Method for carbon dioxide storage utilizing carbon dioxide sequestration in an anhydrite-rich formation
AssigneeKing Fahd University of Petroleum and Minerals
InventorsIsah Mohammed, Dhafer Abdullah Al Shehri, Abubakar Isah, Mohamed Mahmoud
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Abstract
A method for carbon dioxide (CO2) storage includes injecting a brine solution into a subterranean anhydrite-rich formation, then injecting carbon dioxide into the subterranean anhydrite-rich formation and reacting the carbon dioxide with the subterranean anhydrite-rich formation to form one or more minerals thereby sequestering the carbon dioxide in the subterranean anhydrite-rich formation. The temperature in the subterranean anhydrite-rich formation is from 300 Kelvin (K) to 365 K and the pressure in the subterranean anhydrite-rich formation is from 90 bar to 120 bar.
Claims20
A method of carbon dioxide storage, comprising:
- injecting a brine solution into a subterranean anhydrite-rich formation, wherein the subterranean anhydrite-rich formation is anhydrous and free of hydrocarbons;
- injecting carbon dioxide into the subterranean anhydrite-rich formation;
- reacting the carbon dioxide with the subterranean anhydrite-rich formation in the presence of the brine solution to form one or more minerals thereby sequestering the carbon dioxide in the subterranean anhydrite-rich formation,
- wherein a temperature in the subterranean anhydrite-rich formation is from 300 to 365 K,
- wherein a pressure in the subterranean anhydrite-rich formation is from 90 to 120 bar,
- wherein the brine solution comprises sodium chloride, calcium chloride, magnesium chloride, sodium bicarbonate, and sodium sulfate,
- wherein the brine solution comprises ionic concentrations of Na+ in a range from 5,000 to 50,000 parts per million (ppm), Ca2+ in a range from 100 to 1,500 ppm, Mg2+ in a range from 500 to 5,000 ppm, SO42− in a range from 1,000-9,000 ppm, Cl− in a range from 10,000-70,000 ppm, and HCO3− in a range from 10-500 ppm, and
- wherein a mineral content of the subterranean anhydrite-rich formation after the reacting comprises 80 to 90 weight percent (wt. %) anhydrite, 1 to 5 wt. % calcite, 5 to 10 wt. % dolomite, 1 to 5 wt. % scapolite, 0.1 to 1 wt. % quartz;
- 0.1 to 1 wt. % feldspar, and 0.1 to 1 wt. % siderite.
Dependencies are inferred from the claim text.