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Various chemical extractions of Fe and Al from bulk soil samples, including Na-pyrophosphate (Fep, Alp), acid ammonium oxalate (Feo, Alo), and Na-dithionite (Fed, Ald), have been used over the last half century to distinguish soil ages over varying time frames from 102 to 106years and even as far into antiquity as the Oligocene (30×106) years. Problems with mineral/chemical uniformity of sediments,...
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