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Mapping groundwater dynamics in the Netherlands

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Delft University of Technology

Mapping groundwater dynamics in the Netherlands

Three dimensional insight in groundwater systems based on the Dutch national database of suburface information (DINOloket.nl)

Zaadnoordijk, Willem Jan; Lourens, Aris

Publication date 2019

Document Version Final published version

Citation (APA)

Zaadnoordijk, W. J., & Lourens, A. (2019). Mapping groundwater dynamics in the Netherlands: Three dimensional insight in groundwater systems based on the Dutch national database of suburface information (DINOloket.nl). IAH 2019: 46th Congress of the Interational Association of Hydrogeologists, Malaga, Spain. Important note

To cite this publication, please use the final published version (if applicable). Please check the document version above.

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(2)

Mapping groundwater

dynamics in the Netherlands:

three dimensional insight in

groundwater systems based on the

Dutch national database of

subsurface information (DINOloket.nl)

Willem J. Zaadnoordijk1,2, Aris Lourens1

willem_jan.zaadnoordijk@tno.nl

1TNO Geological Survey of the Netherlands – team geomodelling, Utrecht

(3)

Mapping groundwater

dynamics in the Netherlands:

three dimensional insight in

groundwater systems based on the

Dutch national database of

subsurface information (DINOloket.nl)

Willem J. Zaadnoordijk1,2, Aris Lourens1

willem_jan.zaadnoordijk@tno.nl

1TNO Geological Survey of the Netherlands – team geomodelling, Utrecht

(4)

Groundwater time series models

(5)

Noise model

Decomposition of influences in

time series model

(6)

Aspects groundwater dynamics

1. Response time of precipitation response 2. Yearly fluctuation - regime curve

(7)

Characterization impulse response

Temporal moments (raw moments Mk)

M0 – total response

µ = M1/M0 – average response time

Physical meaning – Mk fulfills differential equation similar to groundwater head

Analytic solutions for simple situations like circular island

(8)

Lateral variation response time

(9)

Lateral variation response time

First regional aquifer

% surface water

Surface elevation

(10)

Vertical variation

Difference between first and second regional aquifer

(11)

Vertical variation

Difference between first and second regional aquifer

with hydraulic resistance of aquitard

(12)

Concluding remarks

Groundwater head time series show system characteristics in head response to precipitation

Mapping response time in three dimensions provides insight

Response function may differ even if no head difference

Response integrates over larger area than bore log → → additional information for delineating aquitards

(13)

Contact: willem_jan.zaadnoordijk@tno.nl

Check out:

https://www.dinoloket.nl/ondergrondgegevens

https://www.grondwatertools.nl/grondwatertools-viewer

Thank you for

your attention

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