TY - JOUR
T1 - Time-lapse magnetic resonance sounding measurements for numerical modeling of water flow in variably saturated media
AU - Legchenko, Anatoly
AU - Baltassat, Jean Michel
AU - Duwig, Céline
AU - Boucher, Marie
AU - Girard, Jean François
AU - Soruco, Alvaro
AU - Beauce, Alain
AU - Mathieu, Francis
AU - Legout, Cedric
AU - Descloitres, Marc
AU - Gabriela Patricia, Flores Avilès
N1 - Publisher Copyright:
© 2020 Elsevier B.V.
PY - 2020/4
Y1 - 2020/4
N2 - We presented an innovative hydrogeophysical approach that allows numerical modeling of water flow in a variably saturated media. In our model, we approximated the subsurface by horizontally stratified porous media. The model output was a time varying water content profile. Then, we compared the water content provided by the model with the water content measurements carried out using the time-lapse Magnetic Resonance Sounding (MRS) method. Each MRS sounding provided a water content profile in the unsaturated zone down to twenty meters. The time shift between the profiles corresponded to the time lapse between individual MRS soundings. We minimized the discrepancy between the observed and the modeled MRS signals by varying hydraulic parameters of soil layers in the water flow model. For measuring and processing MRS data, we used NUMIS MRS instrument and SAMOVAR software. We carried out water flow modeling with HYDRUS-1D software. This paper reports our results and summarizes the limitations of the MRS method applied to water content measurements in the unsaturated zone.
AB - We presented an innovative hydrogeophysical approach that allows numerical modeling of water flow in a variably saturated media. In our model, we approximated the subsurface by horizontally stratified porous media. The model output was a time varying water content profile. Then, we compared the water content provided by the model with the water content measurements carried out using the time-lapse Magnetic Resonance Sounding (MRS) method. Each MRS sounding provided a water content profile in the unsaturated zone down to twenty meters. The time shift between the profiles corresponded to the time lapse between individual MRS soundings. We minimized the discrepancy between the observed and the modeled MRS signals by varying hydraulic parameters of soil layers in the water flow model. For measuring and processing MRS data, we used NUMIS MRS instrument and SAMOVAR software. We carried out water flow modeling with HYDRUS-1D software. This paper reports our results and summarizes the limitations of the MRS method applied to water content measurements in the unsaturated zone.
KW - Beauce
KW - Hydrodynamic modeling
KW - MRS
KW - Time-lapse
KW - Villamblain
UR - http://www.scopus.com/inward/record.url?scp=85081658439&partnerID=8YFLogxK
U2 - 10.1016/j.jappgeo.2020.103984
DO - 10.1016/j.jappgeo.2020.103984
M3 - Artículo
AN - SCOPUS:85081658439
SN - 0926-9851
VL - 175
JO - Journal of Applied Geophysics
JF - Journal of Applied Geophysics
M1 - 103984
ER -