Ground Water 1 Flashcards

1
Q

why use GW

A
  • excellent source of potable water
  • largest available reservoir of fresh water
  • resilient to drought
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2
Q

GW uses

A
  • large use in irrigation
  • supplies baseflow to rivers and streams
  • augment river flow in droughts
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3
Q

GW characteristics

A
  • areally distributed
  • slow response
  • low capital but high operational (pumping costs)
  • lack of data thus loads of interpolation
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4
Q

potential sources of GW contamination

A
  • petrol/sewage leaks
  • nitrates (agriculture)
  • landfill
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5
Q

water as a mineral

A
  • anarchic behaviour
  • lead to a bunch of legisation
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6
Q

aquifer materials

A

principle
- chalk
- sandstone
- limestone

superficial
- glacial deposits
- river deposits
- weathering deposits

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7
Q

aquifer definition

A

geological formation capable of yielding economic quantities of water through wells

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8
Q

ground water resource evalation

A

Exploration
- surface/subsurface geological/geophysical data
- surface hydrological data
- hydrogeological data

Evaluation
- getting parameters
- determine yield

Exploration
- well installation
- observation well construction: well screen, gravel pack, development

aiming towards a sustainable reservoir

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9
Q

well installation techniques

A

Shallow
- hand dug
- driven
- bored

Deep = drilling
- cable tool
- rotary
- reverse rotary

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10
Q

getting aquifer parameter

A
  • pumping test = transmissivity, storativity, specific yield
  • piezometer test = permeability
  • lab tests = permeability, porosity, alpha?
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11
Q

evaluation: yield

A

well = max pumping without lowering the water level to below inlet

aquifer = max withdrawal with acceptable reduction in acquifer hydraulic head

catchment = same as aquifer plus no unacceptable changes to the basins hydrological cycle
- forms basis for safe yield

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12
Q

sustainable yield

A
  • less than annual recharge (rainfall, leakages from lakes n dat, artificial)
  • doesnt lower the water table to allow intrusion of water at undesirable quality

catchment water balance
- sustainable lead to a rate of change of ground storage as zero

in general: pumping leads to reduced discharge and increased recharge

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13
Q

groundwater footprinit

A

indication of how stressed an aquifer is

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14
Q
A
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