印度Son Valley盆地Barakar煤层的明确属性及其对煤层气勘探的启示

Susheel Kumar, A. Varma, V. A. Mendhe
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摘要

通过对印度中部Son-Valley煤盆地4个不同地下煤矿的代表性煤样进行现场观测、扫描电镜图像分析和近端分析,评价了煤的清晰属性和煤质,对煤层气远景进行了表征。根据岩石类型组成,煤样可分为榴辉岩-克拉榴辉岩-玻璃质型和榴辉岩-克拉辉岩型。根据岩性的不同,岩缝的发育范围为5 ~ 10 cm-1 ~ 2 ~ 3 cm-1,岩缝密度范围为7 ~ 16 cm-2,表明岩缝发育受岩性的影响。理裂走向主要为NW-SE ~ NNW-SSE和NE-SW ~ ENE-WSW,说明理裂面和理裂面相互垂直。通过对煤样扫描电镜图像的分析,在微观尺度上验证了煤样的清理几何形状,证明了煤样的面清理和煤样的尾清理是相互正交的。煤样的工艺性能为水分(Wa)、挥发分产率(VMdaf)、灰分产率(Ad)分别为0.66 ~ 11.80%、32.0 ~ 50.05和13.23 ~ 43.73 wt.%。煤样的燃料比在1.05 ~ 2.35之间变化,表明煤样属于亚烟煤~烟煤。样品的碳、氢(Cdaf、Hdaf)含量分别为68.89 ~ 86.08和5.22 ~ 6.60 wt.%。van-Krevelen图的H/C和O/C原子比值表明,研究煤中以陆源型干酪根为主,属于天然气成因窗口。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Insights of Cleat Attribute of Barakar Coal Deposits of Son Valley Basin, India: Implication for Coal Bed Methane Exploration
Cleat attributes and coal quality have been evaluated through field observation, SEM images analysis and proximate-ultimate analyses on representative coal samples collected from four different underground coal mines of Son-Valley coal Basin of central India for the characterization of coal bed methane prospective. The coal samples were characterized as durainic-clarodurainic-vitrainic type to durocalrainic-clarainic type based on litho-type composition. Cleats were identified as face cleat and butt cleat range 5-10 cm-1 to 2–3 cm-1 depending on the litho-types whereas, cleat density ranges 7-16 cm-2 revealed that cleat development is influenced by litho-types. The cleat orientation shows two main strikes almost NW-SE to NNW-SSE and NE-SW to ENE-WSW elucidates the face cleat and butt cleats are perpendicular to each other. SEM images for coal samples were analysed to validate the cleat geometry at micro-scale, illustrates that face cleat and butt cleats are orthogonal to each other. The technological properties viz. moisture (Wa), volatile matter yield (VMdaf) ash yield (Ad) of coal samples are placed in the range of 0.66–11.80, 32.0–50.05 and 13.23–43.73 wt.% respectively. The fuel ratios of all the samples varied from 1.05–2.35 indicating that coal samples were of sub-bituminous to bituminous rank. The carbon and hydrogen (Cdaf, Hdaf) content of samples ranges from 68.89–86.08 and 5.22–6.60 wt.% respectively. The atomic ratio H/C and O/C through van-Krevelen diagram demonstrate the predominance of type-III/IV kerogens usually derived from terrestrial source in studied coal belongs to the gas genesis window.
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