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Petrographic and geophysical assessment of coal quality as related to briquetting: the Miocene lignite of the Lower Rhine Basin, Germany

机译:与压块相关的煤质的岩石学和地球物理评估:德国下莱茵盆地的中新世褐煤

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摘要

In the Lower Rhine Basin, Germany, Tertiary lignites are mined primarily for electrical power generation and briquetting purposes. Until 2000, when the mine was closed, coals from the Bergheim open pit mine were used for briquetting. After 2000, briquettes were produced from the Hambach open pit mine but did not show the same quality and hardness as those from the Bergheim pit. In this context, the macropetrographic and microlithotype composition of the Hambach lignites was studied in detail. Samples were taken from the three profiles, S1, S2 and S3, and a well, R1. All of the samples were macropetrographically described, analyzed in their microlithotype composition, and coals from profile S3 were analyzed for their briquetting compression strength. Three horizons of high gelite content were detected in the Main Seam, two of them with negligible thickness and one with a thickness of up to 1 m. Briquettes produced from these horizons are characterized by significantly reduced hardness. By careful interpretation of subtle changes in geophysical log data, it was possible to map the occurrence of these gelite horizons. As a consequence of these studies, an excavation plan was set up by the RWE Rheinbraun to avoiding mining of critical strata for briquetting purposes.
机译:在德国下莱茵盆地,主要开采三重褐煤,用于发电和压块。直到2000年关闭该煤矿时,一直使用Bergheim露天煤矿的煤进行压块。 2000年后,Hambach露天矿生产了煤球,但其质量和硬度与Bergheim矿山不同。在这种情况下,详细研究了哈姆巴赫褐煤的宏观岩石学和微石版型组成。从三个剖面S1,S2和S3以及一口井R1取样。对所有样品进行了宏观岩相描述,并对其微岩型组成进行了分析,并分析了剖面S3中的煤的团块抗压强度。在主煤层中发现了三层胶凝体含量高的层,其中两层的厚度可以忽略不计,而另一层的厚度最大为1 m。从这些视域生产的团块的特征在于硬度显着降低。通过仔细解释地球物理测井数据的细微变化,可以绘制出这些胶凝岩层位的发生情况。这些研究的结果是,RWE Rheinbraun制定了一项开挖计划,以避免为压块目的而开采关键地层。

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