Hydrochemical applications of the analysis of repeated measurements

Abstract

Results corresponding to coincidence and proportionality (by dilution or different contact time with rocks) and not by proportionality of samples, based on determined parameters, are presented. Further applications of the method to the last samples, excluding some parameters to get proportional contents for the rest of the constituents, are included for cases where the lack of proportionality is attributed to the con tact with more than one type or rock or to the occurrence ot a cationic exchange process.

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