The exploitation of unconventional gas deposits that involves the use of hydraulic fracturing has been an intensive topic of research. Hydraulic fracturing (HF) is a process that involves underground injection of a base fluid (water), a proppant (almost always sand), and various chemicals under high pressure (681 atmospheres for the Marcellus Shale, Stringfellow et al., 2014) to stimulate fractures in the rock so that gas and/or oil can flow easily to the surface, where it can be collected, exported, and processed. Used in conjunction with directional drilling (also called horizontal drilling), hydraulic fracturing has enabled previously unreachable or economically unviable deposits of oil and gas to be exploited; these deposits are more commonly referred to as unconventional oil and gas and include shale, tight formations, and coal-bed. This study focuses on the environmental impacts – specifically freshwater ecotoxicity impacts – associated with the release of chemicals present in the fracking fluid used for shale and coal-bed deposits into the atmosphere.
Although shale and coal-bed are both unconventional sources that use hydraulic fracturing, there are important distinctions in the geology that differentiates the two and govern which chemicals are required, the quantities of flowback returned, and produced water generated. For example, the Niobrara Formation (shale) has an average thickness of 240 to 330 feet, located at an average depth of 6,800 feet ranging from 3,000 to 8000 feet (Higley et al., 1995). For shale, once fracturing is completed the oil and gas begins to flow to the surface and not much is left to do at the well until site–closure. On the other hand, coal-bed occurs at shallower depths of 500 to 4100 feet (US EPA, 2004), meaning that less volume of water is required to inundate the entire volume of the borehole emanating from the well at the surface and the thickness is thinner at 10 to 140 feet (US EPA, 2004). Fracking is necessary for shale but not for coal-bed methane, although it is used in most cases. CBM might already have existing fractures, but HF aids to increase their size; shale deposits require fractures to be formed. Gas is not structurally-trapped in coal-bed, instead it is adsorbed within the coal. In CBM the fracking fluid is injected at increasingly high pressures until the coal cannot withstand the pressure. At that point, the produced water and some fracking fluid is pumped to the surface, along with the methane that sorbs out of the coal. CBM produced wet gas as a result of the large quantities of water produced in coal-bed deposits (US EPA, 2004).
The national chemical disclosure registry for hydraulically-fractured oil and gas wells in the United States, FracFocus.org, lists 15, separate chemical categories that are delineated by their chemical function. Chemicals are chosen based on their function, with some chemicals sharing multiple functions. Acids breakdown and initiate the formation of fissures in the rocks. Corrosion inhibitors prevent the pipe and casings from corroding. Biocides kill bacteria and microorganisms that can cause corrosion in the pipes. The base fluid carries all the proppant and chemicals and represents the vast majority of mass of the fluid. Breakers delay breakdown of gels at key points in the fracking process. Clay and shale stabilization and control reduce the amounts of underground clay that gets mixed into the fluid. Crosslinkers maintain the viscosity with increasing temperatures. Friction reducers reduce the friction caused by fluid transport which can increase pump strain and other damaging factors. Gels thicken the water to better suspend the proppant as it moves through the pipe. Non-emulsifiers break apart or otherwise separate the oil and water mixtures. A pH adjusting agent or buffer maintains the effectiveness of other chemicals by reducing the fluids acidity. The proppant aids in maintaining the structural integrity of the newly-formed fractures. Scale inhibitors prevent scale build-up in downhole. Surfactants reduce surface tension of the fluid to increase fluid recovery of the flowback fluid (FracFocus.org), which is the fraction of the injected fracking fluid that returns to the surface.
There is not an industrial consensus on the exact category names. In addition to the FracFocus.org categories, the US Environmental Protection Agency lists emulsifiers, foaming agents, iron control agents, resin curing agents, and solvents. Emulsifiers enable the dispersion of two immiscible fluids into one another. Foaming agents generate and stabilize foam-based fracturing fluids, which are common in coal-bed deposits. Iron precipitation is controlled by the iron controlling agent. When the temperatures downhole are too low, resin curing agents are used to lower the proppant activation temperature. Solvents controls the wetness of contact surfaces and/or they prevent or break apart emulsions (US EPA, 2015). There are some functions which work against each other because different properties are desired when the fluid is being transported underground prior to the well fracture compared to when it is returning or the well is producing.
