The zonal soils in the
south subtropical zone of Fujian are lateritic red soils. A type of dark clayeysoils, which was
historically defined as lateritic red soils, derived from weathering products of the basalts
wasindicated by the investigation results to be markedly different from lateritic red soils and
could be classifiedas Typical Hapluderts. They are distributed as complex zones with the
lateritic red soils. The vertisolsin this region were considered as a type of lithogenic soils and
the vertic chararteristics delay and inhibitthe soils from allitic processes and then formed an
independent soil type. The vertisols have higher fertilityand better agricultural production
characters than the lateritic red soils. The different ways in utilizing andmanaging these soils
arcording to their properties and fertility are also suggested.