Illuviation in a sandy loam texture horizon
4Ct Horizon from a calcic cutanic Luvisol. Thin section C7-7.
Micromorphological features
After browsing these images you should have found, at least, the following characteristics
Sands of: C, quartz; Fk, K-rich feldspar (orthoclase); Mc, microcline; Pl, plagioclase; M, moscovite; Q, quartzite. Gravels of: gQ, quartzite. p, voids; A, clay cotings (clay films). Left side image only with poloarizer, the one on the right side with crossed nicols. |
Imperfections of these thin sections
Obtaining thin sections from such a heterogeneous material (the soil), is a very complex and arduos task; thus, microscopic preparations usually include some imperfections, just as in the examples below, that must be recognized so that they are not confused with soil features.
The anisotropy of the inclusion resin of this thin section appears after a series of irregularities situated preferably over the mineral grains. | ||
In some cases, the mineral grains can detach while sanding and smoothing down the thin section, thus, exihibiting a large relief. |
Soil data
Morphology, phisical and chemical analysis
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This soil was studied by Pilar Alonso Rojo in her PhD Thesis "Cronosecuencias de suelos en la cuenca del rio Tormes". Salamanca. 1989.