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Estimating groundwater mixing and origin in an overexploited aquifer in Guanajuato, Mexico, using stable isotopes (strontium-87, carbon-13, deuterium and oxygen-18).
- Source :
-
Isotopes in Environmental & Health Studies . Dec2007, Vol. 43 Issue 4, p323-338. 16p. 2 Charts, 5 Graphs, 3 Maps. - Publication Year :
- 2007
-
Abstract
- Stable Isotopes (strontium-87, deuterium and oxygen-18, carbon-13) have been used to reveal different sources of groundwater and mixing processes in the aquifer of the Silao-Romita Valley in the state of Guanajuato, Mexico. Calcite dissolution appeared to be the main process of strontium release leading to relatively equal 87Sr/86Sr ratios of 0.7042-0.7062 throughout the study area which could be confirmed by samples of carbonate rocks having similar Sr ratios (0.7041-0.7073). δ13C values (-11.91- -6.87‰ VPDB) of groundwaters confirmed the solution of carbonates but indicated furthermore influences of soil-CO2. Deuterium and 18O contents showed a relatively narrow range of-80.1- -70.0 ‰ VSMOW and-10.2- -8.8 ‰, VSMOW, respectively but are affected by evaporation and mixing processes. The use of δ13C together with 87Sr/86Sr revealed three possible sources: (i) carbonate-controlled waters showing generally higher Sr-concentrations, (ii) fissure waters with low-strontium contents and (iii) infiltrating water which is characterized by low δ13C and 87Sr/86Sr ratios. The third component is affected by evaporation processes taking place before and during infiltration which might be increased by extraction and reinfiltration (irrigation return flow). [ABSTRACT FROM AUTHOR]
Details
- Language :
- English
- ISSN :
- 10256016
- Volume :
- 43
- Issue :
- 4
- Database :
- Academic Search Index
- Journal :
- Isotopes in Environmental & Health Studies
- Publication Type :
- Academic Journal
- Accession number :
- 27625724
- Full Text :
- https://doi.org/10.1080/10256010701701756