Baseflow recession analysis in a large shale play: Climate variability and anthropogenic alterations mask effects of hydraulic fracturing

• Published in: Journal of hydrology (Amsterdam) Vol. 553; pp. 160 - 171
• Main Authors: Arciniega-Esparza, Saúl, Breña-Naranjo, Jose Agustín, Hernández-Espriú, Antonio, Pedrozo-Acuña, Adrián, Scanlon, Bridget R, Nicot, Jean Philippe, Young, Michael H., Wolaver, Brad D., Alcocer-Yamanaka, Victor Hugo
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.10.2017
• Subjects: Baseflow recessions; Drought; Hydraulic fracturing; Texas; Drought; Baseflow recessions; Texas; Hydraulic fracturing
• ISSN: 0022-1694; 1879-2707
• DOI: 10.1016/j.jhydrol.2017.07.059

•We analyze the impacts on baseflow patterns across the Eagle Ford shale play (Texas, USA).•Substantial decline in baseflow components during intensive fracking is observed.•In addition to water use for food and energy, droughts can enhance such decline. Water resources development and landscape alteration exert marked impacts on water-cycle dynamics, including areas subjected to hydraulic fracturing (HF) for exploitation of unconventional oil and gas resources found in shale or tight sandstones. Here we apply a conceptual framework for linking baseflow analysis to changes in water demands from different sectors (e.g. oil/gas extraction, irrigation, and municipal consumption) and climatic variability in the semiarid Eagle Ford play in Texas, USA. We hypothesize that, in water-limited regions, baseflow (Qb) changes are partly due (along with climate variability) to groundwater abstraction. For a more realistic assessment, the analysis was conducted in two different sets of unregulated catchments, located outside and inside the Eagle Ford play. Three periods were considered in the analysis related to HF activities: pre-development (1980–2000), moderate (2001–2008) and intensive (2009–2015) periods. Results indicate that in the Eagle Ford play region, temporal changes in baseflow cannot be directly related to the increase in hydraulic fracturing. Instead, substantial baseflow declines during the intensive period of hydraulic fracturing represent the aggregated effects from the combination of: (1) a historical exceptional drought during 2011–2012; (2) increased groundwater-based irrigation; and (3) an intensive hydraulic fracturing activity.