首页|高温高压条件下单一CO2体系的傅里叶红外光谱定量模型及天然包裹体应用

高温高压条件下单一CO2体系的傅里叶红外光谱定量模型及天然包裹体应用

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傅里叶红外光谱是可以用于定性识别天然流体包裹体组分的原位无损分析技术,目前针对于天然包裹体的温度—压强—组分的定量分析是激光谱学地质应用的重点和难点以及发展方向,傅里叶红外光谱对于天然流体包裹体的定量方法和模型尚未建立.通过高压毛细硅管封装技术结合傅里叶红外光谱仪,对单一 CO2体系2v2+v3和v1+v3伸缩振动双峰进行40~80 ℃,60~500 bar压强范围下红外光谱的采集和观测,获取了不同温度和压强范围下红外光谱参数,通过拟合和计算获取该体系下傅里叶红外光谱的峰面积和峰位移,建立了 CO2的2v2+v3和v1+v3伸缩振动双峰体系下傅里叶红外光谱流体的密度与峰面积,压强与峰面积的标定模型,并明确CO2的2v2+v3和v1+v3伸缩振动双峰形态随温度压强的变化特征,讨论了峰位移随温度和压强的变化.通过单一 CO2组分傅里叶红外光谱定量技术,在40 ℃下,采集莺歌海盆地黄流组储层中石英裂隙内纯CO2包裹体的伸缩振动双峰峰面积来计算的密度,同时在室温下,采集包裹体的拉曼光谱,对比利用两种不同原位分析测试方法所计算密度,验证了傅里叶红外光谱定量分析的可行性,傅里叶红外光谱定量分析相比于拉曼光谱定量分析具有不受实验仪器和环境限制的优点,其定量方法可以避免由于仪器所处不同实验室之间产生的误差.
Quantitative Fourier Infrared Spectroscopy Model of a Single CO2 System Under High Temperature and Pressure and Its Application to Natural Inclusions
Fourier transform infrared spectroscopy is a commonly used in-situ non-destructive analysis technique for qualitatively identifying natural fluid inclusion components.The quantitative analysis of temperature-pressure components of natural inclusions is the focus,as well as the difficulty and development direction of laser spectroscopy geological applications.The quantitative method and Fourier transform infrared spectroscopy model for natural fluid inclusions have not been established.The infrared spectra of a single CO2 system with two stretching vibration peaks of 2v2+v3 and v1+v3 were collected and observed at 40~80 ℃ and 60~500 bar for the first time by high-pressure capillary silicon tube packaging technology combined with Fourier infrared spectrometer.The infrared spectral parameters at different temperature and pressure ranges were obtained.The peak area and peak displacement of the Fourier infrared spectrum under this system were obtained by fitting and calculation.The calibration model of the density and peak area,pressure,and peak area of the Fourier infrared spectrum fluid under the 2v2+v3 and v1+v3 stretching vibration bimodal system of CO2 was established.The variation characteristics of bimodal stretching vibration of 2v2+v3 and v1+v3 of CO2 with temperature and pressure are clarified,and the variation of peak displacement with temperature and pressure is discussed.Using Fourier transform infrared spectroscopy(FT-IR)of a single CO2 component,the densities of pure CO2 inclusions in quartz fractures of the Huangliu Formation reservoir in the Yinggehai Basin were calculated at 40 ℃ by collecting the double peak area of stretching vibration of the inclusions.At the same time,the Raman spectra of the inclusions were collected at room temperature,and the densities calculated by two different in-situ analysis methods were compared to verify the feasibility of FT-IR quantitative analysis.Compared with Raman quantitative analysis,Fourier transform infrared spectroscopy quantitative analysis is not limited by experimental instruments and environment.Its quantitative method can avoid errors caused by different laboratories where the instrument is located.

Fourier infrared spectroscopyCO2Fluid inclusionsYinggehai Basin

黄亚浩、薛一帆、文志刚、陈俊林、乔占峰、刘义承

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长江大学油气地球化学与环境湖北省重点实验室,湖北武汉 430100

中国地质大学(武汉)构造与油气资源教育部重点实验室,湖北武汉 430074

中国石油天然气集团公司碳酸盐岩储层重点实验室,浙江杭州 310023

国家能源碳酸盐岩油气重点实验室,浙江杭州 310023

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傅里叶红外光谱 CO2 流体包裹体 莺歌海盆地

国家自然科学基金项目国家自然科学基金项目中石油碳酸盐岩储层重点实验室开放基金项目

4230215442372169RIPED-2022JS-2382

2024

光谱学与光谱分析
中国光学学会

光谱学与光谱分析

CSTPCD北大核心
影响因子:0.897
ISSN:1000-0593
年,卷(期):2024.44(8)
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