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Dimensional Changes in Geological Sandstone Caused by Wetting

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Bibliographic Details
Title: Dimensional Changes in Geological Sandstone Caused by Wetting
Language: English
Authors: Burkova, Irina (ORCID 0000-0002-3313-0392), Ilin, Eduard (ORCID 0000-0003-3795-8231), Belov, Alexander N. (ORCID 0000-0002-5060-9354), Bezryadin, Alexey (ORCID 0000-0002-4822-6960)
Source: Physics Education. May 2021 56(3).
Availability: IOP Publishing. 190 North Independence Mall West Suite 601, Philadelphia, PA 19106. Tel: 215-627-0880; Fax: 215-627-0879; e-mail: ped@ioppublishing.org; Web site: https://iopscience.iop.org/journal/0031-9120
Peer Reviewed: Y
Page Count: 8
Publication Date: 2021
Document Type: Journal Articles
Reports - Research
Education Level: Higher Education
Postsecondary Education
Descriptors: Science Instruction, Seismology, Geology, Scientific Concepts, Concept Formation, Science Experiments, College Science, Undergraduate Study, Science Laboratories, Laboratory Experiments
DOI: 10.1088/1361-6552/abdea0
ISSN: 0031-9120
Abstract: Induced seismicity has received a lot of attention in recent years. This new natural phenomenon appeared as a result of active human influence on nature. The phenomenon has been detected in places of natural gas and oil recovery, and geological storage of CO[subscript 2]. One of the main reasons for the observed seismic activity is associated with the adsorption-induced deformation of rocks. We present experimental data and a simple model describing adsorption-induced deformation using the example of the Berea sandstone. We suggest a simplified experiment for the undergraduate university laboratory.
Abstractor: As Provided
Entry Date: 2021
Accession Number: EJ1298261
Database: ERIC
Description
Abstract:Induced seismicity has received a lot of attention in recent years. This new natural phenomenon appeared as a result of active human influence on nature. The phenomenon has been detected in places of natural gas and oil recovery, and geological storage of CO[subscript 2]. One of the main reasons for the observed seismic activity is associated with the adsorption-induced deformation of rocks. We present experimental data and a simple model describing adsorption-induced deformation using the example of the Berea sandstone. We suggest a simplified experiment for the undergraduate university laboratory.
ISSN:0031-9120
DOI:10.1088/1361-6552/abdea0