Total volume of pore space ÷ total volume of rock/sediment x100
Or
% Mass change = final madd - dry mass ÷ dry mass x 100
Why is it difficult to achieve porosity above 26%?
Every grain is unequal in size
What is permeability?
Is the ability of a rock/sediment to transmit fluids
What is the equation for permeability?
Permeability = distance fluid travels ÷ time
What are some factors affecting permeability?
-Porosity
-Connectivity of pores
-Sorting
-Diagenesis
-Grain shape
-Packing
-Grain size
-Secondary permeability fractures (faults)
What are aquifers?
Very permeable rocks that can store water underground, such as chalk and sandstone.
What are aquicludes?
Very impermeable rocks that can’t store water such as clay and shale.
What is an aquitard?
A mix between and aquifer and an aquiclude.
What is connate water?
Trapped water in the pores of a rock as the rock formed. Includes water trapped in the original sediment and water released during diagnesis.
What is capillary pressure?
The pressure between two immediate fluids in narrow pore spaces resulting from interactions of forces between the fluids and solid grains.
What’s the different between a saturated and unsaturated material?
Saturated - All pore spaces are occupied by water
Unsaturated - Not all pore spaces occupied by water (is moving through)
What separates the saturated ans unsaturated zone underground?
The water table (the upper surface of the saturated zone)
What is the head relating to the water table
This is the height difference between the top of the water table and the point of escape
What is the equation for the hydraulic gradient?
Head ÷ horizontal distance between the two points
Usually in a ratio
How are cones of depressions made?
When water is abstracted from a well, a hydraulic gradient is created as the rate of eater flowing back into the well from surrounding saturated rocks will be greater at the top of the head. This creates a dome of depression as the rock towards the top is dried faster than below.
Name 4 case studies for aquifers and aquicludes.
London Basin - Artesian basins
Kessingland - Perched aquifer
The Bahamas - Aquifer
Horsey Mere - Aquifer
Sahara desert - Aquifer
The Great Artesian Basin
Explain the London Basin case study (Artesian basin)
London is at the bottom of a basin, with a Chalk aquifer dipping down from the North and then dipping upwards to the South again. This allows for an aversion fountain to be made due to the water coming from a higher place, so more pressure. London is on a clay aquiclude, so will need to drill to access water.
Explain what happens at the Kessingland perched aquifer
Water was perched on a clay lens, which, when dug through, leaked back into the surrounding rocks, so we’ll disappeared.
Explain the conditions of the Bahamas ans what happened with the aquifers there.
Conditions
-Low lying
-Sub-Topical
-Low rainfall
-High evapotranspiration
Aquifer
The water at the top of the lane, above sea level in the rocks, is fresh water from rainfall. Under the rocks, below the sea level, the water in the rocks is sea water. So when a borehole is drilled, they will mix to form brackish water
Explain the conditions at Horsey mere and what happens at the aquifer?
As Horsey mere is located behind dunes that separate it from the North Sea, salt water percolate through the sand and into the peat (incursion).
Fresh water from rain percolate through the sand and mixes with the salt water under the water table, creating brackish water.
It will change in salinity depending on the amount of precipitation.
Explain the conditions in the Sahara Desert and what happens at the aquifer?
-Arid
-Hot
- Formerly wetter
- Fossil groundwater
The exposed sandstone in the mountains where rain water percolate through. This then moves through the aquifer underground and comes back to the surface where sandstone is exposed.
This creates oasis’s
Explain the conditions of the Great Artesian Basin in Eastern Australia and explain what happens there?
European farmers used this for water supply for irrigation and livestock.
In recent years, attempts were made to stop bore holes from freely flowing
Additionally, 1.2km deep creates hot wa5er for geothermal power heated to 98°c in Birdsville, providing 25% of the electricity.
What is a confined aquifer?
Aquifer is covered by an aquiclude