波兰中部科宁褐煤矿垂直和水平段采煤壁中褐煤灰的变化

IF 0.4 Q4 ENVIRONMENTAL SCIENCES
Lilianna Chomiak
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引用次数: 7

摘要

本文主要研究了波兰中部三个褐煤露天矿沿选定剖面和采场壁的褐煤灰分变化。它们属于科宁褐煤矿(Konin Lignite Mine),那里正在开采波兰中部的第一个褐煤煤层,用于发电。褐煤中的灰分含量很重要,因为灰分降低了褐煤的热值。所得结果基于从Drzewce、Tomisławice和Jóźwin IIB露天矿收集的266个褐煤样本。所有样品均按照ISO 1171标准程序进行测试,即首先在850℃的温度下燃烧,然后在干燥的基础上测定灰分含量(Ad),然后计算基本统计参数。所研究的褐煤煤层的特点是沿选定的垂直剖面和褐煤壁以及三个露天矿之间的灰分分布模式是可变的。单个样品的灰分含量在6.5 ~ 69.8%之间,而露天矿的平均灰分含量在9.7 ~ 17.6%之间。Drzewce和Tomisławice的变异系数较大(80.23-96.33%),Jóźwin IIB的变异系数较低(14.53-37.75%)。在这篇文章中,一些床上显著的灰分富集被解释为中新世中期沼泽(后沼泽)发生洪水的结果,但也解释为化学降水的结果。当褐煤燃烧发电时,会产生相对大量的灰。因此,除了识别灰分的化学成分和相外,还建议识别褐煤中的灰分含量,以更好地保护环境。在保护的第一阶段,最好通过分析现场样品的灰分含量来实现。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Variation of lignite ash in vertical and horizontal sections of mining wallsin the Konin Lignite Mine, central Poland
This paper focuses on the variations of lignite ash along selected sections and mining walls from three lignite opencast mines in central Poland. They are owned by the Konin Lignite Mine, where the first Mid-Polish lignite seam is being mined to produce electricity. Ash content in lignite is important because ash lowers the calorific value of the lignite. The results obtained are based on 266 samples of lignite collected from the Drzewce, Tomisławice, and Jóźwin IIB opencasts. All samples were tested according to ISO 1171 standard procedures, that is, they were first burned at a temperature of 850°C, then the ash content was determined on a dry basis (Ad), be-fore the basic statistical parameters were calculated. The studied lignite seam is characterised by a variable distribution pattern of ash both along selected vertical sections and lignite walls, as well as between the three open-casts. The ash content of individual samples ranged from 6.5 to 69.8 wt%, while the average content in opencast mines varied from 9.7 to 17.6 wt%. The coefficient of variation is large (80.23–96.33%) in the case of the Drzewce and Tomisławice, and low to average (14.53–37.75%) in the case of Jóźwin IIB. Significant ash enrichment of some beds is interpreted in this article as a consequence of floods occurring in a Mid-Miocene mire (backswamp), but also of chemical precipitation. When lignite is burned to generate electricity, a relatively large amount of ash is produced. Therefore, recognition of ash content in lignite, in addition to the chemical composition and phase of ash, is recommended to better protect the environment. At the first stage of protection, it can be best achieved by analysing field samples for ash content.
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