Water supply Flashcards

1
Q

What is porosity

A

The volume of pore space

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2
Q

What is permeability

A

Rate at which a fluid flows through a rock

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3
Q

How do you calculate porosity percentage

A

Total volume of pore space/total volume of rock or sediment *100

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4
Q

How do you calculate premeability

A

Distance water has traveled/time taken

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5
Q

What are the factors affecting porosity

A

Rock type
The degree of sorting (well sorted rock has high porosity)
The amount of diagenesis (a loose unconsolidated rock has a much higher porosity than a rock that has undergone compaction
Grain shape (rocks containing rounded grains has a higher porosity than angular)
The packing o the grains
GRAIN SIZE IS NOT A FACTOR IN POROSITY

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6
Q

What are the factors affecting permeability

A
Grain size (course grained rocks have a higher permeability than fine grained rocks because there is less resistance to flow around coarse grains)
High porosity
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7
Q

What is the water table

A

The level at which water sits within the ground

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8
Q

What is the height of the overlying column of water known as

A

The hydro static head

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9
Q

How do you calculate the hydraulic gradient

A

difference in hydro static pressure or head/distance between two points

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10
Q

What is an aquifer

A

A body of porous and permeable rock capable of storing and yielding significant amounts of water

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11
Q

What is a recharge zone

A

Area of an aquifer open to the atmosphere, allowing replenishment of water

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12
Q

What is an aquiclude

A

An impermeable rock that does not transmit water

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13
Q

What are the two main types of aquifers

A

Unconfined aquifer-open to the atmosphere, under atmospheric pressure and is recharged by rainwater from directly above. Water will need to be pumped to the surface from a well or borehole sunk into an unconfined aquifer
Confined aquifer is overlain by impermeable rocks and the groundwater held within it is under hydro static pressure. Groundwater can only be replenished in a confined aquifer if it has recharge zones that are open to the atmosphere

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14
Q

What is a live or fossil aquifer

A

Live-one that is currently being replenished by rainwater via a recharge zone on the surface
Fossil-One that is no longer being replenished and represents a relic of a past wetter climate

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15
Q

What is an artesian basin

A

A large, synclinal confined aquifer under hydrostatic pressure

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16
Q

What is an artesian well

A

Hold water under hydrostatic pressure, which rises up the well on release

17
Q

How is ground water abstracted

A

By sinking a borehole and pumping the water to the surface, as water is pumped up the level of the water table falls, leading to a cone of depression

18
Q

What is the cone of depression

A

Occurs where there is a lowering of the water table in the vicinity of a well

19
Q

What is the draw down

A

Describes the height difference between water table and water level in the well

20
Q

What are the main problems caused by groundwater extraction

A

Lowering of the water table
Subsidence at the surface resulting from the removal of water from the pore spaces of rocks
Salt water encroachment in coastal areas

21
Q

What are the threats to ground water supply

A

Over-pumping

Pollution- groundwater is vulnerable to contamination, once polluted it is difficult to clean

22
Q

What are the sources of groundwater pollution

A

Nitrates, pesticides and microbes from run-off
hydrocarbon and solvents from petrol stations and factories
Toxic fluids from landfill waste disposal sites
Acid mine drainage water containing toxic metals such as lead and cadmium from coal and metal mines

23
Q

What are springs

A

Occur when the water table meets intersects the land surface and groundwater flows out onto the surface

24
Q

What are the types of springs

A

Lithological springs-result in change of rock type, occur where porous and permeable rock overlies impermeable rock, the water table will intersect the land surface at the junction between the two rock types, there will be a spring line along the base of the permeable rock
Springs at faults-If faults have moved porous and permeable rock into contact with an impermeable rock a spring line will occur where the fault plane intersects the land surface
Springs at unconformities-If porous and permeable rock lies uncomfortably on top of impermeable older rock the water table will intersect the land surface at the junction between the two rock types, a spring line will occur where the line of the unconformity intersects the land surface

25
Q

Advantages and Disadvantages of surface water supply

A

Advantages
Easy to abstract
Hydroelectric power generation
Reservoirs can be used for recreation and other purposes

Disadvantages
Water will need treatment
Water levels vary between seasons
Requires construction of environmental damaging dams
Reservoirs eventually silt up
26
Q

Advantages and Disadvantages of ground water

A

Advantages
Rocks at as a natural filter
No evaporation
Pumping cost is usually low

Disadvantages
Requires sedimentary rocks and presence of aquifers 
Surface subsidence
Pollutants have a long residency time
Water might be brackish