微型FT-IR光谱测量CH4:使用高压和高温光学电池 (HPOC) 的实验校准
Yahao Huang1, Chongyang Wu2, Xiaowan Tao3
1Key Lab of Exploration Technologies for Oil and Gas Resources of Ministry of Education, Yangtze University, Wuhan, 430100, China.
Spectrochimica acta. Part A, Molecular and biomolecular spectroscopy
|December 7, 2023
概括
福利埃变换红外光谱法 (FTIR) 现在在液体含量中对甲 (CH4) 进行定量分析. 这种新方法确定了温度,压力和组成,推动了地质学的研究.
科学领域:
- 地质化学 地质化学
- 频谱学是一种光谱学.
- 地质地质地质地质地质地
背景情况:
- 福里埃变换红外光谱法 (FTIR) 是对自然流体内含物的定性分析的一个关键工具.
- 在液体内含的温度,压力和成分的定量确定仍然是一个重大挑战.
研究的目的:
- 使用FTIR建立在蒸汽阶段的甲 (CH4) 的红外定量模型.
- 研究光谱参数与热力学特性 (温度,压力,密度) 之间的关系.
主要方法:
- 毛细血管高压光学电池 (HPOC) 与FTIR的集成.
- 对CH4的C-H对称拉伸带 (v3) 的分析.
- 在受控制的温度 (40-200°C) 和压力 (20-500bar) 下安装和计算红外光谱.
主要成果:
- 建立了光谱参数 (峰值面积,FWHM,高度比,峰值转移) 与CH4密度,温度和压力之间的线性定量关系.
- 峰值面积和FWHM随着压力和密度而增加,随着温度而下降.
- 带的位置随着温度,压力和密度的变化而变化,从而可以确定PVT-x属性.
结论:
- 开发的FTIR方法适用于确定含有CH4的系统的PVT-x特性,包括天然流体含量.
- 由于比尔-兰伯特定律,量化红外线方法是普遍适用的.
- 证明FTIR的可行性用于使用阿尔卑斯山的甲含量进行天然流体含量研究.
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