Boron Isotope Characterization to Design a Frame of Hydrogeological Functioning of a Wetland System (Massif Central, France)
Abstract
Multi-isotopic approaches (Li, Sr, O, H), combined with hydrological tools, have been already applied for tracing the water and dissolved-element fluxes in a peatland in Central France. Here, we applied B isotopes. The 11 B ratios increase from river draining basalts (~ 0‰) up to springs bordering the peatland (> +25‰). Peatland groundwaters have intermediate 11 B: 7.8 to 19.4‰. This range is accompanied by an increase in the Ca contents between the river draining basalts and water in the peatland. In a 11 B vs. Ca/B diagram, the role of water rock interaction and present day fertilizer inputs is evidenced, as for Sr isotopes.
Domains
Earth Sciences
Origin : Publisher files allowed on an open archive