Subsurface Gaseous Hydrocarbons and Carbon Dioxide Recorded During the Trans-Amazon Drilling Project (TADP) in the Acre Basin, Western Amazon
The Trans-Amazon Drilling Project (TADP) drilled a sequence of claystones, siltstones, and sandstones in the Acre sedimentary basin, reaching a final depth of 923 m. This study characterizes the occurrence and compositional variation of light gaseous hydrocarbons detected using the online gas analys...
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Wiley
2025-01-01
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| Series: | Geofluids |
| Online Access: | http://dx.doi.org/10.1155/gfl/6658750 |
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| author | Angela Ethelis Jimenez Martinez André Oliveira Sawakuchi Dailson José Bertassoli Júnior Thomas Wiersberg Siu Mui Tsai Kleiton Rabelo de Araújo Larissa Natsumi Tamura Marcos Bolognini Barbosa Tácio Cordeiro Bicudo Alderlene Pimentel de Brito Ingo Daniel Wahnfried Isaac Salém Azevedo Bezerra Anders Noren Cleverson Guizan Silva Sherilyn Fritz Paul Baker |
| author_facet | Angela Ethelis Jimenez Martinez André Oliveira Sawakuchi Dailson José Bertassoli Júnior Thomas Wiersberg Siu Mui Tsai Kleiton Rabelo de Araújo Larissa Natsumi Tamura Marcos Bolognini Barbosa Tácio Cordeiro Bicudo Alderlene Pimentel de Brito Ingo Daniel Wahnfried Isaac Salém Azevedo Bezerra Anders Noren Cleverson Guizan Silva Sherilyn Fritz Paul Baker |
| author_sort | Angela Ethelis Jimenez Martinez |
| collection | DOAJ |
| description | The Trans-Amazon Drilling Project (TADP) drilled a sequence of claystones, siltstones, and sandstones in the Acre sedimentary basin, reaching a final depth of 923 m. This study characterizes the occurrence and compositional variation of light gaseous hydrocarbons detected using the online gas analysis (OLGA) monitoring system deployed during drilling, along with methane (CH4) and carbon dioxide (CO2) concentrations measured in discrete gas samples extracted from cores during drilling operations. The gaseous hydrocarbons detected by the OLGA system are predominantly CH4 but with the regular presence of ethane (C2H6), propane (C3H8), isobutane (i-C4H10), and n-butane (n-C4H10). Zones with higher CH4, C2H6, and C3H8 concentrations were observed at depth intervals of 250–380 and 420–588 m. These higher concentrations of CH4, C2H6, and C3H8 occur in siltstone or sandstone layers capped by claystones, suggesting that these lithological associations act as stratigraphic gas traps. The Bernard parameter (CH4/C2H6 + C3H8) varied from a low value of 2 at 466 m depth to a maximum value of 1904 at 621 m depth. Stable carbon isotope ratios of CH4 show δ13C values between −35‰ and −25‰, suggesting the nearly ubiquitous presence of thermogenic gas. The discrete gas samples from cores exhibited CO2 concentrations between 230 and 1400 ppm in claystones, 850 and 950 ppm in siltstones, and 240–820 ppm in sandstones, indicating higher concentrations in fine-grained sediments. The CH4 concentration ranges from 2 to 6 ppm in sandstone layers and from 2 to 4 ppm in siltstone and claystone layers. There is no significant correlation between CH4 and CO2 concentrations. These results provide evidence of light hydrocarbon migration from deeper thermally mature source rocks, with entrapment in sandstone layers capped by fine-grained sedimentary rock layers. The high concentration of CO2 relative to CH4 in fine-grained rock layers points to restricted conditions for microbial gas generation in the drilled sediments, possibly due to a combination of low organic carbon content and oxidizing conditions. This is in accordance with the abundance of reddish fine-grained paleosols in the drilled sedimentary units. The combination of online gas monitoring and discrete sampling methods allowed the comparison between gas collected during drilling and in situ gas, contributing to a better understanding of the processes of the subsurface carbon cycle. |
| format | Article |
| id | doaj-art-830b39b85a044a46a00a46dd5d44b00b |
| institution | DOAJ |
| issn | 1468-8123 |
| language | English |
| publishDate | 2025-01-01 |
| publisher | Wiley |
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| series | Geofluids |
