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Coalbed Methane Potential and Coal Characteristics in the Lati Region, Berau Basin, East Kalimantan

机译:加里曼丹东部贝劳盆地拉提地区煤层气潜力和煤特征

摘要

Http://dx.doi.org/10.17014/ijog.vol1no1.20063aA geological research was performed in the Berau Basin, to provide a better understanding on the potential and resources of coalbed methane (CBM) in Berau Regency, East Kalimantan Province, particularly in the Lati Coalfield. Field observation conducted in the coalfield, shows that the banded to bright banded Lati coal is dominated by the bright banded one. Petrographically, the coal consists of vitrinite comprising typical telocollinite and desmocollinite; with rare to sparse exinite, and minor inertinite, and mineral matter. Geochemical analysis shows the range of volatile matter content is from 32.65–39.60%, total sulfur from 0.35–3.04%, ash varies between 2.78–14.50%, and moisture from 12.23–19.98%. Vitrinite reflectance values (Rv), varying from 0.42–0.57%, tend to indicate that the Lati coal rank ranges from sub-bituminous B to high volatile bituminous C category, with low ash content in general. Moreover, the coal maturity level, thermally immature to early mature, leads to the assumption that the expected gas present is suggested to be of biogenic origin. The fairly well cleated Lati coal shows cleat orientations trending north - northeastward, perpendicular to nearly oblique to the syncline axis. Furthermore, coal microcleat occurs as open tensional, sub-curved to curved lines microcracks, diagonally to perpendicular to bedding plane, but some are parallel to the bedding plane. An in-situ coal gas calculation tends to indicate a low to moderate methane content level, with a value of 44.20–47.08 scf/t. However, the Q1 plus Q2 calculation exhibits the gas content ranging from 41.69 to 78.71 scf/t. Moreover, total calculated gas in-place of the P, Q, and R Seams = 5.33 m3/t = 191.56 scf/t.
机译:http://dx.doi.org/10.17014/ijog.vol1no1.20063aA在Berau盆地进行了地质研究,以更好地了解东加里曼丹省Berau摄政区的煤层气(CBM)的潜力和资源,特别是在Lati Coalfield。在煤田中进行的实地观察表明,带状至亮带状的拉提煤以带状亮煤为主。岩石学上,煤由镜质体组成,镜质体包括典型的钙铝矾石和高岭土。稀有稀疏的橄榄岩,稀有的惰质岩和矿物质。地球化学分析显示,挥发性物质含量范围为32.65-39.60%,总硫含量为0.35-3.04%,灰分为2.78-14.50%,水分为12.23-19.98%。玻璃铁矿的反射率值(Rv)在0.42-0.57%之间变化,这往往表明拉提煤的等级范围从次烟煤B到高挥发性烟煤C类,且灰分含量通常较低。此外,由于煤的成熟度水平(从热成熟到早期成熟)导致了这样一个假设,即预期存在的预期气体是生物成因的。裂开度相当良好的Lati煤表现出的割理方向呈北-东北走向,垂直于斜向轴几乎倾斜。此外,煤微裂隙以开放张应力的形式出现,次屈曲成曲线微裂纹,与垂直于顺层平面成对角线,但有些平行于顺层平面。现场煤气计算往往表明甲烷含量低至中等,值为44.20–47.08 scf / t。但是,Q1和Q2计算得出的气体含量范围为41.69至78.71 scf / t。此外,P,Q和R煤层的总计算气体就位= 5.33 m3 / t = 191.56 scf / t。

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