Multi-analytical assessment of shale gas potential in the West Bokaro Basin, India: A clean energy prospect

Manish Kumar Srivastava , Kaushal Kishor , Alok K. Singh , Alok Kumar , Khairul Azlan Mustapha , Amit Saxena
{"title":"Multi-analytical assessment of shale gas potential in the West Bokaro Basin, India: A clean energy prospect","authors":"Manish Kumar Srivastava ,&nbsp;Kaushal Kishor ,&nbsp;Alok K. Singh ,&nbsp;Alok Kumar ,&nbsp;Khairul Azlan Mustapha ,&nbsp;Amit Saxena","doi":"10.1016/j.engeos.2025.100434","DOIUrl":null,"url":null,"abstract":"<div><div>Shale gas, a type of unconventional natural gas found within shale formations, has emerged as a significant source of energy globally. The West Bokaro Basin, part of the Damodar Valley, is known for its rich coal deposits and complex geological history. The basin's stratigraphy includes significant coal-bearing formations interbedded with shales, which may be potential sources of shale gas. The key formations in the basin include the Barakar Formation, which is the primary coal-bearing unit, and the Raniganj Formation, which contains substantial shale intervals. These formations exhibit varying thicknesses, organic content, thermal maturity, and mechanical strength, all of which are critical factors influencing shale gas potential. The assessment of shale gas potential in the West Bokaro Basin involves evaluating the organic richness, thermal maturity, pore characteristics, geochemistry, and mineralogy of the shale formations. Apart from organic richness and thermal maturity, the shale formations must be friable, as they generally lack natural permeability. This study aims to present a comprehensive analysis of the prospects of shale gas in the West Bokaro Basin based on the organic petrography, geochemistry, mineralogical study, Fourier Transform Infrared Spectroscopy (FTIR) analysis, and low-pressure N<sub>2</sub> adsorption analysis. The dark color, greasy touch, and high total organic carbon (<em>TOC</em>) content (5.88 %–22.84 %) provided an initial clue for the shale's potential as a source rock. Results from organic petrographic analysis suggest that these shales contain kerogen type Ⅲ, which is a known indicator of gas-prone zones. The random vitrinite reflectance (<em>R</em><sub>o</sub>, 0.80 %–0.91 %) and the temperature of maximum pyrolysis yield (<em>T</em><sub>max</sub>, 434–448 °C) indicate that the organic matter has attained the sufficient thermal maturity required for the generation of hydrocarbons. FTIR and X-ray diffraction (XRD) analyses identified inorganic entities and high quartz content in the shale samples, confirming their friability. The brittleness index (<em>BI</em>) calculated using X-ray fluorescence (XRF) data showed <em>BI</em> values above 0.48, indicating that the shales are brittle, which is advantageous for hydraulic fracturing. The high quartz content in the shale might act as a natural proppant, enhancing gas extraction efficiency. These findings suggest that the West Bokaro shales hold promise for economically viable shale gas production.</div></div>","PeriodicalId":100469,"journal":{"name":"Energy Geoscience","volume":"6 3","pages":"Article 100434"},"PeriodicalIF":0.0000,"publicationDate":"2025-06-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Energy Geoscience","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2666759225000551","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

Shale gas, a type of unconventional natural gas found within shale formations, has emerged as a significant source of energy globally. The West Bokaro Basin, part of the Damodar Valley, is known for its rich coal deposits and complex geological history. The basin's stratigraphy includes significant coal-bearing formations interbedded with shales, which may be potential sources of shale gas. The key formations in the basin include the Barakar Formation, which is the primary coal-bearing unit, and the Raniganj Formation, which contains substantial shale intervals. These formations exhibit varying thicknesses, organic content, thermal maturity, and mechanical strength, all of which are critical factors influencing shale gas potential. The assessment of shale gas potential in the West Bokaro Basin involves evaluating the organic richness, thermal maturity, pore characteristics, geochemistry, and mineralogy of the shale formations. Apart from organic richness and thermal maturity, the shale formations must be friable, as they generally lack natural permeability. This study aims to present a comprehensive analysis of the prospects of shale gas in the West Bokaro Basin based on the organic petrography, geochemistry, mineralogical study, Fourier Transform Infrared Spectroscopy (FTIR) analysis, and low-pressure N2 adsorption analysis. The dark color, greasy touch, and high total organic carbon (TOC) content (5.88 %–22.84 %) provided an initial clue for the shale's potential as a source rock. Results from organic petrographic analysis suggest that these shales contain kerogen type Ⅲ, which is a known indicator of gas-prone zones. The random vitrinite reflectance (Ro, 0.80 %–0.91 %) and the temperature of maximum pyrolysis yield (Tmax, 434–448 °C) indicate that the organic matter has attained the sufficient thermal maturity required for the generation of hydrocarbons. FTIR and X-ray diffraction (XRD) analyses identified inorganic entities and high quartz content in the shale samples, confirming their friability. The brittleness index (BI) calculated using X-ray fluorescence (XRF) data showed BI values above 0.48, indicating that the shales are brittle, which is advantageous for hydraulic fracturing. The high quartz content in the shale might act as a natural proppant, enhancing gas extraction efficiency. These findings suggest that the West Bokaro shales hold promise for economically viable shale gas production.

Abstract Image

印度西Bokaro盆地页岩气潜力的多重分析评估:清洁能源前景
页岩气是一种在页岩地层中发现的非常规天然气,已成为全球重要的能源来源。西博卡罗盆地是达摩达尔山谷的一部分,以其丰富的煤矿储量和复杂的地质历史而闻名。盆地地层中有大量的含煤地层与页岩互层,可能是页岩气的潜在来源。盆地的关键组包括主要含煤单元Barakar组和含大量页岩层段的Raniganj组。这些地层具有不同的厚度、有机质含量、热成熟度和机械强度,这些都是影响页岩气潜力的关键因素。西Bokaro盆地页岩气潜力评价包括对页岩地层的有机质丰度、热成熟度、孔隙特征、地球化学和矿物学进行评价。除了有机质丰富度和热成熟度外,页岩地层必须易碎,因为它们通常缺乏天然渗透率。基于有机岩石学、地球化学、矿物学、傅里叶变换红外光谱(FTIR)分析和低压氮气吸附分析,对西博卡罗盆地页岩气远景进行了综合分析。深色、油腻感、高总有机碳(TOC)含量(5.88% ~ 22.84%)为页岩作为烃源岩的潜力提供了初步线索。有机岩相分析结果表明,这些页岩含有Ⅲ型干酪根,是已知的易气带标志。随机镜质体反射率(Ro, 0.80% ~ 0.91%)和最大热解产率温度(Tmax, 434 ~ 448℃)表明有机质已达到生成烃所需的热成熟度。FTIR和x射线衍射(XRD)分析发现,页岩样品中存在无机实体和高石英含量,证实了其脆性。利用x射线荧光(XRF)数据计算的脆性指数(BI)值大于0.48,表明页岩呈脆性,有利于水力压裂。页岩中石英含量高,可作为天然支撑剂,提高瓦斯开采效率。这些发现表明,West Bokaro页岩有望实现经济可行的页岩气生产。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
CiteScore
8.20
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信