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Clay content in the A horizon (0-30 cm) is 37 percent. The Kandic (Bt) horizon extends from 30 cm to the bottom of the pit has a clay content of 57 percent, an apparent CEC7 of 4.6 cmols kg-1 clay and a CEC8.2 base saturation of 25 percent. Well drained
Ultisols with a high content of organic carbon in the surface horizons (Humults) are most common in areas that may have been subjected to occasional dusting with volcanic ash. The decomposition of the ash may be responsible for coating and preserving the organic carbon. (Tape is marked in 5 cm squares)
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