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Aquifers of the Scheldt basin Testing the guidance document WATECO & IMPRESS groups Gabrielle Bouleau (ENGREF) & Arnaud Courtecuisse (AEAP)

Aquifers of the Scheldt basin

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Aquifers of the Scheldt basin. Testing the guidance document WATECO & IMPRESS groups Gabrielle Bouleau (ENGREF) & Arnaud Courtecuisse (AEAP). WFD objectives for aquifers. The WFD indicates in Article 4 : - PowerPoint PPT Presentation

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Page 1: Aquifers of the Scheldt basin

Aquifers of the Scheldt basin

Testing the guidance documentWATECO & IMPRESS groups

Gabrielle Bouleau (ENGREF)

& Arnaud Courtecuisse (AEAP)

Page 2: Aquifers of the Scheldt basin

WFD objectives for aquifers

• The WFD indicates in Article 4 :(ii) Member States shall protect, enhance and

restore all bodies of groundwater, ensure a balance between abstraction and recharge of groundwater, with the aim of achieving good groundwater status at the latest 15 years after the date of entry into force of this Directive,

Page 3: Aquifers of the Scheldt basin

Questions for the testing

• Do abstractions exceed the natural recharge (today and in the baseline scenario)?

• If so, what are the possible measures and their cost-effectiveness ?

Page 4: Aquifers of the Scheldt basin

Selection of the case study

• Carboniferous limestone – International Groundwater in the Scheldt basin

• over-exploited• competition between industries• national strategies to avoid a common assessment

– Different definitions of the aquifer• no comparable data

Page 5: Aquifers of the Scheldt basin

Leie

Scheldt

NORD

Chalkaquifer

Coal

Paleozoic

CarboniferousLimestone aquifer

A : holocene andpleistocene

B : eocene andoligocene

Page 6: Aquifers of the Scheldt basin

Selection of the case study

• Chalk aquifer around Lille area • National groundwater in the Scheldt basin• over-exploitation and pollution• alternative resource of the carboniferous

limestone• existing coherent data

Page 7: Aquifers of the Scheldt basin

The 3-steps approach

• Characterisation of groundwaters– 1. Definition of relevant hydrogeological units– 2. Assessment of the natural recharge of each unit– 3. Assessment of abstractions from each unit– 4. Structure of the demand – 5. Evolution of the demand

• Future demand versus natural recharge (gap assessment)

• Cost-effectiveness analysis of possible measures

Page 8: Aquifers of the Scheldt basin

The 3-steps approach

• Characterisation of groundwaters– 1. Definition of relevant hydrogeological units– 2. Assessment of the natural recharge of each unit– 3. Assessment of abstractions from each unit– 4. Structure of the demand – 5. Evolution of the demand

• Future demand versus natural recharge (gap assessment)

• Cost-effectiveness analysis of possible measures

Page 9: Aquifers of the Scheldt basin

Relevant units: assumptions

Seepage

Rainfall +reinfiltration

Naturalevapo-transpiration

rivers

abstractions

abstractions

piezometryabstraction

Rainfall +reinfiltration

abstractions

70 %

Pool model

Page 10: Aquifers of the Scheldt basin

Relevant units in Lille area

Lille Mélantois

RoubaixTourcoing

MouvauxArmentières

Béthune

Lens

La madeleineSt André

Séclin

La lys

La Deûle LaMarque

Flers enEscrébieux

DouaiPecquencourt

Aire surla Lys

Verchin

La ScarpeBassin d ’Orchies

Abstraction areas

Geographical region

Urban area of Lille

Limit ofgroundwatershed

carboniferous

Page 11: Aquifers of the Scheldt basin

Relevant units in Lille area

North ofMélantois

South ofMélantois

Bassind’Orchies

Verchin

La Lys

Abstractions

Rainfall

Pool of groundwater

River Inflow and outflow of the river

Abstractionin order toincrease theLysdischarge

Carboniferous

Page 12: Aquifers of the Scheldt basin

The 3-steps approach

• Characterisation of groundwaters– 1. Definition of relevant hydrogeological units– 2. Assessment of the natural recharge of each unit– 3. Assessment of abstractions from each unit– 4. Structure of the demand – 5. Evolution of the demand

• Future demand versus natural recharge (gap assessment)

• Cost-effectiveness analysis of possible measures

Page 13: Aquifers of the Scheldt basin

Natural recharge of each unit

Pools Natural recharge (source BRGM)North of Mélantois 19,5 Mn m3/yr = 53 400 m3/daySouth of Mélantois 22,5 Mn m3/yr = 61 600 m3/dayBasin of Orchies unknownLys at Aire sur la Lys unknownCenomanian in Verchin unknownCarboniferous limestone 50 Mn m3/yr =137 000 m3/day

