6 Groundwater management Flashcards

1
Q

Evapotranspiration

Evaporation

A

function of solar radiation, temperature, humidity, wind velocity

(1) potential evaporation
(2) actual (real) evaporation

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2
Q

Evapotranspiration

Transpiration

A

plant water consumption (cooling), only during growing period

•birch tree 60-70 l/d, beech tree (100 years old): 400 l/d, sun flower 1 l/d

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3
Q

Evapotranspiration

Interception

A

at plant surfaces (leaves, branches) followed by evaporation

  • evergreen trees (conifer): 30-40% of precipitation throughout the year,
  • decidious trees: 10-20% during winter, 20-30% (or more) during summer
  • agricultural crops: 10-25 % during growing period
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4
Q

Potential evapotranspiration

A

theoretical value asssuming unlimited water available

ETpotduring winter often = real evapotranspiration,
ETpotduring summer often > real evapotranspiration

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5
Q

Empirical methods to calculate Potential Evapotranspiration

A

HAUDE,

SCHENDEL,

THORNTHWAITE;

PENMAN,

IVANOV

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6
Q

Real evapotranspiration

A

possible evapotranspiration, limited by available water quantity

during winter often ETpot = ETreell

during summer often ETpot > ETreell

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7
Q

Measurement of climate parameters - evaporation

A

HELLMANN cup

PENMAN pan

Pottomer

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8
Q

Groundwater recharge

[mm/a]
or
[l/s*km²]

A

GwR = P –ET -Ao

Important methods:

  • from catchment water balance
  • from soil water balance
  • base flow measurements
  • chloride balance
  • lysimeter
  • “peak shift“ (tracer, e.g. isotopes)
  • age stratification…
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9
Q

Chloride balance

A

GwR= P * (Clrain / Clgroundwater)

Assumption: chlorides is conservative tracer

Correction for surface run-off and dry deposition may be necessary

Does not work (well) if additional chloride sources are present:

  • sea spray
  • dry deposition (salt dust in arid regions)
  • air and ground water contamination
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10
Q

Direct measurement of groundwater recharge: Lysimeter

A

Big sample of soil which act like normal soil. when rain event happens, water will flow into the lysimeter and out to the collecting bucket under the sample

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11
Q

Land use and gw recharge

A

Bare soil gives actually much higher groundwater recharge in terms of quantity compared to heavily vegetated surfaces such as forest because big trees intercept much rainfall water and contribute to high evapotranspiration. But cutting down trees is always a bad idea in terms of erosion, CO2 storage, water quality, etc.

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12
Q

Sustainable use of groundwater

A

Sustainability: extraction of groundwater should be smaller (or at least equal) to average (long-term) groundwater recharge
→avoid “groundwater mining“

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13
Q

Managing groundwater use

A

-water demand (min, max, mean)
How much water do I want/need?

-(ground) water availability
Can system cover water demand on a sustainable basis?

-environmental impact
(e.g. on gw dependent ecosystems)
How does the extraction affect nature?

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14
Q

Water demand

A

Population & per capita demand

Population growth (prognosis)

Network coverage

Industry and commerce

Future effects of water savings?

Future effects of increase of GDP?

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15
Q

Minimum –Maximum demand:

A
  • daily fluctuations
  • work days/weekends
  • holidays and vacation
  • seasons
  • special occasions
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16
Q

Availability of groundwater

A
  • groundwater recharge rate
  • catchment area (equipotential map)
  • boundary condition (e.g. rivers)
  • other users
17
Q

Groundwater towards its environmental impact

A
  • groundwater-dependent ecosystems
  • subsidence
  • land requirements (pipelines)
  • impacts on water quality
18
Q

Bank filtration definition

A

an enrichment of groundwater by infiltration water from rivers

19
Q

Bank filtration Advantages

A
# compared to direct intake from river:
- filtration of microoganisms & particles, biological degradation of contaminants in aquifer

compared to groundwater:

  • high yield (if aquifer permeable)
  • often soft water (low carbonate)
20
Q

Bank filtration Disadvantages

A
  • inundation by high waters: well heads need to be pressure tight
  • pumping rate may be restricted at low river water
  • danger of contamination through accidents
21
Q

Artificial recharge of ground water

A

Pumping the water from the river and from there water goes to infiltration pond then infiltrates into the subsurface and then flows to the well