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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Main Authors: Weihong Peng, Menglin Du, Feng Gao, Xuan Dong, Hongmei Cheng
Format: Article
Language:English
Published: MDPI AG 2018-11-01
Series:Energies
Subjects:
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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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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