6 Groundwater management Flashcards
Evapotranspiration
Evaporation
function of solar radiation, temperature, humidity, wind velocity
(1) potential evaporation
(2) actual (real) evaporation
Evapotranspiration
Transpiration
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
Evapotranspiration
Interception
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
Potential evapotranspiration
theoretical value asssuming unlimited water available
ETpotduring winter often = real evapotranspiration,
ETpotduring summer often > real evapotranspiration
Empirical methods to calculate Potential Evapotranspiration
HAUDE,
SCHENDEL,
THORNTHWAITE;
PENMAN,
IVANOV
Real evapotranspiration
possible evapotranspiration, limited by available water quantity
during winter often ETpot = ETreell
during summer often ETpot > ETreell
Measurement of climate parameters - evaporation
HELLMANN cup
PENMAN pan
Pottomer
Groundwater recharge
[mm/a]
or
[l/s*km²]
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…
Chloride balance
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
Direct measurement of groundwater recharge: Lysimeter
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
Land use and gw recharge
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.
Sustainable use of groundwater
Sustainability: extraction of groundwater should be smaller (or at least equal) to average (long-term) groundwater recharge
→avoid “groundwater mining“
Managing groundwater use
-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?
Water demand
Population & per capita demand
Population growth (prognosis)
Network coverage
Industry and commerce
Future effects of water savings?
Future effects of increase of GDP?
Minimum –Maximum demand:
- daily fluctuations
- work days/weekends
- holidays and vacation
- seasons
- special occasions