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- W2022509495 abstract "The iron oxide mineralogy of soils of two river terrace sequences of the rivers Jarama and Henares, Central Spain, which are in close proximity, was studied. The degree of weathering increases with age, as shown by several mineralogical and geochemical indicators, such as the increase in the ratio dithionite extractable (free) Fe / total Fe. Low values for oxalate extractable Fe indicate that the Fe oxides are essentially crystalline. In the Jarama sequence goethite is the dominant pedogenic Fe oxide. In the Henares sequence both goethite and hematite are present in significant amounts. The difference is attributed to pedoenvironmental differences, such as the lower pH and the moister pedoclimate of the Jarama sequence soils. The sensitivity of the goethite-hematite system to pedoenvironmental factors shows the limited value of iron oxides for the estimation of paleoclimatic conditions or relative age in chronosequences, even in relatively small geographical areas." @default.
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- W2022509495 date "1989-06-01" @default.
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- W2022509495 title "Mineralogy of iron oxides in two soil chronosequences of Central Spain" @default.
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- W2022509495 doi "https://doi.org/10.1016/0341-8162(89)90015-5" @default.
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