%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Bergonzini, L.
%A Delalande-Le Mouellic, M.
%A Gherardi, F.
%A Mathe, P. E.
%A Majule, A.
%A Williamson, David
%T Evidence of a water delta O-18 negative shift driven by intensive deep CO2 upflow at Shiwaga gas field (Rungwe, Tanzania)
%D 2018
%L fdi:010073230
%G ENG
%J Environmental Earth Sciences
%@ 1866-6280
%K Gas field ; Stable isotope hydrology ; CO2-H2O interaction ; Water O-18 ; shift ; East African Rift
%K TANZANIE ; SHIWAGA VALLEE
%M ISI:000437228200006
%N 13
%P art. 497 [9 ]
%R 10.1007/s12665-018-7665-2
%U https://www.documentation.ird.fr/hor/fdi:010073230
%> https://www.documentation.ird.fr/intranet/publi/2018/07/010073230.pdf
%V 77
%W Horizon (IRD)
%X Located on the flank of Ngozi volcanoes (Tanzania), the Shiwaga gas field is a spot of intense CO2(g) emanations. Physico-chemical measurements on different types of waters (rivers, puddles, and springs) as water and gas sampling were discontinuously performed over 10 years for equilibrated partial CO2 pressure calculations and stable isotopic analyses. The most striking result shows that meteoric H2O and deep originated CO2(g) exchanges are responsible for a negative O-18-shift of the studied waters in relation with waters electrical conductivity, pH, and pCO(2)eq changes. In spring waters, a maximum shift of - 11.2aEuro degrees in delta O-18 was observed and pCO(2)eq values up to 1196 mbar were computed. Although this trend has already been reported around the world, such extended shift is rarely measured and requires an important amount of CO2(g), with a CO2(g)/H2O ratio up more than 0.5 mol/mol. This approach is useful to better understand the hydro-geochemical processes involved in such environments. Moreover, this study evidences that an inventory as a monitoring of these gas fields are needed for the management of natural hazards and local resources.
%$ 062