water extraction case study Flashcards

(9 cards)

1
Q

where is this case study?

A

RIVER KENNET, in SOUTHERN ENGLAND
drains 1200km2 area in WILTSHIRE + BERKSHIRE

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2
Q

why is water extracted?

A

several urban areas close to the catchment rely on the Kennet basin to meet PUBLIC SUPPLY- also provides for local industries and agriculture
e.g. SWINDON (population of 200,000)

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3
Q

who extracts it and how?

A

THAMES WATER abstracts GROUNDWATER from upper catchment from BOREHOLES- non of this water is returned to this river as waste water

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4
Q

impacts on REGIONAL WATER CYCLE

A
  • rates groundwater extraction EXCEED RATES OF RECHARGE + FALLING WATER TABLE has decreased flows of River Kennet by 10-14%
  • 2003 drought (flows decreased 20%)
  • changes in where water is stored- less flows means less flooding, so less water stored on wetlands on flood plain
  • decreased WATER TABLE results in SPRINGS and STREAMS DRYING UP- threatens ECOSYSTEMS
  • can extract FOSSIL WATER which has been underground for hundreds of years and is DIFFICULT TO REPLACE (NON-RENEWABLE RESOURCE)

OVER-ABSRACTION LEADS TO DECREASED WATER FLOW IN THE KENNET BY 10-14%, DECREASING WETLAND WATER STORAGE/ FLOODPLAIN INUNDUATION

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5
Q

what is water extraction?

A

water extracted from surface + groundwater to meet PUBLIC, INDUSTRIAL, AGRICULTURAL DEMAND
- direct HUMAN INTERVENTION in the WATER CYCLE- changes the DYNAMIC OF RIVER FLOW and GROUNDWATER STORAGE

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6
Q

where is 2nd case study?

A

LONDON

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7
Q

London context

A
  • located in centre of an SYNCLINAL STRUCTURE which forms an ARTESIAN BASIN; groundwater in the chalk trapped between London Clay
  • rainwater enters where it outcrops at edge of basin- groundwater than flows by gravity through chalk to centre of basin
  • so, under natural conditions, the WELLS and BOREHOLES in London are under ARTESIAN PRESSURE
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8
Q

impacts of water extraction in London?

A
  • groundwater from the chalk is an important source of water for the capital
  • but OVER-EXPLOITATION in 19th Century + beginning 20th Century caused DRASTIC DECREASE in level of groundwater (decreased 90M IN CENTRAL LONDON)
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9
Q

how have the impacts changed in London?

A

past 50 years: DECREASED DEMAND for water by industry in London + decreased rates of abstraction allowed water table to recover
in early 90s: INCREASED GROUNDWATER STORAGE, threatening buildings and underground tunnels as INCREASING 3M PER YEAR of water table
- now risen and stable

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