Composition and mineralogy of iron-manganese concretions from some soils of the Indo-Gangetic plain in Northwest India

Iron-manganese concretions from three reference soil series of the Indo-Gangetic plain of Punjab have been investigated for their composition, micromorphology and mineralogy. The data show that amounts of Fe, Mn, Co, Ni, Cu and Zn in the concretions are higher than in the surrounding soil matrix. The contents of Mn, Co and Ni increase and that of Fe decreases with the increasing size of concretions. Cu or Zn contents do not show any systematic differences with concretion size. A major portion of these elements is oxalate- and dithionite-extractable. A minor fraction is present in the silicate structure as well as in the pyrophosphate-extractable forms. The Fe and Mn compounds present in the concretions are x-ray amorphous. The concretions appear to have developed in situ.