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Assessment of Chemistry and Geochemi...

Ghahremani, Nima.

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Assessment of Chemistry and Geochemical Reactions for Alternative Hydraulic Fracturing Water Supplies and Produced Waters.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Assessment of Chemistry and Geochemical Reactions for Alternative Hydraulic Fracturing Water Supplies and Produced Waters./
作者:	Ghahremani, Nima.
出版者:	Ann Arbor : ProQuest Dissertations & Theses, : 2021,
面頁冊數:	165 p.
附註:	Source: Dissertations Abstracts International, Volume: 82-12, Section: B.
Contained By:	Dissertations Abstracts International82-12B.
標題:	Environmental engineering. -
電子資源:	https://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=28496105
ISBN:	9798516061004

Assessment of Chemistry and Geochemical Reactions for Alternative Hydraulic Fracturing Water Supplies and Produced Waters.
Ghahremani, Nima.

Assessment of Chemistry and Geochemical Reactions for Alternative Hydraulic Fracturing Water Supplies and Produced Waters. - Ann Arbor : ProQuest Dissertations & Theses, 2021 - 165 p.

Source: Dissertations Abstracts International, Volume: 82-12, Section: B.

Thesis (Ph.D.)--Texas A&M University - Kingsville, 2021.

This item must not be sold to any third party vendors.

Since the expansion of hydraulic fracturing for oil and gas, use of freshwater resources as a hydraulic fracturing fluid has been increasing rapidly. As many areas across the U.S. are facing drought, the oil and gas industry will require water management strategies that maximize the use of non-potable water. In this study, the feasibility of using brackish groundwater reverse osmosis (RO) desalination reject concentrate and produced water as alternative water supply for frac fluid was evaluated. The results of water chemistries analysis showed a high concentration of alkalinity and sulfate in the RO concentrate. Also, significant concentrations of barium and calcium were observed in the produced water samples. Therefore, the down-hole scaling potential associated with different blend ratios of produced water and RO desalination concentrate were simulated using geochemical modeling software. Results showed possible calcite formation in all simulations. Simulations performed for the desalination concentrate showed less potential for barite formation, whereas a high potential for barite scale formation was observed in model simulations for the produced water (PW) and RO/PW blended samples. Finally, produced water dissolves rare earth elements (REE) as it flows through shale formations. Geochemical analyses of the Marcellus Shale have indicated that geothermal brines contain relatively high concentrations of REE. However, presence of high concentrations of barium can interfere with inductively coupled plasma - mass spectrometry (ICP-MS) analysis of produced water samples for REE due to the formation of polyatomic interferences. As an initial step towards assessing the feasibility of developing an economic strategic element recovery process, an accurate and reliable analytical ICP-MS method was developed to determine concentrations of REE in complex brine matrices with high barium concentrations. As a last step of this study, REE concentrations were analyzed in produced water and desalination concentrate samples.

ISBN: 9798516061004Subjects--Topical Terms:

548583
Environmental engineering.
Subjects--Index Terms:

Hydraulic fracturing

Assessment of Chemistry and Geochemical Reactions for Alternative Hydraulic Fracturing Water Supplies and Produced Waters.
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500 $a Source: Dissertations Abstracts International, Volume: 82-12, Section: B.
500 $a Advisor: Clapp, Lee.
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506 $a This item must not be sold to any third party vendors.
520 $a Since the expansion of hydraulic fracturing for oil and gas, use of freshwater resources as a hydraulic fracturing fluid has been increasing rapidly. As many areas across the U.S. are facing drought, the oil and gas industry will require water management strategies that maximize the use of non-potable water. In this study, the feasibility of using brackish groundwater reverse osmosis (RO) desalination reject concentrate and produced water as alternative water supply for frac fluid was evaluated. The results of water chemistries analysis showed a high concentration of alkalinity and sulfate in the RO concentrate. Also, significant concentrations of barium and calcium were observed in the produced water samples. Therefore, the down-hole scaling potential associated with different blend ratios of produced water and RO desalination concentrate were simulated using geochemical modeling software. Results showed possible calcite formation in all simulations. Simulations performed for the desalination concentrate showed less potential for barite formation, whereas a high potential for barite scale formation was observed in model simulations for the produced water (PW) and RO/PW blended samples. Finally, produced water dissolves rare earth elements (REE) as it flows through shale formations. Geochemical analyses of the Marcellus Shale have indicated that geothermal brines contain relatively high concentrations of REE. However, presence of high concentrations of barium can interfere with inductively coupled plasma - mass spectrometry (ICP-MS) analysis of produced water samples for REE due to the formation of polyatomic interferences. As an initial step towards assessing the feasibility of developing an economic strategic element recovery process, an accurate and reliable analytical ICP-MS method was developed to determine concentrations of REE in complex brine matrices with high barium concentrations. As a last step of this study, REE concentrations were analyzed in produced water and desalination concentrate samples.
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650 4 $a Hydrologic sciences. $3 3168407
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653 $a Produced watars
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