PRODUCED WATER GEOCHEMICAL CHARACTERIZATION FROM A MARCELLUS-SHALE NATURAL GAS WELL RESEARCH SITE
Typical of Marcellus shale-gas wells, total dissolved salt concentrations increased steadily after going into production, reaching 115 grams/L after 30 weeks in production. Organics identified in the wastewater include polycyclic aromatic hydrocarbons, glycol ethers, alkanes, and tertiary and quaternary amines, with glycol ether persisting in the transition from flowback to formation water. Major ions included sodium, calcium, and chloride, with maximum concentrations of 1.3, 0.2, and 1.7 moles/L (M). Lithium, potassium, magnesium, strontium, barium, boron, and bromide were present at concentrations > 1 millimole/L (mM); the relative proportions of these solutes varied by no more than a factor of two. Radium activities increased with time in proportion with these solutes, with 226Ra reaching a maximum of 250 Becquerel/L; 226Ra/228Ra ratios were in the range 10-15. Alkalinity, iron, sulfur, and total dissolved ammonium (NH4T) were present at concentrations exceeding 1 mM, but their proportions were more highly variable.
The composition of wastewater from the storage tank was relatively constant, with compositions near the maximum concentrations observed in water from the separator, although pH was more variable (~3.7 to 7.2). The high dissolved salt and NH4T concentrations pose the greatest threat to aquatic ecosystems impacted by wastewater spills; Ra likely poses the greatest threat to humans.