MN OXIDE CONCENTRATION AS EVIDENCE OF A PATHWAY FOR INFILTRATION OF CRUDE OIL INTO A SHALLOW AQUIFER, WEST TEXAS

Q2 Earth and Planetary Sciences
Rebecca C. Smyth
{"title":"MN OXIDE CONCENTRATION AS EVIDENCE OF A PATHWAY FOR INFILTRATION OF CRUDE OIL INTO A SHALLOW AQUIFER, WEST TEXAS","authors":"Rebecca C. Smyth","doi":"10.1046/j.1526-0984.1999.08046-26.x","DOIUrl":null,"url":null,"abstract":"<p>In November 1991, landowners near Abilene, Texas, found crude oil in their water well. Subsequent drilling (four cores and 30 borings) defined a plume of crude oil (∼300 bbl) floating on shallow, perched groundwater. Data suggest that the oil came from a near-surface leak associated with oil-production activities. Crude oil is present in a thin (0.5 ft), silty sand layer 17.7–19 ft below the surface. Because of water level fluctuation, traces of oil also occur along fractures as deep as 35 ft in two cores collected within the crude-oil plume.</p><p>The presence of manganese (Mn) oxide coatings along fracture surfaces might prove to be a record of the path of oil as it infiltrated the subsurface. Mn oxide minerals are concentrated along fracture surfaces to depths of 20 ft in two cores located nearest the suspected crude-oil source. Changes in redox conditions and increased microbial activity associated with the crude oil probably caused dissolution, followed by reprecipitation and concentration of Mn oxides.</p><p>Other effects of crude-oil degradation include high unsaturated zone methane concentrations in a halo around the oil plume. Methane was measured in boreholes at concentrations mainly between 5–50% but locally as high as 98% at depths of 8–10 ft. The methane is most likely a result of both volatilization and biodegradation of the crude oil. Coincident with the methane plume are zones of high carbon dioxide (as much as 10%) and low oxygen (as little as 1.9%) content.</p>","PeriodicalId":11706,"journal":{"name":"Environmental Geosciences","volume":"6 3","pages":"158-159"},"PeriodicalIF":0.0000,"publicationDate":"2009-08-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1046/j.1526-0984.1999.08046-26.x","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Environmental Geosciences","FirstCategoryId":"1085","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1046/j.1526-0984.1999.08046-26.x","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: 1

Abstract

In November 1991, landowners near Abilene, Texas, found crude oil in their water well. Subsequent drilling (four cores and 30 borings) defined a plume of crude oil (∼300 bbl) floating on shallow, perched groundwater. Data suggest that the oil came from a near-surface leak associated with oil-production activities. Crude oil is present in a thin (0.5 ft), silty sand layer 17.7–19 ft below the surface. Because of water level fluctuation, traces of oil also occur along fractures as deep as 35 ft in two cores collected within the crude-oil plume.

The presence of manganese (Mn) oxide coatings along fracture surfaces might prove to be a record of the path of oil as it infiltrated the subsurface. Mn oxide minerals are concentrated along fracture surfaces to depths of 20 ft in two cores located nearest the suspected crude-oil source. Changes in redox conditions and increased microbial activity associated with the crude oil probably caused dissolution, followed by reprecipitation and concentration of Mn oxides.

Other effects of crude-oil degradation include high unsaturated zone methane concentrations in a halo around the oil plume. Methane was measured in boreholes at concentrations mainly between 5–50% but locally as high as 98% at depths of 8–10 ft. The methane is most likely a result of both volatilization and biodegradation of the crude oil. Coincident with the methane plume are zones of high carbon dioxide (as much as 10%) and low oxygen (as little as 1.9%) content.

氧化锰浓度作为原油渗入德克萨斯州西部浅层含水层途径的证据
1991年11月,德克萨斯州阿比林附近的土地所有者在他们的水井中发现了原油。随后的钻探(4个岩心和30个钻孔)确定了一层原油羽流(约300桶)漂浮在浅层地下水上。数据显示,石油来自与石油生产活动有关的近地表泄漏。原油存在于地表以下17.7-19英尺的薄(0.5英尺)粉砂层中。由于水位的波动,在原油柱中收集的两个岩心中,沿着35英尺深的裂缝也会出现石油痕迹。沿断裂面存在的锰(Mn)氧化物涂层可能被证明是石油渗入地下的路径记录。氧化锰矿物沿着裂缝表面集中到距离疑似原油源最近的两个岩心深处20英尺处。与原油相关的氧化还原条件的变化和微生物活性的增加可能导致溶解,随后是锰氧化物的再沉淀和浓度。原油降解的其他影响包括油羽周围晕区的高不饱和带甲烷浓度。在钻孔中测量到的甲烷浓度主要在5-50%之间,但在8-10英尺深的地方,甲烷浓度高达98%。甲烷很可能是原油挥发和生物降解的结果。与甲烷羽流相一致的是高二氧化碳(高达10%)和低氧(低至1.9%)含量的区域。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Environmental Geosciences
Environmental Geosciences Earth and Planetary Sciences-Earth and Planetary Sciences (all)
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信