Method of abating carbon dioxide and hydrogen sulfide

1. A method for abatement of carbon from carbon dioxide (CO 2 ) and/or sulfur from hydrogen sulfide (H 2 S) by mineralization and precipitation in a geological reservoir comprising reactive rocks thereby mitigating the need for venting carbon dioxide (CO 2 ) and/or hydrogen sulfide (H 2 S) to the atmosphere, comprising:

pumping or transferring water from a water source into an outer pipe of an injection well, said outer pipe having an open end at a depth h1+h2, thereby creating a pressurized water stream in said outer pipe,

pumping a CO 2 and/or H 2 S rich gas into an injection pipe extending downwardly into said injection well inside said outer pipe thereby creating a CO 2 and/or H 2 S rich gas stream comprising pressurized CO 2 , and/or pressurized H 2 S, in said injection pipe;

dissolving substantially all of said pressurized CO 2 and/or H 2 S gas of said CO 2 and/or H 2 S rich gas stream in said pressurized water stream by:

merging said pressurized water stream and said CO 2 and/or H 2 S rich gas stream in said outer pipe by providing said injection pipe with an open end at a depth, h1≥0, where the hydraulic pressure of said water in said outer pipe, p(W), is lower than the pressure of said CO 2 and/or H 2 S, p(CO 2 ) and/or p(H 2 S), in said injection pipe, and

transferring said merged pressurized water and CO 2 and/or H 2 S rich gas streams from said depth h1≥0 to said open end of said outer pipe at said depth h1+h2, where (h1+h2)>h1, at a downward flow velocity, v(W), which relative to a point where the gasses are injected into the injection well, h1≥0, is as a minimum of between 0.4 m/s and 1.4 m/s and thereby ensures that for a given subpart of the water stream the hydraulic pressure of the water is larger than a sum of a partial pressure of the dissolved CO 2 and/or H 2 S after the gasses have been injected into the water and such that a drag force of the downward flowing water into the injection well is higher than an upward flow velocity of said CO 2 and/or H 2 S gas, v(CO 2 ) and/or v(H 2 S), resulting from a buoyant force on bubbles of CO 2 and/or H 2 S gas in said water stream at said depth h1+h2, said bubbles having a diameter less than 6 mm;

keeping a pH of said pressurized water stream containing said dissolved CO 2 and/or H 2 S in said outer pipe between about 2 and 4 to promote dissolution of minerals and leaching of cations from said reactive rocks; and

injecting said pressurized water stream comprising dissolved CO 2 and/or H 2 S in said outer pipe into said geological reservoir comprising said reactive rocks at the open end of said outer pipe at the depth h1+h2, or at a depth>(h1+h2)

thereby promoting dissolution of said minerals from said reactive rocks of said geological reservoir and providing said cations, necessary for carbon and sulfur mineralization and abatement of the carbon and sulfur of said dissolved carbon dioxide (CO 2 ) and/or hydrogen sulfide (H 2 S) in said geological reservoir.

2. The method according to claim 1 , wherein the geological reservoir is a geothermal reservoir.

3. The method according to claim 1 , further including increasing an interfacial area between the CO 2 and/or H 2 S to be dissolved in said water stream by fitting said injection pipe with a means for sparging at a merging point at said depth h1≥0.

4. The method according to claim 1 , wherein the pressure of said CO 2 , p(CO 2 ), at a merging point at said depth hl is between about 20-36 bar.

5. The method according to claim 4 , wherein p(CO 2 ) at the merging point at depth h1 is between about 22-34 bar.

6. The method according to claim 1 , wherein the pressure of said H 2 S, p(H 2 S), at a merging point at said depth h1 is between about 4-8 bar.

7. The method according to claim 6 , wherein p(H 2 S) at the merging point at depth h1 is between about 5-7 bar.

8. The method according to claim 1 , further comprising:

dissolving a tracer substance, in a predetermined molar ratio compared to said dissolved CO 2 and/or H 2 S, in said pressurized water stream at said depth h1≥0 in said outer pipe in said injection well,

establishing a monitoring well being interlinked to said outer pipe of said injection well via a flow path, whereby at least a part of said pressurized water mixed with said dissolved CO 2 and/or H 2 S and said tracer substance flows from said outer pipe of said injection well to said monitoring well via said flow path,

measuring a concentration of CO 2 and/or H 2 S and a tracer substance at said monitoring well and establishing based thereon a molar ratio between CO 2 and/or H 2 S and tracer substance at said monitoring well, and

determining an abatement indicator indicating a degree of CO 2 and/or H 2 S abatement based on comparing the molar ratio between CO 2 and/or H 2 S and the tracer substance at said monitoring well with said predetermined molar ratio in said pressurized water stream at said depth h1 in said outer pipe in said injection well

thereby determining to which extent said geological reservoir possesses the ability to store in mineralogical form the carbon and sulfur of said dissolved CO 2 and/or H 2S.

9. The method according to claim 1 , wherein a pH of said pressurized water stream containing said dissolved CO 2 and/or H 2 S is between about 2.5 and 3.5.