首页> 外文会议>NATO Advanced Research Workshop on Advances in CO2 Geological Sequestration in Eastern and Western European, Countries >STRONTIUM ISOTOPE (~(87)SR/~(86)SR) CHEMISTRY IN PRODUCED OIL FIELD WATERS: THE IE A CO_2 MONITORING AND STORAGE PROJECT
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STRONTIUM ISOTOPE (~(87)SR/~(86)SR) CHEMISTRY IN PRODUCED OIL FIELD WATERS: THE IE A CO_2 MONITORING AND STORAGE PROJECT

机译:锶同位素(〜(87)SR /〜(86)SR)在生产的油田水中化学:IE A CO_2监测和存储项目

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EnCana's CO2 injection EOR project at Weyburn Saskatchewan (Canada) is the focal point of a multi-faceted research program, sponsored by the IEA GHQ R&D and numerous international industrial and government partners. More than yearly strontium isotope, trace element and dissolved gas surveys were conducted by INGV in conjunction with the thrice yearly borehole fluid sampling trips performed by the Canadian partners. This paper focuses on the Sr isotope monitoring. Approximately 25 samples were collected over three years for 87Sr/8flSr analyses. At Weyburn, a water-altemating-gas (WAG) EOR technique is used to inject water and CO2 into the Mississippian Midale reservoir. 87Sr/86Sr ratios for produced fluids fall between 0.7077 and 0.7082, consistent with published values for Mississippian fluids and carbonate minerals. A small 87Sr/86Sr component of this produced fluid is derived from waters of the Cretaceous Mannville aquifer, which has been used for water-flooding EOR since 1959. The progressively more positive Sr isotope trend from 2001 to 2003 may be due to: 1) a smaller Mannville aquifer component in the water flooding process; and/or 2) the dissolution of Mississippian host rocks during the ongoing CO2 injection. Evidence that 87Sr/sf'Sr values are approaching those of Mississippian host-rock values may point towards zones of carbonate dissolution as a result of continuing CO2 injection. This hypothesis is strengthened by δ~(13)C data; ii) preliminary "gross composition" of dissolved gases (H2S, CO2, CH4, He, H2) and iii) by trace elements data.
机译:Encana的Co2注射EOR项目在Weyburn Saskatchewan(加拿大)是由IEA GHQ研发和众多国际工业和政府合作伙伴赞助的多方面研究计划的焦点。通过INGV与加拿大合作伙伴执行的三次钻孔流体采样行为一起进行超过年度同位素,痕量元素和溶解气体调查。本文侧重于SR同位素监测。在三年内收集了大约25个样品,持续87SR / 8FLSR分析。在Weyburn,用于将水和二氧化碳注入密西西比地区水库的水上含水剂(WAG)。 87SR / 86SR生产流体比率在0.7077和0.7082之间,与密西西比液和碳酸盐矿物的公布值一致。该产生的流体的小87SR / 86SR成分衍生自成群部曼诺维尔含水层的水,其自1959年以来已被用于水淹水EOR。2001年至2003年的逐步更积极的SR同位素趋势可能是由于:1)较小的曼弗维尔含水层组件在水利过程中;和/或2)在正在进行的CO2注射期间密西西比宿主岩的解散。证据表明,87SR / SF'SR值接近密西西比宿主岩石的值可能指向碳酸盐溶解区,因为继续CO 2注射。该假设由δ〜(13)C数据加强; ii)通过微量元素数据,溶解气体(H2S,CO 2,CH4,HE,H 2)和III的初步“总成”。

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