Abstract

Travel-time based hydraulic tomography is a promising method to characterize heterogeneity of porous-fractured aquifers. However, there is inevitable noise in field-scale experimental data and many hydraulic signal travel times, which are derived from the pumping test’s first groundwater level derivative drawdown curves and are strongly influenced by noise. The required data processing is thus quite time consuming and often not accurate enough. Therefore, an effective and accurate de-noising method is required for travel time inversion data processing. In this study, a series of hydraulic tomography experiments were conducted at a porous-fractured aquifer test site in Goettingen, Germany. A numerical model was built according to the site’s field conditions and tested based on diagnostic curve analyses of the field experimental data. Gaussian white noise was then added to the model’s calculated pumping test drawdown data to simulate the real noise in the field. Afterward, different de-noising methods were applied to remove it. This study has proven the superiority of the wavelet de-noising approach compared with several other filters. A wavelet de-noising method with calibrated mother wavelet type, de-noising level, and wavelet level was then determined to obtain the most accurate travel time values. Finally, using this most suitable de-noising method, the experimental hydraulic tomography travel time values were calculated from the de-noised data. The travel time inversion based on this de-noised data has shown results consistent with previous work at the test site.

Highlights

  • Hydraulic tomography has proven to be a reliable method to investigate heterogeneity of hydraulic aquifer parameters at a high spatial resolution level [1,2,3,4,5,6,7,8,9,10,11,12,13,14,15]

  • The travel time results for O2M5, O3M5, and O4M5 are missing, because the noise of these field data sets is too high to obtain reliable travel time values

  • The employed travel-time based inversion requires accurate hydraulic signal travel time values, which determine the quality of the inversion result

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Summary

Introduction

Hydraulic tomography has proven to be a reliable method to investigate heterogeneity of hydraulic aquifer parameters at a high spatial resolution level [1,2,3,4,5,6,7,8,9,10,11,12,13,14,15]. The application of hydraulic tomography is based on two main steps: hydraulic aquifer testing using a tomographical setup and an inversion of the obtained experimental response data [14,16]. Hydraulic tomography inversion may be performed using a numerical groundwater flow model and parameter estimation [5,11], providing spatial distribution of hydraulic conductivity (K) and specific storage (Ss) values. This inversion method can provide remarkably accurate inversion results

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