Comparative Evaluation of the Feasibility of Utilizing the Bakken Formation Oil and Gas Field Produced Water for Extraction of Critical Minerals and Salts, with a Focus on the Inyan Kara Formation: An Analysis of Salinity and Infrastructure

Jakaria Md
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Abstract

This study compares the salt concentration and mineral composition of water from the Bakken Formation and the Inyan Kara Formation to assess their suitability for salt/critical minerals extraction. The results reveal that the Bakken Formation exhibits significantly higher levels of dissolved solids, calcium, magnesium, and chloride compared to the Inyan Kara Formation, indicating its potential suitability for salt/critical elements extraction. Conversely, the Inyan Kara Formation water displays higher bicarbonate concentrations, which may limit its applicability in certain salt extraction processes. The Bakken Formation proves more viable for water production due to its existing oil and gas infrastructure and abundant produced water from active and abandoned oil wells. This availability of produced water wells reduces the cost of critical mineral extraction and presents opportunities for water reuse or critical minerals sale, generating additional revenue that could offset recycling and disposal costs. In contrast, the absence of water production wells in the Inyan Kara Formation hinders its economic feasibility for salt/mineral extraction. The Inyan Kara Formation has a higher volume of water, but its lower salt content limits its usefulness for some purposes, especially in the energy industry for recovering rare earth minerals. Considering the higher mineralization, the concentration of key ions, and the presence of water production infrastructure, the Bakken Formation emerges as a more favorable choice for critical mineral extraction. However, factors like environmental impact and extraction costs should be considered in determining the most suitable formation. Despite data limitations, the study utilizes a valuable database to identify regional variations in salt concentrations for critical mineral extraction.
利用巴肯地层油气田采出水提取关键矿物质和盐类的可行性比较评估,重点关注伊尼扬卡拉地层:盐度和基础设施分析
这项研究比较了来自巴肯地层和伊尼扬卡拉地层的水的盐浓度和矿物成分,以评估它们是否适合提取盐/关键矿物。研究结果表明,巴肯地层的溶解固体、钙、镁和氯化物含量明显高于伊尼扬卡拉地层,这表明巴肯地层可能适合提取盐分/关键元素。相反,伊尼扬卡拉地层的水显示出较高的碳酸氢盐浓度,这可能会限制其在某些盐提取工艺中的适用性。巴肯地层现有的石油和天然气基础设施,以及活跃和废弃油井的大量产水,证明其更适合于水的生产。这种产水井的可用性降低了关键矿物的提取成本,并为水的再利用或关键矿物的销售提供了机会,从而产生额外的收入,可以抵消回收和处理成本。相比之下,伊尼扬卡拉地层没有产水井,阻碍了盐/矿物开采的经济可行性。伊尼扬卡拉地层的含水量较高,但含盐量较低,这限制了其在某些方面的用途,特别是在能源行业回收稀土矿物。考虑到较高的矿化度、关键离子的浓度以及水生产基础设施的存在,巴肯地层成为提取关键矿物的更有利选择。不过,在确定最合适的地层时,还应考虑环境影响和提取成本等因素。尽管数据有限,但这项研究利用了一个宝贵的数据库来确定关键矿物提取的盐浓度区域差异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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