Details
| Original language | English |
|---|---|
| Journal | Vadose zone journal |
| Volume | 17 |
| Issue number | 1 |
| Publication status | Published - 14 Jun 2018 |
Abstract
The influence of porous media wettability on the mobility of colloids is mostly unknown. In the present work, organic-matter-coated goethite (OMCG) colloids were percolated through three saturated soil materials differing in wettability: untreated quartz sand and two variants of hydrophobized sand. For each type of sand, three ionic strength levels were applied. Derjaguin–Landau–Verwey– Overbeek (DLVO) and Lewis acid–base extended DLVO (XDLVO) interaction energy profiles were calculated according to contact angles and zeta potentials. Flow column results elucidated that decreasing sand wettability had no relevant effect on OMCG colloid mobility. In contrast, colloid retention increased with ionic strength in each type of sand packing. Classic DLVO interactions could predict trends in colloid retention by the respective characteristics of energy barriers and secondary minima. The extension with Lewis acid–base interactions in the XDLVO approach led to the prediction of significant short-range (∼2 nm) attractive interaction energies between colloids and hydrophobized sand, which were not reflected by colloid breakthrough behavior. This was probably due to substantial energy barriers calculated for larger distances (∼27 to ∼75 nm, depending on ionic strength) between the solid matrix and colloids. It is concluded that the distinct surface roughness of sand grains and colloids probably weakened the strength of the short-range attractive interactions, because larger amounts of surface area were still outside the effective distance for the short-range interactions predicted by XDLVO. Regarding colloidal mobility, we concluded for our saturated porous systems that near-surface attractive XDLVO interaction energies between OMCG colloids and hyrophobized sand did not significantly affect colloid mobility.
ASJC Scopus subject areas
- Agricultural and Biological Sciences(all)
- Soil Science
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In: Vadose zone journal, Vol. 17, No. 1, 14.06.2018.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Iron oxide colloid mobility as affected by solid matrix wetting properties
AU - Carstens, J. F.
AU - Bachmann, J.
AU - Neuweiler, I.
N1 - Funding information: We appreciate the financial support provided by the Niedersachsen Institutes of Technology graduate school GeoFluxes (Top-Down Project 2.1.4) and the Deutsche Forschungsgemeinschaft Research Unit 1806 “SUBSOM” BA 1359/13-1 for this study. We also thank the specialty chemicals group Lanxess for generously providing the colloidal goethite Bayferrox 920 Z free of charge. Moreover, we dearly thank coworkers Marc-Oliver Goebel, Martin Volkmann, and Susanne K. Woche for assistance with the experiments and valuable theoretical input.
PY - 2018/6/14
Y1 - 2018/6/14
N2 - The influence of porous media wettability on the mobility of colloids is mostly unknown. In the present work, organic-matter-coated goethite (OMCG) colloids were percolated through three saturated soil materials differing in wettability: untreated quartz sand and two variants of hydrophobized sand. For each type of sand, three ionic strength levels were applied. Derjaguin–Landau–Verwey– Overbeek (DLVO) and Lewis acid–base extended DLVO (XDLVO) interaction energy profiles were calculated according to contact angles and zeta potentials. Flow column results elucidated that decreasing sand wettability had no relevant effect on OMCG colloid mobility. In contrast, colloid retention increased with ionic strength in each type of sand packing. Classic DLVO interactions could predict trends in colloid retention by the respective characteristics of energy barriers and secondary minima. The extension with Lewis acid–base interactions in the XDLVO approach led to the prediction of significant short-range (∼2 nm) attractive interaction energies between colloids and hydrophobized sand, which were not reflected by colloid breakthrough behavior. This was probably due to substantial energy barriers calculated for larger distances (∼27 to ∼75 nm, depending on ionic strength) between the solid matrix and colloids. It is concluded that the distinct surface roughness of sand grains and colloids probably weakened the strength of the short-range attractive interactions, because larger amounts of surface area were still outside the effective distance for the short-range interactions predicted by XDLVO. Regarding colloidal mobility, we concluded for our saturated porous systems that near-surface attractive XDLVO interaction energies between OMCG colloids and hyrophobized sand did not significantly affect colloid mobility.
AB - The influence of porous media wettability on the mobility of colloids is mostly unknown. In the present work, organic-matter-coated goethite (OMCG) colloids were percolated through three saturated soil materials differing in wettability: untreated quartz sand and two variants of hydrophobized sand. For each type of sand, three ionic strength levels were applied. Derjaguin–Landau–Verwey– Overbeek (DLVO) and Lewis acid–base extended DLVO (XDLVO) interaction energy profiles were calculated according to contact angles and zeta potentials. Flow column results elucidated that decreasing sand wettability had no relevant effect on OMCG colloid mobility. In contrast, colloid retention increased with ionic strength in each type of sand packing. Classic DLVO interactions could predict trends in colloid retention by the respective characteristics of energy barriers and secondary minima. The extension with Lewis acid–base interactions in the XDLVO approach led to the prediction of significant short-range (∼2 nm) attractive interaction energies between colloids and hydrophobized sand, which were not reflected by colloid breakthrough behavior. This was probably due to substantial energy barriers calculated for larger distances (∼27 to ∼75 nm, depending on ionic strength) between the solid matrix and colloids. It is concluded that the distinct surface roughness of sand grains and colloids probably weakened the strength of the short-range attractive interactions, because larger amounts of surface area were still outside the effective distance for the short-range interactions predicted by XDLVO. Regarding colloidal mobility, we concluded for our saturated porous systems that near-surface attractive XDLVO interaction energies between OMCG colloids and hyrophobized sand did not significantly affect colloid mobility.
UR - http://www.scopus.com/inward/record.url?scp=85053463930&partnerID=8YFLogxK
U2 - 10.2136/vzj2017.11.0203
DO - 10.2136/vzj2017.11.0203
M3 - Article
AN - SCOPUS:85053463930
VL - 17
JO - Vadose zone journal
JF - Vadose zone journal
SN - 1539-1663
IS - 1
ER -