371
Views
5
CrossRef citations to date
0
Altmetric
Research Article

Experimental study on the causes and critical conditions of toxic gases in hydraulically fractured oil wells

ORCID Icon, , ORCID Icon, &
Pages 2963-2971 | Received 14 Nov 2019, Accepted 04 Aug 2020, Published online: 17 Aug 2020
 

ABSTRACT

Hydraulic fracturing is the most preferred oil well stimulation technology worldwide. In fractured oil wells, toxic gases (hydrogen sulfide and carbon monoxide) present a problem when the produced water is reclaimed as base fluid for fracturing. These gases can cause equipment corrosion, environment pollution, and adversely affect the operational personnel’s health. Extant research focuses on toxic gases produced at high temperatures (>200 °C). Therefore, this paper examines the causes and critical conditions for toxic gas formation in fractured wells in conventional reservoirs at low temperatures (<160 °C) through a series of laboratory experiments that include bacterial culture and heating experiments. The results show that for temperature in the range 40–60 °C, the presence of sulfate-reducing bacteria in the produced water is the main cause of hydrogen sulfide production in fractured wells. However, when the temperature is higher than 102 °C, the sulfur compounds (potassium persulfate and sodium sulfite) in the fracturing fluid and crude oil can produce hydrogen sulfide by thermochemical sulfate reduction. In addition, when the temperature is higher than 75 °C, oxygenated compounds (aldehydes) in crude oil can produce carbon monoxide by decarbonylation. Both processes can occur simultaneously when the temperature is higher than 102 °C. This paper is of great significance in controlling the formation of toxic gases in fractured wells.

Acknowledgments

The authors thank No. 9 oil production plant of Daqing oil field branch of PetroChina Co. Ltd. for providing the materials for this study and to the National Natural Science Foundations of China for funding this study (Ratification No. 51574089).

Additional information

Funding

This work was supported by the National Natural Science Foundation of China [51574089].

Reprints and Corporate Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

To request a reprint or corporate permissions for this article, please click on the relevant link below:

Academic Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

Obtain permissions instantly via Rightslink by clicking on the button below:

If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.