• 主题
高级搜索  >
历史搜索 清空历史
首页> 外文期刊>Arabian journal of geosciences >Sulfur content in coal formed during different geologic periods in the Guangxi Province and the relationship with the depositional environment
【24h】

Sulfur content in coal formed during different geologic periods in the Guangxi Province and the relationship with the depositional environment

机译：广西不同地质时期形成的煤中硫含量及与沉积环境的关系

获取原文
获取原文并翻译 | 示例
           
页面导航
  • 摘要
  • 著录项
  • 相似文献
  • 相关主题

摘要

To understand the distribution regularity of sulfur in coal formed during different geologic periods and their related controlling factors, we obtained statistics on the sulfur content in the coal samples from different regions of the Guangxi Province. Based on the results, we drew the following conclusions. First, the contents of the sulfur forms vary significantly in the coal samples. The sulfide and organic sulfur content account for a relatively high proportion of the total sulfur content while the sulfate sulfur content is relatively low (i.e., 1.29-15.72%, average=4.83%). Between these factors, the sulfide sulfur content in early Carboniferous coal is slightly higher than the organic sulfur content, while the organic sulfur content in late Permian, Early Jurassic, and Tertiary coal is higher than the sulfide sulfur content, represented by Heshan coal. Second, coals formed in early Carboniferous, late Permian, and Early Jurassic mainly contain high-sulfur coals. In contrast, Neogene coals, with relatively poor sulfur content, are the major source of low-sulfur coals in the Guangxi Province. In this study, the sulfur content in coal formed in early Carboniferous and late Permian is >= 4%; thus, this coal belongs to the super-high organic sulfur (SHOS). Finally, we discuss the spatial distribution characteristics of the sulfur content in coals formed during various geologic periods and their controlling factors. The results indicate that the content and form depend on the paleogeographic conditions during the geologic period of formation.
机译：要了解在不同地质时期形成的煤中硫的分布规律及其相关的控制因素，我们得到了广西不同地区煤样中硫含量的统计数据。根据结果​​，我们提出了以下结论。首先，硫形式的内容物在煤样中变化显着变化。硫化物和有机硫含量占硫含量的相对高的比例，而硫酸硫含量相对较低（即1.29-15.72％，平均= 4.83％）。在这些因素之间，早期石炭煤中的硫化物硫含量略高于有机硫含量，而最初二叠纪，早期侏罗纪和三级煤中的有机硫含量高于Heshan煤所代表的硫化物硫含量。二，在早期石炭系中形成的煤，已故的二叠纪和早期侏罗纪主要含有高硫煤。相比之下，硫含量相对较差的新生煤是广西低硫煤的主要来源。在这项研究中，早期石炭系和晚期二叠液中形成的煤中的硫含量为> = 4％;因此，这种煤属于超高有机硫（SHOS）。最后，我们讨论了在各种地质时期形成的煤中硫含量的空间分布特征及其控制因素。结果表明内容和形式取决于地质期间的古地理条件。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱：kefu@zhangqiaokeyan.com

京公网安备：11010802029741号 ICP备案号：京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有

  • 客服微信

  • 服务号