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Quantitative analysis of kerogen content and mineralogy in shale cuttings by Diffuse Reflectance Infrared Fourier Transform Spectroscopy

机译:通过漫反射红外傅里叶变换光谱法测量分析页岩扦插中的岩岩含量和矿物学

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Diffuse reflectance infrared Fourier transform spectroscopy(DRIFTS) has been used for qualitative investigation of hydrocarbons,source rocks,core and cuttings.However,in the past,quantitative analysis has been unreliable.In the DRIFTS technique,an infrared laser shines onto the material and a detector measures the reflected light intensity as a function of frequency.The reflected light frequency spectrum is related to characteristic vibrational modes of elemental bonds in the material.In some cases these modes have been linked to compounds or minerals. This paper demonstrates that quantitative analysis of kerogen,calcite,illite,kaolinite, quartz,dolomite and smectite is possible for cuttings obtained from a well drilled with oil-based mud in a formation in Texas.The cuttings mineral concentrations solved from DRIFTS spectra were compared with mineralogy determined by the highly accurate transmission dual-range Fourier transform infrared(DRFT-IR) technique developed in our laboratory and the concentrations are similar to within a few percent.The kerogen content from DRIFTS was compared to the organic carbon content determined by a LECO elemental analyzer and the agreement is better than ± 1 wt % kerogen. Our procedure removed the oil-based mud from the cuttings sample and then reduced the particle size.The samples were analyzed with a Bruker Alpha-R DRIFTS unit over the range of 375 – 4000 cm~(-1) .After converting the reflectance data to Kubelka-Munk units, the spectra were analyzed by assuming that the Beer-Lambert law holds at every wavelength.In this analysis,the mineralogy was determined from over 2500 simultaneous least squares solutions of the unknown absorbance as a linear combination of the mineral standard spectra.Mineral concentrations were evaluated with artificial mixtures of minerals and by comparison with the DRFT-IR and LECO measurements on well cuttings.
机译:弥漫反射率红外傅里叶变换光谱(漂移)已被用于定性调查碳氢化合物,源岩,芯和切割。然而,在过去,定量分析一直不可靠。在漂移技术中,红外激光闪耀在材料上闪耀检测器测量反射的光强度作为频率的函数。反射的光频谱与材料中元素键的特征振动模式有关。在某些情况下,这些模式已与化合物或矿物质有关。本文表明,在德克萨斯州的形成中从钻井井钻井钻井井中获得的切屑,可以对角蛋白,方解石,伊利钠,高岭土,石英,白云石和蒙脱石的定量分析。比较了从漂移光谱溶解的切割矿物质浓度通过在我们的实验室开发的高度精确的传输双级傅里叶变换红外(DRFT-IR)技术确定的矿物学,浓度类似于少量的浓度。将来自漂移的基因素含量与由a确定的有机碳含量进行比较。 LECO元素分析仪和协议优于±1wt%的角膜原。我们的程序从切屑样品中取出了油基泥浆,然后降低了粒度。用Bruker alpha-R漂移单元分析样品,在375-4000cm〜(1)范围内。转换反射数据对于Kubelka-Munk单位,通过假设啤酒兰伯特法在每一个波长处持有啤酒 - 兰伯特法律来分析光谱。在该分析中,矿物学从2500多个最小二乘溶液中确定了未知吸光度的同时最小二乘溶液,作为矿泉标准的线性组合用矿物的人工混合物评价光谱。通过对井切屑的DRFT-IR和LECO测量进行比较。

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