Monitoring of CO2 storage in a depleted natural gas reservoir: Gas geochemistry from the CO2CRC Otway Project, Australia

被引:72
作者
Boreham, Chris [1 ,2 ]
Underschultz, Jim [2 ,3 ]
Stalker, Linda [2 ,3 ]
Kirste, Dirk [2 ,4 ]
Freifeld, Barry [5 ]
Jenkins, Charles [2 ,6 ]
Ennis-King, Jonathan [2 ,7 ]
机构
[1] Geosci Australia, Canberra, ACT 2601, Australia
[2] CO2CRC, Canberra, ACT 2601, Australia
[3] CSIRO Earth Sci & Resource Engn, Bentley, WA 6102, Australia
[4] Simon Fraser Univ, Dept Earth Sci, Burnaby, BC V5A 1S6, Canada
[5] Univ Calif Berkeley, Lawrence Berkeley Lab, Berkeley, CA 94720 USA
[6] CSIRO Earth Sci & Resource Engn, Canberra, ACT 2601, Australia
[7] CSIRO Earth Sci & Resource Engn, Clayton, Vic 3169, Australia
关键词
Otway Basin; Carbon dioxide; Methane; Geosequestration; Depleted natural gas reservoir; Gas geochemistry; Carbon isotopes; Tracers; Waxy hydrocarbons; Monitoring; ISOTOPIC FRACTIONATION; SITE; HYDROCARBONS; TEMPERATURE; PREDICTIONS; INJECTION; SYSTEMS; WATER; H2S;
D O I
10.1016/j.ijggc.2011.03.011
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The CO2CRC Otway Project in southwestern Victoria, Australia has injected over 17 months 65,445 tonnes of a mixed CO2-CH4 fluid into the water leg of a depleted natural gas reservoir at a depth of similar to 2 km. Pressurized sub-surface fluids were collected from the Naylor-1 observation well using a tri-level U-tube sampling system located near the crest of the fault-bounded anticlinal trap, 300 m up-dip of the CRC-1 gas injection well. Relative to the pre-injection gas-water contact (GWC), only the shallowest U-tube initially accessed the residual methane gas cap. The pre-injection gas cap at Naylor-1 contains CO2 at 1.5 mol% compared to 75.4 mol% for the injected gas from the Buttress-1 supply well and its CO2 is depleted in C-13 by 4.5 parts per thousand VPDB compared to the injected supercritical CO2. Additional assurance of the arrival of injected gas at the observation well is provided by the use of the added tracer compounds, CD4, Kr and SF6 in the injected gas stream. The initial breakthrough of the migrating dissolved CO2 front occurs between 100 and 121 days after CO2 injection began, as evidenced by positive responses of both the natural and artificial tracers at the middle U-tube, located an average 2.3 m below the pre-injection GWC. The major CO2 increase to similar to 60 mol% and transition from sampling formation water with dissolved gas to sampling free gas occurred several weeks after the initial breakthrough. After another similar to 3 months the CO2 content in the lowest U-tube, a further average 4.5 m deeper, increased to similar to 60 mol%, similarly accompanied by a transition to sampling predominantly gases. Around this time, the CO2 content of the upper U-tube, located in the gas cap and an average 10.4 m above the pre-injection GWC, increased to similar to 20 mol%. Subsequently, the CO2 content in the upper U-tube approaches 30 mol% while the lower two U-tubes show a gradual decrease in CO2 to similar to 48 mol%, resulting from mixing of injected and indigenous fluids and partitioning between dissolved and free gas phases. Lessons learnt from the CO2CRC Otway Project have enabled us to better anticipate the challenges for rapid deployment of carbon storage in a commercial environment at much larger scales. Crown Copyright (C) 2011 Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:1039 / 1054
页数:16
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