groundwater Flashcards

1
Q

importance of hydrologic cycle

A

without it there would be no clouds, rivers, glaciers, oceans, groundwater, plate tectonics, rock cycle, or life on Earth

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2
Q

in excavations and tunnels, what are some dangers of groundwater and solutions

A
  • inflow during construction

- artificially lower water table

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3
Q

aquifers

A

saturated rock/soil layers forming a reservoir for groundwater. contains pores or open spaces to hold water and these pores are generally all connected.

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4
Q

4 types of aquifer

A
  1. unconfined
  2. confined
  3. semi-confined (leaky)
  4. perched
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5
Q

unconfined aquifer

A

water table is exposed to the atmosphere and continuous so it is free to rise and fall

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6
Q

confined aquifer

A

the groundwater is isolated from the atmosphere by less permeable layers, subject to higher than atmospheric pressure

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7
Q

aquitard

A

less permeable layer than aquifer

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8
Q

aquiclude

A

impermeable layer

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9
Q

semi-confined aquifer

A

recharge or discharge occurs through the confining layers (aquitards)

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10
Q

perched aquifer

A

water table discontinuous, exposed to atmosphere, free to rise and fall

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11
Q

2 aquifer properties

A

storage and flow

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12
Q

porosity

A

percentage of aquifer consisting of pore space. larger pore space = larger porosity = larger water holding capacity

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13
Q

permeability

A

capacity of aquifer to transmit water through its pore spaces. related to the connectivity of pores

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14
Q

2 forms of porosity

A
  1. primary porosity - pores space created during aquifer formation
  2. secondary porosity - pore space formed through fracturing and weathering of aquifer
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15
Q

what type of porosity dominates in sedimentary rocks?

A

primary porosity

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16
Q

hydraulic head (h)

A

height above a datum of a column of water that can be supported by the hydraulic pressure at a given point in an aquifer.
used to determine hydraulic gradient

17
Q

hydraulic gradient (i)

A

rate of change in hydraulic head (h) per unit distance of flow in a given direction. equates to slope of water table ro piezometric surface

18
Q

Darcy’s law (Q)

A

measures flow rate of water draining through porous material. Applies at macroscopic level

19
Q

hydraulic conductivity (k)

A

rate of flow through a unit cross-sectional area of a material under a unit hydraulic gradient (1)

20
Q

anisotropic

A

k varies with direction

21
Q

isotropic

A

k is the same in all directions

22
Q

homogenous

A

k is the same in all positions

23
Q

heterogenous

A

k is different in different positions

24
Q

are aquifers heterogenous or homogenous?

A

heterogenous

25
Q

easy or hard to quantify anistropy and heterogenity in aquifer

A

hard because of the high degrees

26
Q

groundwater is full of particle mater and polluted with sea water and NO3….
TRUE/FALSE

A

true apart from particles filtered out as it flows through the ground

27
Q

some dangerous pollutants in groundwater

A
  • Fe and Mn ions, from rocks , encrusts pipes and favours bacterial growth
  • NO3- too much is toxic to babies and cattle.
  • faeces from sewage leak
28
Q

cone of depression

A

as groundwater is extracted, flow is induced towards well. The velocity and pressure increases towards the well and thus cone forms, centred on the well. Decreases pressure away from the well which can lead to settlement.