{"title":"在密歇根盆地的Bass Islands白云岩进行二氧化碳注入测试,测试结果和油藏性能","authors":"J. Sminchak, N. Gupta, J. Gerst","doi":"10.1306/EG.04080909001","DOIUrl":null,"url":null,"abstract":"Analysis of well test results and reservoir behavior is presented for a 10,241-t carbon dioxide (CO2) injection test in the Michigan Basin. The test site was located in Otsego County, Michigan, and was part of the Midwest Regional Carbon Sequestration Partnership (MRCSP) program. The injection target was a deep saline rock formation, named the Bass Islands Dolomite, at a depth of 1049–1071 m (3442–3514 ft). Rock core tests on this formation suggested an average permeability of 22 md and porosity of 13% across 22 m (72 ft). Hydraulic monitoring included metering injection at the wellhead and downhole pressure and temperature logging in the injection well and a nearby deep monitoring well. Pressure response curves were analyzed for a step-rate injection and shut-in recovery tests. Downhole pressure in the injection well was approximately 13,800–13,930 kPa at injection rates of 400–600 t CO2 per day. Step-rate injection testing suggested that injection rates of several hundred thousand metric tons CO2 per year may be sustainable in a single well. Injection test pressure falloff analysis showed that the overall reservoir permeability may be more than twice as high as indicated from rock core tests. This successful test provides extremely valuable field information on all aspects of the CO2 storage feasibility for both the test region and the broader deployment of the technology.","PeriodicalId":11706,"journal":{"name":"Environmental Geosciences","volume":"16 1","pages":"153-162"},"PeriodicalIF":0.0000,"publicationDate":"2009-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1306/EG.04080909001","citationCount":"18","resultStr":"{\"title\":\"Well test results and reservoir performance for a carbon dioxide injection test in the Bass Islands Dolomite in the Michigan Basin\",\"authors\":\"J. Sminchak, N. Gupta, J. Gerst\",\"doi\":\"10.1306/EG.04080909001\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Analysis of well test results and reservoir behavior is presented for a 10,241-t carbon dioxide (CO2) injection test in the Michigan Basin. The test site was located in Otsego County, Michigan, and was part of the Midwest Regional Carbon Sequestration Partnership (MRCSP) program. The injection target was a deep saline rock formation, named the Bass Islands Dolomite, at a depth of 1049–1071 m (3442–3514 ft). Rock core tests on this formation suggested an average permeability of 22 md and porosity of 13% across 22 m (72 ft). Hydraulic monitoring included metering injection at the wellhead and downhole pressure and temperature logging in the injection well and a nearby deep monitoring well. Pressure response curves were analyzed for a step-rate injection and shut-in recovery tests. Downhole pressure in the injection well was approximately 13,800–13,930 kPa at injection rates of 400–600 t CO2 per day. Step-rate injection testing suggested that injection rates of several hundred thousand metric tons CO2 per year may be sustainable in a single well. Injection test pressure falloff analysis showed that the overall reservoir permeability may be more than twice as high as indicated from rock core tests. This successful test provides extremely valuable field information on all aspects of the CO2 storage feasibility for both the test region and the broader deployment of the technology.\",\"PeriodicalId\":11706,\"journal\":{\"name\":\"Environmental Geosciences\",\"volume\":\"16 1\",\"pages\":\"153-162\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2009-09-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1306/EG.04080909001\",\"citationCount\":\"18\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Environmental Geosciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1306/EG.04080909001\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"Earth and Planetary Sciences\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Environmental Geosciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1306/EG.04080909001","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
引用次数: 18
摘要
介绍了密歇根盆地10241吨二氧化碳(CO2)注入试验的试井结果和储层动态分析。该试验场位于密歇根州奥特塞戈县,是中西部地区碳封存伙伴关系(MRCSP)计划的一部分。注入目标是深度1049-1071米(3442-3514英尺)、名为Bass Islands Dolomite的深层咸化岩层。岩心测试表明,该地层的平均渗透率为22 md,孔隙度为13%,跨度为22 m (72 ft)。水力监测包括井口计量注入、注入井和附近深监测井的井下压力和温度测井。分析了阶梯速率注入和关井采收率测试的压力响应曲线。注水井的井下压力约为13800 - 13930 kPa,注气量为400-600 t /天。阶梯速率注入测试表明,在单井中,每年几十万公吨二氧化碳的注入速率是可持续的。注入试验压力下降分析表明,储层整体渗透率可能比岩心试验结果高两倍以上。这次成功的测试为测试区域和更广泛的技术部署提供了非常有价值的现场信息,包括二氧化碳封存可行性的各个方面。
Well test results and reservoir performance for a carbon dioxide injection test in the Bass Islands Dolomite in the Michigan Basin
Analysis of well test results and reservoir behavior is presented for a 10,241-t carbon dioxide (CO2) injection test in the Michigan Basin. The test site was located in Otsego County, Michigan, and was part of the Midwest Regional Carbon Sequestration Partnership (MRCSP) program. The injection target was a deep saline rock formation, named the Bass Islands Dolomite, at a depth of 1049–1071 m (3442–3514 ft). Rock core tests on this formation suggested an average permeability of 22 md and porosity of 13% across 22 m (72 ft). Hydraulic monitoring included metering injection at the wellhead and downhole pressure and temperature logging in the injection well and a nearby deep monitoring well. Pressure response curves were analyzed for a step-rate injection and shut-in recovery tests. Downhole pressure in the injection well was approximately 13,800–13,930 kPa at injection rates of 400–600 t CO2 per day. Step-rate injection testing suggested that injection rates of several hundred thousand metric tons CO2 per year may be sustainable in a single well. Injection test pressure falloff analysis showed that the overall reservoir permeability may be more than twice as high as indicated from rock core tests. This successful test provides extremely valuable field information on all aspects of the CO2 storage feasibility for both the test region and the broader deployment of the technology.