GROUNDWATER SUPPLIES Flashcards

1
Q

is the water found underground in the cracks and spaces in soil, sand and rock

A

Groundwater

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2
Q

usually composed of gravel, sand, and sandstone

A

Aquifer

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3
Q

allow water to pass through as they have large connected spaces that make them permeable.

A

Aquifer

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4
Q

refers to the amount of water that a rock or aquifer can provide.

A

Water Yield

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5
Q

It’s a measure of the quantity of water that can be extracted from the geological formations.

A

Water Yield

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6
Q

Why is groundwater important as a water source?

A

*reliable during droughts and not easily depleted
*generally easier and cheaper to treat than surface water

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7
Q

Prolific sources of underground water

A

*Sedimentary Rocks
*Sandstones
*Limestones
*The Chalk

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8
Q

not an indicator of its ability to give a good water yield

A

Rock Porosity

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9
Q

is also a determining factor for good water yield

A

Permeability

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10
Q

*high porosity
*lack permeability
*limited water yield

A

Clays and Silts

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11
Q

*high porosity
*prolific yielder of water *extensive network of fissures can store large quantities of water and readily release it.

A

Solid Chalk

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12
Q

*yielding large quantities of water in wet weather
*drains rapidly in dry conditions *resulting in a low water yield

A

Limestone

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13
Q

Formations Used for Water Supply; These are so widespread that, despite their varying yields, they form the principal source of water supply.

A

*Shallow Alluvial Strata
*Sands and Gravels of Tertiary or Recent age

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14
Q

use different methods and screening techniques to access thebest quality or quantity of water regardless if they are shallow ordeep.

A

Boreholes

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15
Q

has a borehole sunk from their base to intercept main water-bearing strata, sealed to prevent surface water entry.

A

Large-diameter wells (15-25 m deep)

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16
Q

sometimes have adits or unlined tunnels driven below ground,intercepting more water-bearing fissures.

A

Older wells

17
Q

involves sinking several moderately sized boreholes in a spacedpattern, collecting their yields together.

A

Well field

18
Q

using porous or unjointed pipes, can abstract shallowgroundwater from river beds or banksusing

A

Collector wells and galleries

19
Q

can be driven into a hillside to tap the water table.

A

Collector wells and galleries

20
Q

rate of discharge where the
water is transferred under a
hydraulic gradient over a unit
width of an aquifer

A

Transmissivity (T)

21
Q

the amount of water released
from an aquifer when a unit fall
in the water table occurs.

A

Storage coefficient (S’)

22
Q

intrinsic characteristic of a
substance and refers to the amount
of void or empty space in each
material.

A

Porosity (n)

23
Q

Water movement through rock or
soil depends on porosity, which
relates to the

A

Hydraulic conductivity and
permeability

24
Q

a measure of how easily water can
pass through soil or rock.

A

Hydraulic conductivity and
permeability

25
Q

storage term for unconfined aquifer where the amount of water from the unconfined aquifer releases from the
storage per unit surface area of the aquifer per unit decline in the water table

A

Specific yield (Sy)

26
Q

aims to find how much water a well or borehole will presently yield

A

Test pumping

27
Q

Heavy chisel is suspended on a cable
Cable is shortened and released
alternately
Progress:
Slow
Dependent on
the hardness of
formation
Can be delayed
due to resharpening
of drill chisel

A

Cable-Operated Chisel

28
Q

Operates using compressed air
10 times faster in hard rock compared to a cable-operated chisel
Used for small boreholes (about 300 mm ⌀)
Unsuitable for soft formations & inoperable in deep depths of water

A

‘Down The Hole’ Hammer

29
Q

Used for large boreholes
More expensive than percussion drilling
May be difficult penetrating hard boulders
Has toothed cutters of hard steel that rotate and break up the formation
Used for holes of substantially smaller
diameter

A

Rotary Drilling - Roller Rock Bit