低Mr碳化合物是在煤的水性和干性热解过程中产生的
1Institute of Geophysics and Planetary Physics, University of California, Los Angeles 90024, USA.
Nature
|October 24, 1985
概括
实验室热解实验模拟了沉积盆地的有机物质成熟过程. 蒙特莫里隆石的干热解显示了低分子量碳化合物生成的催化剂,与水性条件不同,影响了对天然气形成的理解.
科学领域:
- 地质化学 地质化学
- 有机地化学 有机地化学
- 沉积地质学 沉积地质学
背景情况:
- 使用实验室热解来模拟沉积盆地有机物成熟是正在进行的科学辩论的主题.
- 了解碳化合物生成需要对自然成熟过程进行准确的建模.
研究的目的:
- 在水性和干性热解实验期间调查碳化合物生成.
- 为了比较矿物质的催化作用,特别是蒙莫里隆石,在不同的热解条件下.
- 分析低分子量碳化合物和烯酸的生产.
主要方法:
- 在有机物质上进行水性和干性热解实验.
- 在干燥热解条件下使用蒙特莫里隆尼特粘土.
- 分析生成的碳化合物,包括低分子质量分数和烯酸 (C2-C6范围).
主要成果:
- 在蒙特莫里隆石的存在下干热解显示了对低分子质量碳化合物生成的催化作用.
- 水性热解没有表现出类似的催化效应,可能是由于粘土酸度降低.
- 在C2-C6范围内的烯酸在300°C的水性和干性热解中产生了相当数量的烯酸.
结论:
- 矿物 - 素相互作用在模拟成熟过程中显著影响碳化合物生成.
- 氨酸在地质时间上的不稳定性可能解释了它们在一些自然样本中的缺席.
- 这些发现增强了我们对天然气形成过程和沉积岩中的煤素-矿物相互作用的理解.
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