@Article{Lima_etal2023,
author="Lima, G. F. C.
and Filho, C. A. de C.
and Ferreira, V. G.
and Lima, J. da S. D.
and Marques, E. D.
and Minardi, P. S. P.
and Dalm{\'a}zio, I.
and Moreira, R. M.",
title="Establishing a water baseline for the unconventional gas industry: A multiple environmental isotopes assessment (18O, 2H, 3H, 13C, and 14C) of surface and groundwater in the S{\~a}o Francisco Basin, Brazil",
journal="Applied Geochemistry",
year="2023",
volume="159",
pages="105818",
optkeywords="Fracking",
optkeywords="Groundwater dating",
optkeywords="Indai{\'a} river",
optkeywords="Isotopes assessment",
optkeywords="Shale gas",
optkeywords="Unconventional hydrocarbons",
abstract="Unconventional hydrocarbon production has become the target of an intensive environmental debate due to the risks it poses to water resources. Fracking, while enabling the extraction of oil and gas from ultra-low permeability reservoirs, also possesses the risk of polluting water systems through failures from hydraulic fracturing and its associated procedures. The need to foster national industrial development with a transitional energy matrix has led Brazil to discuss the environmental suitability before producing its large unconventional reserves. Many studies have highlighted the need for a robust environmental characterization before the development of the unconventional industry. In this sense, multiple environmental isotopes may work as a proxy for identifying water contamination right from the early stages. Environmental isotopes may also be applied to enhance the understanding of the natural geochemical processes intrinsic to a given area. This study presents an environmental isotopes baseline for the groundwater and riverine water systems within the S{\~a}o Francisco Basin, a proven tight gas reservoir in Brazil, in a pre-operational context. $\delta$18O, $\delta$2H, 3H, $\delta$13C, and $\Delta$14C were evaluated in three different seasons in groundwater and surface water samples, along with other auxiliary parameters such as physical-chemical parameters (in situ), major ions, and d-excess. The $\delta$2H and $\delta$18O in surface water shows an upstream {\textrightarrow} downstream enrichment trend, with some variations suggesting baseflow interactions in the surface water systems. An evaporation line for the study area was defined as $\delta$2H = 4.6903 $\delta$18O + 10.362. $\delta$13C indicates a mutual dissolution of silicates and carbonates in the groundwater system and suggests a group of samples highly related to the recharge areas. Groundwater dating denotes the Serra da Saudade Formation as a modern fractured aquifer with a strong recharge capacity. These findings support stakeholders in environmental monitoring and management of the unconventional gas industry.",
optnote="exported from refbase (http://www.uhydro.de/base/show.php?record=173), last updated on Fri, 26 Jan 2024 13:19:04 +0100",
issn="0883-2927",
opturl="https://www.sciencedirect.com/science/article/pii/S0883292723002639"
}