Estimation of saturated hydraulic conductivity from ring infiltrometer test taking into account the surface moisture stain extension

Title:

Estimation of saturated hydraulic conductivity from ring infiltrometer test taking into account the surface moisture stain extension

Creator:

Réfloch, Aurore, Gaudet, Jean-Paul, Laurent, and Rossier, Yvan

Identifier:

https://cdk.lib.cas.cz/client/handle/uuid:060b78f6-812d-464a-840c-53c6b808fcc7
uuid:060b78f6-812d-464a-840c-53c6b808fcc7
doi:10.1515/johh-2017-0019

Subject:

ring infiltrometer test, infiltration basin, numerical modeling, saturated hydraulic conductivity, and anisotropy of hydraulic conductivity.

Type:

article, model:article, and TEXT

Description:

A large single-ring infiltrometer test was performed in order to characterize the saturated hydraulic conductivity below an infiltration basin in the well field of Lyon (France). Two kinds of data are recorded during the experiment: the volume of water infiltrated over time and the extension of the moisture stain around the ring. Then numerical analysis was performed to determine the saturated hydraulic conductivity of the soil by calibration. Considering an isotropic hydraulic conductivity, the saturated hydraulic conductivity of the alluvial deposits is estimated at 3.8 10–6 m s–1. However, with this assumption, we are not able to represent accurately the extension of the moisture stain around the ring. When anisotropy of hydraulic conductivity is introduced, experimental data and simulation results are in good agreement, both for the volume of water infiltrated over time and the extension of the moisture stain. The vertical saturated hydraulic conductivity in the anisotropic configuration is 4.75 times smaller than in the isotropic configuration (8.0 10–7 m s–1), and the horizontal saturated hydraulic conductivity is 125 times higher than the vertical saturated hydraulic conductivity (1.0 10–4 m s–1).

Language:

Slovak

Rights:

http://creativecommons.org/licenses/by-nc-sa/4.0/
policy:public

Source:

Journal of hydrology and hydromechanics | 2017 Volume:65 | Number:3

Harvested from:

CDK

Metadata only:

false