Abstract
The spatial distribution of porosity and continuity of pore space in glass bead and soil aggregate systems has been characterised by application of computer-assisted tomography to gamma-ray attenuation measurements. It has been demonstrated that a useful empirical relationship between hydraulic conductivity and pore size and continuity for the glass bead system as measured by CAT scanning can be derived.
Original language | English |
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Pages (from-to) | 671-678 |
Journal | Australian Journal of Soil Research |
Volume | 34 |
DOIs | |
Publication status | Published - 1996 |