CO2 Brine Database

General Information
Geologic Parameters
1 Depth to Top:
2 Permeability/Hydraulic Conductivity:
3 Formation Thickness:
4 Net Sand Thickness:
5 Percent Shale:
6 Continuity:
7 Top Seal Thickness:
8 Continuity of top seal:
9 Hydrocarbon Production:
10 Fluid Residence Time:
11 Flow Direction Elevation:
12 CO₂ Solubility Brine	12a Temperature:
	12b Pressure:
	12c Salinity:
13 Rock/Water Reaction:
14 Rock Porosity:
15 Water Chemistry:
16 Rock Mineralogy:

Glen Canyon Group, Sevier Basin and Kaiparowitz Bench

Comments on Geologic Parameters

13 Rock/Water Reaction:

Some data on rock/water reaction were provided by Freethey and Cordy (1991), but the emphasis of their research is on ground-water chemistry. Potential for mineral interaction with high-CO2 brines is low in these mature sandstones.

13 Reference:

Freethey, G. W., and Cordy, G. E., 1991, Geohydrology of Mesozoic rocks in the Upper Colorado River Basin-excluding the San Juan Basin-in Arizona, Colorado, New Mexico, Utah, and Wyoming: U.S. Geological Survey, Professional Paper 1411-C, 118 p.