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| 001 | 22938 | ||
| 005 | 20200702121628.0 | ||
| 024 | 7 | _ | |2 DOI |a 10.2136/vzj2011.0115 |
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| 037 | _ | _ | |a PreJuSER-22938 |
| 041 | _ | _ | |a eng |
| 082 | _ | _ | |a 550 |
| 084 | _ | _ | |2 WoS |a Environmental Sciences |
| 084 | _ | _ | |2 WoS |a Soil Science |
| 084 | _ | _ | |2 WoS |a Water Resources |
| 100 | 1 | _ | |0 P:(DE-Juel1)129501 |a Mboh, C.M. |b 0 |u FZJ |
| 245 | _ | _ | |a Coupled Hydrogeophysical Inversion of Streaming Potential Signals for Unsaturated Soil Hydraulic Properties |
| 260 | _ | _ | |a Madison, Wis. |b SSSA |c 2012 |
| 336 | 7 | _ | |a Journal Article |0 PUB:(DE-HGF)16 |2 PUB:(DE-HGF) |
| 336 | 7 | _ | |a Output Types/Journal article |2 DataCite |
| 336 | 7 | _ | |a Journal Article |0 0 |2 EndNote |
| 336 | 7 | _ | |a ARTICLE |2 BibTeX |
| 336 | 7 | _ | |a JOURNAL_ARTICLE |2 ORCID |
| 336 | 7 | _ | |a article |2 DRIVER |
| 440 | _ | 0 | |0 10301 |a Vadose Zone Journal |v 11 |x 1539-1663 |y 2 |
| 500 | _ | _ | |3 POF3_Assignment on 2016-02-29 |
| 500 | _ | _ | |a C.M. Mboh and J. A. Huisman gratefully acknowledge support by Grants HU1312/2-1 and HU1312/2-2 of the Deutsche Forschungsgemeinschaft. |
| 520 | _ | _ | |a Streaming potential (SPs) is the electric potential generated by fluid flow in a charged porous medium. The SPs signals are related to pore water velocity, bulk electrical conductivity, pore water charge excess, and soil porosity. While several studies have estimated hydraulic properties of the saturated zone from SPs, there have been fewer attempts to infer unsaturated hydraulic properties from SPs. From numerical and laboratory experiments in which infiltration and subsequent drainage was monitored with nonpolarizable Ag/AgCl electrodes and tensiometers, we showed that it is feasible to estimate three key Mualemvan Genuchten hydraulic parameters (fitting parameters alpha and n and saturated hydraulic conductivity K-s) and Archie's saturation exponent (n(a)) using a coupled hydrogeophysical inversion approach. In addition to a reasonably good estimate of n(a), coupled hydrogeophysical inversion of actual SPs measurements during drainage provided estimates of alpha, n, and K-s that were comparable to those obtained from an independent inversion of the tensiometric data (matric heads). We concluded that coupled hydrogeophysical inversion of time-lapse SPs signals is a promising method for hydraulic characterization of the vadose zone. Accurate modeling of SPs signals is essential for reliable inversion results, but there is still debate about the appropriate model for the voltage coupling coefficient at partial saturation. Our experimental data showed a nonlinear and monotonic decrease in the absolute voltage coupling coefficient with decreasing saturation. A comparison of several available models with our experimental data showed that models that consider the relative permeability and the relative electrical conductivity in addition to the saturated coupling coefficient and water saturation were most appropriate. |
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| 700 | 1 | _ | |0 P:(DE-Juel1)129472 |a Huisman, J.A. |b 1 |u FZJ |
| 700 | 1 | _ | |0 P:(DE-Juel1)133962 |a Zimmermann, E. |b 2 |u FZJ |
| 700 | 1 | _ | |0 P:(DE-Juel1)129549 |a Vereecken, H. |b 3 |u FZJ |
| 773 | _ | _ | |0 PERI:(DE-600)2088189-7 |a 10.2136/vzj2011.0115 |g Vol. 11 |n 2 |q 11 |t Vadose zone journal |v 11 |x 1539-1663 |y 2012 |
| 856 | 7 | _ | |u http://dx.doi.org/10.2136/vzj2011.0115 |
| 909 | C | O | |o oai:juser.fz-juelich.de:22938 |p VDB |p VDB:Earth_Environment |
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| 914 | 1 | _ | |y 2012 |
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