Page 116 - E-BOOK English
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Haplic Luvisols







                     Haplic Luvisols have a typical expres- runoff is slow to moderate. They are very deep

            sion of certain features and only used if none  and  characterized by a brown or dark brown
            of the preceding qualifiers applies.             silt loam or loam A horizon, overlying a brown

                     Kamphaeng Saen series (Ks) is a         or strong brown silt loam, silty clay loam or

            representative of Haplic Luvisols. Kamphaeng     loam argillic B horizon and sandy loam or loamy
            Saen soils are formed from alluvium and          sand texture may occur in the lower part of the

            occur on coalescing fan or old levees and        B horizon within 150 cm. Soil pH is neutral to
            breach deposits of the terrace. Relief is flat to    moderately alkaline (pH 7.0-8.0). All horizons

            undulating. Slopes are 1-5 percent.              contain abundant mica flakes. Intensive farming
            These soils occupy large extent  in the          is used in most areas of this soil. However, a

            southwestern part of the Central Plain. Drainage   consistent water supply and fertility management
            is well drained. Permeability is moderate and    are required to obtain higher yield.


















































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