In order to calculate the chronology of hydrothermal deposits precipitated from hot springs at Marítaro, Los Azufres geothermal field, Mexico, their
224Ra,
226Ra,
228Ra and
210Pb activities were measured. Hot springs contain large amounts of
226Ra which should be trapped in the lattice of precipitated minerals or be adsorbed on authigenic minerals. Since the time of deposition, a precise chronology can be obtained by measuring the daughter product
210Pb produced
in situ, assuming a closed system. The final goal of the study was to test whether
210Pb-
226Ra chronology could record past changes in the geothermal regime of the area. A 50-cm long sediment core was sampled but measured
226Ra,
228Ra and
210Pb activities were much lower than expected. The
226Ra activity ranges from 0.5 to 1.1 dpm/g
rock which contrast with the high
226Ra content measured in the geothermal wells and hot springs of the Los Azufres field (from 118 to 3098 dpm/g
water). This depleted content can be explained by the highly acidic conditions (pH < 3) of the Marítaro hot springs which have inhibited radium adsorption on secondary minerals. The absence of a clear trend in the
210Pb/
226Ra activity ratio with depth might indicate that the system was not completely closed in the past to the exportation of
210Pb by acid leaching or
222Rn diffusion. Given these limitations, an average age of the bulk deposit was constrained at 20-50 yrs using the measured
210Pb/
226Ra activity ratios.
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