Difference between revisions of "Soils of the North and South"
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Revision as of 06:35, 16 January 2008
Geographical Regions
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Soils of the North and South. Soil Samples in Jars.
Left: the rich loam of the alluvial deposits of the central Green Mountains. This is a representative sample of Northern soil—brown in color.
On the right: a sample of soil from a Central Tennessee roadbed (Cannon County, 1998). This soil contains a substantial amount of iron oxide, a geological mix characteristic of the American South. This a rich, terra-cotta red soil pigmentation is prevalent in a wide swath from Virginia to Oklahoma and from Florida to Texas.
The major chemical components of soil are: sand (chemically silicon dioxide {SiO2} or quartz); clay (often used by chemists to denote hydrated silicate of alumina (Al2O3•2SiO2•2H2O); chalk (CaCo3); and humus, decaying vegetable and animal matter (peat is probably the least nasty smelling of this category).
These two types of distinct soil colors are caused by oxidization, one of the major categories of study in which the Museum is immersed. The bonding of oxygen to other molecules is not only one of the most characteristic functions of all living organisms, but it is the chief means of the decay and even of the entropy of the same.
To those who have traveled widely in the United States they are as representative of the two regions of the country as the Blue and Grey of Civil War uniforms.
