Articles | Volume 18, issue 12
Hydrol. Earth Syst. Sci., 18, 5255–5269, 2014
https://doi.org/10.5194/hess-18-5255-2014
Hydrol. Earth Syst. Sci., 18, 5255–5269, 2014
https://doi.org/10.5194/hess-18-5255-2014

Research article 16 Dec 2014

Research article | 16 Dec 2014

Relations between macropore network characteristics and the degree of preferential solute transport

M. Larsbo et al.

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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (Editor review) (13 Oct 2014) by Mauro Giudici
AR by Mats Larsbo on behalf of the Authors (20 Oct 2014)  Author's response    Manuscript
ED: Publish subject to minor revisions (Editor review) (29 Oct 2014) by Mauro Giudici
AR by Mats Larsbo on behalf of the Authors (03 Nov 2014)  Author's response    Manuscript
ED: Publish subject to technical corrections (05 Nov 2014) by Mauro Giudici
AR by Mats Larsbo on behalf of the Authors (07 Nov 2014)  Author's response    Manuscript
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Short summary
The characteristics of the macropore network determine the potential for fast transport of solutes through soil. Such characteristics computed from 3-dimensional X-ray tomography images were combined with measured solute breakthrough curves and near-saturated hydraulic conductivities. At a given flow rate, smaller macroporosities, poorer local connectivity of the macropore network and smaller near-saturated hydraulic conductivities resulted in a greater degree of preferential transport.