2014
DOI: 10.1021/es404050r
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Source and Fate of Hydraulic Fracturing Water in the Barnett Shale: A Historical Perspective

Abstract: Considerable controversy continues about water availability for and potential impacts of hydraulic fracturing (HF) of hydrocarbon assets on water resources. Our objective was to quantify HF water volume in terms of source, reuse, and disposal, using the Barnett Shale in Texas as a case study. Data were obtained from commercial and state databases, river authorities, groundwater conservation districts, and operators. Cumulative water use from ∼ 18,000 (mostly horizontal) wells since 1981 through 2012 totaled ∼ … Show more

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Cited by 190 publications
(108 citation statements)
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“…The solid line is the fitted model (Eqs. (1) and (3)) to determine slip length (b). All experiments were carried out at room temperature (296 K).…”
Section: Afm Metrology To Measure Slip Lengthmentioning
confidence: 99%
See 2 more Smart Citations
“…The solid line is the fitted model (Eqs. (1) and (3)) to determine slip length (b). All experiments were carried out at room temperature (296 K).…”
Section: Afm Metrology To Measure Slip Lengthmentioning
confidence: 99%
“…Fluid losses of as much http://dx.doi.org/10.1016/j.fuel.2015.08.017 0016-2361/Ó 2015 Elsevier Ltd. All rights reserved. as 90% have been reported in shale strata [1,2]. Major loss of injected hydraulic fracture fluid in shale raises important technical, economical, and environmental concerns [3,4].…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…The initial rate at which produced water flows to the surface (e.g. within the first 10 days) also influences the viability of reuse as low initial produced water volume flow rates making the logistics of reuse more difficult [3,5].…”
Section: Introductionmentioning
confidence: 99%
“…vibrations and seismic tremors that may affect the existing infrastructure and stability of morphological elements), − grounds and soils and their mechanical properties, organic matter content and biophilic substances and potential contamination, − surface waters and groundwater, taking into account hazards related to excessive depletion of available resources and deterioration of water condition, consequently the contamination with substances from the surface or migrating with technological and reservoir fluids from the geological formations and possible aftermath of such changes to water-dependent ecosystems ( Table 1). Field works were preceeded by a detailed analysis of geological and hydrogeological conditions of particular research areas, taking into account the degree of confinement of potential reservoir rocks and identification of possible migration pathways of technological and reservoir fluids to usable/fresh groundwater horizons and land surface [18,[25][26][27]. The full cycle of research has been conducted in following sequences: 1. identification of the local conditions and field studies planning, 2. examination of the baseline status of the environment prior to the commencement of exploration, 3. studies while drilling vertical/directional wells, 4. studies during hydraulic fracture stimulation and gas flow testing, 5. examination of the status of the environment on completion of drill site operations, 6. monitoring of the status of the environment after the completion of downhole operations.…”
Section: Introductionmentioning
confidence: 99%