TY - JOUR
T1 - High-resolution moisture profiles from full-waveform probabilistic inversion of TDR signals
AU - Laloy, Eric
AU - Huisman, Johan Alexander
AU - Jacques, Diederik
N1 - Score = 10
PY - 2014/11
Y1 - 2014/11
N2 - This study presents an novel Bayesian inversion scheme for high-dimensional undetermined TDR waveform inversion. The methodology quantifies uncertainty in the moisture content distribution, using a Gaussian Markov random field (GMRF) prior as regularization operator. A spatial resolution of 1cm along a 70-cm long TDR probe is considered for the inferred moisture content. Numerical testing shows that the proposed inversion approach works very well in case of a perfect model and Gaussian measurement errors. Real-world application results are generally satisfying. For a series of TDR measurements made during imbibition and evaporation from a laboratory soil column, the average root-mean-square error (RMSE) between maximum a posteriori (MAP) moisture distribution and reference TDR measurements is 0.04cm³cm-3. This RMSE value reduces to less than 0.02cm³cm-3 for a field application in a podzol soil. The observed model-data discrepancies are primarily due to model inadequacy, such as our simplified modeling of the bulk soil electrical conductivity profile. Among the important issues that should be addressed in future work are the explicit inference of the soil electrical conductivity profile along with the other sampled variables, the modeling of the temperature-dependence of the coaxial cable properties and the definition of an appropriate statistical model of the residual errors.
AB - This study presents an novel Bayesian inversion scheme for high-dimensional undetermined TDR waveform inversion. The methodology quantifies uncertainty in the moisture content distribution, using a Gaussian Markov random field (GMRF) prior as regularization operator. A spatial resolution of 1cm along a 70-cm long TDR probe is considered for the inferred moisture content. Numerical testing shows that the proposed inversion approach works very well in case of a perfect model and Gaussian measurement errors. Real-world application results are generally satisfying. For a series of TDR measurements made during imbibition and evaporation from a laboratory soil column, the average root-mean-square error (RMSE) between maximum a posteriori (MAP) moisture distribution and reference TDR measurements is 0.04cm³cm-3. This RMSE value reduces to less than 0.02cm³cm-3 for a field application in a podzol soil. The observed model-data discrepancies are primarily due to model inadequacy, such as our simplified modeling of the bulk soil electrical conductivity profile. Among the important issues that should be addressed in future work are the explicit inference of the soil electrical conductivity profile along with the other sampled variables, the modeling of the temperature-dependence of the coaxial cable properties and the definition of an appropriate statistical model of the residual errors.
KW - Spatial TDR
KW - full waveform inversion
KW - MCMC
KW - soil moisture profile
UR - http://ecm.sckcen.be/OTCS/llisapi.dll/open/ezp_137266
UR - http://knowledgecentre.sckcen.be/so2/bibref/11922
U2 - 10.1016/j.jhydrol.2014.10.005
DO - 10.1016/j.jhydrol.2014.10.005
M3 - Article
SN - 0022-1694
VL - 519
SP - 2121
EP - 2135
JO - Journal of Hydrology
JF - Journal of Hydrology
IS - Part B
ER -