Page 65 - E-BOOK English
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Haplic Ferralsols
Haplic Ferralsols have a typical expression
of certain.
Tha Mai series (Ti) is a representative of
Haplic Ferralsols. Tha Mai soils are formed from basalt
and occurred on basalt terrain dominated in the east.
Relief is gently undulating to undulating. Slope ranges
from 2-12 percent. Drainage is well drained,
permeability is moderate to slow and surface runoff
is rapid. They are very deep soils and characterized
by a dark reddish brown clay surface or A horizon
overlying a dark reddish brown or reddish brown silty
clay or clay oxic B horizon. Soil pH is a moderately
acid to neutral (pH 6.0-7.0) at the surface layer and a
very strongly acid to strongly acid (pH 4.5-5.5) in the
subsoil. Land use limitation are low fertility and lack
of water supply for crop production.
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