Produced water is a term often used synonymously or confused with flowback water; indeed, many definitions exist for both terms and how the exact definitions are employed depends on the specific study, sources, agency, etc. (US EPA, 2015). Produced water is the naturally-occurring underground water that is not sourced from the injected fluid. It is impossible to differentiate between the two water streams that is emptied into the disposal pits, so for simplicity they are often lumped together and called produced water. For purposes of this paper they will be mentioned separately because the focus is on the chemicals in the fracking fluid, which entirely returns in the flowback water, but in the real world they are all part of the same water stream (American Water Works Association, 2013).
Geological formations do not adhere to geopolitical boundaries, but, fortunately, in Colorado Weld County sits on top of the largest shale formation, the Denver-Julesburg (DJ) Basin, almost exclusively. Weld County has 37% of all hydraulically-fractured wells in the state, and nearly half of all producing wells, and for this reason Weld County was chosen as the focus for the shale wells. Las Animas County sits on top of the Raton Basin, which is a coal-bed deposit with 6.5% of all wells in Colorado and was chosen as the location of the coal-bed analysis (Hamm, 2015). Much of the fracking fluid initially injected underground remains there, but the exact figures vary widely between wells and by local geology. The wells used for the assessment in Weld County were drilled into the Niobrara play, which is in the DJ Basin. Flowback volumes for the Niobrara play are approximately between 8 and 27% (US EPA, 2015) of that which is injected, averaging 17.5%; average values for the DJ Basin as a whole range between 15 and 30% (Boschee, 2014). Flowback data for coal-bed deposits is more difficult to find, and we relied on data from Puri et al. (1991) which states that 61% of the injected volume returns as flowback over a 19 day period. Most injection periods do not last long, approximately ten (Mantell, 2013; Clark et al., 2012) to fourteen (Jiang et al., 2014) days. These two values – 17.5% for Weld County and 61% for Las Animas County – were used as the specific flowback values for wells located in those respective counties throughout the assessment.
Relatively little research has been done to quantify the impacts (National Toxics Network, 2013) from the chemicals used in the hydraulic fracturing fluid due to the numerous chemicals14 employed in each well’s fracking fluid. Many fracking studies focus on the greenhouse gas emissions for the oil and gas well life-cycle, with some focusing only on methane leakage15–18. Less emphasis is on non-shale sources of unconventional fossil fuels and their comparative impacts with one another; most assessments compare a specific unconventional source of oil or gas (usually shale) with already well-researched sources of conventional oil or gas19. The Marcellus shale is the most well-researched deposit in the United States, resulting in the most available and easily accessible data than other locations. Since most data are generic, and are not specific to areas most findings have to be interpreted at a relatively macro-level for screening 20. Higher resolution impact assessments are relatively sparse due to lack of specific local data and educated assumptions required, multiple data sources, or tedious workload involved.
Even the studies1 that do focus on the chemicals, usually only assess chemicals that are already known through lists and reports put together by other organizations5,14, and most do not take empirical fluids and break them down to their constituents. In many cases, when there exists a list of chemicals, many of the chemicals have not been studied, or assessed: an Australian study found only two out of 23 of the chemicals have been researched in any detail21.
There is no standardized source that contains all the necessary property data, and they have to be collated from multiple sources22–24 and prediction models need to be used if data is not available25. A proper analysis involves finding each chemical’s applicable physio-chemical, human health, and ecotoxicity properties is a laborious process that depends on the data availability for the chemicals. If no experimental data exists, which is the case for many chemicals, the data must be predicted through modeling efforts.
The goal of this work is to devise a standardized source for all the data required to undergo chemical impact assessments and to develop, for the first time, characterization factors using USEtox that can be utilized within the existing impact assessment methodology such as TRACI26 with an aim to carry out impact assessment on any well level. This study focuses on the development of freshwater ecotoxicity characterization factors using USEtox. Further, another goal is to utilize these developed characterization factors to perform a comparative freshwater ecotoxicity assessment for fracking and coal bed methane wells.
Few studies focus on Colorado fracking operations and their impact, so the standardized methodology was applied to oil and gas wells in Weld County and coal-bed methane wells in Las Animas County to (1) generate novel categorization factors for chemicals, (2) determine the average impact per well in each county, and (3) determine which of these unconventional sources has a larger impact per unit of energy generated from an average well.