{"title":"美国缅因州受污染裂缝灰岩注汽试点研究:井眼雷达反射数据建模与分析","authors":"C. Grégoire, J. Lane, P. Joesten","doi":"10.1109/AGPR.2005.1487846","DOIUrl":null,"url":null,"abstract":"AbslructSteam-enhanced remediation (SER) has been successfully used to remove DNAPL and LNAPL contaminants in porous media. Between August and November 2002, SER was tested in fractured limestone at the former Loring Air Force Base, in Maine, USA. During the SER investigation, the U.S. Geological Survey conducted a series of borehole radar surveys to evaluate the effectiveness of radar methods for monitoring the movement of steam and heat through the fractured limestone. The data were collected before steam injection, 10 days after the beginning of injection, and at the end of injection. In this paper, reflection-mode borehole radar data from wells JBW-7816 and JBW-7817A are presented and discussed. Theoretical modeling was performed to predict the variation of fracture reflectivity owed to heating, to show displacement of water and to assess the effect of SER at the site. Analysis of the radar profile data indicates some variations resulting from heating (increase of continuity of reflectors, attenuation of deeper reflections) but no substantial variation of traveltimes. Spectral content analysis of several individual reflections surrounding the boreholes was used to investigate the replacement of water by steam in the fractures. Observed decrease in radar reflectivity was too small to be explained by a replacement of water by steam, except for two high-amplitude reflectors, which disappeared near the end of the injection; moreover, no change of polarity, consistent with steam replacing water, was observed. The decrease of amplitude was greater for reflectors near well JBW-7817A and is explained by a greater heating around this well. John W. Lane Jr., Peter K. Joesten U.S. Geological Survey, Branch of Geophysics 11 Sherman Place, Unit 5015, Storrs Mansfield, CT 06269, United States jwlane@usgs.gov , pjoesten@usgs.gov","PeriodicalId":272364,"journal":{"name":"Proceedings of the 3rd International Workshop on Advanced Ground Penetrating Radar, 2005. IWAGPR 2005.","volume":"223 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2005-05-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Steam injection pilot study in a contaminated fractured limestone (Maine, USA): modeling and analysis of borehole radar reflection data\",\"authors\":\"C. Grégoire, J. Lane, P. Joesten\",\"doi\":\"10.1109/AGPR.2005.1487846\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"AbslructSteam-enhanced remediation (SER) has been successfully used to remove DNAPL and LNAPL contaminants in porous media. Between August and November 2002, SER was tested in fractured limestone at the former Loring Air Force Base, in Maine, USA. During the SER investigation, the U.S. Geological Survey conducted a series of borehole radar surveys to evaluate the effectiveness of radar methods for monitoring the movement of steam and heat through the fractured limestone. The data were collected before steam injection, 10 days after the beginning of injection, and at the end of injection. In this paper, reflection-mode borehole radar data from wells JBW-7816 and JBW-7817A are presented and discussed. Theoretical modeling was performed to predict the variation of fracture reflectivity owed to heating, to show displacement of water and to assess the effect of SER at the site. Analysis of the radar profile data indicates some variations resulting from heating (increase of continuity of reflectors, attenuation of deeper reflections) but no substantial variation of traveltimes. Spectral content analysis of several individual reflections surrounding the boreholes was used to investigate the replacement of water by steam in the fractures. Observed decrease in radar reflectivity was too small to be explained by a replacement of water by steam, except for two high-amplitude reflectors, which disappeared near the end of the injection; moreover, no change of polarity, consistent with steam replacing water, was observed. The decrease of amplitude was greater for reflectors near well JBW-7817A and is explained by a greater heating around this well. John W. Lane Jr., Peter K. Joesten U.S. Geological Survey, Branch of Geophysics 11 Sherman Place, Unit 5015, Storrs Mansfield, CT 06269, United States jwlane@usgs.gov , pjoesten@usgs.gov\",\"PeriodicalId\":272364,\"journal\":{\"name\":\"Proceedings of the 3rd International Workshop on Advanced Ground Penetrating Radar, 2005. 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引用次数: 0
摘要
蒸汽增强修复(SER)已成功用于去除多孔介质中的DNAPL和LNAPL污染物。2002年8月至11月期间,SER在美国缅因州前洛林空军基地的断裂石灰岩中进行了测试。在SER调查期间,美国地质调查局进行了一系列的钻孔雷达调查,以评估雷达方法监测蒸汽和热量通过裂缝石灰岩运动的有效性。数据分别在注汽前、注汽开始后10天和注汽结束时采集。本文介绍并讨论了JBW-7816井和JBW-7817A井的反射模式井眼雷达数据。通过理论建模来预测加热引起的裂缝反射率变化,显示水的位移,并评估SER在现场的影响。对雷达廓线资料的分析表明,加热引起了一些变化(反射器的连续性增加,较深反射的衰减),但旅行时间没有实质性变化。利用钻孔周围几个单独反射的光谱含量分析,研究了裂缝中蒸汽对水的替代作用。观测到的雷达反射率的下降太小,不能用蒸汽代替水来解释,除了两个高振幅反射器,它们在注入结束时消失;此外,没有观察到极性的变化,与蒸汽取代水一致。JBW-7817A井附近反射器的振幅下降幅度更大,这是由于该井周围的加热更大。美国地质调查局地球物理分处11 Sherman Place 5015单元,斯托尔斯曼斯菲尔德,CT 06269 jwlane@usgs.gov, pjoesten@usgs.gov
Steam injection pilot study in a contaminated fractured limestone (Maine, USA): modeling and analysis of borehole radar reflection data
AbslructSteam-enhanced remediation (SER) has been successfully used to remove DNAPL and LNAPL contaminants in porous media. Between August and November 2002, SER was tested in fractured limestone at the former Loring Air Force Base, in Maine, USA. During the SER investigation, the U.S. Geological Survey conducted a series of borehole radar surveys to evaluate the effectiveness of radar methods for monitoring the movement of steam and heat through the fractured limestone. The data were collected before steam injection, 10 days after the beginning of injection, and at the end of injection. In this paper, reflection-mode borehole radar data from wells JBW-7816 and JBW-7817A are presented and discussed. Theoretical modeling was performed to predict the variation of fracture reflectivity owed to heating, to show displacement of water and to assess the effect of SER at the site. Analysis of the radar profile data indicates some variations resulting from heating (increase of continuity of reflectors, attenuation of deeper reflections) but no substantial variation of traveltimes. Spectral content analysis of several individual reflections surrounding the boreholes was used to investigate the replacement of water by steam in the fractures. Observed decrease in radar reflectivity was too small to be explained by a replacement of water by steam, except for two high-amplitude reflectors, which disappeared near the end of the injection; moreover, no change of polarity, consistent with steam replacing water, was observed. The decrease of amplitude was greater for reflectors near well JBW-7817A and is explained by a greater heating around this well. John W. Lane Jr., Peter K. Joesten U.S. Geological Survey, Branch of Geophysics 11 Sherman Place, Unit 5015, Storrs Mansfield, CT 06269, United States jwlane@usgs.gov , pjoesten@usgs.gov