Assessment of groundwater recharge processes through karst vadose zone by cave percolation monitoring

Amael Poulain, Arnaud Watlet, Olivier Kaufmann, Michel Van Camp, Hervé Jourde, Naomi Mazzilli, Gaëtan Rochez, Romain Deleu, Yves Quinif, Vincent Hallet (Supervisor)

Research output: Contribution to journalArticle

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Abstract

Recharge processes of karst aquifers are difficult to assess given their strong heterogeneity and the poorly known effect of vadose zone on infiltration. However, recharge assessment is crucial for the evaluation of groundwater resources. Moreover, the vulnerability of karst aquifers depends on vadose zone behaviour because it is the place where most contamination takes place. In this work, an in situ experimental approach was performed to identify and quantify flow and storage processes occurring in karst vadose zone. Cave percolation monitoring and dye tracing were used to investigate unsaturated zone hydrological processes. Two flow components (diffuse and quick) were identified and, respectively, account for 66% and 34% of the recharge. Quickflow was found to be the result of bypass phenomenon in vadose zone related to water saturation. We identify the role of epikarst as a shunting area, most of the storage in the vadose zone occurring via the diffuse flow component in low permeability zones. Relationship between rainfall intensity and transit velocity was demonstrated, with 5 times higher velocities for the quick recharge mode than the diffuse mode. Modelling approach with KarstMod software allowed to simulate the hybrid recharge through vadose zone and shows promising chances to properly assess the recharge processes in karst aquifer based on simple physical models.

Original languageEnglish
Pages (from-to)2069-2083
Number of pages15
JournalHydrological Processes
Volume32
Issue number13
Early online date9 May 2018
DOIs
Publication statusPublished - 30 Jun 2018

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vadose zone
cave
karst
recharge
groundwater
monitoring
aquifer
bypass
groundwater resource
precipitation intensity
dye
vulnerability
infiltration
saturation
permeability
software
modeling

Keywords

  • karst aquifer
  • vardose zone
  • cave monithoring
  • dye tracing
  • stalactite drip
  • groundwater recharge
  • epikarst
  • cave monitoring
  • vadose zone

Cite this

Poulain, Amael ; Watlet, Arnaud ; Kaufmann, Olivier ; Van Camp, Michel ; Jourde, Hervé ; Mazzilli, Naomi ; Rochez, Gaëtan ; Deleu, Romain ; Quinif, Yves ; Hallet, Vincent. / Assessment of groundwater recharge processes through karst vadose zone by cave percolation monitoring. In: Hydrological Processes. 2018 ; Vol. 32, No. 13. pp. 2069-2083.
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Poulain, A, Watlet, A, Kaufmann, O, Van Camp, M, Jourde, H, Mazzilli, N, Rochez, G, Deleu, R, Quinif, Y & Hallet, V 2018, 'Assessment of groundwater recharge processes through karst vadose zone by cave percolation monitoring', Hydrological Processes, vol. 32, no. 13, pp. 2069-2083. https://doi.org/10.1002/hyp.13138

Assessment of groundwater recharge processes through karst vadose zone by cave percolation monitoring. / Poulain, Amael; Watlet, Arnaud; Kaufmann, Olivier; Van Camp, Michel; Jourde, Hervé; Mazzilli, Naomi; Rochez, Gaëtan; Deleu, Romain; Quinif, Yves; Hallet, Vincent (Supervisor).

In: Hydrological Processes, Vol. 32, No. 13, 30.06.2018, p. 2069-2083.

Research output: Contribution to journalArticle

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T1 - Assessment of groundwater recharge processes through karst vadose zone by cave percolation monitoring

AU - Poulain, Amael

AU - Watlet, Arnaud

AU - Kaufmann, Olivier

AU - Van Camp, Michel

AU - Jourde, Hervé

AU - Mazzilli, Naomi

AU - Rochez, Gaëtan

AU - Deleu, Romain

AU - Quinif, Yves

A2 - Hallet, Vincent

PY - 2018/6/30

Y1 - 2018/6/30

N2 - Recharge processes of karst aquifers are difficult to assess given their strong heterogeneity and the poorly known effect of vadose zone on infiltration. However, recharge assessment is crucial for the evaluation of groundwater resources. Moreover, the vulnerability of karst aquifers depends on vadose zone behaviour because it is the place where most contamination takes place. In this work, an in situ experimental approach was performed to identify and quantify flow and storage processes occurring in karst vadose zone. Cave percolation monitoring and dye tracing were used to investigate unsaturated zone hydrological processes. Two flow components (diffuse and quick) were identified and, respectively, account for 66% and 34% of the recharge. Quickflow was found to be the result of bypass phenomenon in vadose zone related to water saturation. We identify the role of epikarst as a shunting area, most of the storage in the vadose zone occurring via the diffuse flow component in low permeability zones. Relationship between rainfall intensity and transit velocity was demonstrated, with 5 times higher velocities for the quick recharge mode than the diffuse mode. Modelling approach with KarstMod software allowed to simulate the hybrid recharge through vadose zone and shows promising chances to properly assess the recharge processes in karst aquifer based on simple physical models.

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KW - karst

KW - zone vadose

KW - essai de traçage

KW - fluorimètre

KW - uranine

KW - karst aquifer

KW - vardose zone

KW - cave monithoring

KW - dye tracing

KW - stalactite drip

KW - groundwater recharge

KW - epikarst

KW - cave monitoring

KW - vadose zone

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DO - 10.1002/hyp.13138

M3 - Article

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SP - 2069

EP - 2083

JO - Hydrological Processes

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SN - 0885-6087

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