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Onset of the Asphaltene Flocculation and Asphaltene Hydrodynamic Radius Determination Using H-Diffusion- Ordered Spectroscopy DOSY NMR

机译:使用H-扩散排序光谱法DOSY NMR沥青质絮凝和沥青质流体动力学半径测定的发作

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During EOR recovery processes, asphaltenes macromolecules can flocculate and cause drastic changes in the petrophysical properties of the reservoir, therefore it is very important to determine the time at the flocculation begins and further the size of the aggregates, since ultimately this depends on whether these can be trapped in the porous media. This work aims to evaluate the change in the asphaltene hydrodynamic radius of at different concentrations of n-heptane and to detect the onset asphaltene floculation using a new technique known as 1H Diffusion ordered spectroscopy-NMR (DOSY-NMR). H-DOSY NMR is a method based on the pulsed field gradient spin-echo from nuclear magnetic resonance (PFGSE NMR) and it allows the identification of the molecular components of a mixture sample and at the same time obtain information of their size through the diffusion coefficient. For our specific case, the asphaltene hydrodynamic radius was 16.8 ? and the onset of asphaltene floculation can be observed when the concentration of solvent n- heptane was 30 wt %.
机译:在EOR恢复过程中,沥青质大分子可以絮凝和引起储层的岩石物理特性的剧烈变化,因此确定絮凝的时间开始并进一步为聚集体的尺寸非常重要,因为这取决于这些是否可以被困在多孔介质中。这项工作旨在评估不同浓度的正庚烷的沥青质流体动力半径的变化,并使用称为1H扩散有序光谱-NMR(Dosy-NMR)的新技术检测起始沥青质絮凝。 H-MOSY NMR是一种基于核磁共振(PFGSE NMR)的脉冲场梯度自旋回波的方法,允许识别混合物样品的分子量,同时通过扩散获得其大小的信息系数。对于我们的特定情况,沥青质流体动力半径为16.8?当溶剂N-庚烷的浓度为30wt%时,可以观察到沥青质絮凝的开始。

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