Different definitions: different values

Page 14: Aquifers of the Scheldt basin

The 3-steps approach

• Characterisation of groundwaters– 1. Definition of relevant hydrogeological units– 2. Assessment of the natural recharge of each unit– 3. Assessment of abstractions from each unit– 4. Structure of the demand – 5. Evolution of the demand

• Future demand versus natural recharge (gap assessment)

• Cost-effectiveness analysis of possible measures

Page 15: Aquifers of the Scheldt basin

Abstractions from each unit

Municipality

Domestic users

Industrial users

Municipal uses

Losses

Agricultural users

Industrial users

agricultural users

Domestic individual users

Information registeredby water agencies andState offices

Information registered bypublic water services

Often underestimated

Page 16: Aquifers of the Scheldt basin

The 3-steps approach

• Characterisation of groundwaters– 1. Definition of relevant hydrogeological units– 2. Assessment of the natural recharge of each unit– 3. Assessment of abstractions from each unit– 4. Structure of the demand – 5. Evolution of the demand

• Future demand versus natural recharge (gap assessment)

• Cost-effectiveness analysis of possible measures

Page 17: Aquifers of the Scheldt basin

Structure of the demand

0

20 000

40 000

60 000

80 000

100 000

120 000

m3/dayH

ouse

hold

s

Mun

icip

aliti

es

Indu

stry

Agr

icul

ture

Leak

ages

Lille

indu

strie

lle

Oth

erm

unic

ipal

ities

Data for 2000

Page 18: Aquifers of the Scheldt basin

The 3-steps approach

• Characterisation of groundwaters– 1. Definition of relevant hydrogeological units– 2. Assessment of the natural recharge of each unit– 3. Assessment of abstractions from each unit– 4. Structure of the demand – 5. Evolution of the demand

• Future demand versus natural recharge (gap assessment)

• Cost-effectiveness analysis of possible measures

Page 19: Aquifers of the Scheldt basin

Evolution of the demand

• no change in the population and economic developments• no change in consuming behaviours• no change in distribution of abstraction

• Consequences by the year 2015:• same situation as in 2000, no measure implemented.

To be negotiated

Page 20: Aquifers of the Scheldt basin

The 3-steps approach

• Characterisation of groundwaters– 1. Definition of relevant hydrogeological units– 2. Assessment of the natural recharge of each unit– 3. Assessment of abstractions from each unit– 4. Structure of the demand – 5. Evolution of the demand

• Future demand versus natural recharge (gap assessment)

• Cost-effectiveness analysis of possible measures

Page 21: Aquifers of the Scheldt basin

Gap assessmentGroundwater pool Abstraction for

the area ofLille in m3/day

proportion rechargein m3/day

rateabstraction/recharge

Carboniferous 30 000 16% unknownNorth of Mélantois 26 000 14% 53 000 49 %South of Mélantois 64 000 34% 61 000 105 %Basin of Orchies 31 000 16% unknownLys river 38 000 20% unknownTotal 189 000 100%

Target for the testing: 70 % 10 200 m3/day needed

Page 22: Aquifers of the Scheldt basin

The 3-steps approach

• Characterisation of groundwaters– 1. Definition of relevant hydrogeological units– 2. Assessment of the natural recharge of each unit– 3. Assessment of abstractions from each unit– 4. Structure of the demand – 5. Evolution of the demand

• Future demand versus natural recharge (gap assessment)

• Cost-effectiveness analysis of possible measures

Page 23: Aquifers of the Scheldt basin

Cost-effectiveness of measures

0

20 000

40 000

60 000

80 000

100 000

120 000

m3/dayH

ouse

hold

s

Mun

icip

aliti

es

Indu

stry

Agr

icul

ture

Leak

ages

Lille

indu

strie

lle

Oth

erm

unic

ipal

ities

Reduction of losses

Communication campaign for reduction of the water demand

Page 24: Aquifers of the Scheldt basin

Communication campaign

Population Cost water-savings Alcobendas 100 000 410 600 1 650Lille area 1 000 000 10 200

m3/inhabitant Cost (E) /inhabitantAlcobendas 6 4,106Lille area 3,72 2,55

Global cost of 2 550 000 Euros for Lille Area

Less water income Less maintenance ?Higher price ?

Page 25: Aquifers of the Scheldt basin

Conclusion of the testing

• Relevant scale: • public water services + self services

• to take into account possible shifts

• Natural recharge and abstractions assessment• Strategic information

• Common monitoring needed

• Indirect effects of water savings• feedbacks on price or maintenance