Since many of the phenomena occurring in soil are related to grain and pore
sizes and their distribution, investigation on a micrometric scale is of g
reat importance. Also, the investigation should be non-invasive in order to
avoid disturbing the region of interest of the sample. Many techniques fro
m various areas of science have been adapted to make such investigations, b
ut most of them are invasive or can only analyze global soil properties. Th
us an X-ray tomograph was developed at Embrapa-Agricultural Instrumentation
, to scan images of soil samples on a micrometric scale. A microtomographic
image of a sieved soil sample, presenting aggregates from 212 mu m to 150
mu m and pores of 100 mu m, is shown. Pores of the same size can also be se
en in a microtomograph of a sand column, composed of two layers with granul
ometries of 106 mu m to 149 mu m and 297 mu m to 500 mu m. A microtomograph
of a column composed of three layers of an orthoclasius powder is also pre
sented. A slight variation in density along the column height can be observ
ed. (C) 1999 Elsevier Science S.A. All rights reserved.