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By MacColl L. A.

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Madison, WI: Soil Science Society of America, 1985. Soil Survey Staff. Soil Taxonomy: A Basic System of Soil Classification for Making and Interpreting Soil Surveys. S. Government Printing Office. 1975. REFERENCES 1. gov/gallery/state_soils/. 2. cgi?. 3. ). Soil Color. Madison, WI: Soil Science Society of America, 1993. CHAPTER 2 SOIL BASICS II MICROSCOPIC TO ATOMIC ORBITAL DESCRIPTION SOIL CHEMICAL CHARACTERISTICS OF In this chapter soil components will first be considered as individual independent, noninteracting entities.

Because the particles are smaller, they have a larger surface area, that is, more surface per unit mass. This results in the availability of a greater number of bonds for chemical reactions. However, again, although the amount of surface area can be measured, the availability of silicon, oxygen lone pairs of electrons, and hydroxy groups for chemical reaction cannot be known exactly [1]. 3. 002 mm in diameter. They are significantly different from sand and silt separates both physically 26 soil basics ii and chemically.

For silicon, aluminum as Al3+ and iron as Fe3+ will fit without causing too much distortion of the clay structure. 3). The two 2 : 1 clay types are distinguished by the type of substitution in the layers. Nonexpanding fine grained mica-type clay has isomorphous substitution of Al3+ in the silicon tetrahedral sheet. Thus, in a tetrahedral sheet of fine mica, aluminum may be substituted for a silicon atom. 3. Two types of isomorphous substitution. The middle structure is a two-dimensional representations of clay without isomorphous substitution.

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