Page 28 - World Reference Base for Soil Resources of Thailand
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Land Development Department Library
The representatives of Acrisols in Thailand
Gleyic Acrisols
Gleyic Acrisols have gleyic properties, a layer
of ≥ 25 cm thick and start at the depth of ≤40 cm
from the mineral surface. Besides, these soils have
reducing conditions in some parts of every sublayer.
Buntharik series (Bt) is a representative of
Gleyic Acrisols. Buntharik soils are formed from
a washed deposit of sandstone and occur on
coalescing colluvial and alluvial fans. Relief is
flat to undulating which slopes range from 0-5
percent. Drainage is moderately well in topsoil
and poor in the subsoil. They are deep soils and
are characterized by a very dark grayish brown or
grayish-brown loamy sand or sandy loam A horizon
overlying a light gray or very pale brown loamy sand
or sandy loam, which in turn overlies a light brownish
gray or very pale brown sandy clay loam or sandy
clay with common to many prominent red mottles
in argillic B horizons. Scattered weathering sandstone
fragments occur at some depth below 100 cm from
the surface soil. Soil pH is very strongly acid to
moderately acid (pH 4.5-6.0). These soils have low
fertility that should be improved by applications of
chemical fertilizers, manure, organic fertilizers. Besides,
farm pond is needed for agricultural water supply.
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