Conclusions

• Hunton aquifer

  • Upper Middle Devonian
  • Lower Middle Devonian
  • Silurian Reefs

• TDS distribution observed correlates well with the 10,000 ppm line proposed by Schnoebelen et al (1995)

• ~1 TCF of net pore volume is available in the Hunton aquifer for CO2 sequestration in the study area

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