| spelling | doaj-art-830b39b85a044a46a00a46dd5d44b00b2025-08-20T02:56:20ZengWileyGeofluids1468-81232025-01-01202510.1155/gfl/6658750Subsurface Gaseous Hydrocarbons and Carbon Dioxide Recorded During the Trans-Amazon Drilling Project (TADP) in the Acre Basin, Western AmazonAngela Ethelis Jimenez Martinez0André Oliveira Sawakuchi1Dailson José Bertassoli Júnior2Thomas Wiersberg3Siu Mui Tsai4Kleiton Rabelo de Araújo5Larissa Natsumi Tamura6Marcos Bolognini Barbosa7Tácio Cordeiro Bicudo8Alderlene Pimentel de Brito9Ingo Daniel Wahnfried10Isaac Salém Azevedo Bezerra11Anders Noren12Cleverson Guizan Silva13Sherilyn Fritz14Paul Baker15Institute of GeosciencesInstitute of GeosciencesInstitute of GeosciencesGFZ Helmholtz Centre for GeosciencesCell and Molecular Biology LaboratoryInstitute of GeosciencesInstitute of GeosciencesInstitute of GeosciencesInstitute of GeosciencesUniversidade Federal do AmazonasUniversidade Federal do AmazonasInstitute of GeosciencesContinental Scientific Drilling FacilityDepartment of Geology and Marine Geophysics-LAGEMADepartment of Earth and Atmospheric SciencesDepartment of Earth and Climate SciencesThe Trans-Amazon Drilling Project (TADP) drilled a sequence of claystones, siltstones, and sandstones in the Acre sedimentary basin, reaching a final depth of 923 m. This study characterizes the occurrence and compositional variation of light gaseous hydrocarbons detected using the online gas analysis (OLGA) monitoring system deployed during drilling, along with methane (CH4) and carbon dioxide (CO2) concentrations measured in discrete gas samples extracted from cores during drilling operations. The gaseous hydrocarbons detected by the OLGA system are predominantly CH4 but with the regular presence of ethane (C2H6), propane (C3H8), isobutane (i-C4H10), and n-butane (n-C4H10). Zones with higher CH4, C2H6, and C3H8 concentrations were observed at depth intervals of 250–380 and 420–588 m. These higher concentrations of CH4, C2H6, and C3H8 occur in siltstone or sandstone layers capped by claystones, suggesting that these lithological associations act as stratigraphic gas traps. The Bernard parameter (CH4/C2H6 + C3H8) varied from a low value of 2 at 466 m depth to a maximum value of 1904 at 621 m depth. Stable carbon isotope ratios of CH4 show δ13C values between −35‰ and −25‰, suggesting the nearly ubiquitous presence of thermogenic gas. The discrete gas samples from cores exhibited CO2 concentrations between 230 and 1400 ppm in claystones, 850 and 950 ppm in siltstones, and 240–820 ppm in sandstones, indicating higher concentrations in fine-grained sediments. The CH4 concentration ranges from 2 to 6 ppm in sandstone layers and from 2 to 4 ppm in siltstone and claystone layers. There is no significant correlation between CH4 and CO2 concentrations. These results provide evidence of light hydrocarbon migration from deeper thermally mature source rocks, with entrapment in sandstone layers capped by fine-grained sedimentary rock layers. The high concentration of CO2 relative to CH4 in fine-grained rock layers points to restricted conditions for microbial gas generation in the drilled sediments, possibly due to a combination of low organic carbon content and oxidizing conditions. This is in accordance with the abundance of reddish fine-grained paleosols in the drilled sedimentary units. The combination of online gas monitoring and discrete sampling methods allowed the comparison between gas collected during drilling and in situ gas, contributing to a better understanding of the processes of the subsurface carbon cycle.http://dx.doi.org/10.1155/gfl/6658750 |
| spellingShingle | Angela Ethelis Jimenez Martinez André Oliveira Sawakuchi Dailson José Bertassoli Júnior Thomas Wiersberg Siu Mui Tsai Kleiton Rabelo de Araújo Larissa Natsumi Tamura Marcos Bolognini Barbosa Tácio Cordeiro Bicudo Alderlene Pimentel de Brito Ingo Daniel Wahnfried Isaac Salém Azevedo Bezerra Anders Noren Cleverson Guizan Silva Sherilyn Fritz Paul Baker Subsurface Gaseous Hydrocarbons and Carbon Dioxide Recorded During the Trans-Amazon Drilling Project (TADP) in the Acre Basin, Western Amazon Geofluids |
| title | Subsurface Gaseous Hydrocarbons and Carbon Dioxide Recorded During the Trans-Amazon Drilling Project (TADP) in the Acre Basin, Western Amazon |
| title_full | Subsurface Gaseous Hydrocarbons and Carbon Dioxide Recorded During the Trans-Amazon Drilling Project (TADP) in the Acre Basin, Western Amazon |
| title_fullStr | Subsurface Gaseous Hydrocarbons and Carbon Dioxide Recorded During the Trans-Amazon Drilling Project (TADP) in the Acre Basin, Western Amazon |
| title_full_unstemmed | Subsurface Gaseous Hydrocarbons and Carbon Dioxide Recorded During the Trans-Amazon Drilling Project (TADP) in the Acre Basin, Western Amazon |
| title_short | Subsurface Gaseous Hydrocarbons and Carbon Dioxide Recorded During the Trans-Amazon Drilling Project (TADP) in the Acre Basin, Western Amazon |
| title_sort | subsurface gaseous hydrocarbons and carbon dioxide recorded during the trans amazon drilling project tadp in the acre basin western amazon |
| url | http://dx.doi.org/10.1155/gfl/6658750 |
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