Articles | Volume 2, issue 2
SOIL, 2, 211–220, 2016
https://doi.org/10.5194/soil-2-211-2016
SOIL, 2, 211–220, 2016
https://doi.org/10.5194/soil-2-211-2016
Original research article
19 May 2016
Original research article | 19 May 2016

Synchrotron microtomographic quantification of geometrical soil pore characteristics affected by compaction

Ranjith P. Udawatta et al.

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Cited articles

Al-Raoush, R. I.: Extraction of physically-realistic pore network properties from three-dimensional synchrotron microtomography images of unconsolidated porous media, PhD Diss., Louisiana State University, Baton Rouge, LA, p. 173, 2002.
Asseng, S., Alymore, L. A. G., MacFall, J. S., Hopmans, J. W., and Gregory, P. J.: Computer-assisted tomography and magnetic resonance imaging, in: Techniques for studying roots, edited by: Smit, A. L., Bengough, A. G., Engels, C., van Noordwijk, M., Pellerin, S., and van de Geijn, S. C., Springer, Berlin, 343–363, 2000.
Assouline, S.: Modeling soil compaction under uniaxial compression, Soil Sci. Soc. Am. J., 66, 1784–1787, 2002.
Assouline, S.: Rainfall-induced soil surface sealing: a critical review of observations, conceptual models and solutions, Vadose Zone J., 3, 570–591, 2004.
Assouline, S.: Modeling the relationship between soil bulk density and water retention curve, Vadose Zone J., 5, 554–563, 2006a.
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Short summary
Soil compaction degrades soil structure and affects water, heat, and gas exchange as well as root penetration and crop production. The objective of this study was to use X-ray computed microtomography (CMT) techniques to compare differences in geometrical soil pore parameters as influenced by compaction of two different aggregate size classes.