A New Analysis Model for Potential Contamination of a Shallow Aquifer from a Hydraulically-Fractured Shale
Hydraulic fracturing (HF) is widely used in shale gas development, which may cause some heavy metals release from shale formations. These contaminants could transport from the fractured shale reservoirs to shallow aquifers. Thus, it is necessary to assess the impact of pollution in shallow aquifers....
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MDPI AG
2018-11-01
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Online Access: | https://www.mdpi.com/1996-1073/11/11/3010 |
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author | Weihong Peng Menglin Du Feng Gao Xuan Dong Hongmei Cheng |
author_facet | Weihong Peng Menglin Du Feng Gao Xuan Dong Hongmei Cheng |
author_sort | Weihong Peng |
collection | DOAJ |
description | Hydraulic fracturing (HF) is widely used in shale gas development, which may cause some heavy metals release from shale formations. These contaminants could transport from the fractured shale reservoirs to shallow aquifers. Thus, it is necessary to assess the impact of pollution in shallow aquifers. In this paper, a new analysis model, considering geological distributions, discrete natural fractures (NFs) and faults, is developed to analyze the migration mechanism of contaminants. Furthermore, the alkali erosion of rock caused by high-pH drilling of fluids, is considered in this paper. The numerical results suggest that both NFs and alkali erosion could reduce the time required for contaminants migrating to aquifers. When NFs and alkali erosion are both considered, the migration time will be shortened by 51 years. Alkali erosion makes the impact of NFs, on the contaminant migration, more significant. The migration time decreases with increasing pH values, while the accumulation is on the opposite side. Compared with pH 12.0, the migration time would be increased by 45 years and 29 years for pH 11.0 and 11.5, respectively. However, the migration time for pH 12.5 and 13.0 were found to be decreased by 82 years and 180 years, respectively. Alkali erosion could increase the rock permeability, and the elevated permeability would further enhance the migration velocity of the contaminants, which might play a major role in assessing the potential contamination of shallow aquifers. |
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issn | 1996-1073 |
language | English |
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spelling | doaj.art-3212fe826cb2407d955e67c7418ffde82022-12-22T02:07:36ZengMDPI AGEnergies1996-10732018-11-011111301010.3390/en11113010en11113010A New Analysis Model for Potential Contamination of a Shallow Aquifer from a Hydraulically-Fractured ShaleWeihong Peng0Menglin Du1Feng Gao2Xuan Dong3Hongmei Cheng4School of Mechanics and Civil Engineering, China University of Mining and Technology, Xuzhou 221116, ChinaSchool of Mechanics and Civil Engineering, China University of Mining and Technology, Xuzhou 221116, ChinaSchool of Mechanics and Civil Engineering, China University of Mining and Technology, Xuzhou 221116, ChinaSchool of Mechanics and Civil Engineering, China University of Mining and Technology, Xuzhou 221116, ChinaSchool of Mechanics and Civil Engineering, China University of Mining and Technology, Xuzhou 221116, ChinaHydraulic fracturing (HF) is widely used in shale gas development, which may cause some heavy metals release from shale formations. These contaminants could transport from the fractured shale reservoirs to shallow aquifers. Thus, it is necessary to assess the impact of pollution in shallow aquifers. In this paper, a new analysis model, considering geological distributions, discrete natural fractures (NFs) and faults, is developed to analyze the migration mechanism of contaminants. Furthermore, the alkali erosion of rock caused by high-pH drilling of fluids, is considered in this paper. The numerical results suggest that both NFs and alkali erosion could reduce the time required for contaminants migrating to aquifers. When NFs and alkali erosion are both considered, the migration time will be shortened by 51 years. Alkali erosion makes the impact of NFs, on the contaminant migration, more significant. The migration time decreases with increasing pH values, while the accumulation is on the opposite side. Compared with pH 12.0, the migration time would be increased by 45 years and 29 years for pH 11.0 and 11.5, respectively. However, the migration time for pH 12.5 and 13.0 were found to be decreased by 82 years and 180 years, respectively. Alkali erosion could increase the rock permeability, and the elevated permeability would further enhance the migration velocity of the contaminants, which might play a major role in assessing the potential contamination of shallow aquifers.https://www.mdpi.com/1996-1073/11/11/3010hydraulic fracturingdiscrete natural fracturesmigration mechanismalkali erosionhigh-pH drilling fluid |
spellingShingle | Weihong Peng Menglin Du Feng Gao Xuan Dong Hongmei Cheng A New Analysis Model for Potential Contamination of a Shallow Aquifer from a Hydraulically-Fractured Shale Energies hydraulic fracturing discrete natural fractures migration mechanism alkali erosion high-pH drilling fluid |
title | A New Analysis Model for Potential Contamination of a Shallow Aquifer from a Hydraulically-Fractured Shale |
title_full | A New Analysis Model for Potential Contamination of a Shallow Aquifer from a Hydraulically-Fractured Shale |
title_fullStr | A New Analysis Model for Potential Contamination of a Shallow Aquifer from a Hydraulically-Fractured Shale |
title_full_unstemmed | A New Analysis Model for Potential Contamination of a Shallow Aquifer from a Hydraulically-Fractured Shale |
title_short | A New Analysis Model for Potential Contamination of a Shallow Aquifer from a Hydraulically-Fractured Shale |
title_sort | new analysis model for potential contamination of a shallow aquifer from a hydraulically fractured shale |
topic | hydraulic fracturing discrete natural fractures migration mechanism alkali erosion high-pH drilling fluid |
url | https://www.mdpi.com/1996-1073/11/11/3010 |
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