Abstract
Samples taken from loess and paleosols were examined for carbonate content. The main results were as follows: 1) The carbonate content measured differed significantly when the samples were analysed jointly with the concretions occurring in them or separately from these constituents. 2) Solubility of different carbonates (calcite, dolomite, aragonite etc.) was found different. This factor also might have influenced the measured total amounts of carbonates.
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