
The approach to describing thin sections depends on the purpose of the study. There are two main approaches:
Thin section descriptions should begin with an examination of the section with the naked eye (1X magnification). Use a light talbe or hold the section up to a light source to help identify major pedological feature. Homogeneous zones can then be identified which will be examined separately under the microscope. Alternatively, it is sometimes useful to examine the block from which the thin section was obtained to see if there were any areas that were not impregnated or to examine the macrostructure. If the impregnating solution contains a dye, the macropore structure is often better illustrated on the polished block. At this stage it is sometimes useful to study the field description to see if items noted earlier can be seen in the thin section. If features observed in the field ar not present in the thin section, the thin section may not be representative of the soil material. Some micromorphologists even complete a macrmorphological description of the thin section first. This approach helps bridge the gap between the field relationships and micromorphology.
Prior to starting to describe the thin section under the microscope, it is useful to first scan the entire section using different magnifications to see the variation in microstructure, groundmass, and pedofeatures that are present. When soil profiles have been sampled, it is also useful to quickly scan the thin sections from adjacent horizons to gain an overall view of the material.
Begin the examination o fthe slide under the petrographic
microscope with the lowest power available. On most scopes this
will be 20-25X magnification. Use crossed and uncrossed
polarized light to identify major feature. Within each major
feature, use increased magnification to identify additional
detail. Fitz Patrick (1993) lists the summary stages for
describing a thin section as follows:
1. 20-25X magnification in plane, crossed and circular polarized light.
2.100X magnification in plane, crossed and circular polarized light.
Mineral material Matrix Structure and pores Coatings and other surface features Weathering features Segregations, concretions, nodules and concentrations Particle size distribution Rock types Other features Organic matter Roots Microorganisms Fanual features
This page (http://www.ces.ncsu.edu/plymouth/programs/descript.html) created by
Vera MacConnell, Research Technician, I on December 1, 1997.
Last Updated on December 12, 1997.