Time-lapse borehole radar for monitoring rainfall infiltration through podosol horizons in a sandy vadose zone

• Published in: Water resources research 2014-03, Vol.50 (3), p.2140-2163
• Main Authors: Strobach, Elmar, Harris, B. D., Dupuis, J. C., Kepic, A. W.
• Format: Article
• Language: English
• Subjects: Boreholes; crosswell radar; Evapotranspiration; Moisture content; Radar; Rainfall infiltration; Recharge; Soil horizons; Soil moisture; Trends; Unsaturated flow; Vadose water; Water balance; Water content; water infiltration; Water table
• ISSN: 0043-1397; 1944-7973
• DOI: 10.1002/2013WR014331

The shallow aquifer on the Gnangara Mound, north of Perth, Western Australia, is recharged by winter rainfall. Water infiltrates through a sandy Podosol where cemented accumulation (B‐) horizons are common. They are water retentive and may impede recharge. To observe wetting fronts and the influence of soil horizons on unsaturated flow, we deployed time‐lapse borehole radar techniques sensitive to soil moisture variations during an annual recharge cycle. Zero‐offset crosswell profiling (ZOP) and vertical radar profiling (VRP) measurements were performed at six sites on a monthly basis before, during, and after annual rainfall in 2011. Water content profiles are derived from ZOP logs acquired in closely spaced wells. Sites with small separation between wells present potential repeatability and accuracy difficulties. Such problems could be lessened by (i) ZOP saturated zone velocity matching of time‐lapse curves, and (ii) matching of ZOP and VRP results. The moisture contents for the baseline condition and subsequent observations are computed using the Topp relationship. Time‐lapse moisture curves reveal characteristic vadose zone infiltration regimes. Examples are (I) full recharge potential after 200 mm rainfall, (II) delayed wetting and impeded recharge, and (III) no recharge below 7 m depth. Seasonal infiltration trends derived from long‐term time‐lapse neutron logging at several sites are shown to be comparable with infiltration trends recovered from time‐lapse crosswell radar measurements. However, radar measurements sample a larger volume of earth while being safer to deploy than the neutron method which employs a radioactive source. For the regime (III) site, where time‐lapse radar indicates no net recharge or zero flux to the water table, a simple water balance provides an evapotranspiration value of 620 mm for the study period. This value compares favorably to previous studies at similar test sites in the region. Our six field examples demonstrate application of time‐lapse borehole radar for characterizing rainfall infiltration. Key Points Time‐lapse borehole radar case study for water infiltration monitoring Podosol accumulation horizons impede wetting front development Combination of ZOP and VRP BHR methods can improve accuracy