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Microbial Metabolism and Community Dynamics in Hydraulic Fracturing Fluids Recovered From Deep Hydrocarbon-Rich Shale
Hydraulic fracturing is a prominent method of natural gas production that uses injected, high-pressure fluids to fracture low permeability, hydrocarbon rich strata such as shale. Upon completion of a well, the fluid returns to the surface (produced water) and contains natural gas, subsurface constit...
Autores principales: | , , , , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Frontiers Media S.A.
2019
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6422894/ https://www.ncbi.nlm.nih.gov/pubmed/30915042 http://dx.doi.org/10.3389/fmicb.2019.00376 |
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author | Morono, Yuki Wishart, Jessie R. Ito, Motoo Ijiri, Akira Hoshino, Tatsuhiko Torres, Marta Verba, Circe Terada, Takeshi Inagaki, Fumio Colwell, Frederick S. |
author_facet | Morono, Yuki Wishart, Jessie R. Ito, Motoo Ijiri, Akira Hoshino, Tatsuhiko Torres, Marta Verba, Circe Terada, Takeshi Inagaki, Fumio Colwell, Frederick S. |
author_sort | Morono, Yuki |
collection | PubMed |
description | Hydraulic fracturing is a prominent method of natural gas production that uses injected, high-pressure fluids to fracture low permeability, hydrocarbon rich strata such as shale. Upon completion of a well, the fluid returns to the surface (produced water) and contains natural gas, subsurface constituents, and microorganisms (Barbot et al., 2013; Daly et al., 2016). While the microbial community of the produced fluids has been studied in multiple gas wells, the activity of these microorganisms and their relation to biogeochemical activity is not well understood. In this experiment, we supplemented produced fluid with (13)C-labeled carbon sources (glucose, acetate, bicarbonate, methanol, or methane), and (15)N-labeled ammonium chloride in order to isotopically trace microbial activity over multiple day in anoxic incubations. Nanoscale secondary ion mass spectrometry (NanoSIMS) was used to generate isotopic images of (13)C and (15)N incorporation in individual cells, while isotope ratio monitoring–gas chromatography–mass spectrometry (IRM–GC–MS) was used to measure (13)CO(2), and (13)CH(4) as metabolic byproducts. Glucose, acetate, and methanol were all assimilated by microorganisms under anoxic conditions. (13)CO(2) production was only observed with glucose as a substrate indicating that catabolic activity was limited to this condition. The microbial communities observed at 0, 19, and 32 days of incubation did not vary between different carbon sources, were low in diversity, and composed primarily of the class Clostridia. The primary genera detected in the incubations, Halanaerobium and Fusibacter, are known to be adapted to harsh physical and chemical conditions consistent with those that occur in the hydrofracturing environment. This study provides evidence that microorganisms in produced fluid are revivable in laboratory incubations and retained the ability to metabolize added carbon and nitrogen substrates. |
format | Online Article Text |
id | pubmed-6422894 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2019 |
publisher | Frontiers Media S.A. |
record_format | MEDLINE/PubMed |
spelling | pubmed-64228942019-03-26 Microbial Metabolism and Community Dynamics in Hydraulic Fracturing Fluids Recovered From Deep Hydrocarbon-Rich Shale Morono, Yuki Wishart, Jessie R. Ito, Motoo Ijiri, Akira Hoshino, Tatsuhiko Torres, Marta Verba, Circe Terada, Takeshi Inagaki, Fumio Colwell, Frederick S. Front Microbiol Microbiology Hydraulic fracturing is a prominent method of natural gas production that uses injected, high-pressure fluids to fracture low permeability, hydrocarbon rich strata such as shale. Upon completion of a well, the fluid returns to the surface (produced water) and contains natural gas, subsurface constituents, and microorganisms (Barbot et al., 2013; Daly et al., 2016). While the microbial community of the produced fluids has been studied in multiple gas wells, the activity of these microorganisms and their relation to biogeochemical activity is not well understood. In this experiment, we supplemented produced fluid with (13)C-labeled carbon sources (glucose, acetate, bicarbonate, methanol, or methane), and (15)N-labeled ammonium chloride in order to isotopically trace microbial activity over multiple day in anoxic incubations. Nanoscale secondary ion mass spectrometry (NanoSIMS) was used to generate isotopic images of (13)C and (15)N incorporation in individual cells, while isotope ratio monitoring–gas chromatography–mass spectrometry (IRM–GC–MS) was used to measure (13)CO(2), and (13)CH(4) as metabolic byproducts. Glucose, acetate, and methanol were all assimilated by microorganisms under anoxic conditions. (13)CO(2) production was only observed with glucose as a substrate indicating that catabolic activity was limited to this condition. The microbial communities observed at 0, 19, and 32 days of incubation did not vary between different carbon sources, were low in diversity, and composed primarily of the class Clostridia. The primary genera detected in the incubations, Halanaerobium and Fusibacter, are known to be adapted to harsh physical and chemical conditions consistent with those that occur in the hydrofracturing environment. This study provides evidence that microorganisms in produced fluid are revivable in laboratory incubations and retained the ability to metabolize added carbon and nitrogen substrates. Frontiers Media S.A. 2019-03-12 /pmc/articles/PMC6422894/ /pubmed/30915042 http://dx.doi.org/10.3389/fmicb.2019.00376 Text en Copyright © 2019 Morono, Wishart, Ito, Ijiri, Hoshino, Torres, Verba, Terada, Inagaki and Colwell. http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms. |
spellingShingle | Microbiology Morono, Yuki Wishart, Jessie R. Ito, Motoo Ijiri, Akira Hoshino, Tatsuhiko Torres, Marta Verba, Circe Terada, Takeshi Inagaki, Fumio Colwell, Frederick S. Microbial Metabolism and Community Dynamics in Hydraulic Fracturing Fluids Recovered From Deep Hydrocarbon-Rich Shale |
title | Microbial Metabolism and Community Dynamics in Hydraulic Fracturing Fluids Recovered From Deep Hydrocarbon-Rich Shale |
title_full | Microbial Metabolism and Community Dynamics in Hydraulic Fracturing Fluids Recovered From Deep Hydrocarbon-Rich Shale |
title_fullStr | Microbial Metabolism and Community Dynamics in Hydraulic Fracturing Fluids Recovered From Deep Hydrocarbon-Rich Shale |
title_full_unstemmed | Microbial Metabolism and Community Dynamics in Hydraulic Fracturing Fluids Recovered From Deep Hydrocarbon-Rich Shale |
title_short | Microbial Metabolism and Community Dynamics in Hydraulic Fracturing Fluids Recovered From Deep Hydrocarbon-Rich Shale |
title_sort | microbial metabolism and community dynamics in hydraulic fracturing fluids recovered from deep hydrocarbon-rich shale |
topic | Microbiology |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6422894/ https://www.ncbi.nlm.nih.gov/pubmed/30915042 http://dx.doi.org/10.3389/fmicb.2019.00376 |
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