Testing the usefulness of 222Rn to complement conventional hydrochemical data to trace groundwater provenance in complex multi-layered aquifers. Application to the Úbeda aquifer system (Jaén, SE Spain)

Author:

Ortega L.ORCID,Manzano M.,Rodríguez-Arévalo J.

Funder

Spanish Ministry of Science and Innovation

Publisher

Elsevier BV

Subject

Pollution,Waste Management and Disposal,Environmental Chemistry,Environmental Engineering

Reference48 articles.

1. Chemical and isotopic (δ18O‰, δ2H‰, δ13C‰, 222Rn) multi-tracing for groundwater conceptual model of carbonate aquifer (Gran Sasso INFN underground laboratory – central Italy);Adinolfi Falcone;J. Hydrol.,2008

2. Mechanism of radon release in rock matrices and into groundwaters;Andrews;Trans. Inst. Min. Metall. Sec.,1972

3. The Los Pedroches Batholith (Sern Spain): polyphase interplay between shear zones in transtension and setting of granites;Aranguren;Petrol. Struct. Geol.,1997

4. Geochemical significance of aquitards;Back,1985

5. Radon: A Tracer for Geological;Baskaran,2016

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