The present article deals with a description about the micromorphological features on the soil fabric of the paddy soils (known as Baity or white soil).They occur in areas of Hefei,Anhwei province.The study of 3μ thin-sections of undisturbed soil horizon indicated that the classification of the fabric of the soil according to its arrangement of the mineral grains and the matrix may be in general divided into two parts,e.i.,aggregative and reparative.However,it was found that the strongly and continuously arranged particle-chains (0.7-0.9μ) were the basic structure of the fabric.Microchemical investigations also showed that the downward movement of clay is associated with the eluviation of the.iron materials in the upper part of soil profile.