Water Catchment Issues (fact Sheets 1-2) Flashcards

1
Q

Hydrology

Definition

A

The science of the distribution and movement of water.

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2
Q

Greatest natural hazard to people is…

A

flooding

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3
Q

Water controls the movement of…

A

nitrates, lake eutrophication
acid rain, river acidification
landfill leachates, pollution of ground water
movement of sediment to rivers, soil erosion

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4
Q

Water resource

A

Total amount of water available in the environment

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5
Q

Water supply

A

Quantity of water abstracted from the environment

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6
Q

Eutrophication

A

Nitrogen or phosphorus enrichment of rivers and lakes that results in algal blooms that deplete oxygen levels and hence affect fish and macro-invertebrate populations

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7
Q

Leachates

A

Mostly dissolved substances moving within subsurface (ie, below ground surface) water flow

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8
Q

Catchment

A

The area of land that delivers all of its directly received precipitation (minus evaporation) to a point on a river

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9
Q

Point on a river that measure catchment

A

gaging station

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10
Q

Watershed

A

Edge/boundary of catchment

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11
Q

Catchment water budget/ water balance

A

States that the water lost by the catchment (as riverflow or evapotranspiration), plus any change in subsurface water storage is equal to the incoming precipitation.

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12
Q

Catchment water budget equation

A

P = E + Q (±∆S)

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13
Q

What does P stand for in the catchment water-budget equation

and units

A
P= precipitation
units = mm hr-1
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14
Q

What does E stand for in the catchment water-budget equation

and units

A
E= Evapotranspiration
units = mm hr-1
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15
Q

What does Q stand for in the catchment water-budget equation

and units

A
Q= river discharge
units= M3 S-1 (cumecs)
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16
Q

What does ∆S stand for in the catchment water-budget equation

A

∆S= change in subsurface water storage

17
Q

Discharge per unit catchment area

A

Q/A (catchment area)
m3 S-1/m2,
=q ms-1

18
Q

When can ∆S be omitted from the equation?

A

over the period of a year (or more) the ∆S averages to 0 so can be omitted from the equation

19
Q

What normally defines river catchments?

A

surface topography,
the assumption that water entering the subsurface hydrological systems eventually emerges within the same river catchment

20
Q

When the catchment can be wrong

3

A
  1. different rock-head topography of surface of impermeable to ground surface
  2. dipping impermeable strata
  3. karstic systems (caves)
21
Q

Where catchments ‘leak’ water …

A

this exchange of subsurface waters is called ‘deep seepage’

22
Q

When leakage of water is below the river outlet gauge…

A

gauge underflow

23
Q

Typical size of experimental catchments

A

1-10km2 in area

24
Q

Precipitation

A

Water reaching a catchment as rainfall, snow, hail, dew or occult (i.e. mist/fog) forms

25
Q

Headwaters

A

Tributary streams close to the source (i.e. head) of a large river

26
Q

Hydrological cycle

A

The concept that evaporation gives water for precipitation, which becomes subsurface water, then river-water, then sea-water and evaporation once more.

27
Q

Evapotranspiration

A

The water lost to the atmosphere by open-water evaporation, water intercepted by the vegetation and directly re-evaporated, plus biological transpiration from plants.

28
Q

Subsurface water

A

All water below the ground surface, including ‘soil water’ (i.e. the subsurface systems close to the ground surface or water in the unsaturated zone) and groundwater (water below a regional water-table)