Soils 205- General Soils
Lecture 3- Soil Color
I. Causes of soil color
a. organic matter-

b. Primary minerals, CaCO3, salts, unweathered volcanic ash-
c. Ferric iron (Fe+3) -

d. Ferrous iron (Fe+2) - greenish/blue = gleyed colors
II. Description of soil color
a. Soil color is described using the Munsell color system. There are three parts to the complete color designation; the hue, value, and chroma.
i. Hue defines the dominant spectral color
ii. Value indicates the lightness or darkness of a color
iii. Chroma is a measure of the brightness or intensity of a color
The hue, value, and chroma can each be
found on the pages of a Munsell color book.
When describing soil color, soil is held up to and matched with a chip in the Munsell color book. The color is given an alpha-numerical value and a written name. For example, if a soil color matches the chip circled below, the color would have a hue of 10YR (from the upper rt. hand corner of the page), a value of 4 (left side of page), and a chroma of 2 (bottom of page). The Munsell designation is always written in the format of hue value/chroma. On the page facing the color chips (not shown) in the Munsell book, the written name of the color will be given. For example, 10YR 4/2 is dark brown.
