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The iron oxide mineralogy of three soils from the Ha'apai Group (c. latitude 19°50¿S., longitude 174°30' W.), Kingdom of Tonga, has been investigated. The Group consists mainly of an archipelago of low coral atolls. Soils are formed in the andesitic tephra which overlie the coral. Accessions of marine salts are high and give rise to high soil pH values (7) and high concentrations of exchangeable cations. The soils are dark reddish brown to reddish brown in colour, with limited colour differentiation with soil depth, and they are not hqdromorphic. The results of study of whole soils and size fractions by chemical extraction, X-ray diffraction, differential thermal analysis, Moessbauer spectroscopy, and by measurement of variation of magnetic attraction following heating to various temperatures, lead to the following conclusions: iron oxide minerals comprise 7-12% by weight of the soils; the predominant clay size iron oxide is very poorly crystalline aluminium-substituted lepidocrocite (ã-Fe 0.8Al 0.2,OOH); ferrihydrite is probably also present in the clay fraction; lepidocrocite and ferrihydrite together account for 50-60% of the total iron in the soils studied; magnetite, probably partially oxidized towards maghemite, is present, particularly in sand and silt fractions, and accounts for about 10% of the total iron in the soils. The remainder of the total iron occurs in unweathered minerals in the silt and sand fractions and in the structure of halloysite in the clay fraction. The common soil iron oxides, goethite and hematite, have not been detected. Although the occurrence of lepidocrocite is usually linked with hydromorphic soil conditions, this report, along with others, suggest that it is also found under non-hydromorphic conditions.
Childs et al. (Thu,) studied this question.