9th conference on limestone hydrogeology in besançon 9ième colloque d'hydrogéologie en pays...

9th Conference on Limestone Hydrogeology in Besançon

9ième Colloque d'Hydrogéologie en Pays

Calcaire à BesançonSession 4

Metrology and data transmission

“Artificial neural network for karst aquifer sustainable

management”

Marc Lambert

Manager of Syndicat des Eaux du Vivier

http://sites.google.com/site/h2karst/home/logo-h2karst.jpg?attredirects=0

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The Syndicat des Eaux du Vivier« SEV » in a few figures

– 5 municipalities including the city of Niort

– about 100.000 people depending on the Vivier karstic spring

– 650 km water networks, 36000 compteurs, 5 main water resources

– 60 agents, in public management– Hospitals, industry with SEVESO sites,

schools…)



3

What are the mains problems?– Agricultural area with intensive

production– Competition with water supply– Limited and fragile underground

resources, with 2 observed karstic collapses in Vivier spring

– Quality problems due to nitrates and pesticides



4

Our main purposes about quantity

– Securize water supply on our area– Understand and anticipate needs

(peaks, periodicity)– Understand and modelize water

resources (rain effect, cycles, pumping effects…)

– Criterion:

« water resources always > peak needs »



5

Geological context9th Conference on Limestone Hydrogeology in Besançon


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Geological context (AB cut)9th Conference on Limestone Hydrogeology in Besançon


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Vivier karst observed behaviour



8

Effects of pumpings forirrigation and water supply


IMPACT DES PRELEVEMENTS AGRICOLES SUR LA RESSOURCE DE NIORT

-3.00

-2.00

-1.00

0.00

1.00

2.00

3.00

oct-01 avr-02 oct-02 avr-03 oct-03 avr-04 oct-04

SEMESTRES SECS / DE RECHARGE

Dé

bit

So

urc

e (

m3

/s)

/Niv

Pu

its

(-m

)

0.00

0.10

0.20

0.30

0.40

0.50

0.60

0.70

0.80

0.90

1.00

PR

EL

EV

EM

EN

TS

(A

EP

/AG

RI)

m3

/s

canal

rabattement dans lepuits du Vivier (m)

besoin Niort (V+G)(m3/s moyensmensuels)

Irrigation (m3/smoyens mensuels)données estiméespour secteur 13


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Methodology followed– 1 : Data collecting, selecting…and mining

(ACP, geostatistics, wavelets…)– 2 : Modelling with different techniques

(lumped modelling of rainfall – runoff and rainfall aquifer level, inverse modelling using fourier analysis, neural networks…)

– 3: Forecasting with rainfall simulation– 4: Managing resources…ie how to keep

« water resources always > peak needs »



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Rainfall data analysis9th Conference on Limestone Hydrogeology in Besançon


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Inverse modelling (TEMPO BRGM)



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Inverse modelling (TEMPO BRGM)



13

Hydrological modelling (GARDENIA BRGM)


RUMAX déficit maximal du sol

RUIPER Hauteur d'équiRuissellement Percolation

THG Temps ½ percolation

Percolation(RECHARGE de la nappe)

PLUIE EFFICACE

Q = SURF * EC + Qo NP = G / S + NB

Écoulement total(DEBIT du cours d'eau)

Niveau Piézom. NPDébit Q

PLUIE ETP

Surface du bassin versant

14

Hydrological modelling (GARDENIA BRGM)


15

Artificial neural network modelling (Neuro one Netral)


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Artificial neural network modelling

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Example of use of this model:Crisis anticipation and management

CROISEMENT ENTRE RESSOURCES DISPONIBLES ET BESOINS - ETIAGE 2005

0

10000

20000

30000

40000

50000

60000

70000

80000

01/01/05 01/07/05 01/01/06

vo

lum

es

en

m3

/j

-3.5

-3

-2.5

-2

-1.5

-1

-0.5

0

0.5

rab

att

eme

nt

(<0

) et

plu

ie (>

0)

en

m

Ress.princ.V+GI+GIII+Canal(m3/j)

Consommationm3/j

Secoursnécessaire m3/j

pluies (m)

rabattementVivier (m)

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Conclusion: advantages of ANN tools

– After choosing a good model, easy qnalytical formulation under Excel…

– « Intelligent » black box, but to use under constraints (learning sets must include extrem years)

– Easy to use for simulations (pumpings for irrigation or water supply, climate…)

– Easy to use for sensitivity analysis

9th conference on limestone hydrogeology in besançon 9ième colloque d'hydrogéologie en pays...

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